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GEOSCIENCE ASSESSMENT OFFICE

ASSESSMENT REPORT ON GEOCHEMICAL SURVEY ON CLAIMS IN MANN AND

DUFFTWPS IN THE PORCUPINE MINING DIVISION

PREPARED BY:

Elaine Basa, P.Geo.

UTM Zone 17 - NAD 83 Projection

5410000N to 5412000N and

494000E to 497000E UTM NTS 42A1NW

For

Grupo Moje Limited

Tres-Or Resources Ltd and SNL Enterprises Inc

April 24, 2006

SUMMARY

Tres-Or Resources ltd. has a group of 3 claims (12 units) contiguous with an optioned block of 19 single-unit claims straddling NE Duff and NW Mann Twps in the Porcupine Mining District approximately 46 km NE of Timmins and 25km south of Cochrane and along the Frederick House River. Tres-Or Resources Ltd is the operator within an agreement with SNL Enterprises Inc. Tres-Or is exploring the Mann Property for nickel and platinum group metals. The claims are situated within the Mann Intrusive complex, a large ultramafic intrusion with over 40km strike length and over 1.5km width. Recent work by Tres-Or confirmed that, locally, the ultramafic sequence dips to the east and the favorable clinopyroxenite horizon reached drill thickness of 13.8 m. Several CuNi showings occur within the complex. As well, previous work on the chemistry of the ultramafic rocks on the Mann property has found similar chemistry to that of the nearby Alexo Ni-Cu deposit. Anomalous PGE mineralization (>150 ppb PGE + Au) over considerable widths has been identified. This mineralization was measured from rock saw channel sampling returning up to 654 ppb PGE + Au over 12.20m and one diamond drill hole that returned 238 ppb PGE + Au over a core length of 10.70m.

Subsequently, a ground magnetometer survey was done over the property as well as a structural analysis and petrological work. Based on the ground magnetics, an MMI geochemical survey was initiated to cover two mag highs and a mag low. The results of this MMI survey were sent to Dr. Mark Fedikow of Mount Morgan Resources Ltd for interpretation. His report is included as an appendix with all the raw and reformatted data and plots.

Costs included in the report cover the cutting of a base line and flagging a grid for MMI sampling as well as the associated costs of the survey and processing of the samples as well as the reporting costs.

The survey was able to define an extensive Zn and Cd anomalous response. The specific response indicates the response is due to bedrockhosted base metal mineralization. Adjacent, non-coincident Au and Ag moderately anomalous response ratios were also indicated. Recommendations, based on the MMI-M geochemical survey, include geological modeling, expansion of the grid to define boundaries of the anomalous responses as well as the integration of all geophysical, geological and geochemical data.

2

TABLE OF CONTENTS

SUMMARy ........................................................................................................... 2 INTRODUCTION ................. , .......................... , ..................................................... 4 PROPERTY DESCRIPTION AND LOCATION AND ACCESS .................... , ....... 5 REGIONAL AND PROPERTY GEOLOGy ........................................................... 8 WORK PROGRAM ............................................................................................... 8 DiSCUSSiON ..................................................................................................... 12 RECOMMENDATIONS ....... ............................................................................... 13 REFERENCES ................................................................................................... 14

TABLE OF FIGURES

Figure 1. Regional Location Map ...................................................... 6 Figure 2. Mann Property Location Map ............................................. 7 Figure 3. Grid and Sample Location Map ........................................... 9 Figure 4. Sample Location Map ...................................................... 10 Figure 5. Vertical Magnetic Gradient with 2003 Megatem Conductors

.................................................................................................. 11

3

INTRODUCTION

Tres-Or Resources Ltd is exploring the ~!3nn Project for platinum group

elements. The property, which consists of 22 claims (Table 1) covers 496

hectares (ha.), is located in Mann Township and Duff Township, within the

Porcupine Mining Division of Ontario. The claims are situated within the Mann

intrusive complex, a large ultramafic intrusion, which extends for 40 kilometres of

strike length with a width of greater than 1.5 kilometres. Several nickel-copper

(Ni-Cu) showings have been identified within the Mann intrusive complex. The

complex consists of several layers of ultramafic intrusions, potentially host to

magmatic, low-sulphide disseminated PGM. Past work has identified significant

anomalous platinum group element (PGE) mineralization (>150 ppb PGE + Au)

over considerable widths. The PGE mineralization includes rock saw channel

samples which returned up to 654 ppb PGE + Au over 12.20 metres (m) and one

diamond drill hole which returned 238 ppb PGE + Au over a core length of 10.70

metres. The disseminated mineralization is restricted predominantly to the

clinopyroxenite unit. Locally this is associated with intense chlorite alteration and

secondary clinopyroxene indicating hydrothermal origin remobilization (Goode

and Crocket, 1999).

Because outcrop is exposed very locally, near the bridge over the Frederick

House River, the majority of the work has been concentrated near the exposed

areas. After the government Megatem survey was flown and released in 2003,

ground geophysics was completed over the property. The survey delineated

several anomalies - both positive and negative. Due to the mineralization, as

well as the alteration haloes, the company tested both mag highs and lows with

MMI-M geochemistry. Due to budget constraints, the survey was modified from

the originally proposed survey boundaries. Fewer lines cut the mag anomalies.

However, several anomalous values were identified and subsequently,

recommendations include expanding the MMI survey based on those anomalous

response ratios.

4

PROPERTY DESCRIPTION AND LOCA TION AND ACCESS

The Mann Project is located 46 km north of Timmins, Ontario (Figure 1) within

Duff Township and Mann Township, of the Porcupine Mining Division. The claims

are situated in the northwest corner of Mann Township and the northeast corner

of Duff Township (Figure 2). The project is centered at 48°52'N and 81°02', in

map sheet NTS 42A1NW. The Mann Project consists of 22 contiguous claims

consisting of 31 claim units covering 496 ha. The 19 single-unit claims originally

registered to Leonard Hill of South Porcupine, Ontario, since deceased, are

currently registered (100%) to his daughter, Janet Richard. The three remaining

claims, totaling 12 units, are registered in the name of Tres-Or Resources with a

due date of October 20, 2006.

Table 1. Property Claim List

Township Claim Number Recording Claim Due Recorded holder

Date Date

DUFF 1154619 1990-J ul-19 2007-Jul-19 Janet Richard DUFF 1154620 1990-Jul-19 2007 -J ul-19 Janet Richard DUFF 1154621 1990-Jul-19 2007-Jul-19 Janet Richard DUFF 1154622 1990-J ul-19 2007-Jul-19 Janet Richard MANN 1154611 1990-Jul-19 2008-Jul-19 Janet Richard MANN 1154612 1990-Jul-19 2008-Jul-19 Janet Richard MANN 1154613 1990-J ul-19 2008-Jul-19 Janet Richard MANN 1154614 1990-Jul-19 2007-Jul-19 Janet Richard MANN 1154615 1990-Jul-19 2008-Jul-19 Janet Richard MANN 1154616 1990-Jul-19 2008-Jul-19 Janet Richard MANN 1154617 1990-Jul-19 2008-Jul-19 Janet Richard MANN 1154618 1990-Jul-19 2008-Jul-19 Janet Richard MANN 1154624 1990-Sep-20 2007 -Sep-20 Janet Richard MANN 1154625 1990-Sep-20 2007 -Sep-20 Janet Richard MANN 1154626 1990-Sep-20 2008-Sep-20 Janet Richard MANN 1154627 1990-Sep-20 2007 -Sep-20 Janet Richard MANN 1154628 1990-Sep-20 2007 -Sep-20 Janet Richard MANN 1154629 1990-Sep-20 2007 -Sep-20 Janet Richard MANN 1190501 1992-Jul-28 2008-Jul-28 Janet Richard DUFF 1219619 2004-0ct-20 2006-0ct-20 Tres-Or Resources Ltd. DUFF 1219621 2004-0ct-20 2006-0ct-20 Tres-Or Resources Ltd. MANN 3006946 2004-0ct-20 2006-0ct-20 Tres-Or Resources Ltd.

5

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REGIONAL AND PROPERTY GEOLOGY

A detailed description of the regional and local geology can be found in a

previous report written by A.Tims in Apri1200S. A description of previous work

on the property is also covered in that report.

WORK PROGRAM

The survey consisting of a cut base line and flagged tie lines over which a

variable-spaced MMI-M geochemical survey was completed. Originally proposed

as a SOO-sample survey, budget constraints demanded a reduction to 133

samples - including duplicate samples. Based on the government-flown

megatem survey in 2003 and subsequent ground geophysics, three mag targets

had been identified as warranting geochemical analysis. To maintain coverage

of all three targets, line spacing and sample spacing were varied to provide

closer spacing directly over the targets and reduced coverage marginal to the

targets. Figures 3, 4 and S show the grid with respect to the geophysical targets

as identified by the 2003 Megatem survey as well as location of the geochemical

samples.

Sampling data is included in the appendix of Dr. Fedikow's interpretive

geochemical report forming the appendix to this report.

A crew of 3 to 4 geotechnicians were contracted to complete the survey. The

crew was trained in the proper sampling technique unique to MMI surveys. All

were familiar with geochemical sampling tools and procedures.

8

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11

TRES-OR RESOURCES - SNL ENTERPRISES Grid and Sample Locations

November 2005

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TRES-OR RESOURCES - SNL ENTERPRISES Vertical Magnetic Gradient

with 2003 Megatem Conductors December 2005

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DISCUSSION

The Mann property covers the hinge zone of a parasitic fold on the southern arm of an east dipping synclinally folded multiphase tholeiitic intrusion. The three phases of the intrusion that have been found to date are sulphide undersaturated (Vaillancourt et aI, 2003). Late stage stratabound disseminated sulphides in the central portions of the intrusive are identified as expected. The Mann Intrusion is a layered complex, becoming more felsic towards the top of the intrusion. Serpentine and clinopyroxene variably alter the originally layered peridotite and pyroxenite lithologies. The relative proportion of each alteration assemblage has determined the amount of ductile versus brittle deformation the lithologies have undergone. Although all lithological contacts show evidence of faulting the amount of movement is considered minimal (Tims, 2005). Faulted contacts between the peridotite and clinopyroxenite are exposed north of the bridge, where a discrete moderate to steeply dipping fault plane strikes NE, and, to the south of the bridge as a sinuous 1 m wide shear zone dipping east and indicating the clinopyroxenite is structurally above the peridotite. The ENE dipping contact for the PGE bearing clinopyroxenite unit should remain consistent over the immediate area of the study (Tims, 2005). The chlorite-altered clinopyroxenite unit hosts hydrothermal disseminated mineralization. This unit is referred to as Type IVc by Vaillancourt et aI, 2003. The alteration is characterized by a loss of Si02, Ti02, AI203, Fe, Na, and net gains in MgO, CaO, Cr, Cu, Ni, PGE's, Y and Zr and seems to be semi conformable to the clinopyroxenite-peridotite contact. The style of alteration and mineralization is similar to North American Palladium's Lac des lies open pit mine north of Thunder Bay, Ontario where open pit reserves stand at 26 million tonnes at 1.72g/t Pd and 0.19 g/t Pt. In the case of the Lac des lies mine the alteration event encountered an intrusive breccia at the contact between separate intrusive phases and literally flooded a very large volume of permeable host rock. The potential for primary stratabound disseminated PGE mineralization exists within the Mann Intrusive.

12

The geochemical survey has isolated high to moderate and low-contrast base and precious metal MMI-M anomalies. The anomaly is primarily an E-W-trending Zn-Cd assemblage with lesser, marginal Au and Ag. The presence of coincident Zn and Cd responses confirm the anomaly identifies bedrock-hosted Zn-rich mineralization. Further MMI sampling may be able to delineate the mineralized clinopyroxenite unit, or the clinopyroxenite-peridotite contact. An expanded sampling program is recommended. Drill testing can then be proposed once geochemical analysis has been performed. Drilling can then determine whether the geochemical anomalies are identifying the contact or the alteration. This determination can then be used to direct additional drilling.

RECOMMENDATIONS The previous drill program collared into the footwall of the clinopyroxenite PGE horizon and drilled down dip never intersecting the mineralization. Due to the depth of overburden on much of the property, prior to any further drilling, additional geochemical sampling should be completed. A program of 1500 additional samples is recommended. Based on the existing geophysics and merged geochemical data, a drill program can be initiated to, initially, identify the source of anomalous zinc, whether associated with the clinopyroxenite-peridotite contact or alteration. Any future drilling should take the shallow ENE dip of the clinopyroxenite horizon into account. The six-unit claim, 3006946, staked in October of 2004 also covers an untested fold hinge. Overburden cover in the area is tota/. To drill test the PGE horizon and the area of the second fold hinge the following expenditures are recommended:

·Additional MMI-M sampling -1500 samples ............................... $100,000 • Drill Program 1 OOOm ................................................................. $100,000 • Report & Analysis ......................................................................... $20,000 • Subtotal ....................................................................................... $220,000 ·100/0 Contingency .......................................................................... $22,000 • Management .................................................................................. $25000 Tota.l ............................................................................................. $226 550

13

REFERENCES

Barrie, C.T., Corfu, F., Davis, P., MacEachern, D., and Coutts, A., 2001. Geochemistry and genesis of Komatiite-basalt hosted magmatic sulphide Mineralization, Dundonald Township, Kidd/Munro assemblage, Abitibi subprovince, Canada; Economic Geology, v. 94.

Barrie, C.T., 1999a. Geology of the Mann area; Ontario Geological Survey, Preliminary Map P.3391, scale 1:50,000.

Dunn, D. St. C., 2001, Report on the May/June Diamond Drill Program - Mann Project, report prepared to Broadlands Resources Ltd. and Tres-Or Resources Ltd.

Good, D., and Crocket, J., and Barnett, R.L. A secondary clinopyroxenitechlorite-spinel assemblage in clinopyroxenite of the Mann Complex, Abitibi Belt, Ontario; an unusual hydrothermal alteration suite mafic/ultramafic intrusion, Mann Township, Ontario; Economic Geology Monograph 10.

Gourlay, AW. 2003. Independent Geological Report on the Mann Project For: Tres-Or Resources Ltd. 43-101 Report. SEDAR

Hunt, D.S., and Richard, J.A, Mann Township, District of Cochrane; Ontario Geological Survey Preliminary Map P. 755. Scale 1:15,840.

Keast, T., 2000. Geological Report on the Mann Project for Tres-Or Resources Ltd.

Ontario Geological Survey, 2002. Ontario airborne geophysical surveys, magnetic and electromagnetic data, Timmins area MEGATEM®; Ontario Geological Survey, Geophysical Data Set 1041

Tims, A 2005. Assessment Report on the Structural Geology, Petrology and Geochemistry of the Mann Township Property for: Tres-Or Resources ltd. and SNL Enterprises Inc.

14

STATEMENT OF QUALIFICATION

To accompany the report entitled: Assessment Report on Geochemical Survey on Claims in Mann and Duff Townships, Porcupine Mining District for Tres-Or Resources Ltd and SNL Enterprises Inc., April 24, 2006.

I, Elaine Ba§a, of the city of Temiskaming Shores, in the Province of Ontario, Canada, hereby certifY as follows concerning my report on the Tres-Or Resources Ltd.' s and Arctic Star Diamonds Corp.'s Savard Township property, Ontario, 2006:

1. I graduated from Carleton University in 1985 with a degree of Bachelor of Science, Honours Geology.

2. I am a Professional Geologist and a member of Professional Geoscientists of Ontario (member number 0895).

3. I have worked continuously in the mining industry for the past 20 years. 4. The attached report is a product of:

a) data provided to me by the property owner b) reports identified in the reference section of this report

5. I am acting as consulting geologist and Project Manager of the Mann Twp Property for Tres-Or Resources Ltd. I have verified the reported work and all related expenses.

Dated this 5th day of December, 2006 in Temiskaming Shores, Ontario

Elaine Ba§a, P.Geo.

LIST OF PERSONNEL

Mann Twp- line cutting & MMI sampling Field Crew

Joey Ethier Box 59, North Cobalt, ON POJ lRO 705-676-6417

Glen Coyne R.R. # 1, Notre Dame du Nord, PQ JOZ 3BO 819-723-2656

Supervision, Geology, Report Writing

Elaine BaSa, P.Geo. Box 847, Haileybury, ON PO] lKO 705-672-3551

Martin Ethier Box 304, Haileybury, ON POJ lKO 705-672-5814

Sample processing

SGS Minerals Services SGS Canada Inc 1885 Leslie Street, Don Mills, ON M3B 2M3 416-445-5755

Geochemical Consultant

Mount Morgan Resources Ltd Dr. Mark Fedikow 34 Wellesley Court, Winnipeg, MB R3P lX8 204-487-9627

Kyle Derasp 146 Third Ave, Apt B Timmins, ON

Bruce Pigeon Box 256, Verner, ON POH 2MO

C. James Laidlaw R.R. # 3, Madoc, ON KOK 2KO 613-473-5065

15

APPENDIX 1

A Mobile Metal Ions Process (MMI-M) Soil Geochemical Survey for Tres-Or Resources - Interpretations and Recommendations

Report by Dr. Mark Fedikow - Mount Morgan Resources Ltd.

A Mobile Metal Ions Process (MMI-M) Soil Geochemical Survey For Tres-Or ResourcesInterpretations

and Recommendations

Prepared For:

Tres-Or Resources and SNL Enterprises P.O. Box 178, 449 Lakeview Ave

North Cobalt, ON POJ 1 RO 705-672-5644 - phone

705-672-5924 - fax

February 2006

Prepared By: Mount Morgan Resources Ltd.,

34 Wellesley Court, Winnipeg, Manitoba, Canada

R3P 1X8 Tel.lFax. : 204-487-9627

E-mail: [email protected]@allstream.net

EXECUTIVE SUMMARY

The Tres-Or MMI-M survey, based on a composite inorganic-organic dataset, has

defined an extensive east-west anomalous response comprising the metals Zn and

Cd. The coincidence of ZnRR and CdRR in the MMI-M results indicates the Zn-Cd

Signature is not related to anthropogenic contamination from logging activity but

rather to bedrock-hosted base metal mineralization. Adjacent to the Zn-Cd anomaly

on the west end of the grid are non-coincident Au and Ag responses that have

moderate-contrast RR. The variation in sampling density on the grid has not skewed

the MMI-M responses. The compositing of organic and inorganic MMI-M

geochemistry has not masked the presence of the Zn-Cd anomaly but it is noted that

elements such as U and Pb are enriched in the organiC samples. Future MMI-M

surveys should avoid the collection of organic samples and all efforts directed

towards acquiring inorganic material. This may require the use of an auger. Prior to

exploration follow-up of these results it is strongly suggested that all available

geological and geophysical data be reviewed with the aim of confirming the

presence of the east-west Zn-Cd anomaly. Modeling of geophysical responses over

this anomaly will confirm the attitude required for a successful drill test of the

geological-geophysical-geochemical multivariate anomaly.

Tres-Or MMI-M Survey 2 Mount Morgan Resources Ltd.

PREAMBLE

The exploitation of mineral commodities in the near-surface geological

environment has become increasingly difficult due to the exhaustion of

mineralization exposed at surface and the mantling of prospective bedrock by

glacially transported till and its derivatives. Thick glaciofluvial and glaciolacustrine

sediments topped by organic deposits make mineral exploration in these terrains

challenging. For this reason a plethora of innovative exploration geochemical

selective and partial digestions, coupled with state-of-the-art instrumentation

capable of measuring concentrations in the parts per billion (ppb) and sub-parts

per billion range, have been developed. These techniques offer the explorationist

tools to "see through" overburden and derive useful mineral exploration data for

integration with geology and geophysics and ultimately for drill-testing

multivariate anomalies.

The proprietary Mobile Metal Ions Process (MMI) soil geochemical technique has

been utilized on a wide range of commodity types from base and precious metals

to diamonds worldwide. The Process is based upon proprietary partial extraction

techniques, specific combinations of ligands to keep metals in solution, and relies

on strict adherence to sampling protocols usually established during an

orientation program. Geochemical data resulting from MMI analysis of improperly

collected soils cannot be ameliorated with univariate and/or multivariate statistical

and graphical solutions.


The recognition of anomalies in geochemical data has progressed from simple

visual inspection in small data sets to multivariate, parametric and non

parametric or robust statistical methods for large datasets usually extracted from

regional geochemical surveys. Derived parameters from these statistical

exercises, such as factor scores or discriminant functions, have been

successfully utilized in reducing a large number of potentially useful variables to

a select few variables that identify and localize anomalous geochemical

signatures. These statistical approaches have been required to manipulate

accurate and precise, low-cost, multi-element geochemical data.

The MMI technology uses a different approach to exploration geochemistry by

analyzing soils for a select few commodity elements upon which to base property

evaluations. Having stated this, the MMI-M multi-element suite that was utilized

to analyze inorganic soils from the Tres-Or survey comprises analyses for 38

elements. These comprise a mUlti-element suite that reports ppb and sub-ppb

analyses for base and precious metals, pathfinder elements for these

commodities, as well as elements useful for mapping bedrock geology obscured

by glacial overburden and its derivatives. The large number of elements in the

database provides an opportunity to assess an area of interest for a wide range

of metallic mineral deposits with only minor drawbacks in terms of lower limits of

determination. The specific details of this assessment are described below.


TERMS OF REFERENCE

The author of this report was contracted by Elaine Basa of Tres-Or Resources to

undertake an interpretation of a Mobile Metal Ions (MMI-M) soil geochemical

survey that was recently completed on their property. The following report is

based upon data supplied by E. Basa.

PURPOSE OF THE SURVEY

The MMI-M survey undertaken by Tres-Or is an attempt to assess their poorly

exposed property for potential to host base and precious metal mineral deposits

utilizing Mobile Metal Ions soil geochemistry. The approach is designed to

determine whether anomalous concentrations of bedrock-hosted base and or

precious metals are present in the survey area. Delineation of these anomalies

would provide focus for follow-up geophysical surveys and subsequent drill

testing.

SAMPLE COLLECTION AND ANALYSIS Sampling and analytical protocols were obtained from discussions with staff of

SGS Mineral Services (Toronto) as well as a review of these protocols that are

available on the MMI website (www.mmigeochem.com).

In MMI surveys there are some general approaches that are used to guide

sample collection including preferred depths of sampling and these are described

briefly here. Additional information is also available from the MMI website.


Soil samples, each weighing approximately 250 grams, are normally coJlected at

25-m stations in precious metal exploration and up to 50 m in the case of base

metals. Sample spacing should be established on the basis of a "best-estimate"

of the likely target being sought with estimates from historical data or exploration

results from nearby programs. Sample locations are documented according to

grid coordinates and GPS readings at each station. Samples are normally

collected from a consistent depth of 10-25 cm beneath the point at which soil

formation is initiated in the particular landscape environment where the survey is

taking place. The depth of sample collection and the targeting of high-contrast

base and precious metal residence sites may be different than that utilized for

this survey although this can only be determined by an orientation survey based

on a program of vertical profiling. Samples are normally collected with a stiff vinyl

trowel after the initial sample pit was dug with a shovel. The shovel is clean

without paint or rust. In particularly hostile overburden scenarios where

significant thicknesses of organic soils are encountered, samples may be

collected with an auger. A Dutch auger has been found to be particularly useful

for this purpose. Samples are bagged on site without preparation and shipped to

SGS Laboratories (Toronto, Ont.) for MMI-M analysis. The MMI-M is a neutral

extraction, as compared to an acid extraction for MMI-A and a base for MMI-B.

Analytical finish for all extractions is by inductively coupled plasma-mass

spectrometry (ICP-MS).


Of the 132 samples collected for the survey all but 10 were clays collected from

an environment dominated by moraine. The 10 non-clay samples were peat.

The samples submitted to SGS for analysis should include field duplicates,

replicates or standards although analytical duplicates and standard MMI

reference samples are utilized by SGS Mineral Services (Toronto) to monitor

analytical accuracy and precision. The author of this report was not involved in

the sample collection for this survey.

It is noted that the survey was conducted in an environment described as logged,

reforested and scarified with significant variability in slope (to >40 degrees) and

as such is considered to have been undertaken in a "disturbed" overburden

setting.

DATA TREATMENT AND PRESENTATION

Analytical data was examined visually for analyses less than the lower limit of

detection «LLD) for ICP-MS. Data <LLD were replaced with a value % of the

LLD for statistical calculations and graphical representation. The 25th percentile

for these data was determined using the software program SYST AT (V10) and

the arithmetic mean of the lower quartile used to normalize all analyses. The

normalized data represent "response ratios" which were utilized in subsequent

plots. Zeros resulting from this calculation are replaced with "1". Response ratios

are a simple way to compare MMI data collected from different grids, areas and


environments from year to year. This normalized approach also significantly

removes or "smoothes" analytical variability due to inconsistent dissolution or

instrument instability. Sample descriptions are reproduced in Appendix 1 and

analytical data with analytical duplicates as received from Tres-Or are presented

in Appendix 2. Edited analytical data and calculated response ratios with grid and

UTM coordinates are presented in Appendix 3. Peat sample MMI-M

geochemistry is also summarized in Appendix 3.

Response ratios from the Tres-Or survey are presented as individual and

combined element colored bubble plots. The color intensity and diameter of the

bubbles corresponds to the magnitude of the metal contents determined by MMI

M at that site for any particular element. The bubble plots are presented in

Appendix 4 and were produced with Vertical Mapper, a module within MAPINFO

(V10). In addition to the bubble plots, the results are also presented as geo

referenced "tiff" files that can be integrated with additional layers of data for

interpretation purposes. A "zipped" version of the plots is also presented. The

initial interpretation of the geochemical responses of the data are described

below and include a separate discussion on the inorganic ("clay") samples as

well as the organic or "peat" samples.


RESULTS

Data Reproducibility-Analytical Duplicates

Duplicate sample analyses are presented in Appendix 2 and permit an

assessment of the ability to reproduce analyses at a wide range in concentration

levels. Some variance is noted in select elements/duplicate pairs for inorganic

soils. These include the non-commodity elements Nb «0.5 vs. 0.7 ppb), Zr (18

vs. 6 ppb), Th (19.7 vs. 8.8 ppb) as well as select rare earth elements ("REE")

including Ce, Eu and Nd. At lower levels of concentration two duplicate pairs

exhibit some variance for Zn «20 vs. 20 ppb and <20 and 30 ppb). Variability is

not consistent and appears to be confined to select pairs of samples. It is noted

that excellent reproducibility is achieved for Au at low levels of concentration «2

ppb) and also for Cu, Pb and Ni (one exception 9 vs. 38 ppb) at widely variable

concentration levels. It is noted that all duplicate pairs for the elements As, Bi,

Sb, Sn, Te, TI and Ware <LLD and as such cannot be assessed for analytical

reproducibility.

When data is displayed as response ratiOS, much of the impact of variance in the

dataset can be avoided with the result that anomalous responses will not be

missed. In reviewing duplicate pair analyses it is advisable to assess the

responses as a percentage with an acceptable reproducibility of up to 35%. In

the Tres-Or survey, despite the presence of some variability in MMI-M analyses,

the data is interpreted not to be a hindrance to anomaly recognition.


Data Description

Table 1 provides the 25th percentiles and backgrounds used for the calculation

of response ratios for the Tres-Or inorganic soils. The Tres-Or dataset is marked

by a number of elements that have numerous samples at or below the lower limit

of determination (LLD). These include the elements As, Bi, Cd, Ce, Co, La, Mo,

Nb, Nd, Pd, Pr, Sb, Sm, Sn, Te, Ti, TI, W, Zn and Zr. Restricted ranges in

response ratios are noted for Ag, Ba, Ca, Pb and some intermediate and heavy

rare earth elements. These elements are typically less mobile than Cu or Zn and

their presence in measurable quantities in a small number of samples is

testament to this. The high percentage of samples with Bi, Cd, Sn, Wand Pd

contents <LLD in this survey is not surprising given their very low mobility in the

surficial/secondary environment. In this regard, any MMI-M analysis for Pd that is

>LLD should be reviewed with care for its overall significance in the survey. An

MMI analysis for Pd above the LLD should be field checked for possible

association with platinum group metal geological environments. In the absence

of coincident, elevated Cd responses with high-contrast Zn response ratios in

some samples can be cause for concern. Generally, coincident Zn- Cd

responses are interpreted to represent bedrock-hosted sphalerite mineralization.

The absence of Cd is suggestive of the derivation of Zn from the inclusion of fine

grained, well-humified organic material. This can result in what has been

described as a "false" gepchemical anomaly. There is good Zn-Cd coincidence in

the Tres-Or samples. The very wide range in Ag, Cd, Ce and other REE, Co, Cu,


Ni, Pb and Zn is noted and can often be an indication of two populations of data-

background and anomalous.

Table 1. Summary of 25th percentiles and backgrounds used for the calculation of response ratios, Tres Or MMI-M

survey.

ELEMENT 25th PERCENTILE BACKGROUND

Ag 6.6 31.8 As 5 1 Au 0.05 0.05 Sa 538 329 Si 0.5 1 Ca 496.1 401 Cd 5 5 Ce 2.5 2.5 Co 5.2 2.8 Cu 369 215 Dy 5.7 4 Er 3.49 2.5 Eu 0.51 0.3 Gd 4.7 2.8 La 0.5 1 Mg 46.9 26.3 Mo 2.5 1 Nb 0.25 0.25 Nd 0.5 1 Ni 48.9 20.4 Pb 29.1 14.7 Pd 0.5 1 Pr 0.5 1 Rb 34.9 22 Sb 0.5 Sm 1.5 0.6 Sn 0.5 1 Sr 1049 903 Te 5 1 Th 2.04 1.15 Ti 1.5 1.5 TI 0.25 1 U 4.4 2.8 W 0.5 Y 23.5 16

Yb 3.6 2.4 Zn 10 10 Zr 2.5 1


The diagnostic signal of a significantly mineralized zone will produce moderate

to high-contrast apical responses over the target; however, away from the

mineralization at "background" locations there may be no trace of the presence of

a specific metal in the analYSis. This is another consideration when viewing MMI

data-the presence of significant numbers of elements < the lower limit of

determination (LLD) is not necessarily cause for concern or that the MMI

extraction is not working or has been "buffered" by soil composition. The MMI

process is designed to only extract metals that are moving from source to surface

and characteristically report metal contents in low ppb concentrations.

Sampling Materials

The nature of the material collected from the Tres-Or survey area for MMI-M

analysiS was predominantly clay (122 of 132 samples) from a moraine. The ten

samples that were not clay were a suite of multi-colored peat. Care was taken to

exclude any significant organic component from the inorganic samples.

Method of Interpretation

Multivariate statistical and graphical techniques were not utilized for the

interpretation of MMI data in the Tres-Or survey. A simple visual and graphical

approach was used for the interpretation of MMI-M data. Subsequent to the

calculation and plotting of response ratios the plots are examined for anomalous

spikes or groups of elevated responses for single and/or coincident elements.

Element groupings such as Au-Ag, Au-Ag-Pd, Zn-Cd, Ni-Co, Ni-Co-Ag and Ni-Cu


all have relevance to underlying geological conditions and their contained

mineralization and are used to assist the rankings of any particular MMI response

in terms of follow-up. Generally, a response ratio of >20 or 20 times background

is an initial indication of a low contrast anomalous response although this

"threshold" is not universal. A response of between 20 and 50 is used as a

moderate response with RR>50 being referred to as high contrast. Often, pattern

recognition in the interpretation of geochemical data is paramount.

Spearman Rank Correlation Coefficient Matrix

A particularly useful method of assessing a multi-element database is by

examining inter-element relationships and relating these to plausible geological

interpretations or "cause and effect" relationships. This method was used in the

assessment of the Tres-Or dataset. Data are not transformed (log-log, power

transform, etc) but are interpreted with the use of a Spearman-Rank non

parametriC matrix.

The results of this assessment are presented in their entirety in Table 2 and an

abbreviated version is given be/ow. The abbreviated version includes those

elements interpreted to be significant in terms of plausible mineral potential in the

survey area and those elements that provide an indirect measure of analytical

accuracy.

Ties-Or MMI-M Survey 13 Mount Morgan Resources Ltd.

Results

Table 2 (abbreviated) summarizes a suite of inter-correlated element pairs with

elevated correlation coefficients ("r"). These couplings are indicative of plausible

geological and geochemical criteria that are indicative of bona fide geochemical

responses to bedrock and contained mineralization.

The precious metal Au-Ag element pair is a geological and geochemical coupling

between two elements that are commonly observed in association with one

another in a precious metal mineralized system. There is also a significant

correlation between Ag and Cu indicative of an association of Ag with base

metals, another commonplace scenario in mineralized environments. Of some

interest is the Ag-Ca-Sr inter-correlation. This group of elements could indicate

the presence of carbonate alteration associated with precious metal vein systems

such as Au-Ag with some base metals present (Le., Ag-Cu). These inter

correlated precious-base metal pairs are "expected" in a mineralized environment

and suggestive of elements that may be useful to define anomalous geochemical

patterns in the overall dataset.

In addition to precious +/- base metal element pairs there are also Significant

correlation coefficients reported for the base metals. These include the highest Ur"

in the Spearman Rank matrix for the Zn-Cd (0.729) correlation as well as the

couplings for Pb-Cd and Co-Pb. These element pairs are suggestive of a base

metal mineralized environment comprising sphalerite (Zn-Cd), galena (Pb) and


iron sulphides (Co). The presence of a Zn-Cd is considered to be a necessary

association to discriminate between bona fide bedrock-hosted sphalerite

mineralization and possible Zn-additions through anthropogenic contamination.

The presence of this coupling in the Tres-Or data is signaling the presence of a

potential Zn-rich mineralized environment on the surveyed property.

A series of significant "lithologically-sensitive" inter-correlated element pairs are

also present in Table 2. These include Mg-Ca; Mg-Sr and Ca-Sr. Typically these

three elements are indicators of the presence of mafic or possibly ultramafic

lithologies in the subsurface. Similarly, the presence of elevated REE and

possibly U and Th are likewise indicators of felsic lithologies. The variation of

these lithologic indicators on the Tres-Or property are discussed in the upcoming

section encapsulating the Vertical Mapper bubble plots that addresses MMI-M

element suite variability on the survey grid.

Table 2 (abbreviated). Summary of significant inter-element relationships in the Tres..()r MMI-M survey based on a Spearman-Rank correlation coefficient matrix. ELEMENT PAIR CORRELATION COEFFICIENT "R"

Ag-Au 0.493 Ag-Cu 0.629 Ag-Ca 0.659 Ag-Sr 0.474

Cu-Mg 0.389

Zn-Cd 0.729 Pb-Cd 0.413 Co-Cd 0.542

Mg-Sr 0.56 Mg-Ca 0.407 Ca-Sr 0.677


Geochemical Anomalies-Vertical Mapper Bubble Plots

The variation in concentration of the MMI-M suite of elements in samples

collected from the Tres-Or survey grid were interpreted with the use of Vertical

Mapper bubble plots. These plots are presented in Appendix 4. The following

observations are noted from a review of these graphics.

Precious Metals

AuRR: A single-sample, moderate-contrast Au response is present in the area

midway between lines 1800E and 2000E. This single anomalous response of

26RR occurs at the end of a sampling transect and as such is considered open

to the southwest of the survey area. Scattered single-sample responses with RR

of between 5 and 10 are present on the remainder of the grid but these

responses are interpreted as insignificant.

AgRR: The AgRR responses in the Tres-Or MMI-M survey are low-contrast

«20RR) with a maximum of 15RR. Interestingly, the AgRR form a cluster of

multi-sample, low-contrast responses in the southwest corner of the grid. There

is no correspondence between the RR26 Au response and elevated Ag

responses.

Base Metals

ZnRR: Very high-contrast Zn responses of up to 160RR or 160 times

background are present in the survey area. There appears to be an east-west

"band" of elevated Zn (RR20 to 160) that occupies the central area of the grid


and stretches from line 2600E to line 1900E. There are also low-contrast, mainly

single sample responses on the grid but these are interpreted to be subsidiary to

the "east-west" anomaly. It is noted that the AuRR and AgRR precious metal

response occurs to the west and south of the ZnRR east-west anomaly although

there is near coincidence between the 160RR Zn response and the overall Au-Ag

response in this area.

Attention should be brought to the nature of the samples that comprise the ZnRR

response in the Tres-Or survey. Portions of the east-west trend comprise

geochemical responses from peat samples. Although this does not necessarily

negate the ZnRR anomaly care in interpretation must be exercised. This is

discussed in an upcoming section.

CdRR: Although the Cr responses on the grid are of low-contrast (maximum RR

to 14) their coincidence with Zn responses is excellent. This coincidence was

identified in the Spearman-Rank correlation coefficient matrix that was described

earlier. As a stand-alone element, the Cd responses do not form a readily

identifiable anomaly but do substantiate the presence of a high-contrast Zn

response on the grid.

There is a range of RR for Cd of 4-1 0 in the peat samples and there is no

obvious relationship between the magnitude of the Zn response and that of Cd in

the peat samples. This is addressed further in an upcoming section.


PbRR: The Pb responses from the Tres-Or grid have maxima of 27RR and are

broadly coincident with those for Zn. The highest PbRR occurs on line 1950E at

the northern end of the line. This site represents the last sample collected from

this particular transect and for this reason, as well as an adjacent low-contrast

response on line 2000E, the Pb response is considered to be open to the north. It

is noted that this response comes from a sample of peat.

CuRR: Only low-contrast CuRR were obtained from the grid with maxima of

11 RR. The majority of these low-contrast responses occur at the western end of

the grid in the general area of strong Zn-Cd responses. On the basis of the low

CuRR data there would appear to be no significant source of Cu mineralization in

the bedrock underlying the survey area.

Lithologically Sensitive Elements (Ca+Mg+Sr, Ce and Ti)

The lithologically sensitive suite of MMI elements can be used to detect changes

in subsurface geology and identify lithologic associations with the commodity

elements. This permits an assessment of the validity of the MMI response in

terms of geology and contributions of mobile metal ions from the bedrock to the

overall geochemical response for any given MMI-M element.

CeRR: High-contrast (RR to 204) Ce responses tend to dominate the eastern

end of the grid on the southern portions of lines 2600E and 2800E. Elsewhere on

the grid high-contrast responses are restricted to one- or two-sample responses.


In terms of the contribution of peat samples to the CeRR these are considered

negligible for most samples with a range in RR of 1-18. It is possible the

southeast corner of the grid is underlain by a felsic lithology.

TiRR: Often, the TiRR can effectively discriminate mafic from felsic lithologies in

the underlying bedrock or the presence of a unique lithology with strongly

elevated Ti. The TiRR results from the Tres-Or grid have maximum RR of 76 but

generally form erratic and scattered single-site elevated responses and does not

define a pattern that could be attributed to a single lithology. There is a

suggestion of a zone of elevated Ti in the southeast grid area, which would

correspond to the Ce anomaly, discussed earlier.

(MgRR + CaRR + SrRR): Although the additive parameter MgRR + CaRR +

SrRR has low-contrast response ratios (maximum = 11) the majority of these

responses occur west of line 2000E. This pattern is suggestive of a lithologic

change to a more mafic rock type from east to west. This response does coincide

with the highest ZnRR of 160, AuRR of 26 and AgRR of 15.

Peat and Inorganic Samples

The Tres-Or database is characterized by a mixture of primarily inorganic, clay

rich soil and organic soil described as peat. The varying capacities of both of

these sampling media requires that initially their geochemical responses be

assessed separately.


A total of 10 peat samples were sampled during the MMI survey and analyses

indicate only a few MMI-M suite elements are significantly elevated in the organic

samples. The ranges for these elements include ZnRR (9-67), PbRR (1-27),

NiRR (1-12), Nd (1-27) and U (1-21). Of interest in this survey is the presence of

elevated Zn responses in the peat samples. The remainder of the peats have

moderate to low contrast responses and are not significant in terms of "masking"

a Zn anomaly originating in the inorganic soils.

A significant number of peat samples were collected from lines 2600 E and

2250E with single samples from lines 2050E and 1950E. Elevated ZnRR were

obtained from grid references 150N, 350N and 525N on line 2600E with a range

in RR of 17-66 and on line 2250E at 400N and 525N (50RR and 67RR,

respectively). A single elevated response of 67RR was obtained from 500N on

line 2050E. These responses contribute significantly to the "east-west" anomaly

described above although it is noted that the highest ZnRR of 160 was obtained

from an inorganic sample at grid location 475N on line 1900E. This is an

indication that the ZnRR anomaly developed in an east-west orientation is a

composite anomalous response comprising both organic and inorganic soil.

Recommendations based on this observation for exploration follow-up are given

below.


OBSERVATIONS

The MMI-M survey on the Tres-Or grid has defined an extensive base metal

anomalous response primarily for In but also including some elevated Au and

Ag. Although these elevated responses do not coincide they occur as discrete

and adjacent responses.

Base metal anomalies based on the lnRR and to a lesser extent PbRR are

moderate to high-contrast and are extensive, multi-sample and need to be

followed up with ground geophysical surveys or integrated with existing ground

geophysical data. The coincidence between In and Cd, like the required

coincidence between Au and Ag, within the base metal anomalies is interpreted

to represent the presence of bedrock-hosted sphalerite mineralization. Of some

importance is the presence of a composite In anomaly based on elevated In in

organic soil (peat) and inorganic soil (clay). The relatively small number of peat

samples in the survey (n=10) makes a statistical review and comparison with the

inorganic soils impractical. Visual assessment indicates a broad range in

response ratios for In in the peat and is suggestive of two possible data

populations representing anomalous and background. When these results are

integrated with the inorganic soils an east-west response becomes apparent and

should be the focus of follow-up exploration. Recommendations to this effect are

given below.


In addition to elevated ZnRR in the peat these samples also have elevated Pb

and U, typically enriched in fine-grained well-humified peat.

Survey results may be somewhat skewed by the change in sampling density

near the west end of the grid where Significantly elevated ZnRR are documented

(RR=160) and where low- to moderate-contrast precious metal responses are

present. Nevertheless this change in sampling pattern has resulted in the

definition of an anomalous multi-element and multi-sample base and precious

metal anomaly that extends westward at least to line 1900E.

Results for lithologically sensitive MMI-M suite elements indicates a potentially

felsic lithology underlies the eastern grid area. The western grid area is marked

by a more mafic to intermediate response. This apparent lithologic change has

no effect on the disposition of the ZnRR east-west anomaly. The coincidence of

ZnRR with CdRR indicates the bedrock underlying this anomaly has an MMI-M

signature indicative of Zn (sphalerite) mineralization.

CONCLUSIONS AND RECOMMENDATIONS

The following conclusions are evident from this MMI-M survey on the Tres

Or grid.

1. The survey has successfully demonstrated that MMI-M partial extractions on

organic and inorganic soil samples collected from the Tres-Or grid have

Tres-Or MMf-M Survey 22 Mount Morgan Resources Ltd.

isolated high to moderate and low-contrast MMI-M base and precious metal

anomalies. This anomaly is primarily an east-west-trending Zn-Cd

assemblage with lesser Au and Ag.

2. The highest ZnRR response is a 160RR obtained from line 1900E at station

475N. This result when integrated with the organic soil results helps to

substantiate the presence of the anomalous Zn response. The presence of

coincident Cd responses with those for Zn satisfy the desired requirements of

an MMI-M anomaly for bedrock-hosted Zn-rich mineralization

3. Sampling materials collected for MMI analysis are effective and appropriate

sample media for an MMI-M survey. Sample collection appears to have been

satisfactorily undertaken in this survey.

4. The analyses generated by the MMI-M extraction are accurate and precise

and are effective for the detection of high-contrast anomalies.

The recommendations that flow from this survey are as follows:

1. The MMI process does not indicate the grade of mineralization responsible for

the production of an MMI anomaly nor does it indicate the depth of the source

region for the anomaly. Accordingly, it is strongly recommended that an

attempt at modeling the geological setting of the target mineralization based


on their geophysical responses with emphasis on depth to source be

undertaken prior to a diamond drill program. This exercise can greatly assist

the drilling when attempting to provide explanations for the geological context

of geophysical and MMI anomalies.

2. The presence of elevated MMI-M element suite signatures at the ends of

some of the sampling transects indicates the potential for expanding the MMI

survey to truncate or elucidate these anomalous responses.

3. Prior to drill testing all MMI-M geochemical information should be integrated

with available geophysical and geological data.

4. A program of QAlQC sample collection should be maintained and expanded

to include Standard Reference Materials designed for MMI-M extraction.

Mark Fedikow

Mount Morgan Resources Ltd.

Winnipeg, Manitoba

February 6, 2006


MarkA.F. Fedikow, HB.Sc., M.Sc., Ph.D., P. Eng. P.Geo.

Consulting Geologist and Geochemist Mount Morgan Resources Ltd.

34 Wellesley Court Winnipeg, Manitoba R3P 1X8

Tel/Fax: 204-487-9627 Email: [email protected]@allstream.net

CERTIFICATE of AUTHOR

I, Mark A.F. Fedikow, HB.Sc., M.Sc., Ph.D., P.Eng., P.Geo., do hereby certify that:

1. I am currently a self-employed Consulting Geologist/Geochemist with an office at:

34 Wellesley Court, Winnipeg, Manitoba, Canada R3P 1X8.

2. I graduated with a degree in Honors Geology (B.Sc.) from the University of Windsor (Windsor, Ont.) in 1975. In addition, I earned an M.Sc. in geophysics and geochemistry from the University of Windsor and a Doctor of Philosophy (Ph.D.) in exploration geochemistry from the School of Applied Geology, University of New South Wales (Sydney) in 1982.

3. I am a Member of the Association of Professional Engineers and Geoscientists of Manitoba. I am also a Fellow of the Association of Exploration (Applied) Geochemists, and a Member of the Prospectors and Developers Association of Canada.

4. I have worked as a geologist for a total of thirty years since my graduation from university; as a graduate student, as an employee of major and junior mining companies, the Manitoba Geological Survey and as an independent consultant.

5. I have read the definition of "qualified person" set out in National Instrument 43-101 ("NI 43-101") and certify that by reason of my education, affiliation with a professional association (as defined in NI 43-101) and past relevant work experience, I fulfill the requirements to be a "qualified person" for the purposes of NI 43-101.

6. I am responsible for the preparation of the technical report titled II A Mobile Metal Ions Process (MMI-M) Soil Geochemical Survey For Tres-Or Resources - Interpretations and Recommendations".

7. I have not had prior involvement with the property that is the subject of the Technical Report.

8. I am not aware of any material fact or material change with respect to the subject matter of the Technical Report that is not reflected in the Technical Report, the omission to disclose which makes the Technical Report misleading.

9. I am independent of the issuer applying all of the tests in section 1.5 of National Instrument 43-101.

10. I consent to the filing of the Technical Report with any stock exchanges or other regulatory authority and any publication by them, including electronic publication in the public company files on the web-sites accessible by the public, of the Technical Report.

Dated this 6th Day of February, 2006.

Signed by Mark Fedikow

Signature of Qualified Person

"M.A.F. Fedikow" Print name of Qualified Person

APPENDIX I

Sample Descriptions

Sample Line Station Easting Northing Terrain Soil Type Slope Steepness

Slope Drainage Vegetation State

Material Colour

Number Direction Thickness

Mool 1800E 725N 495147 5411260 morain day flat gentle(1-5') poor scrub mix logged till>lm BNWH

Moo2 1800E 675N 495122 5411208 morain day flat gentle(1-5') poor scrub mix logged till>lm GYWH

MOOJ 1800E 625N 495103 5411163 morain clay flat genlle(1-5') poor scrub mix logged till>lm BNWH

MOO4 1800E 575N 495086 5411128 morain clay flat gentle(1-5') poor scrub mix logged tiU>lm BNWH

MOOS 1800E 550N 495073 5411107 morain clay moderate(5-20') N+ moderate scrub mix logged tiH>lm GYWH

MOO6 1800E 525N 495064 5411084 morain clay moderate(5-20') N- moderate scrub mix logged till>lm BNWH

Moo7 1800E SOON 495048 5411062 morain clay flat gentle(1-5') poor scrub mix logged till>lm BNRD

MOOS 1800E 475N 495040 5411031 morain clay flat gentle(l-5') poor scrub mix logged till>lm BNRD

MOO9 1800E 450N 495028 5411011 moraln clay flat gentle(1-5') poor scrub mix Iwoed till>lm GYWH

MOlO lBOOE 425N 495025 5410992 morain clay flat genlle(1-5') poor scrub mix logged till>lm BNRD

MOll 1800E 375N 49SOO2 5410947 morain clay moderate(5-20') E- well deciduous natural till>lm BNRD

M012 1800E 325N 494976 5410906 morain day steep(20-40') E- well deciduous natural till>lm BN

M013 1850E 375N 495025 5410904 moraln clay moderate{5-20') E- well scrub mix iOQged titl>lm BNRD

M014 1850E 425N 495052 5410948 morain clay flat genlle(1-5') poor scrub mix logged till>lm RD

M015 1850E 450N 495065 5410994 morain day flat gentle(1-5') poor scrub mix logged till>lm BNGY

M016 lB50E 47SN 495075 5411013 morain day flat gentle(l-S') poor scrub mix Iogaed till>lm BN

M017 1850E SOON 495086 5411031 morain clay flat gentle(l-S') poor scrub mix logged till>lm GYWH

M018 1850E S2SN 495117 5411055 Morain clay flat genlle(l-S') E- moderate scrub mix logged till>lm GYWH

M019 1850E S50N 495122 5411071 morain ctav flat gentle(l-S') poor scrub mix Iwaed till>lm GYWH

M020 1850E 57SN 495137 5411086 morain clay flat gentle(l-S') poor scrub mix logged till>lm GY BN

M021 1850E 62SN 495163 5411126 morain clay flat genlle(l-S') poor scrub mix logged till>lm GYWH

M022 1850E 67SN 495195 5411177 Morain clay flat gentle(l-S') poor scrub mix logaed till>lm GYWH

M023 1850E 725N 495225 5411210 morain clay flat gentle(1-5') poor scrub mix logged till>lm YLWH

M024 1900E 725N 495245 5411201 morain clay flat gentle(l -S') poor scrub mix logged till>lm GYWH

M025 1900E 875N 495221 5411159 morain clay flat gentle(1-5') poor scrub mix logged till>lm GYWH

M026 1900E 625N 495187 5411112 morain clay flat genlle(1-5') poor scrub mix loaaed till>lm GYWH

M027 1900E 575N 495166 5411077 morain clay flat gentle(1-5') poor scrub mix logged till>lm GYWH

M028 1900E 550N 495159 5411042 moraln clay flat genlle(1-5') poor scrub mix logged till>lm BN

M029 1900E 525N 495143 5411032 morain clay flat genlle(1 -5') poor scrub mix Iwaed till>lm BNGY

M030 1900E SOON 495143 5411014 morain day flat genlle(1 -5") poor scrub mix logged tiH>lm BNGY

M031 1900E SOON 495140 5411014 morain day flat genlle(1-5') poor scrub mix logged till>lm BNGY

M032 1900E 475N 495125 5410986 morain clay flat genlle(1-5') poor scrub mix Iwaed peal BL

M033 1900E 450N 495107 5410964 moraln clay . flat genlle(1-5') poor scrub mix logged till>lm BN

M034 1900E 425N 495106 5410939 morain clay flat genlle(1 -5') poor scrub mix logged till>lm BNRD

M035 1900E 375N 495078 5410894 Morain clay flat genlle(l-5') poor scrub mix Iwged tiH>lm GYWH

M036 1950E 425N 495135 5410931 morain day flat aenlle(1-5') poor scrub mix logged tiH>lm GYWH

M037 1950E 450N 495134 5410944 morain clay flat genlle(1-5') poor scrub mix logged till>lm BLGY

M036 1950E 475N 495160 5410969 morain clay flat genlle(1-5') poor scrub mix iOQged till>lm BNWH

M039 1950E SOON 495178 5410984 morain clay flat genlle(l-5') poor scrub mix Iwoed WI>lm BNWH

M040 1950E 525N 495187 5411010 morain day flat aenlle(1 -5') poor scrub mix . logged till>lm BNGY

M041 1950E 550N 495199 5411033 morain clay flat gentle(1-5') poor scrub mix logged till>lm YL

M042 1950E 575N 495211 5411048 morain clay flat gentle(l-S') poor scrub mix loaaed till>lm BNYL

M043 1950E 625N 495233 5411094 mora In clay flat aenlle(1-5') . . poor scrub mix logged till>lm BNYL

M044 1950E 675N 495259 5411141 morain clay flat genlle(1-5' ) poor scrub mix logged till>lm YL

M045 1950E 725N 496282 6411182 moraln peat flat gentle(l -S') poor scrub mix 1000ged till>lm YL

M046 2000E 725N 495320 5411160 morain clay flat aentle(1-5') jl<lOr scrub mix logged till>lm GY

M047 2000E 675N 495301 5411109 morai" clay flat genlle(1-5') poor scrub mix logged till>lm BN

M048 2000E 625N 495275 5411068 morain clay flat genlle(1 -5') poor scrub mix logged till>lm BNYL

M049 2000E 57SN 495259 5411019 morain clay flat genlle(1 -5') poor scrub mix logged till>lm BN

M050 2000E 550N 495239 5410986 morain clay flat gentle(1 -5') poor scrub mix loaaed till>lm BN

M051 2000E 52SN 495235 5410979 morain clay flat aentle{1-5') poor scrub mix logged till>lm BN

M052 2000E SOON 495219 5410955 morain clay flat gentle(1-5') poor scrub mix logged till>lm BNGY

M053 2000E 47SN 495213 5410936 moraln clay flat genlle(1-5') poor saubmix logged IiII>lm BNYL

M054 2000E 450N 495195 5410910 morain clay flat gentle(1-5') poor scrub mix logged till>lm BN

M055 2000E 425N 495190 5410885 morain clay flat genlle(1-5') moderate scrub mix Iwaed till>lm BNYL

M056 2050E 450N 495232 5410904 Morain clay flat genlle(1-5' ) poor scrub mix . logged till>lm GY

M057 2060E SOON 495257 5410940 moraln peat flat gentle{1-5') poor scrub mix IOQlled tlll>lm BL

M058 2050E 550N 495301 5410965 morain clay flat genlle(1-5') poor scrub mix logged till>lm GYBN

M059 2050E 600N 495333 5410994 morain clay flat genUe(1 -5') poor scrub mix IOQlled till>lm BNYL



Material Colour


M060 2100E SOON 495349 5410995 morain peat flat gentle(l-5') poor scrub mix logged till>lm BL

M061 2100E SOON 495352 5410996 moraln peat flat gentle(l-5') poor scrub mix logged till>lm BL

M062 2100E 550N 495333 5410957 moraln peat flat genlle(1-5' ) poor scrub mix logged till>lm BL

M063 2100E SOON 495306 5410905 morain clay flat gentle(1-5') poor scrub mix logged till>lm GY

M064 2100E 450N 495277 5410864 morain day flat gentle(l-5') poor scrub mix logged till>lm YL

M065 2100E 400N 495251 5410820 morain day flat gende(1-5' ) poor scrub mix logged till>lm YL

M066 2150E SOON 495349 5410881 morain day flat gende(1-5') poor scrub mix logged till>lm GY

M007 2350E SOON 495514 5410783 morain day flat gende(1-5') poor coniferous natural till>lm BNGY

M068 2350E 525N 495530 5410803 moraln day flat genlle(1-5') poor coniferous natural till>lm BN

M069 2350E 550N 495541 5410822 morain clay flat gende(1-5') poor coniferous natural till>lm BN

M070 2350E 575N 495548 5410850 morain clay flat genUe(1-5') poor coniferous natural till>lm BN

M071 2350E SOON 495582 5410872 morain day flat genUe(1-5') poor coniferous natural titl>lm BN

M072 2350E 625N 495578 5410911 morain clay flat gentle(l-5' ) N- moderate coniferous natural till>lm BN

M073 2350E 650N 495588 5410930 moraln day flat genlle(1-5') moderate coniferous natural till>lm BN

M074 2250E 650N 495514 5410965 morain day flat genlle(1-5' ) moderate coniferous natural till>lm BN

M075 2250E 625N 495490 5410935 morain clay flat gentle(1-5') moderate coniferous natural till>lm BN

M076 2250E 600N 495488 5410922 morain clay flat gentle(l-5' ) moderate coniferous natural till>lm BN

M077 2250E 575N 495473 5410909 mora In peat flat g8ntle(1-5') poor deciduous natural tlll>lm BN

M078 2250E 550N 495458 5410880 moraln peat flat gentle{l-5') poor deciduous natural tlil>lm BL

M079 2250E 525N 495446 5410852 moraln peat flat gentle{l-5') poo~ deciduous natural tlil>lm BL

M080 2250E SOON 495436 5410832 morain clay flat genlle(l-5') poor deciduous logged till>lm GY

M081 2250E 475N 495424 5410810 morain day flat genlle(1-5') poor scrub mix logged till>lm BNGY

M082 2250E 450N 495410 5410766 morain day flat~enlleil-5') poor scrub mix 10000ed till>lm GYWH

M083 2250E 425N 495390 5410764 morain day flat genlle(1-5') poor deciduous logged till>lm YL

M084 2250E 400N 495377 5410750 morain peat flat gentle(l-5') poor scrub mix logged tlil>lm BL

M085 2250E 375N 495364 5410720 morain day flat gende(1-5') poor deciduous logged till>lm GY

M066 2250E 350N 495346 5410693 morain day flat genUe(l-5') poor scrub mix logged till>lm GY

M087 2250E 300N 495323 5410657 morain clay flat genlle(l-5') moderate coniferous logged till>lm BNWH

M088 2250E 250N 495306 5410621 morain clay moderate(~20') N+ well coniferous logged till>lm BN

M089 2250E 200N 495276 5410582 morain clay moderate(~20') N+ well coniferous logged tiU>lm BNWH

M090 2250E 200N 495280 5410580 morain day moderate(~20') well coniferous logged till>lm BNWH

M091 2800E 300N 495821 5410410 morain day flat genUe(1-5' ) poor scrub mix natural till>lm BNYL

M092 2BOOE 350N 495846 5410451 morain day flat genlle(1-5') poor deciduous natural till>lm BNYL

M093 2800E 400N 495873 5410493 morain day flat genlle(1-5') poor coniferous natural till>lm BNYL

M094 2800E 425N 495890 5410506 morain day flat genlle(1 -5') poor coniferous natural till>lm BNYL

M095 2BOOE 450N 495903 5410523 morain day flat gentle(1-5') poor coniferous natural till>lm BNYL

M096 2BOOE 475N 495919 5410547 morain clay flat genlle(1-5' ) poor coniferous natural tin>lm BNYL

M097 2800E 500N 495923 5410578 morain clay flatgenlle(1-5') ~poor coniferous natural tiII>lm BNYL

M098 2800E 525N 495943 5410586 morain day flat genlle(1-5' ) poor scrub mix natural till>lm BN

M099 2BOOE 550N 495939 5410622 morain day flat genlle(1 -5' ) poor scrub mix natural till>lm BN

M100 2BOOE 575N 495936 5410649 morain clay flat genlle(1-5') poor scrub mix natural till>lm BN

M101 2800E SOON 495968 5410665 morain day flat_gentle{1 -5') . moderate scrub mix natural till>lm BN

M102 2BOOE 650N 495981 5410709 morain day moderate(~20') N- moderate scrub mix natural till>lm BN

M103 2600E 650N 495821 5410818 moraln peat flat gentle( 1-5') poor bog natural peat BL

M104 2SOOE BOON 495803 5410758 morain day flat genlle(1-5') ~poor bog natural till>lm BN

M105 2SOOE 575N 495779 5410739 morain day flat genIl9(1-5') poor bog natural till>lm BLBN

M106 2SOOE 550N 495772 5410715 morain day moderate(~20') moderate bog natural till>lm BNYL

Ml07 2600E 625N 495758 5410692 moraln peat flat gentle(l-5') moderate scrub mix natural tlll>lm BL

M108 2SOOE 500N 495741 5410668 morain day flat genUe{1 -5' ) moderate coniferous natural till>lm BN



Malerial Colour


Ml09 2600E 475N 495726 5410650 morain day flat genUe(1-5°) moderate coniferous natural till>lm BN

Mll0 2600E 4SON 495713 5410623 morain day flatgenIle(1-5°) moderate saubmix natural till>lm BL

Mlll 2600E 425N 495698 5410601 morain day flat genlle(1-5°) moderate scrub mix natural till>lm GY

Ml12 2600E 400N 495681 5410579 morain day flat genlle(1-5°) moderate deciduous natural till>lm BNGY

Ml13 2600E 360N 495655 5410543 moraln peat flat genlle{l-5°) moderate deciduous natural peat BL

Ml14 2600E 300N 495622 5410499 morain day moderate(5-20") N- well deciduous natural till>lm BN

Ml15 2600E 2SON 495584 5410458 morain clay flat genlle(1-5°) moderate scrub mix natural tiH>lm GL

Ml16 2600E 200N 495562 5410423 morain clay flat gentle(1-5°) moderate scrub mix natural till>lm BN

M117 2600E 150N 495528 5410383 moraln peat nat lIenUe{l-S0) poor scrub mix logged til1>1m BL

Ml18 2600E lOON 495499 5410347 morain clay flat genUe(1-5°) moderato coniferous lo!Ioed till>lm BNYL

M133 2600E lOON 495500 5410343 morain clay flat gentle(l-5°) moderate coniferous logged till>lm BNYL

M119 2600E SON 495471 5410297 morain day flat oontle(1-5°) moderate coniferous logged till>lm BN YL

M120 2800E 200N 495767 5410311 morain day flat genUe{1-5") well deciduous natural tiU>lm BNYL

M121 2800E 2SON 495795 5410352 morain day flat gentle(1-S0) moderate deciduous natural till>lm BNYL

M122 22SOE 1 SON 495278 5410551 morain day moderate(5-200) moderate coniferous natural till>lm BNYL

M123 2350E 47SN 495513 5410753 till day flat genUe(1-5°) moderate coniferous natural till>lm GY

M124 2350E 4SON 495506 5410729 till day flat gentle(1-S0) moderate coniferous natural till>lm GY

M12S 23SOE 42SN 495484 5410709 till clay flat gentle(l-5°) poor deciduous natural till>lm YL

M126 23SOE 400N 495467 5410686 tilVmuskeg day flat gentle(1-5°) poor deciduous natural till>lm YL

M127 2350E 375N 495452 5410659 till clay flat gentle(1-5°) poor coniferous logged till>lm GYWH

M128 23SOE 350N 495448 5410643 till clay flat genlle(1-5°) poor saubmix logged till>lm GYYL

M129 2350E 300N 495417 5410596 tilVrnuskeg day flat gentle(l-5") poor deciduous logged till>lm BNYl

M130 23S0E 250N 495388 5410561 till day flat genUe(1-S0) poor coniferous logged till>lm GYYL

M131 2350E 200N 495360 5410522 tilVmuskeg clay flat gentle(l-5°) poor deciduous logged till>lm BNYL

M132 2350E 1 SON 495324 5410484 till day flat genUe(1-5°) poor coniferous logged till>lm BNYL

flat gentIe(1-S0)

moderate(5-2O") N+ well coniferous natural bare rock BL - blaclk

outcrop till steep(20-400) N - moderate deciduous logged till pociket<l m BN - brown

moraln sand v/steep(>400) E+ poor scrub mix reforested till>lm RD - red

day E- mix scarified GY - grey

peat fire YL - yellow

grass WH-white

bog GN - green

ON - orange

APPENDIX II

Analytical Data with Analytical Duplicates as received from Tres-Or Resources Ltd.

Raw Analyses

ANALYTE Ag As Au Sa Bi Ca Cd Ce Co Cu !Oy Er Eu Gd La Mg MO Nb Nd NI METHOD MMloM5 MMloM5 MMloM5 MMloM5 MMI-M5 MMloM5 MMloM5 MMloM5 MMI·M5 MMI-M5 MMloM5 MMI-M5 MMI·M5 MMI-M5 MMI·M5 MMloM5 MMloM5 MMI·M5 MMI·M6 MMI·M6 DETECTION 1 10 0.1 10 1 10 10 5 5 10 1 0.5 0.6 1 1 1 6 0.5 1 5 UNITS PPB PPB PPB PPB PPB PPM PPB PPB PPB PPB PPB PPB PPB PPB PPB PPM PPB PPB PPB PPB M001 9 <10 0.2 880 <1 370 <10 <5 23 430 3 2 0.5 4 <1 120 <5 <0.5 <1 101 M002 21 <10 0.3 990 <1 810 <10 <5 17 660 12 8 1 10 <1 152 <5 <0.5 <1 56 M003 8 <10 0.2 740 <1 510 <10 <5 7 410 5 3.1 0.6 6 <1 128 <5 <0.5 <1 26 M004 10 <10 0.2 460 <1 540 <10 <5 <5 520 6 4.6 <0.5 4 <1 135 <5 <0.5 <1 60 M005 14 <10 <0.1 890 <1 670 <10 <5 13 1010 9 5.6 '0.8 8 <1 165 <5 <0.5 <1 37 M006 15 <10 0.1 620 <1 710 <10 <5 <5 590 8 5.7 <0.5 5 <1 121 <5 <0.5 <1 60 M007 33 <10 0.4 890 <1 920 <10 <5 5 520 21 18.6 0.8 12 2 106 <5 <0.5 2 <5 M008 28 <10 0.2 530 <1 760 <10 <5 8 780 10 7.7 <0.5 5 <1 130 <5 <0.5 <1 36 MOog 24 <10 0.2 800 <1 840 <10 <5 <5 320 11 8.9 <0.5 6 <1 103 <5 <0.5 <1 <5 M010 22 <10 0.3 710 <1 750 <10 6 <5 480 26 24 1.3 16 5 67 <5 <0.5 6 <5 M011 17 <10 0.2 830 <1 890 <10 <5 <5 480 15 15 <0.5 7 <1 124 <5 <0.5 <1 <5 M012 29 <10 0.2 600 <1 770 <10 <5 5 300 7 7 <0.5 3 <1 109 <5 <0.5 <1 8 M013 17 <10 0.4 600 <1 730 <10 <5 7 920 17 17.9 0.5 8 <1 83 <5 <0.5 <1 <5 M014 44 <10 0.3 550 <1 670 <10 <5 7 780 15 11.7 0.5 9 <1 121 <5 <0.5 <1 43 M015 19 <10 0.2 580 <1 680 <10 <5 8 550 9 6.2 0.6 7 <1 130 <5 <0.5 <1 23 M016 24 <10 0.3 820 <1 980 <10 <5 6 610 8 8.2 <0.5 3 <1 172 <5 <0.5 <1 22 M017 6 <10 0.2 1080 <1 650 <10 <5 <5 510 5 2.6 0.7 6 <1 171 <5 <0.5 <1 12 M018 9 <10 <0.1 1170 <1 640 <10 <5 14 800 5 3 0.8 6 <1 175 <5 <0.5 <1 30 M019 4 <10 0.1 1110 <1 530 <10 <5 7 600 7 3.4 1.5 10 <1 119 <5 <0.5 9 24 M020 7 <10 <0.1 910 <1 610 <10 72 <5 520 12 4.8 4.5 25 34 105 <5 <0.5 73 132 M021 7 <10 <0.1 580 <1 620 <10 <5 <5 500 6 2.9 1.4 9 <1 121 <5 <0.5 3 129 M022 8 <10 <0.1 960 <1 610 <10 <5 <5 640 5 2.2 1 7 <1 152 <5 <0.5 1 71 M023 2 <10 <0.1 1100 <1 470 <10 8 <5 340 7 3.3 2 12 4 103 <5 <0.5 18 27 M024 6 <10 <0.1 1070 <1 590 <10 <5 <5 380 6 3 1.3 9 <1 134 <5 <0.5 3 123 M025 <1 <10 <0.1 1140 <1 440 <10 33 10 470 5 2.4 1.1 7 <1 117 <5 <0.5 7 35 M026 2 <10 0.1 1240 <1 450 <10 6 5 330 5 2.6 1.3 8 <1 122 <5 <0.5 9 21 M027 3 <10 0.1 1210 <1 500 <10 7 9 360 6 2.9 1.4 9 <1 129 <5 <0.5 10 29 M028 8 <10 <0.1 1130 <1 630 <10 <5 <5 440 6 3.2 1.1 8 <1 164 <5 <0.5 1 37 M029 5 <10 0.2 1220 <1 560 <10 <5 <5 440 6 3.1 1.4 9 <1 150 <5 <0.5 7 14 M030 23 <10 <0.1 950 <1 640 <10 <5 25 2220 13 7.2 1.3 13 <1 161 <5 <0.5 <1 525 M031 20 <10 <0.1 840 <1 600 <10 <5 24 1510 8 5.4 <0.5 6 <1 157 <5 <0.5 <1 307 M032 1 <10 <0.1 250 <1 560 70 <5 11 100 1 0.9 <0.5 <1 <1 26 10 <0.5 <1 68 M033 8 <10 <0.1 770 <1 600 <10 <5 9 580 4 2.2 <0.5 4 <1 133 <5 <0.5 <1 92 M034 18 <10 0.2 960 <1 660 <10 <5 9 740 7 5 <0.5 5 <1 145 <5 <0.5 <1 137 M035 11 <10 1.3 1310 <1 640 <10 <5 11 910 12 6.4 1.8 14 <1 151 <5 <0.5 3 64 M036 10 <10 <0.1 880 <1 620 <10 <5 27 1230 8 4.5 1.3 9 <1 106 <5 <0.5 5 213 M037 13 <10 <0.1 550 <1 610 <10 <5 9 460 4 3 <0.5 2 <1 141 <5 <0.5 <1 64 M038 6 <10 0.2 980 <1 520 <10 8 7 470 6 3 1.6 9 1 115 <5 <0.5 12 45 M039 16 <10 <0.1 620 <1 710 <10 <5 6 860 6 4.7 <0.5 4 <1 107 <5 <0.5 <1 138 M040 6 <10 <0.1 760 <1 550 <10 <5 5 390 7 3.7 1.2 8 <1 116 <5 <0.5 3 74 M041 8 <10 0.3 600 <1 460 <10 18 <5 460 8 3.4 2.9 16 10 90 <5 <0.5 36 85 M042 13 <10 <0.1 1180 <1 640 <10 <5 6 520 6 3 1.3 8 <1 157 <5 <0.5 4 94 M043 16 <10 <0.1 570 <1 650 <10 <5 7 630 5 3.2 <0.5 3 <1 125 <5 <0.5 <1 89 M044 4 <10 <0.1 1050 <1 560 <10 <5 <5 390 5 2.2 1.4 8 <1 122 <5 <0.5 9 50 M045 <1 <10 <0.1 240 <1 440 30 17 107 90 6 5.5 0.8 5 7 33 <5 <0.5 11 63 M046 23 <10 <0.1 990 <1 680 30 361 122 750 17 10.4 4.8 26 119 66 <5 1.2 121 378

Raw Analyses

ANALYTE Ag All Au Sa Bi Ca Cd Ce Co Cu 'Oy IEr Eu Gd La Mil Mo Nb Nd NI METHOD MMI-II5 MMI-M5 MMI-M5 MMI-M5 MMI-MS MMI-M5 MMI-IIS MMI-M5 MMI-M5 MMI-MS MMI-M5 MMI-M5 MMI-MS MMI-MS MMI-M5 MMI-MS MMI-II5 MMI-M5 MMI-M5 MMI-MS DETECTION 1 10 0.1 10 1 10 10 5 5 10 1 0.5 0.5 1 1 1 5 0.5 1 5 UNITS PPB PPB PPB PPB PPB PPM PPB PPB PPB PPB PPB PPB PPB PPB PPB PPM PPB PPB PPB PPB M047 7 <10 <0.1 880 <1 600 <10 100 30 360 11 5.6 3.8 19 34 104 <5 <0.5 62 171 M048 13 <10 0.1 350 <1 460 <10 <5 <5 490 5 3.3 <0.5 3 <1 120 <5 <0.5 <1 96 M049 23 <10 <0.1 660 <1 660 <10 <5 6 1060 7 4.3 0.6 6 <1 155 <5 <0.5 <1 136 M050 17 <10 0.2 400 <1 640 <10 <5 5 590 6 4.6 <0.5 4 <1 119 <5 <0.5 <1 96 M051 15 <10 0.1 380 <1 660 <10 <5 9 760 4 3.6 <0.5 2 <1 110 <5 <0.5 <1 132 M052 12 <10 <0.1 490 <1 570 <10 <5 8 570 5 4 <0.5 4 <1 105 <5 <0.5 <1 123 M053 11 <10 <0.1 440 <1 670 10 <5 9 770 7 5.3 0.5 6 <1 89 <5 <0.5 <1 223 M054 16 <10 <0.1 570 <1 600 <10 <5 11 600 5 4.4 <0.5 3 <1 143 <5 <0.5 <1 131 M055 9 <10 <0.1 640 <1 550 <10 <5 7 760 8 5.1 1.4 9 <1 113 <5 <0.5 5 76 M056 9 <10 <0.1 640 <1 570 30 127 25 400 20 11.9 3.5 20 52 56 <5 <0.5 60 347 M057 2 <10 <0.1 510 <1 570 30 44 89 240 19 13.7 2.1 13 19 48 <5 <0.5 27 243 M058 8 <10 <0.1 560 <1 670 30 87 23 500 11 7.8 2.4 14 30 61 <5 <0.5 42 251 M059 10 <10 <0.1 440 <1 530 <10 <5 8 530 6 3.9 <0.5 5 <1 120 <5 <0.5 <1 132 M060 1 <10 <0.1 200 <1 420 40 19 25 170 10 6.8 1.2 8 10 34 <5 <0.5 16 134 M061 3 <10 <0.1 200 <1 470 40 18 21 270 9 6 1.2 7 9 30 <5 <0.5 15 147 M062 1 <10 <0.1 140 <1 460 60 6 23 120 4 3.5 <0.5 3 2 27 <5 <0.5 4 105 M063 5 <10 <0.1 550 <1 640 <10 <5 11 310 5 3.1 0.8 6 <1 76 <5 <0.5 5 140 M064 5 <10 <0.1 630 <1 480 10 510 111 610 32 16.5 10.4 56 230 86 <5 1.6 253 203 M065 8 <10 <0.1 720 <1 590 <10 32 25 630 8 4.8 1.7 12 18 89 <5 <0.5 25 158 M066 8 <10 <0.1 490 <1 590 <10 <5 <5 430 5 3.6 <0.5 3 <1 120 <5 <0.5 <1 101 M067 12 <10 <0.1 1250 <1 640 <10 69 6 650 23 12 6.2 36 62 111 <5 <0.5 91 140 M068 12 <10 <0.1 500 <1 560 <10 <5 10 600 4 3.7 <0.5 3 <1 97 <5 <0.5 <1 192 MOS9 10 <10 <0.1 430 <1 550 <10 <5 5 470 6 5 <0.5 5 <1 122 <5 <0.5 <1 100 M070 21 <10 0.3 510 <1 650 <10 6 8 650 16 16.3 0.9 9 5 66 <5 <0.5 6 96 M071 14 <10 0.5 1160 <1 580 <10 237 11 800 49 52.8 7 40 181 27 <5 0.7 167 74 M072 7 <10 0.2 850 <1 430 10 201 17 190 28 14 8.7 39 95 43 <5 1.1 159 40 M073 30 <10 0.3 730 <1 660 <10 6 7 550 6 4.7 0.8 5 7 36 <5 <0.5 12 89 M074 15 <10 0.3 1120 <1 650 <10 52 5 380 14 10.2 2.8 15 36 43 <5 <0.5 56 84 M075 18 <10 0.3 1180 <1 710 <10 18 <5 410 10 9.9 1.4 9 13 39 <5 <0.5 21 53 M076 15 <10 0.2 830 <1 630 <10 17 7 700 9 8.8 1.2 7 13 26 <5 <0.5 19 172 M077 3 <10 <0.1 350 <1 460 30 15 17 180 8 7.4 1 6 8 10 <5 <0.5 13 143 M078 3 <10 <0.1 380 <1 480 20 36 13 180 12 10.5 1.6 9 18 23 <5 <0.5 27 202 M079 <1 <10 <0.1 140 <1 320 50 7 50 110 5 7.3 <0.5 3 3 13 <5 <0.5 5 44 M080 3 <10 <0.1 780 <1 490 10 146 10 190 15 11.3 2.9 15 55 47 <5 0.8 68 124 M081 8 <10 0.2 960 <1 560 <10 32 <5 320 6 4.3 1.3 7 19 73 <5 <0.5 28 126 M082 4 <10 <0.1 400 <1 540 10 26 9 260 5 4.5 0.8 5 12 45 <5 <0.5 16 173 MOS3 9 <10 0.2 940 <1 580 <10 18 17 390 5 4.8 0.6 4 8 30 <5 <0.5 11 128 M084 1 <10 <0.1 180 <1 370 40 9 41 270 5 5 0.5 3 4 10 <5 <0.5 7 112 MOS5 5 <10 0.1 390 <1 450 20 57 119 880 12 13.9 1.2 7 27 16 <5 <0.5 28 295 M086 7 <10 0.1 780 <1 550 <10 36 9 350 8 6.2 1.3 7 23 40 <5 <0.5 27 175 M087 12 <10 0.2 480 <1 470 <10 79 8 760 20 14.5 4.2 22 51 55 <5 <0.5 76 235 MOS8 12 <10 0.3 290 <1 410 <10 <5 8 220 7 5.7 0.7 5 2 51 <5 <0.5 6 <5 M089 7 <10 0.2 950 <1 620 <10 8 <5 250 5 5.2 0.6 3 5 37 <5 <0.5 8 49 M090 8 <10 0.2 900 <1 620 <10 10 6 260 5 4.4 0.6 4 6 33 <5 <0.5 10 56 M091 5 <10 0.1 910 <1 560 <10 108 <5 400 16 7.4 5.3 25 57 94 <5 <0.5 96 106 M092 7 <10 <0.1 950 <1 500 <10 104 <5 480 10 4.5 3.9 18 44 75 <5 <0.5 74 87

Raw Analyses

ANALYTE Ag As Au Ba Bi Ca Cd Ce Co Cu Oy Er Eu Gd La .~. Mo Nb Nd Ni METHOD MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 DETECTION 1 10 0.1 10 1 10 10 5 5 10 1 0.5 0.5 1 1 1 5 0.5 1 5 UNITS PPB PPB PPB PPB PPB PPM PPB PPB PPB PPB PPB PPB PPB PPB PPB PPM PPB PPB PPB PPB M093 14 <10 0.2 930 <1 580 <10 12 13 750 10 10.8 0.9 6 9 71 <5 <0.5 15 89 M094 18 <10 0.3 700 <1 490 <10 11 9 790 12 12.7 1.1 8 10 49 <5 <0.5 16 151 M095 30 <10 0.4 340 <1 380 <10 <5 <5 460 10 9.8 0.8 6 3 73 <5 <0.5 18 9 M096 19 <10 0.2 1340 <1 580 <10 45 16 1080 19 14.3 2.9 17 30 79 <5 <0.5 48 185 Moo7 21 <10 0.3 590 <1 490 <10 13 <5 560 11 10.8 1.2 7 11 45 <5 <0.5 18 114 Moo8 25 <10 0.3 970 <1 700 <10 <5 10 280 4 3.2 0.5 3 2 69 <5 <0.5 5 <5 Moo9 21 <10 0.2 1120 <1 640 <10 10 6 1070 10 9 1.4 8 15 75 <5 <0.5 22 181 M100 16 <10 0.3 470 <1 470 <10 13 18 630 10 11.3 1.2 7 8 20 <5 <0.5 14 241 M101 22 <10 0.3 1580 <1 650 <10 24 <5 810 13 10.7 2.1 13 22 105 <5 <0.5 32 163 M102 18 <10 0.2 860 <1 560 <10 8 <5 370 6 3.1 1.4 7 6 75 <5 <0.5 15 43 M103 2 <10 <0.1 230 <1 340 30 9 14 230 4 3.7 <0.5 2 5 18 <5 <0.5 7 135 M104 15 <10 0.1 790 <1 550 <10 24 9 670 6 3.8 2 10 20 80 <5 <0.5 35 161 M105 14 <10 0.4 960 <1 650 <10 <5 12 580 6 5.6 0.7 5 2 66 <5 <0.5 6 20 M106 20 <10 0.2 810 <1 580 <10 7 16 640 6 5.1 0.7 5 5 75 <5 <0.5 11 72 M107 2 <10 <0.1 210 <1 400 30 <5 18 250 1 1.1 <0.5 <1 2 13 <5 <0.5 3 135 M108 13 <10 0.2 670 <1 500 <10 <5 <5 640 5 3.9 0.6 4 1 107 <5 <0.5 5 70 M109 10 <10 0.2 1110 <1 580 <10 44 130 870 8 6.9 1 6 14 61 <5 <0.5 21 263 M110 12 <10 <0.1 490 <1 510 40 29 30 2370 7 7.3 0.7 4 15 29 <5 0.6 15 226 M111 15 <10 <0.1 810 <1 610 <10 16 38 610 6 5.4 0.7 5 7 42 <5 <0.5 12 133 M112 12 <10 0.2 880 <1 570 <10 20 13 600 8 4 2.1 11 9 90 <5 <0.5 22 125 M113 1 <10 <0.1 190 <1 430 30 <5 17 50 <1 1.1 <0.5 <1 1 16 <5 <0.5 1 29 M114 2 <10 0.1 570 <1 440 <10 495 11 200 31 15.5 10.1 44 173 75 <5 1.3 229 104 M115 15 <10 0.2 650 <1 530 <10 6 <5 670 4 3.2 0.8 4 5 91 <5 <0.5 11 139 M116 14 <10 0.1 1120 <1 650 20 30 27 770 9 8.7 1 7 11 29 <5 <0.5 16 348 M117 2 <10 0.2 150 <1 320 40 9 20 160 5 4.9 0.5 3 5 14 <5 <0.5 7 107 M118 7 <10 0.2 660 <1 450 <10 23 20 520 8 9.3 0.7 5 10 42 <5 <0.5 13 136 M119 7 <10 0.2 840 <1 500 <10 85 6 380 9 4.6 3.4 15 39 87 <5 <0.5 64 92 M120 4 <10 0.2 860 <1 480 <10 130 <5 250 11 5.3 3.7 16 40 76 <5 <0.5 71 13 M121 9 <10 0.2 930 <1 620 <10 47 5 430 10 7 2 11 19 75 <5 <0.5 32 99 M122 9 <10 <0.1 1040 <1 580 <10 33 16 390 4 3.8 0.6 3 6 65 <5 <0.5 10 201 M123 10 <10 0.2 1070 <1 560 <10 34 <5 430 11 4.7 3.9 19 .35 90 <5 <0.5 62 50 M124 20 <10 0.4 900 <1 630 <10 <5 20 520 7 8.2 0.6 4 2 49 <5 <0.5 5 28 M125 6 <10 0.2 740 <1 400 <10 9 11 240 5 2.9 1.4 7 7 71 <5 <0.5 18 21 M126 10 <10 0.1 940 <1 480 <10 35 8 540 8 4.6 2.6 13 27 86 <5 <0.5 46 122 M127 9 <10 0.2 570 <1 570 <10 6 18 530 4 3.6 <0.5 3 2 38 <5 <0.5 5 199 M128 9 <10 0.2 700 <1 550 <10 14 <5 460 5 3.4 1.4 7 15 76 <5 <0.5 26 86 M129 9 <10 0.2 760 <1 470 <10 13 6 390 7 3.9 1.7 9 11 75 <5 <0.5 25 51 M130 11 <10 0.2 560 <1 610 <10 8 11 500 4 4.6 <0.5 3 5 21 <5 <0.5 7 162 M131 10 <10 0.3 850 <1 570 <10 6 9 450 3 3.3 <0.5 2 4 56 <5 <0.5 5 106 M132 6 <10 0.2 530 <1 500 <10 13 25 600 3 3.2 <0.5 2 9 57 <5 0.5 10 116 M133 5 <10 0.2 1000 <1 530 <10 283 16 400 29 16.6 8.3 39 104 87 <5 0.6 168 83

Raw Analyses

Analytical Duplicates

ANALYTE Ag As Au Sa Bi Ca Cd Ce Co Cu Dy Er Eu Gd La MSl Mo Nb Nd NI METHOD MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-MS MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-MS DETECTION 1 10 0.1 10 1 10 10 5 5 10 1 0.5 0.5 1 1 1 5 0.5 1 5 UNITS PPB PPB PPB PPB PPB PPM PPB PPB PPB PPB PPB PPB PPB PPB PPB PPM PPB PPB PPB PPB

Moo1 9 <10 0.2 880 <1 370 <10 <5 23 430 3 2 0.5 4 <1 120 <5 <0.5 <1 101 DUP-MOO1 8 <10 0.2 1010 <1 510 <10 37 31 690 10 5.3 2.5 15 5 147 <5 <0.5 20 129

M013 17 <10 0.4 600 <1 730 <10 <5 7 920 17 17.9 0.5 8 <1 83 <5 <0.5 <1 <5 DUP-M013 13 <10 0.3 730 <1 720 <10 <5 6 840 13 14.9 <0.5 5 <1 82 <5 <0.5 <1 <5

M025 <1 <10 <0.1 1140 <1 440 <10 33 10 470 5 2.4 1.1 7 <1 117 <5 <0.5 7 35 DUP-M025 2 <10 <0.1 1120 <1 480 <10 30 7 380 5 2.5 1.1 7 <1 130 <5 <0.5 6 26

M037 13 <10 <0.1 550 <1 610 <10 <5 9 460 4 3 <0.5 2 <1 141 <5 <0.5 <1 64 DUP-M037 8 <10 <0.1 710 <1 440 <10 <5 11 300 5 2.9 0.7 5 <1 120 <5 <0.5 <1 50

M049 23 <10 <0.1 660 <1 660 <10 <5 6 1060 7 4.3 0.6 6 <1 155 <5 <0.5 <1 136 DUP-M049 20 <10 <0.1 620 <1 530 <10 <5 9 910 6 4.4 <0.5 5 <1 110 <5 <0.5 <1 122

M061 3 <10 <0.1 200 <1 470 40 18 21 270 9 6 1.2 7 9 30 <5 <0.5 15 147 DUP-M061 4 <10 <0.1 270 <1 470 30 10 26 310 8 6.2 0.7 5 5 24 <5 <0.5 8 228

M071 14 <10 0.5 1160 <1 580 <10 237 11 600 49 52.8 7 40 181 27 <5 0.7 167 74 DUP-M071 12 <10 0.3 1180 <1 580 <10 273 8 590 48 51.7 7 38 195 38 <5 <0.5 179 58

M083 9 <10 0.2 940 <1 580 <10 18 17 390 5 4.8 0.6 4 8 30 <5 <0.5 11 128 DUP-M083 11 <10 0.2 950 <1 550 <10 10 21 420 5 5.6 <0.5 3 5 35 <5 <0.5 8 105

M095 30 <10 0.4 340 <1 380 <10 <5 <5 460 10 9.8 0.8 6 3 73 <5 <0.5 18 9 DUP-M095 30 <10 0.4 410 <1 410 <10 <5 6 710 9 11.6 0.8 6 6 62 <5 <0.5 30 38

M107 2 <10 <0.1 210 <1 400 30 <5 18 250 1 1.1 <0.5 <1 2 13 <5 <0.5 3 135 DUP-M107 2 <10 <0.1 150 <1 280 30 <5 26 360 1 1.4 <0.5 <1 <1 13 <5 <0.5 1 138

M119 7 <10 0.2 840 <1 500 <10 85 6 380 9 4.6 3.4 15 39 87 <5 <0.5 64 92 DUP-M119 11 <10 0.2 880 <1 570 <10 33 12 590 7 5.2 1.6 8 17 90 <5 <0.5 28 124

M131 10 <10 0.3 850 <1 570 <10 6 9 450 3 3.3 <0.5 2 4 56 <5 <0.5 5 106 DUP-M131 12 <10 0.2 1040 <1 600 <10 7 10 540 4 5 <0.5 3 4 51 <5 <0.5 6 156

Raw Analyses

ANALYTE Pb Pd Pr Rb Sb 8m 8n Sr Te Th TI n U W V Vb Zn Zr METHOD MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MM!-M5 MMI-M5 MMI-M5 MMI-M5 MMI-M5 MMI-MIS MMI-M5 MMI-M5 MMI-M5 MMf-M5 MMI-M5 MMI-M5 DETECTION 10 1 1 5 1 1 1 10 10 0.5 3 0.5 1 1 5 1 20 5 UNITS PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB Mool 50 <1 <1 20 <1 1 <1 1160 <10 2.1 <3 <0.5 2 <1 17 2 <20 <5 M002 60 <1 <1 24 <1 2 <1 1780 <10 4.7 <3 <0.5 6 <1 51 6 <20 <5 M003 60 <1 <1 22 <1 1 <1 1230 <10 2.6 <3 <0.5 1 <1 28 3 <20 <5 MOO4 20 <1 <1 83 <1 <1 <1 1100 <10 3.9 <3 <0.5 14 <1 22 4 <20 <5 M005 80 <1 <1 44 <1 2 <1 1580 <10 2.2 <3 <0.5 4 <1 37 5 <20 <5 MOOS 20 <1 <1 78 <1 <1 <1 1100 <10 6.7 <3 <0.5 10 <1 29 5 <20 <5 M007 50 <1 <1 51 <1 1 <1 1860 <10 4 <3 <0.5 7 <1 77 17 <20 <5 M008 40 <1 <1 42 <1 <1 <1 1390 <10 1.8 <3 <0.5 6 <1 31 7 <20 <5 M009 30 <1 <1 74 <1 <1 <1 1750 <10 3.2 <3 <0.5 7 <1 39 7 <20 <5 M010 40 <1 2 34 <1 2 <1 1460 <10 2.3 <3 <0.5 5 <1 101 21 <20 <5 MOll 50 <1 <1 47 <1 <1 <1 1740 <10 2.5 <3 <0.5 5 <1 51 14 20 <5 M012 20 <1 <1 55 <1 <1 <1 1340 <10 1.9 <3 <0.5 6 <1 24 6 <20 <5 M013 30 <1 <1 85 <1 <1 <1 1390 <10 2.2 <3 <0.5 5 <1 55 17 <20 <5 M014 40 <1 <1 35 <1 <1 <1 1200 <10 2.1 <3 <0.5 6 <1 57 10 <20 <5 M015 70 <1 <1 39 <1 <1 <1 1150 <10 1.8 <3 <0.5 1 <1 38 5 <20 <5 M016 30 <1 <1 47 <1 <1 <1 2060 <10 1 <3 <0.5 8 <1 29 8 <20 <5 M017 50 <1 <1 41 <1 2 <1 2030 <10 0.8 <3 <0.5 6 <1 25 2 <20 <5 M018 80 <1 <1 21 <1 2 <1 2020 <10 0.8 <3 <0.5 4 <1 26 2<20 <5 M019 50 <1 1 24 <1 5 <1 1440 <10 4.1 6 <0.5 4 <1 40 3 <20 9 M020 10 <1 16 70 <1 18 <1 990 <10 27.4 11 <0.5 20 <1 54 4<20 12 M021 10 <1 <1 62 <1 4 <1 1070 <10 10.2 7 <0.5 18 <1 26 2 <20 8 M022 40 <1 <1 32 <1 2 <1 1530 <10 1.6 6 <0.5 2 <1 24 2 <20 <5 M023 40 <1 3 38 <1 7 <1 1180 <10 4.2 15 <0.5 1 <1 37 3 <20 8 M024 20 <1 <1 35 <1 4 <1 1550 <10 3.5 7 <0.5 9 <1 30 3 <20 6 M025 90 <1 <1 21 <1 3 <1 1200 <10 4.3 <3 <0.5 4 <1 25 2 <20 7 M026 50 <1 1 24 <1 5 <1 1530 <10 2.4 <3 <0.5 5 <1 29 2 <20 6 M027 60 <1 1 25 <1 5 <1 1570 <10 3.1 <3 <0.5 3 <1 33 2 <20 7 M028 50 <1 <1 40 <1 3 <1 2030 <10 1.4 <3 <0.5 5 <1 30 3 <20 <5 M029 60 <1 <1 35 <1 4 <1 1610 <10 2 <3 <0.5 5 <1 36 3 <20 6 M030 60 <1 <1 41 <1 2 <1 1750 <10 2.6 7 <0.5 38 <1 49 6 <20 6 M031 40 <1 <1 38 <1 <1 <1 1710 <10 0.9 <3 <0.5 33 <1 28 5 <20 <5 M032 20 <1 <1 <5 <1 <1 <1 1140 <10 <0.5 <3 <0.5 4 <1 7 1 1600 <5 M033 50 <1 <1 46 <1 <1 <1 1180 <10 2.1 <3 <0.5 21 <1 21 2 <20 <5 M034 90 <1 <1 70 <1 <1 <1 1770 <10 1 <3 <0.5 7 <1 28 4 <20 <5 M035 110 <1 <1 44 <1 4 <1 1270 <10 3.7 <3 <0.5 3 <1 54 5 <20 <5 M036 90 <1 <1 49 <1 4 <1 1380 <10 8 <3 <0.5 28 <1 36 4 20 <5 M037 40 <1 <1 42 <1 <1 <1 1970 <10 1.1 <3 <0.5 19 <1 13 3 <20 <5 M038 50 <1 2 42 <1 5 <1 1230 <10 4 5 <0.5 19 <1 33 2 <20 7 M039 30 <1 <1 59 <1 <1 <1 1750 <10 2.1 <3 <0.5 14 <1 23 4 <20 <5 M040 30 <1 <1 38 <1 3 17 1110 <10 6.8 8 <0.5 13 <1 27 3 70 9 M041 20 <1 6 32 <1 11 <1 780 <10 8.2 16 <0.5 14 <1 40 3 <20 10 M042 40 <1 <1 47 <1 3 <1 1830 <10 2.8 <3 <0.5 11 <1 30 2 <20 5 M043 20 <1 <1 41 <1 <1 <1 1240 <10 2.1 <3 <0.5 5 <1 19 3 <20 <5 M044 30 <1 1 8 <1 5 <1 1190 <10 3 <3 <0.5 3 <1 27 2 <20 7 M045 400 <1 3 17 <1 3 <1 860 <10 1.5 15 <0.5 17 <1 36 6 280 <5 M046 230 <1 34 167 <1 20 <1 1190 <10 21.8 12 <0.5 36 <1 83 10 410 11

Raw Analyses

ANALYTE Pb Pd Pr Rb Sb Sm Sn Sr Te Th TI TI U W V Vb Zn Zr METHOD MMloMS MMI...,S MMI-MS MMI-MS MMI-MS MMI-MS MMI-MS MMI-MS MMI...,S MMloMS MMI...,S MMI...,5 MMI-MS MMI-M5 MMI-M5 MMI-MS MMI-MS MMI-MS DETECTION 10 1 1 S 1 1 1 10 10 0.5 3 0.5 1 1 S 1 20 S UNITS PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB M047 30 <1 14 64 <1 14 <1 1080 <10 34.7 20 <0.5 15 1 50 4 90 11 M048 10 <1 <1 38 <1 <1 <1 950 <10 4.7 <3 <0.5 7 <1 15 3 <20 7 M049 30 <1 <1 42 <1 <1 <1 1530 <10 2.2 <3 <0.5 9 <1 29 4 <20 <5 M050 30 <1 <1 69 <1 <1 <1 1200 <10 5.3 <3 <0.5 10 <1 20 4 <20 <5 M051 20 <1 <1 91 <1 <1 <1 1220 <10 3.8 <3 <0.5 11 <1 16 3 <20 <5 M052 30 <1 <1 44 <1 <1 <1 1200 <10 4 <3 <0.5 11 <1 18 4 <20 <5 M053 40 <1 <1 95 <1 1 <1 1230 <10 6.7 <3 <0.5 15 <1 30 5 50 <5 M054 50 <1 <1 26 <1 <1 <1 1760 <10 1.2 <3 <0.5 11 <1 16 5 <20 <5 M055 80 <1 <1 47 <1 4 <1 1040 <10 12.2 4 <0.5 4 <1 39 5 50 11 M056 290 <1 15 113 <1 13 <1 1130 <10 8.4 4 <0.5 41 <1 110 10 260 <5 M057 280 <1 7 81 <1 7 <1 1240 <10 6.2 9 <0.5 46 <1 116 13 670 <5 M058 70 <1 10 56 <1 9 <1 1540 <10 7.6 <3 <0.5 135 <1 57 7 130 <5 M059 30 <1 <1 48 <1 <1 <1 1290 <10 4.3 5 <0.5 18 <1 21 3 <20 7 M060 160 <1 4 22 <1 4 <1 900 <10 2.5 17 <0.5 115 <1 74 6 470 <5 MOS1 130 <1 3 25 <1 4 <1 910 <10 1.9 12 <0.5 89 <1 68 6 260 <5 MOS2 120 <1 <1 <5 <1 1 <1 970 <10 0.5 <3 <0.5 28 <1 28 3 660 <5 MOS3 30 <1 <1 46 <1 3 <1 1490 <10 5 <3 <0.5 6 <1 21 3 60 <5 M064 140 <1 69 76 <1 44 <1 840 <10 60.1 88 <0.5 52 <1 155 14 410 29 MOS5 40 <1 6 42 <1 6 <1 1090 <10 9 5 <0.5 13 <1 36 4 90 <5 MOSS 30 <1 <1 31 <1 <1 <1 1430 <10 3 6 <0.5 5 <1 17 4 30 <5 MOS7 50 <1 20 43 <1 22 3 1430 <10 30.2 4 <0.5 10 <1 94 9 <20 11 M068 30 <1 <1 37 <1 <1 <1 1590 <10 2 <3 <0.5 7 <1 16 4 <20 <5 MOS9 30 <1 <1 54 <1 <1 <1 1230 <10 5.6 <3 <0.5 12 <1 24 5 <20 6 M070 60 <1 2 62 <1 2 <1 1420 <10 7.1 <3 <0.5 5 <1 58 17 <20 <5 M071 100 <1 42 98 <1 30 <1 1470 <10 8 <3 <0.5 4 <1 220 49 30 8 M072 150 <1 34 146 <1 36 <1 720 <10 34.3 59 <0.5 10 <1 119 11 300 49 M073 20 <1 3 97 <1 3 <1 1490 <10 2.6 <3 <0.5 3 <1 22 4 <20 <5 M074 20 <1 12 92 <1 12 <1 1050 <10 13.7 <3 <0.5 6 <1 57 9 40 8 M075 30 <1 4 63 <1 5 <1 1390 <10 5.8 <3 <0.5 3 <1 39 9 <20 <5 M076 40 <1 4 71 <1 4 <1 1200 <10 3.4 <3 <0.5 4 <1 38 8 70 <5 M077 90 <1 3 37 <1 4 <1 980 <10 0.9 <3 <0.5 20 <1 49 7 90 <5 M078 140 <1 6 37 <1 7 <1 1090 <10 3.3 6 <0.5 58 <1 69 9 130 <5 M079 150 <1 1 13 <1 2 <1 690 <10 1.5 16 <0.5 12 <1 36 8 670 <5 MOSO 60 <1 16 65 <1 13 <1 970 <10 13.1 43 <0.5 10 <1 69 10 340 13 M081 20 <1 6 26 <1 6 <1 1170 <10 5.7 <3 <0.5 3 <1 25 4 40 <5 M082 20 <1 4 46 <1 3 <1 1020 <10 3.1 <3 <0.5 9 <1 23 4 120 <5 M083 40 <1 2 46 <1 2 <1 1390 <10 2.7 <3 <0.5 11 <1 22 5 90 <5 MOM 50 <1 1 9 <1 2 <1 540 <10 0.6 7 <0.5 10 <1 30 5 500 <5 M085 110 <1 7 74 <1 5 <1 790 <10 3.5 <3 <0.5 14 <1 63 13 270 <5 M086 20 <1 6 64 <1 6 <1 950 <10 6.2 <3 <0.5 5 <1 32 6 220 <5 M087 40 <1 16 102 <1 17 <1 790 <10 11.3 <3 <0.5 15 <1 86 12 <20 7 M088 <10 <1 1 41 <1 2 <1 1070 <10 1.9 <3 <0.5 4 <1 22 5 <20 <5 M089 40 <1 2 67 <1 2 <1 1180 <10 3.2 <3 <0.5 3 <1 17 5 90 <5 M090 40 <1 2 65 <1 3 <1 1110 <10 3.9 <3 <0.5 4 <1 16 4 150 <5 M091 30 <1 19 39 <1 21 <1 1100 <10 33.9 <3 <0.5 6 <1 69 5 <20 29 M092 10 <1 15 49 <1 16 <1 1040 <10 24.9 4 <0.5 20 <1 47 3 40 19

Raw Analyses

ANALYTE Pb Pd Pr Rb Sb Sm Sn Sr Te Th TI TI U W Y Yb Zn Zr METHOD MMI-MS MMI-M5 MMI-MS MMI-MS MMI-MS MMI-MS MMI-MS MMI-MS MMI-MS MMI-MS MMI-MS MMI-MS MMI-MS MMI-MS MMI-MS MMI-MS MMI-M5 MMI-MS DETECTION 10 1 1 S 1 1 1 10 10 O.S 3 O.S 1 1 S 1 20 S UNITS PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB M093 50 <1 3 40 <1 4 <1 1260 <10 3.7 <3 <0.5 4 <1 32 11 <20 <5 M094 60 <1 3 32 <1 4 <1 1040 <10 3.2 <3 <0.5 2 <1 40 12 <20 <5 M095 30 <1 1 54 <1 3 <1 1050 <10 1.3 <3 <0.5 2 <1 34 9 <20 <5 M096 80 <1 10 78 <1 11 <1 1240 <10 10.6 <3 <0.5 12 <1 68 12 <20 <5 M097 30 <1 4 45 <1 4 <1 1140 <10 3.7 <3 <0.5 3 <1 37 10 <20 <5 M098 20 <1 <1 66 <1 2 <1 1380 <10 0.9 <3 <0.5 3 <1 14 3 <20 <5 M099 40 <1 5 52 <1 6 <1 1310 <10 3.5 <3 <0.5 3 <1 38 8 <20 <5 M100 30 <1 3 68 <1 4 <1 1010 <10 2.4 <3 <0.5 2 <1 43 11 <20 <5 M101 30 <1 7 16 <1 8 <1 1350 <10 5.8 <3 <0.5 6 <1 48 9 <20 <5 M102 <10 <1 3 16 <1 5 <1 890 <10 5.4 <3 <0.5 4 <1 25 3 <20 6 M103 100 <1 2 19 <1 2 <1 760 <10 <0.5 <3 <0.5 3 <1 24 3 170 <5 M104 20 <1 7 75 <1 8 <1 1120 <10 7.7 <3 <0.5 15 <1 32 3 <20 6 M105 30 <1 <1 23 <1 2 <1 1210 <10 1.5 <3 <0.5 2 <1 23 5 <20 <5 M106 20 <1 2 55 <1 3 <1 1280 <10 3 <3 <0.5 3 <1 21 5 <20 <5 M107 30 <1 <1 5 <1 <1 <1 820 <10 <0.5 <3 <0.5 8 <1 7 <1 420 <5 M108 20 <1 <1 24 <1 2 <1 1670 <10 1.2 <3 <0.5 3 <1 19 4 <20 <5 M109 30 <1 4 42 <1 4 <1 1680 <10 6.9 <3 <0.5 10 <1 31 7 120 <5 M110 220 <1 4 40 <1 3 <1 1090 <10 1.6 <3 <0.5 295 <1 35 8 150 <5 M111 30 <1 2 43 <1 3 <1 1770 <10 2 <3 <0.5 19 <1 23 5 50 <5 M112 30 <1 4 32 <1 7 <1 1360 <10 4.9 <3 <0.5 6 <1 38 3 <20 7 M113 <10 <1 <1 <5 <1 <1 <1 1000 <10 <0.5 <3 <0.5 3 <1 5 1 660 <5 M114 160 <1 54 80 <1 44 <1 730 <10 61.1 114 <0.5 16 <1 143 12 220 71 M115 <10 <1 2 61 <1 3 <1 1230 <10 3.6 <3 <0.5 7 <1 19 3 <20 <5 M116 30 <1 3 53 <1 4 <1 1290 <10 3.3 <3 <0.5 3 <1 32 9 150 <5 M117 50 <1 1 10 <1 2 <1 630 <10 1.5 <3 <0.5 15 <1 33 4 490 <5 M118 30 <1 3 64 <1 3 <1 1130 <10 4.9 <3 <0.5 3 <1 33 9 180 <5 M119 <10 <1 13 41 <1 14 <1 1170 <10 19.7 41 <0.5 16 <1 43 4 60 18 M120 10 <1 15 68 <1 15 <1 800 <10 49.6 25 <0.5 12 <1 44 4 <20 39 M121 20 <1 6 43 <1 8 <1 1300 <10 9 <3 <0.5 5 <1 39 6 40 <5 M122 20 <1 2 50 <1 3 <1 1330 <10 4.3 <3 <0.5 10 <1 15 4 60 <5 M123 20 <1 12 32 <1 15 <1 1100 <10 12.1 <3 <0.5 4 <1 49 3 30 14 M124 60 <1 <1 41 <1 2 <1 1330 <10 1.4 <3 <0.5 2 <1 26 8 <20 <5 M125 20 <1 3 13 <1 5 <1 760 <10 4.2 <3 <0.5 1 <1 27 2 <20 8 M126 20 <1 9 55 <1 11 <1 1260 <10 11.3 11 <0.5 24 <1 39 4 <20 16 M127 30 <1 <1 21 <1 1 <1 1040 <10 2 <3 <0.5 3 <1 15 4 40 <5 M128 <10 <1 5 46 <1 5 <1 950 <10 9.1 <3 <0.5 7 <1 24 3 60 8 M129 20 <1 5 32 <1 7 <1 870 <10 9.1 5 <0.5 14 <1 33 3 <20 12 M130 20 <1 1 69 <1 2 <1 1090 <10 2.7 <3 <0.5 5 <1 15 5 110 <5 M131 40 <1 1 43 <1 1 <1 1530 <10 1.2 <3 <0.5 5 <1 14 3 60 <5 M132 80 <1 2 29 <1 2 <1 860 <10 3 <3 <0.5 12 <1 14 3 250 <5 M133 60 <1 37 80 <1 35 <1 1020 <10 79.5 42 <0.5 15 <1 127 14 290 70

Raw Analyses

Analytical Duplicates

ANALYTE Pb Pd Pr Rb Sb Sm Sn Sr Te Th TI TI U W V Vb Zn Zr METHOD MMI-MS MMI-MS MMI-M5 MMI-MS MMI-M5 MMI-M5 MMI-M5 MMI-MS MMI-M5 MMI-MS MMI-M5 MMI-M5 MMI-MS MMI-MS MMI-MS MMI-M5 MMI-M5 MMI-MS DETECTION 10 1 1 5 1 1 1 10 10 O.S 3 0.5 1 1 5 1 20 5 UNITS PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB PPB

M001 50 <1 <1 20 <1 1 <1 1160 <10 2.1 <3 <0.5 2 <1 17 2 <20 <5 DUP-M001 70 <1 3 29 <1 8 <1 1530 <10 4.9 <3 <0.5 5 <1 51 4 <20 7

M013 30 <1 <1 85 <1 <1 <1 1390 <10 2.2 <3 <0.5 5 <1 55 17 <20 <5 DUP-M013 30 <1 <1 77 <1 <1 <1 1440 <10 1.7 <3 <0.5 4 <1 39 14 20 <5

M025 90 <1 <1 21 <1 3 <1 1200 <10 4.3 <3 <0.5 4 <1 25 2 <20 7 DUP-M025 70 <1 <1 19 <1 3 <1 1280 <10 3.6 4 <0.5 4 <1 25 2 <20 6

M037 40 <1 <1 42 <1 <1 <1 1970 <10 1.1 <3 <0.5 19 <1 13 3 <20 <5 DUP-M037 30 <1 <1 30 <1 2 <1 1510 <10 1.9 <3 <0.5 9 <1 20 3 <20 6

M049 30 <1 <1 42 <1 <1 <1 1530 <10 2.2 <3 <0.5 9 <1 29 4 <20 <5 DUP-M049 30 <1 <1 39 <1 <1 <1 1310 <10 1.1 <3 <0.5 8 <1 23 4 <20 <5

M061 130 <1 3 25 <1 4 <1 910 <10 1.9 12 <0.5 89 <1 68 6 260 <5 DUP-M061 110 <1 2 36 <1 2 <1 990 <10 1.3 9 <0.5 117 <1 60 6 270 <5

M071 100 <1 42 98 <1 30 <1 1470 <10 8 <3 <0.5 4 <1 220 49 30 8 DUP-M071 110 <1 46 88 <1 31 <1 1410 <10 7.1 <3 <0.5 4 <1 202 48 <20 7

M083 40 <1 2 46 <1 2 <1 1390 <10 2.7 <3 <0.5 11 <1 22 5 90 <5 DUP-M083 50 <1 2 40 <1 2 <1 1600 <10 1.6 <3 <0.5 11 <1 18 6 70 <5

M095 30 <1 1 54 <1 3 <1 1050 <10 1.3 <3 <0.5 2 <1 34 9 <20 <5 DUP-M095 30 <1 2 60 <1 3 <1 1090 <10 1.8 <3 <0.5 3 <1 31 12 <20 <5

M107 30 <1 <1 5 <1 <1 <1 820 <10 <0.5 <3 <0.5 8 <1 7 <1 420 <5 DUP-M107 50 <1 <1 <5 <1 <1 <1 620 <10 <0.5 <3 <0.5 6 <1 7 1 480 <5

M119 <10 <1 13 41 <1 14 <1 1170 <10 19.7 41 <0.5 16 <1 43 4 60 18 DUP-M119 20 <1 6 47 <1 6 <1 1310 <10 8.8 <3 <0.5 16 <1 29 5 80 6

M131 40 <1 1 43 <1 1 <1 1530 <10 1.2 <3 <0.5 5 <1 14 3 60 <5 DUP-M131 40 <1 1 62 <1 1 <1 1660 <10 1.3 <3 <0.5 6 <1 17 6 100 <5

APPENDIX III

Edited Analytical Data and Calculated Response Ratios with Grid and UTM Co-ordinates

~\D83Zon.'7 ANALYTE I Line 8tatIOn EaSllng I NOrthing lAg AgRR AI AlRR Au AuRR 'Ba ~R 8 1 181RR ca ICaRA ,Cd ICdRR ICe caRR ICo CoRR .Cu CuRR :Oy IDyRR Er ErRR Eu 'EuRR IGd LaRR M001 1800E 725N <495147 5411 260 9 3 5 1 0.2 4 880 3 0.5 1 370 1 5 1 2.5 1 23 8 <430 2 3 1 2 1 0.5 2 4 1 0.5 1 MOO2 1800E 675N <495122 5411208 21 7 5 1 0.3 6 990 3 0.5 1 810 2 5 1 2.5 1 17 6 660 3 12 3 8 3 1 3 10 4 0 .5 1 MOO3 1800E 625N 495103 5411163 8 3 5 1 0.2 <4 740 2 0.5 1 510 1 5 1 2.5 1 7 3 <410 2 5 1 3.1 1 0.6 2 6 2 0.5 1 MOO4 1800E 575N 49S086 5411128 10 3 5 1 0.2 <4 460 1 0.5 1 540 1 5 1 2.5 1 2.5 1 520 2 6 2 <4.6 2 0.25 1 4 1 0.5 1 M005 1800E 5SON 495073 5411107 14 5 5 1 0.05 1 890 3 0.5 1 670 2 5 1 2.5 1 13 5 1010 5 9 2 5.6 2 0.8 3 8 3 0 .5 1 MOO6 1800E 525N 495064 5411084 15 5 5 1 0.1 2 620 2 0.5 1 710 2 5 1 2.5 1 2.5 1 590 3 8 2 5.7 2 0.25 1 5 2 0.5 1 M007 1800E SOON 495048 5411062 33 11 5 1 0,4 8 890 3 0.5 1 920 2 5 1 2.5 1 5 2 520 2 21 5 18.6 7 0.8 3 12 4 2 4 MOOS 1800E 475N 495040 5411031 28 9 5 1 0.2 4 530 2 0.5 1 760 2 5 1 2.5 1 8 3 780 4 10 3 7.7 3 0.25 1 5 2 0.5 1 MOO9 1800E <4SON <49S028 5411011 24 8 5 1 0.2 4 800 2 0 .5 1 840 2 5 1 2 .5 1 2.5 1 320 1 11 3 8.9 4 0.25 1 6 2 0 .5 1 M010 1800E 425N 495025 5410992 22 7 5 1 0.3 6 710 2 0.5 1 7SO 2 5 1 6 2 2.5 1 480 2 26 7 24 10 1.3 4 16 6 5 10 M011 1800E 375N <49SOO2 5410947 17 6 5 1 0.2 4 830 3 0.5 1 890 2 5 1 2.5 1 2.5 1 480 2 15 4 15 6 0.25 1 7 3 0.5 1 M012 1800E 325N 494976 5410906 29 10 5 1 0.2 <4 600 2 0.5 1 770 2 5 1 2.5 1 5 2 300 1 7 2 7 3 0.25 1 3 1 0.5 1 M013 1850E 375N 495025 541090<4 17 6 5 1 0.4 8 600 2 0.5 1 730 2 5 1 2.5 1 7 3 920 <4 17 4 17.9 7 0.5 2 8 3 0.5 1 M014 18SOE 425N <49S052 5410946 44 15 5 1 0.3 6 550 2 0.5 1 670 2 5 1 2.5 1 7 3 780 <4 15 4 11 .7 5 0.5 2 9 3 0.5 1 M015 1850E <4SON 495065 5410994 19 6 5 1 0.2 4 580 2 0.5 1 680 2 5 1 2.5 1 8 3 5SO 3 9 2 6.2 2 0.6 2 7 3 0.5 1 M016 1850E <475N 495075 5411013 24 8 5 1 0.3 6 820 2 0.5 1 980 2 5 1 2.5 1 6 2 610 3 8 2 8.2 3 0.25 1 3 1 0.5 1 M017 1850E SOON <495086 5411031 6 2 5 1 0.2 <4 1080 3 0.5 1 6SO 2 5 1 2.5 1 2.5 1 510 2 5 1 2.6 1 0.7 2 6 2 0.5 1 M018 18SOE 525N 495117 5411055 9 3 5 1 0.05 1 1170 4 0.5 1 640 2 5 1 2.5 1 1<4 5 800 <4 5 1 3 1 0.8 3 6 2 0.5 1 M019 1850E 5SON <495122 5411071 4 1 5 1 0.1 2 1110 3 0.5 1 530 1 5 1 2.5 1 7 3 600 3 7 2 3.4 1 1.5 5 10 <4 0.5 1 M020 18SOE 575N <495137 5411086 7 2 5 1 0.05 1 910 3 0.5 1 610 2 5 1 72 29 2.5 1 520 2 12 3 4.8 2 4.5 15 25 9 34 68 M021 1850E 625N <495163 5411126 7 2 5 1 0.05 1 580 2 0.5 1 620 2 5 1 2.5 1 2.5 1 500 2 6 2 2.9 1 1.4 5 9 3 0 .5 1 M022 18SOE 675N <495195 5411177 8 3 5 1 0.05 1 960 3 0.5 1 610 2 5 1 2.5 1 2 .5 1 640 3 5 1 2.2 1 1 3 7 3 0.5 1 M023 1850E 725N <495225 5411 210 2 2 5 1 0.05 1 1100 3 0 .5 1 <470 1 5 1 8 3 2.5 1 J.4() 2 7 2 3.3 1 2 7 12 <4 <4 8 M024 1900E 725N 495245 5411 201 6 2 5 1 0.05 1 1070 3 0.5 1 590 1 5 1 2.5 1 2.5 1 380 2 6 2 3 1 1.3 4 9 3 0.5 1 M025 1900E 675N 495221 54111 59 0.5 1 5 1 0.05 1 1140 3 0.5 1 440 1 5 1 33 13 10 <4 470 2 5 1 2.4 1 1.1 <4 7 3 0.5 1 M026 1900E 625N <495187 541111 2 2 2 5 1 0 .1 2 1240 4 0.5 1 450 1 5 1 6 2 5 2 330 2 5 1 2.6 1 1.3 4 8 3 0 .5 1 M027 1900E 575N 495166 5411077 3 1 5 1 0.1 2 1210 <4 0.5 1 SOO 1 5 1 7 3 9 3 360 2 6 2 2.9 1 1.4 5 9 3 0.5 1 M028 1900E 550N 495159 5411042 8 3 5 1 0.05 1 1130 3 0.5 1 630 2 5 1 2.5 1 2.5 1 440 2 6 2 3.2 1 1.1 <4 8 3 0.5 1 M029 1900E 525N 4951<43 5411032 5 2 5 1 0.2 <4 1220 4 0.5 1 560 1 5 1 2.5 1 2.5 1 440 2 6 2 3.1 1 1.4 5 9 3 0.5 1 M030 1900E SOON 495143 5411014 23 8 5 1 0.05 1 9SO 3 0.5 1 640 2 5 1 2.5 1 25 9 2220 10 13 3 7.2 3 1.3 4 13 5 0.5 1 M031 1900E SOON 4951<40 541101<4 20 7 5 1 0.05 1 640 2 0.5 1 600 1 5 1 2 .5 1 24 9 1510 7 8 2 5.4 2 0.25 1 6 2 0.5 1 M032 1900E 475N <495125 5410986 1 1 5 1 0.05 1 2SO 1 0.5 1 560 1 70 14 2.5 1 11 4 100 1 1 1 0.9 1 0.25 1 0.5 1 0.5 1 M033 1900E 4SON 495107 5410964 8 3 5 1 0.05 1 770 2 0.5 1 600 1 5 1 2.5 1 9 3 580 3 <4 1 2.2 1 0.25 1 4 1 0.5 1 M034 1900E 425N <495106 5410939 18 6 5 1 0.2 4 960 3 0.5 1 660 2 5 1 2.5 1 9 3 7<40 3 7 2 5 2 0.25 1 5 2 0.5 1 M035 1900E 375N 49S078 5410894 11 4 5 1 1.3 26 1310 4 0.5 1 640 2 5 1 2.5 1 11 4 910 4 12 3 6.4 3 1.8 6 14 5 0.5 1 M036 19SOE <425N 495135 5410931 10 3 5 1 0.05 1 880 3 0.5 1 620 2 5 1 2.5 1 27 10 1230 6 8 2 4.5 2 1.3 4 9 3 0 .5 1 M037 1950E 450N 495134 5410944 13 <4 5 1 0.05 1 5SO 2 0.5 1 610 2 5 1 2.5 1 9 3 460 2 4 1 3 1 0.25 1 2 1 0.5 1 M038 1950E <475N 495160 5410969 6 2 5 1 0.2 4 980 3 0.5 1 520 1 5 1 8 3 7 3 <470 2 6 2 3 1 1.6 5 9 3 1 2 M039 19SOE SOON 495178 5410984 16 5 5 1 0.05 1 620 2 0.5 1 710 2 5 1 2.5 1 6 2 860 4 6 2 4.7 2 0.25 1 4 1 0.5 1 M040 19SOE 525N 495187 5411010 6 2 5 1 0.05 1 760 2 0.5 1 550 1 5 1 2.5 1 5 2 390 2 7 2 3.7 1 1.2 4 8 3 0.5 1 M041 19SOE 5SON 495199 5411033 8 3 5 1 0.3 6 600 2 0.5 1 460 1 5 1 18 7 2.5 1 460 2 8 2 3.4 1 2.9 10 16 6 10 20 M042 19SOE 575N 495211 5411048 13 4 5 1 0.05 1 1180 4 0.5 1 640 2 5 1 2.5 1 6 2 620 3 6 2 3 1 1.3 4 8 3 0.5 1 M043 19SOE 625N 495233 5411094 16 5 5 1 0.05 1 570 2 0.5 1 650 2 5 1 2.5 1 7 3 630 3 5 1 3.2 1 0.25 1 3 1 0.5 1 M0<44 1950E 675N 495259 5411141 <4 1 5 1 0 .05 1 10SO 3 0.5 1 560 1 5 1 2 .5 1 2.5 1 390 2 5 1 2.2 1 1.4 5 8 3 0.5 1 'MotS 1950E 721;'" 4115282 6411182 0.5 1 6 1 0.05 1 240 1 0.5 1 .-.0 1 30 6 17 1 107 38 90 1 6 2 6.6 2 o.a 3 6 'Z 1 14 M046 2000E 725N 495320 5411160 23 8 5 1 0.05 1 990 3 0.5 1 660 2 30 6 361 144 122 44 750 3 17 4 10.<4 4 4.8 16 26 9 119 238 M047 2000E 675N 495301 5411109 7 2 5 1 0.05 1 880 3 0.5 1 600 1 5 1 100 40 30 11 360 2 11 3 5.6 2 3.8 13 19 7 34 68 M048 2ODOE 625N 495275 5411068 13 4 5 1 0.1 2 3SO 1 0.5 1 460 1 5 1 2.5 1 2.5 1 490 2 5 1 3.3 1 0.25 1 3 1 0.5 1

NADl3 Zone 17 ANALYTE Line station Eating Northing lAg AgRR As AsRR Au AuRR Ba BaRR BI BIRR C. C.R~ Cd CdM Ce CeRR ICo CoR~ Cu CuM lOy I[)yR~ Er ErRR Eu EuRR Gd GdR~ La LaRR

M049 2000E 575N 495259 5411019 23 8 5 1 0.05 1 660 2 0.5 1 660 2 5 1 2.5 1 6 2 1060 5 7 2 4.3 2 0.6 2 6 2 0.5 1

M050 2000E 550N 495239 5410986 17 6 5 1 0.2 4 400 1 0.5 1 640 2 5 1 2.5 1 5 2 590 3 6 2 4.6 2 0.25 1 4 1 0.5 1

M051 2000E 525N 495235 5410979 15 5 5 1 0.1 2 380 1 0.5 1 660 2 5 1 2 .5 1 9 3 760 4 4 1 3.6 1 0.25 1 2 1 0.5 1

M052 2000E SOON 495219 5410955 12 4 5 1 0.05 1 490 1 0.5 1 570 1 5 1 2 .5 1 8 3 570 3 5 1 4 2 0.25 1 4 1 0 .5 1

M053 2000E 475N 495213 5410936 11 4 5 1 0.05 1 440 1 0 .5 1 670 2 10 2 2.5 1 9 3 770 4 7 2 5.3 2 0.5 2 6 2 0.5 1

M054 2000E 450N 495195 5410910 16 5 5 1 0.05 1 570 2 0.5 1 600 1 5 1 2.5 1 11 4 600 3 5 1 4.4 2 0.25 1 3 1 0 .5 1

M055 2000E 425N 495190 541 0885 9 3 5 1 0.05 1 640 2 0.5 1 550 1 5 1 2.5 1 7 3 760 4 8 2 5.1 2 1.4 5 9 3 0.5 1

M056 2050E 450N 495232 5410904 9 3 5 1 0.05 1 640 2 0.5 1 570 1 30 6 127 51 25 9 400 2 20 5 11 .9 5 3.5 12 20 7 52 104

IMOS7 2050E 500N 495257 6410940 2 2 5 1 0.05 1 510 2 0.6 1 570 1 30 6 44 18 89 32 240 1 19 6 13.7 6 2.1 7 13 5 19 38 M058 2050E 550N 495301 5410965 8 3 5 1 0.05 1 560 2 0.5 1 670 2 30 6 87 35 23 8 SOO 2 11 3 7.8 3 2.4 8 14 5 30 60

M059 2050E 600N 495333 5410994 10 3 5 1 0.05 1 440 1 0.5 1 530 1 5 1 2.5 1 8 3 530 2 6 2 3.9 2 0.25 1 5 2 0.5 1

M060 2100E 600N 495349 5410995 1 1 5 1 0.05 1 200 1 0.5 1 420 1 40 8 19 8 25 9 170 1 10 3 6.8 3 1.2 4 8 3 10 20

M061 2100E 600N 495352 541 0996 3 1 5 1 0.05 1 200 1 0.5 1 470 1 40 8 18 7 21 8 270 1 9 2 6 2 1.2 4 7 3 9 18

M062 2100E 550N 495333 541 0957 1 1 5 1 0.05 1 140 1 0.5 1 460 1 60 12 6 2 23 8 120 1 4 1 3.5 1 0.25 1 3 1 2 4

M063 2100E SOON 495306 5410905 5 2 5 1 0.05 1 550 2 0.5 1 640 2 5 1 2.5 1 11 4 310 1 5 1 3.1 1 0.8 3 6 2 0.5 1

M064 2100E 450N 495277 5410864 5 2 5 1 0.05 1 630 2 0.5 1 480 1 10 2 510 204 111 40 610 3 32 8 16.5 7 10.4 35 56 20 230 460

MOOS 2100E 400N 495251 5410820 8 3 5 1 0.05 1 720 2 0.5 1 590 1 5 1 32 13 25 9 630 3 8 2 4.8 2 1.7 6 12 4 18 36

M066 2150E SOON 495349 5410881 8 3 5 1 0.05 1 490 1 0.5 1 590 1 5 1 2.5 1 2.5 1 430 2 5 1 3.6 1 0.25 1 3 1 0.5 1

M067 2350E SOON 495514 5410783 12 4 5 1 0.05 1 1250 4 0.5 1 640 2 5 1 69 28 6 2 650 3 23 6 12 5 6.2 21 36 13 62 124

M068 2350E 525N 495530 5410803 12 4 5 1 0.05 1 SOO 2 0.5 1 560 1 5 1 2.5 1 10 4 600 3 4 1 3.7 1 0.25 1 3 1 0.5 1

M069 2350E 550N 495541 5410822 10 3 5 1 0.05 1 430 1 0.5 1 550 1 5 1 2.5 1 5 2 470 2 6 2 5 2 0.25 1 5 2 0.5 1

M070 2350E 575N 495548 5410850 21 7 5 1 0.3 6 510 2 0.5 1 650 2 5 1 6 2 8 3 650 3 16 4 16.3 7 0.9 3 9 3 5 10

M071 2350E SOON 495562 5410872 14 5 5 1 0.5 10 1160 4 0.5 1 580 1 5 1 237 95 11 4 SOO 3 49 12 52.8 21 7 23 40 14 181 362

MOl2 2350E 625N 495578 5410911 7 2 5 1 0.2 4 850 3 0.5 1 430 1 10 2 201 80 17 6 190 1 28 7 14 6 8.7 29 39 14 95 190

M073 2350E 650N 495588 5410930 30 11 5 1 0.3 6 730 2 0.5 1 660 2 5 1 6 2 7 3 550 3 6 2 4.7 2 0.8 3 5 2 7 14

M074 2250E 650N 495514 5410965 15 5 5 1 0.3 6 1120 3 0.5 1 650 2 5 1 52 21 5 2 380 2 14 4 10.2 4 2.8 9 15 5 36 72

M075 2250E 625N 495490 5410935 18 6 5 1 0.3 6 1180 4 0.5 1 710 2 5 1 18 7 2 .5 1 410 2 10 3 9.9 4 1.4 5 9 3 13 26

M076 2250E SOON 495488 5410922 15 5 5 1 0.2 4 830 3 0.5 1 630 2 5 1 17 7 7 3 700 3 9 2 8.8 4 1.2 4 7 3 13 26

MJl7 2250E i57!1H 495473 5410909 3 1 6 1 0.05 1 350 1 0.5 1 460 1 30 6 16 6 17 6 180 1 8 2 7.4 3 1 3 6 2 8 18

M078 2250E 5ij()H 495458 6410680 3 1 5 1 0.05 1 380 1 0.6 1 480 1 20 4 36 14 13 5 180 1 12 3 10.5 4 1.6 5 9 3 18 36 M()79 2250E 626N 495446 641(1852 0.6 1 5 1 0.05 1 140 1 0.5 1 320 1 60 10 7 3 .>;) 18 110 1 5 1 7.3 3 0.25 1 3 1 3 6 M080 2250E SOON 495436 5410832 3 1 5 1 0.05 1 780 2 0 .5 1 490 1 10 2 146 58 10 4 190 1 15 4 11 .3 5 2.9 10 15 5 55 110

MOB 1 2250E 475N 495424 5410810 8 3 5 1 0.2 4 960 3 0.5 1 560 1 5 1 32 13 2.5 1 320 1 6 2 4.3 2 1.3 4 7 3 19 38 M082 2250E 450N 495410 5410786 4 1 5 1 0.05 1 400 1 0.5 1 540 1 10 2 26 10 9 3 260 1 5 1 4.5 2 0.8 3 5 2 12 24

M083 2250E 425N 495390 5410764 9 3 5 1 0.2 4 940 3 0.5 1 580 1 5 1 18 7 17 6 390 2 5 1 4.8 2 0.6 2 4 1 8 16

M084 2260~ 400N :.'15;>77 6410750 1 1 6 1 0.06 1 180 1 O./'i 1 370 1 40 8 9 4 41 16 270 1 6 1 6 2 0.6 2 3 1 .. 8 MOBS 2250E 375N 495364 5410720 5 2 5 1 0.1 2 390 1 0.5 1 450 1 20 4 57 23 119 43 880 4 12 3 13.9 6 1.2 4 7 3 27 54 M086 2250E 350N 495346 5410693 7 2 5 1 0.1 2 780 2 0.5 1 550 1 5 1 36 14 9 3 350 2 8 2 6.2 2 1.3 4 7 3 23 46

M087 2250E 300N 495323 5410657 12 4 5 1 0.2 4 480 1 0.5 1 470 1 5 1 79 32 8 3 760 4 20 5 14.5 6 4.2 14 22 8 51 102

M088 2250E 250N 495308 5410621 12 4 5 1 0.3 6 290 1 0.5 1 410 1 5 1 2.5 1 8 3 220 1 7 2 5.7 2 0.7 2 5 2 2 4

MOB9 2250E 200N 495276 5410562 7 2 5 1 0.2 4 950 3 0.5 1 620 2 5 1 8 3 2.5 1 250 1 5 1 5.2 2 0.6 2 3 1 5 10

M090 2250E 200N 495280 5410560 8 3 5 1 0.2 4 900 3 0.5 1 620 2 5 1 10 4 6 2 260 1 5 1 4.4 2 0.6 2 4 1 6 12

M091 2800E 300N 495821 5410410 5 2 5 1 0.1 2 910 3 0.5 1 560 1 5 1 108 43 2.5 1 400 2 16 4 7.4 3 5.3 18 25 9 57 114

M092 2800E 350N 495846 5410451 7 2 5 1 0.05 1 950 3 0.5 1 SOO 1 5 1 104 42 2.5 1 480 2 10 3 4.5 2 3.9 13 18 6 44 88

M093 2800E 400N 495873 5410493 14 5 5 1 0.2 4 930 3 0.5 1 580 1 5 1 12 5 13 5 750 3 10 3 10.8 4 0.9 3 6 2 9 18

M094 2800E 425N 495890 5410506 18 6 5 1 0.3 6 700 2 0.5 1 490 1 5 1 11 4 9 3 790 4 12 3 12.7 5 1.1 4 6 3 10 20

MOSS 2800E 450N 495903 5410523 30 11 5 1 0.4 8 340 1 0.5 1 380 1 5 1 2.5 1 2.5 1 460 2 10 3 9.8 4 0.8 3 6 2 3 6

M096 2800E 475N 495919 5410547 19 6 5 1 0.2 4 1340 4 0.5 1 580 1 5 1 45 18 16 6 1080 5 19 5 14.3 6 2.9 10 17 6 30 60

NA083 Zone 17 ANALYTE Une Station Entillg Northtl15l !~ A~RR As AsRR Au AuRR sa BaRR BI BIRR Ca CaRR Cd CdRR Ce C4tRR Co CaRR Cu CuM OY DvRR Er ErftR Eu EuRR Gel GdRR La LaRR M097 2800E 500N 495923 5410578 21 7 5 1 0.3 6 590 2 0.5 1 490 1 5 1 13 5 2.5 1 560 3 11 3 10.8 4 1.2 4 7 3 11 22 M098 2800E 525N 495943 5410586 25 8 5 1 0.3 6 970 3 0.5 1 700 2 5 1 2.5 1 10 4 280 1 4 1 3.2 1 0.5 2 3 1 2 4 MOS9 2800E 550N 495939 5410622 21 7 5 1 0.2 4 1120 3 0.5 1 640 2 5 1 10 4 6 2 1070 5 10 3 9 4 1.4 5 8 3 15 30 M100 2800E 575N 495936 5410649 16 5 5 1 0.3 6 470 1 0.5 1 470 1 5 1 13 5 18 6 630 3 10 3 11 .3 5 1.2 4 7 3 8 16 M101 2800E 600N 495966 5410665 22 7 5 1 0.3 6 1560 5 0.5 1 650 2 5 1 24 10 2.5 1 810 4 13 3 10.7 4 2.1 7 13 5 22 44 M102 2800E 850N 495981 5410709 18 6 5 1 0.2 4 860 3 0.5 1 560 1 5 1 8 3 2.5 1 370 2 6 2 3.1 1 1.4 5 7 3 6 12 MI03 2&JOE 650 ... W't~1 541::818 2 2 5 1 0.05 1 230 1 0." 1 3<10 i 30 6 9 4 14 5 230 1 .- 3.7 1 0.25 1 2 1 IS 10 M104 2600E 600N 495803 5410758 15 5 5 1 0.1 2 790 2 0.5 1 550 1 5 1 24 10 9 3 670 3 6 2 3.8 2 2 7 10 4 20 40 M105 2600E 575N 495n9 5410739 14 5 5 1 0.4 8 960 3 0.5 1 650 2 5 1 2.5 1 12 4 580 3 6 2 5.6 2 0.7 2 5 2 2 4 M106 2600E 550N 495n 2 541071 5 20 7 5 1 0.2 4 810 2 0.5 1 580 1 5 1 7 3 16 6 640 3 6 2 5.1 2 0.7 2 5 2 5 10 Mt07 2600E 525N 495758 J41u,,92 2 2 5 1 0.05 1 210 1 0.5 1 400 1 30 6 2.5 1 18 6 250 1 1 1 1.1 1 0.25 1 0.5 1 2 4 M108 2600E SOON 495741 5410666 13 4 5 1 0.2 4 670 2 0.5 1 SOO 1 5 1 2.5 1 2.5 1 640 3 5 1 3.9 2 0.6 2 4 1 1 2 Ml09 2600E 475N 495126 5410650 10 3 5 1 0.2 4 1110 3 0.5 1 560 1 5 1 44 18 130 46 870 4 8 2 6.9 3 1 3 6 2 14 28 M110 2600E 450N 49571 3 5410623 12 4 5 1 0.05 1 490 1 0.5 1 510 1 40 8 29 12 30 11 2370 11 7 2 7.3 3 0.7 2 4 1 15 30 M111 2600E 425N 495698 5410601 15 5 5 1 0.05 1 810 2 0.5 1 610 2 5 1 16 6 38 14 610 3 6 2 5.4 2 0.7 2 5 2 7 14 M112 2600E 400N 495681 5410579 12 4 5 1 0.2 4 880 3 0.5 1 570 1 5 1 20 8 13 5 600 3 8 2 4 2 2.1 7 11 4 9 18 ~··1"l3 2600E 350 ... 19~55 _,,;,-W 1 I 5 1 0.5 1 90 1 0.5 1 430 1 30 6 2.5 1 ,~ 6 00 1 0.5 1 1.1 1 0.25 1 0.5 1 1 2 M114 2600E 300N 495622 5410499 2 2 5 1 0.1 2 570 2 0.5 1 440 1 5 1 495 198 11 4 200 1 31 8 15.5 6 10.1 34 44 16 173 346 M11 5 2600E 250N 495584 5410458 15 5 5 1 0.2 4 850 2 0.5 1 530 1 5 1 6 2 2.5 1 670 3 4 1 3.2 1 0.8 3 4 1 5 10 M11 6 2600E 200N 495562 5410423 14 5 5 1 0.1 2 1120 3 0.5 1 650 2 20 4 30 12 27 10 no 4 9 2 8.7 3 1 3 7 3 11 22 Mi17 2600E ~l)JN 49S5;!8 54',0383 2 2 5 1 0.2 4 150 1 0.5 1 320 1 ." 8 9 4 20 7 160 1 5 1 4.9 2 0.5 2 3 1 5 10 M118 2600E 100N 495499 5410347 7 2 5 1 0.2 4 880 2 0.5 1 450 1 5 1 23 9 20 7 520 2 8 2 9.3 4 0.7 2 5 2 10 20 M119 2600E 50N 495471 5410297 7 2 5 1 0.2 4 840 3 0.5 1 SOO 1 5 1 85 34 6 2 380 2 9 2 4.6 2 3.4 11 15 5 39 78 M120 2800E 200N 495767 5410311 4 1 5 1 0.2 4 860 3 0.5 1 480 1 5 1 130 52 2.5 1 250 1 11 3 5.3 2 3.7 12 16 6 40 80 M1 21 2800E 250N 495795 541 0352 9 3 5 1 0.2 4 930 3 0.5 1 620 2 5 1 47 19 5 2 430 2 10 3 7 3 2 7 11 4 19 38 M1 22 2250E 150N 495278 5410551 9 3 5 1 0.05 1 1040 3 0.5 1 580 1 5 1 33 13 16 6 390 2 4 1 3.8 2 0.6 2 3 1 6 12 M1 23 2350E 475N 495513 5410753 10 3 5 1 0.2 4 1070 3 0.5 1 560 1 5 1 34 14 2.5 1 430 2 11 3 4.7 2 3.9 13 19 7 35 70 M1 24 2350E 450N 495506 5410729 20 7 5 1 0.4 8 900 3 0.5 1 630 2 5 1 2.5 1 20 7 520 2 7 2 8.2 3 0.6 2 4 1 2 4 M125 2350E 425N 495484 5410709 6 2 5 1 0.2 4 740 2 0.5 1 400 1 5 1 9 4 11 4 240 1 5 1 2.9 1 1.4 5 7 3 7 14 M126 2350E 400N 495467 5410686 10 3 5 1 0.1 2 940 3 0.5 1 480 1 5 1 35 14 8 3 540 3 8 2 4.6 2 2.6 9 13 5 27 54 M127 2350E 375N 495452 5410659 9 3 5 1 0.2 4 570 2 0.5 1 570 1 5 1 6 2 18 6 530 2 4 1 3.6 1 0.25 1 3 1 2 4 M1 28 2350E 350N 495448 5410643 9 3 5 1 0.2 4 700 2 0.5 1 550 1 5 1 14 6 2.5 1 460 2 5 1 3.4 1 1.4 5 7 3 15 30 M129 2350E 300N 495417 5410596 9 3 5 1 0.2 4 760 2 0.5 1 470 1 5 1 13 5 6 2 390 2 7 2 3.9 2 1.7 6 9 3 11 22 M130 2350E 250N 495388 5410561 11 4 5 1 0.2 4 560 2 0.5 1 610 2 5 1 8 3 11 4 500 2 4 1 4.6 2 0.25 1 3 1 5 10 M131 2350E 200N 495380 5410522 10 3 5 1 0.3 6 850 3 0.5 1 570 1 5 1 6 2 9 3 450 2 3 1 3.3 1 0.25 1 2 1 4 8 M132 2350E 1 SON 495324 5410484 6 2 5 1 0.2 4 530 2 0.5 1 SOO 1 5 1 13 5 25 9 600 3 3 1 3.2 1 0.25 1 2 1 9 18

Peat Samples (n=10)

IANAtYTE lOne IStation tEasting INOI1iilng lAg IAgRR IAi tAiRR 'XU IAuRR 'ea I BaRR lSI IBIRR ICa IcaRRlcd IcaRRle; IceRRlco ICORRIcu ICuRRlDi IDiRRIEi IEIRR lEu IEURRIGa 'GdRRjG tGRR\

M045 1950E 125N 495282 5411182 0.5 1 5 1 0.05 1 240 1 0.5 1 440 1 30 6 17 7 107 38 90 1 6 2 5.5 2 0.8 3 5 2 7 14 M057 2050E SOON 495257 5410940 2 2 5 1 0.05 1 510 2 0.5 1 570 1 30 6 44 18 89 32 240 1 19 5 13.7 5 2.1 7 13 5 19 38 MOn 2250E 575N 495473 5410909 3 1 5 1 0.05 1 350 1 0.5 1 460 1 30 6 15 6 17 6 180 1 8 2 7.4 3 1 3 6 2 8 16 M078 2250E 550N 495456 5410880 3 1 5 1 0.05 1 380 1 0.5 1 480 1 20 4 36 14 13 5 180 1 12 3 10.5 4 1.6 5 9 3 18 36 M079 2250E 525N 495446 5410852 0.5 1 5 1 0.05 1 140 1 0.5 1 320 1 50 10 7 3 50 18 110 1 5 1 7.3 3 0.25 1 3 1 3 6 M084 2250E 400N 4953n 5410750 1 1 5 1 0.05 1 180 1 0.5 1 370 1 40 8 9 4 41 15 270 1 5 1 5 2 0.5 2 3 1 4 8 M103 2600E 650N 495821 5410818 2 2 5 1 0.05 1 230 1 0.5 1 340 1 30 6 9 4 14 5 230 1 4 1 3.7 1 0.25 1 2 1 5 10 Ml07 2600E 525N 495758 541 0692 2 2 5 1 0.05 1 210 1 0.5 1 400 1 30 6 2.5 1 18 6 250 1 1 1 1.1 1 0.25 1 0.5 1 2 4 M113 2600E 350N 495655 5410543 1 1 5 1 0.05 1 190 1 0.5 1 430 1 30 6 2.5 1 17 6 50 1 0.5 1 1.1 1 0.25 1 0.5 1 1 2 M117 2600E 150N 495528 5410383 2 2 5 1 0.2 4 150 1 0.5 1 320 1 40 8 9 4 20 7 160 1 5 1 4.9 2 0.5 2 3 1 5 10

NAD83Zone 17 IANALYTE Line station It:astlng Mg Mg~ IMO lJe1c)RF iNb IN~ INd lNaKfC NI INlftK If'D f'DKfC IPd paRR pr f'rftK lUI SbRR ISm SrnRJ ISn SnR~ Sr ISrRR !Ta TeftK Th ThftK M001 1800E 725N 495147 5411260 120 5 2.5 1 0.25 1 0.5 1 101 5 50 3 0.5 1 0.5 1 20 1 0.5 1 1 2 0.5 1 1160 1 5 1 2.1 2 M002 1800E 675N 495122 5411208 152 6 2.5 1 0.25 1 0.5 1 56 3 60 4 0.5 1 0.5 1 24 1 0.5 1 2 3 0.5 1 1780 2 5 1 4 ,7 4 M003 1800E 625N 495103 5411163 128 5 2.5 1 0.25 1 0.5 1 26 1 60 4 a,s 1 0.5 1 22 1 0.5 1 1 2 0,5 1 1230 1 5 1 2,6 2 MOO4 1800E 575N 495086 5411128 135 5 2.5 1 0.25 1 0.5 1 60 3 20 1 0.5 1 0.5 1 83 4 0.5 1 0.5 1 0.5 1 1100 1 5 1 3 .9 3 MOOS 1800E 550N 495073 5411107 165 6 2.5 1 0.25 1 0.5 1 37 2 80 5 0,5 1 0.5 1 44 2 0.5 1 2 3 0.5 1 1580 2 5 1 2,2 2 MOO6 1800E 525N 495064 5411084 121 5 2.5 1 0.25 1 a,s 1 60 3 20 1 0,5 1 0.5 1 78 4 a,s 1 0.5 1 0.5 1 1100 1 5 1 6 .7 6 M007 1800E SOON 495048 5411062 106 4 2.5 1 0.25 1 2 4 2.5 1 50 3 0.5 1 a,s 1 51 2 0.5 1 1 2 0.5 1 1860 2 5 1 4 3 MOO8 1800E 475N 495040 5411031 130 5 2.5 1 0.25 1 0.5 1 36 2 40 3 0.5 1 0.5 1 42 2 0.5 1 0.5 1 0.5 1 1390 2 5 1 1.8 2 Moog 1800E 450N 495028 5411011 103 4 2.5 1 0.25 1 0,5 1 2.5 1 30 2 0.5 1 0,5 1 74 3 a,s 1 0,5 1 0.5 1 1750 2 5 1 3,2 3 M010 1800E 425N 495025 5410992 67 3 2.5 1 0.25 1 6 12 2,5 1 40 3 0.5 1 2 4 34 2 0.5 1 2 3 0.5 1 1460 2 5 1 2.3 2 M011 1800E 375N 49SOO2 5410947 124 5 2.5 1 0.25 1 0.5 1 2.5 1 50 3 0,5 1 0.5 1 47 2 0.5 1 0.5 1 0.5 1 1740 2 5 1 2,5 2 M012 1800E 325N 494976 5410906 109 4 2.5 1 0.25 1 a,s 1 8 1 20 1 0.5 1 0.5 1 55 3 0.5 1 0.5 1 0.5 1 1340 1 5 1 1.9 2 M013 1850E 375N 495025 5410904 83 3 2.5 1 0.25 1 0.5 1 2.5 1 30 2 0.5 1 0.5 1 85 4 0.5 1 0.5 1 0.5 1 1390 2 5 1 2.2 2 M014 1850E 425N 495052 5410946 121 5 2.5 1 0.25 1 0.5 1 43 2 40 3 0.5 1 0.5 1 35 2 0.5 1 0.5 1 0.5 1 1200 1 5 1 2.1 2 M015 1850E 450N 495065 5410994 130 5 2.5 1 0.25 1 0.5 1 23 1 70 5 0.5 1 0.5 1 39 2 0.5 1 0.5 1 0.5 1 1150 1 5 1 1.8 2 M016 1850E 475N 495075 5411013 172 7 2.5 1 0.25 1 0.5 1 22 1 30 2 0,5 1 0.5 1 47 2 0.5 1 0.5 1 0.5 1 2060 2 5 1 1 1 M017 1850E SOON 495086 5411031 171 7 2,5 1 0.25 1 0.5 1 12 2 50 3 0.5 1 0.5 1 41 2 0.5 1 2 3 0.5 1 2030 2 5 1 0,8 1 M018 1850E 525N 495117 5411055 175 7 2,5 1 0.25 1 0.5 1 30 1 80 5 0.5 1 0.5 1 21 1 0,5 1 2 3 0.5 1 2020 2 5 1 0,8 1 M019 1850E SOON 495122 5411071 119 5 2,5 1 0,25 1 9 18 24 1 50 3 0,5 1 1 2 24 1 0.5 1 5 8 0.5 1 1440 2 5 1 4.1 4 M020 1850E 575N 495137 5411086 105 4 2.5 1 0.25 1 73 146 132 7 10 1 0,5 1 16 32 70 3 0.5 1 18 30 0,5 1 990 1 5 1 27.4 24 M021 1850E 625N 495163 5411126 121 5 2,5 1 0.25 1 3 6 129 6 10 1 0.5 1 a,s 1 62 3 0,5 1 4 7 0.5 1 1070 1 5 1 10.2 9 M022 1850E 675N 495195 5411177 152 6 2.5 1 0.25 1 1 2 71 3 40 3 0.5 1 0.5 1 32 1 0.5 1 2 3 0.5 1 1530 2 5 1 1.6 1 M023 1850E 725N 495225 5411210 103 4 2.5 1 0,25 1 18 36 27 1 40 3 a,s 1 3 6 38 2 0.5 1 7 12 0,5 1 1180 1 5 1 4 .2 4 M024 1900E 725N 495245 5411201 134 5 2.5 1 0.25 1 3 6 123 6 20 1 0,5 1 0.5 1 35 2 0,5 1 4 7 0.5 1 1550 2 5 1 3.5 3 M025 1900E 675N 495221 54111 59 117 4 2,5 1 0,25 1 7 14 35 2 90 6 0,5 1 0.5 1 21 1 0,5 1 3 5 0.5 1 1200 1 5 1 4,3 4 M026 1900E 625N 495187 5411112 122 5 2,5 1 0.25 1 9 18 21 1 50 3 0,5 1 1 2 24 1 0.5 1 5 8 0.5 1 1530 2 5 1 2,4 2 M027 1900E 575N 495166 5411077 129 5 2.5 1 0.25 1 10 20 29 1 60 4 0.5 1 1 2 25 1 0,5 1 5 8 0.5 1 1570 2 5 1 3.1 3 M028 1900E 550N 495159 5411042 164 6 2,5 1 0.25 1 1 2 37 2 50 3 0.5 1 0.5 1 40 2 0.5 1 3 5 0.5 1 2030 2 5 1 1.4 1 M029 1900E 525N 495143 5411032 150 6 2.5 1 0,25 1 7 14 14 2 60 4 0.5 1 0.5 1 35 2 0,5 1 4 7 0.5 1 1610 2 5 1 2 2 M030 1900E SOON 495143 5411014 161 6 2,5 1 0,25 1 0.5 1 525 26 60 4 0.5 1 a,s 1 41 2 a,s 1 2 3 0.5 1 1750 2 5 1 2.6 2 M031 1900E SOON 495140 5411014 157 6 2.5 1 0.25 1 0.5 1 307 15 40 3 0.5 1 0.5 1 38 2 0.5 1 0,5 1 0.5 1 1710 2 5 1 0 ,9 1 M032 1900E 475N 4951 25 5410986 26 1 10 1 0.25 1 0.5 1 68 3 20 1 0.5 1 0.5 1 2.5 1 0,5 1 0.5 1 0.5 1 1140 1 5 1 0.25 1 M033 1900E 450N 495107 5410964 133 5 2,5 1 0.25 1 a,s 1 92 5 50 3 0,5 1 0.5 1 46 2 0.5 1 0.5 1 0.5 1 1180 1 5 1 2,1 2 M034 1900E 425N 495106 5410939 145 6 2,5 1 0.25 1 0.5 1 137 7 90 6 0.5 1 0.5 1 70 3 0,5 1 0.5 1 0.5 1 1770 2 5 1 1 1 M035 1900E 375N 495078 5410894 151 6 2.5 1 0,25 1 3 6 64 3 110 7 0.5 1 0.5 1 44 2 a,s 1 4 7 0.5 1 1270 1 5 1 3,7 3 M036 1950E 425N 495135 5410931 106 4 2.5 1 0,25 1 5 10 213 11 90 6 0.5 1 0.5 1 49 2 a,s 1 4 7 0.5 1 1380 2 5 1 8 7 M037 1950E 450N 495134 5410944 141 5 2.5 1 0.25 1 0.5 1 64 3 40 3 0.5 1 0,5 1 42 2 0.5 1 0.5 1 0.5 1 1970 2 5 1 1.1 1 M038 1950E 475N 495160 5410969 115 4 2.5 1 0.25 1 12 24 45 2 50 3 0.5 1 2 4 42 2 0.5 1 5 8 a,s 1 1230 1 5 1 4 3 M039 1950E SOON 495178 5410984 107 4 2.5 1 0.25 1 0.5 1 138 7 30 2 0.5 1 0.5 1 59 3 0.5 1 0.5 1 0.5 1 1750 2 5 1 2.1 2 M040 1950E 525N 495187 5411010 116 4 2.5 1 0.25 1 3 6 74 4 30 2 0.5 1 0.5 1 38 2 0,5 1 3 5 17 34 1110 1 5 1 6 .8 6 M041 1950E SOON 495199 5411033 90 3 2.5 1 0.25 1 36 72 85 4 20 1 0,5 1 6 12 32 1 0.5 1 11 18 0.5 1 780 1 5 1 8.2 7 M042 1950E 575N 495211 5411048 157 6 2.5 1 0.25 1 4 8 94 5 40 3 0.5 1 0.5 1 47 2 0,5 1 3 5 0.5 1 1830 2 5 1 2.8 2 M043 1950E 625N 495233 5411094 125 5 2.5 1 0.25 1 0.5 1 89 4 20 1 0.5 1 a,s 1 41 2 a,s 1 0.5 1 0.5 1 1240 1 5 1 2.1 2 M044 1950E 675N 495259 5411141 122 5 2,5 1 0.25 1 9 18 50 2 30 2 0.5 1 1 2 8 1 0,5 1 5 8 0.5 1 1190 1 5 1 3 3 M0.45 1950E 725N 4\15282 541118~ 33 1 2.5 1 0.25 1 11 22 63 3 400 27 0.5 1 3 6 17 1 0.5 1 3 5 0,5 1 .J6O 1 6 1 1.6 1 M046 2000E 725N 495320 5411160 66 3 2,5 1 1,2 5 121 242 378 19 230 16 0.5 1 34 68 167 8 0.5 1 20 33 0.5 1 1190 1 5 1 21 .8 19 M047 2000E 675N 495301 5411109 104 4 2.5 1 0.25 1 62 124 171 8 30 2 0.5 1 14 28 64 3 0,5 1 14 23 0.5 1 1080 1 5 1 34.7 30 M048 2000E 625N 495275 5411068 120 5 2.5 1 0,25 1 0.5 1 96 5 10 1 0 .5 1 0.5 1 38 2 0.5 1 0.5 1 0,5 1 950 1 5 1 4.7 4

NAD83 Zone 17 ANALYTE Line Station Eastlng Northing Mg MgRR Mo MoRF Nb NbRR Nd NeIRA NI NIRR Pb PbRR Pd PdRR IPr PrRR Rb RbRR Sb SbRR Sm SmRF Sn SnRA Sr SrRR Te TeRR Th ThRR M049 2000E 575N 495259 5411019 155 6 2.5 1 0.25 1 0.5 1 136 7 30 2 0.5 1 0.5 1 42 2 0.5 1 0.5 1 0.5 1 1530 2 5 1 2.2 2 MOSO 2000E 550N 495239 5410986 119 5 2.5 1 0.25 1 0.5 1 96 5 30 2 0.5 1 0.5 1 69 3 0.5 1 0.5 1 0.5 1 1200 1 5 1 5.3 5 M051 2000E 525N 495235 5410979 110 4 2.5 1 0.25 1 0.5 1 132 7 20 1 0.5 1 0.5 1 91 4 0.5 1 0.5 1 0.5 1 1220 1 5 1 3.8 3 M052 2000E SOON 495219 5410955 105 4 2.5 1 0.25 1 0.5 1 123 6 30 2 0.5 1 0.5 1 44 2 0.5 1 0.5 1 0.5 1 1200 1 5 1 4 3 M053 2000E 475N 495213 5410936 89 3 2.5 1 0.25 1 0.5 1 223 12 40 3 0.5 1 0.5 1 95 4 0.5 1 1 2 0.5 1 1230 1 5 1 6 .7 6 M054 2000E 450N 495195 5410910 143 5 2.5 1 0.25 1 0.5 1 131 6 50 3 0.5 1 0.5 1 26 1 0.5 1 0.5 1 0.5 1 1760 2 5 1 1.2 1 M055 2000E 425N 495190 5410885 113 4 2.5 1 0.25 1 5 10 76 4 80 5 0.5 1 0.5 1 47 2 0.5 1 4 7 0.5 1 1040 1 5 1 12.2 11 M056 20SOE 450N 495232 5410904 56 2 2.5 1 0.25 1 60 120 347 17 290 20 0.5 1 15 30 113 5 0.5 1 13 22 0.5 1 1130 1 5 1 8.4 7 M057 2050E 500N 495257 6410940 48 2 2.5 1 0.25 1 27 54 243 12 280 19 0.6 1 7 14 81 4 0.5 1 7 12 0.5 1 1240 1 5 1 6.2 5 M058 20SOE 550N 495301 5410965 61 2 2.5 1 0.25 1 42 84 251 12 70 5 0.5 1 10 20 56 3 0.5 1 9 15 0.5 1 1540 2 5 1 7.6 7 M059 2050E 600N 495333 5410994 120 5 2.5 1 0.25 1 0.5 1 132 7 30 2 0.5 1 0.5 1 48 2 0.5 1 0.5 1 0.5 1 1290 1 5 1 4.3 4 M060 2100E 600N 495349 541 0995 34 1 2.5 1 0.25 1 16 32 134 7 160 11 0.5 1 4 8 22 1 0.5 1 4 7 0.5 1 900 1 5 1 2.5 2 M061 2100E 600N 495352 5410996 30 1 2.5 1 0.25 1 15 30 147 7 130 9 0.5 1 3 6 25 1 0.5 1 4 7 0.5 1 910 1 5 1 1.9 2 M062 2100E 550N 495333 541 0957 27 1 2.5 1 0.25 1 4 8 105 5 120 8 0.5 1 0.5 1 2.5 1 0.5 1 1 2 0.5 1 970 1 5 1 0 .5 1 M063 2100E SOON 495306 5410905 76 3 2.5 1 0.25 1 5 10 140 7 30 2 0.5 1 0.5 1 46 2 0.5 1 3 5 0.5 1 1490 2 5 1 5 4 M064 2100E 4SON 495277 541 0864 86 3 2.5 1 1.6 6 253 506 203 11 140 10 0.5 1 69 138 76 3 0.5 1 44 73 0.5 1 840 1 5 1 60.1 52 MOOS 21 ODE 400N 495251 5410820 89 3 2.5 1 0.25 1 25 50 158 8 40 3 0.5 1 6 12 42 2 0.5 1 6 10 0.5 1 1090 1 5 1 9 8 M066 21SOE 500N 495349 5410881 120 5 2.5 1 0.25 1 0.5 1 101 5 30 2 0.5 1 0.5 1 31 1 0.5 1 0.5 1 0.5 1 1430 2 5 1 3 3 M007 23SOE 500N 495514 5410783 111 4 2.5 1 0.25 1 91 182 140 7 50 3 0.5 1 20 40 43 2 0.5 1 22 37 3 6 1430 2 5 1 30.2 26 M068 2350E 525N 495530 5410803 97 4 2.5 1 0.25 1 0.5 1 192 9 30 2 0.5 1 0.5 1 37 2 0.5 1 0.5 1 0.5 1 1590 2 5 1 2 2 M069 2350E 5SON 495541 5410822 122 5 2.5 1 0.25 1 0.5 1 100 5 30 2 0.5 1 0.5 1 54 2 0.5 1 0.5 1 0.5 1 1230 1 5 1 5.6 5 M070 23SOE 575N 495548 5410850 66 3 2.5 1 0.25 1 6 12 96 5 60 4 0.5 1 2 4 62 3 0.5 1 2 3 0.5 1 1420 2 5 1 7.1 6 M071 2350E 600N 495562 5410872 27 1 2.5 1 0.7 3 167 334 74 4 100 7 0.5 1 42 84 98 4 0.5 1 30 SO 0.5 1 1470 2 5 1 8 7 M072 2350E 625N 495578 5410911 43 2 2.5 1 1.1 4 159 318 40 2 150 10 0.5 1 34 68 146 7 0.5 1 36 60 0.5 1 720 1 5 1 34.3 30 M073 23SOE 6SON 495588 5410930 38 1 2.5 1 0.25 1 12 24 89 4 20 1 0.5 1 3 6 97 4 0.5 1 3 5 0.5 1 1490 2 5 1 2.6 2 M074 22SOE 650N 495514 5410965 43 2 2.5 1 0.25 1 56 11 2 84 4 20 1 0.5 1 12 24 92 4 0.5 1 12 20 0.5 1 1050 1 5 1 13.7 12 M075 2250E 625N 495490 5410935 39 1 2.5 1 0.25 1 21 42 53 3 30 2 0.5 1 4 8 63 3 0.5 1 5 8 0.5 1 1390 2 5 1 5.8 5 M076 22SOE 600N 495488 5410922 26 1 2.5 1 0.25 1 19 38 172 8 40 3 0.5 1 4 8 71 3 0.5 1 4 7 0.5 1 1200 1 5 1 3.4 3 IWln 2250E 576H 495473 5410909 ~O 1 2.5 1 0.25 1 13 26 143 7 90 6 0.5 1 3 6 37 2 0.5 1 .- 7 0.5 1 980 1 5 1 0.9 1 I M078 2250E SOON 495458 64'0880 23 1 2.5 1 0.25 1 27 54 202 10 1~ 10 0.5 1 6 12 37 2 0.5 1 7 12 0.5 1 1090 1 6 1 3.3 3 Ma79 2250E 525N 496446 5410852 13 1 2.5 1 0.25 1 5 10 .... 2 150 10 0.5 1 1 2 13 1 0.5 1 2 3 0.5 1 690 1 5 1 1.5 1 M080 22SOE SOON 495436 5410832 47 2 2.5 1 0.8 3 68 136 124 6 60 4 0.5 1 16 32 65 3 0.5 1 13 22 0.5 1 970 1 5 1 13.1 11 M081 2250E 475N 495424 5410810 73 3 2.5 1 0.25 1 28 56 126 6 20 1 0.5 1 6 12 26 1 0.5 1 6 10 0.5 1 1170 1 5 1 5.7 5 M082 2250E 450N 495410 5410786 45 2 2.5 1 0.25 1 16 32 173 9 20 1 0.5 1 4 8 46 2 0.5 1 3 5 0.5 1 1020 1 5 1 3.1 3 M083 22SOE 425N 495390 5410764 30 1 2.5 1 0.25 1 11 22 128 6 40 3 0.5 1 2 4 46 2 0.5 1 2 3 0.5 1 1390 2 5 1 2.7 2 IM084 l260E 400N 495377 54' 0750 10 1 2.5 1 0.25 1 7 14 112 6 50 3 0.5 1 1 2 9 1 0.5 1 2 3 0.5 1 540 1 5 1 0.6 1 M085 22SOE 375N 495364 5410720 16 1 2.5 1 0.25 1 28 56 295 15 110 7 0.5 1 7 14 74 3 0.5 1 5 8 0.5 1 790 1 5 1 3.5 3 M086 22SOE 350N 495346 5410693 40 2 2.5 1 0.25 1 27 54 175 9 20 1 0.5 1 6 12 84 3 0.5 1 6 10 0.5 1 950 1 5 1 6 .2 5 M087 22SOE 300N 495323 5410657 55 2 2.5 1 0.25 1 76 152 235 12 40 3 0.5 1 16 32 102 5 0.5 1 17 28 0.5 1 790 1 5 1 11 .3 10 M088 2250E 250N 495308 5410621 51 2 2.5 1 0.25 1 6 12 2.5 1 5 0 0.5 1 1 2 41 2 0.5 1 2 3 0.5 1 1070 1 5 1 1.9 2 M089 22SOE 200N 495276 5410562 37 1 2.5 1 0.25 1 8 16 49 2 40 3 0.5 1 2 4 67 3 0.5 1 2 3 0.5 1 1180 1 5 1 3.2 3 M090 22SOE 200N 495280 5410560 33 1 2.5 1 0.25 1 10 20 56 3 40 3 0.5 1 2 .. 65 3 0.5 1 3 5 0.5 1 1110 1 5 1 3.9 3 M091 2800E 300N 495821 5410410 94 4 2.5 1 0.25 1 96 192 106 5 30 2 0.5 1 19 38 39 2 0.5 1 21 35 0.5 1 1100 1 5 1 33.9 29 M092 2800E 350N 495846 5410451 75 3 2.5 1 0.25 1 74 148 87 .. 10 1 0.5 1 15 30 49 2 0.5 1 16 27 0.5 1 1040 1 5 1 24.9 22 M093 2800E 400N 495873 5410493 71 3 2.5 1 0.25 1 15 30 89 4 50 3 0.5 1 3 6 40 2 0.5 1 4 7 0.5 1 1260 1 5 1 3.7 3 M094 2800E 425N 495890 5410506 49 2 2.5 1 0.25 1 16 32 151 7 60 4 0.5 1 3 6 32 1 0.5 1 4 7 0.5 1 1040 1 5 1 3.2 3 M095 2800E 4SON 495903 5410523 73 3 2.5 1 0.25 1 18 36 9 1 30 2 0.5 1 1 2 54 2 0.5 1 3 5 0.5 1 1050 1 5 1 1.3 1 M096 2800E 475N 49591 9 5410547 79 3 2.5 1 0.25 1 48 96 185 9 80 5 0.5 1 10 20 78 .. 0.5 1 11 18 0.5 1 1240 1 5 1 10.6 9

NAD83 Zone 17

~YTE Une Station Entlng Northing IMg MjlRj; Mo MoR~ Nb NbR~ Nd NdRfi NI NIRR Pb PbRR Pd PdRR Pr PrRR Rb RbRR Sb SbRR Sm SmRf Sn SnRR Sr SrRR Te TeRR Th ThRR M097 2800E 500N 495923 5410578 45 2 2.5 1 0.25 1 18 36 114 6 30 2 0.5 1 4 8 45 2 0.5 1 4 7 0.5 1 1140 1 5 1 3.7 3 M098 2800E 525N 495943 5410586 69 3 2.5 1 0.25 1 5 10 2.5 1 20 1 0.5 1 0.5 1 66 3 0.5 1 2 3 0.5 1 1380 2 5 1 0.9 1 M099 2800E 550N 495939 5410622 75 3 2.5 1 0.25 1 22 44 181 9 40 3 0.5 1 5 10 52 2 0.5 1 6 10 0.5 1 1310 1 5 1 3.5 3 M100 2800E 575N 495938 5410649 20 1 2.5 1 0.25 1 14 28 241 12 30 2 0.5 1 3 6 68 3 0.5 1 4 7 0.5 1 1010 1 5 1 2.4 2 M101 2800E 800N 495966 5410665 105 4 2.5 1 0.25 1 32 64 163 8 30 2 0.5 1 7 14 16 1 0.5 1 8 13 0.5 1 1350 1 5 1 5.8 5 M102 2800E 650N 495981 5410709 75 3 2.5 1 0.25 1 15 30 43 2 5 1 0.5 1 3 6 16 1 0.5 1 5 8 0.5 1 890 1 5 1 5.4 5

"-'03 2UOOE 650N 49582 ~10818 18 1 2.5 1 0.2a 1 7 14 135 7 100 7 0.5 1 2 • 19 1 0.5 1 2 3 0.5 1 760 1 5 1 0.25 1 M104 2600E 600N 495803 5410758 80 3 2.5 1 0.25 1 35 70 161 8 20 1 0.5 1 7 14 75 3 0.5 1 8 13 0.5 1 1120 1 5 1 7.7 7 M105 2600E 575N 495779 5410739 66 3 2.5 1 0.25 1 6 12 20 2 30 2 0.5 1 0.5 1 23 1 0.5 1 2 3 0.5 1 1210 1 5 1 1.5 1 M106 2600E 550N 495772 541071 5 75 3 2.5 1 0.25 1 11 22 72 4 20 1 0.5 1 2 4 55 3 0.5 1 3 5 0.5 1 1280 1 5 1 3 3 M107 2600E 525N 495758 5410692 13 1 2.5 1 0.25 1 3 6 135 7 JO 2 0.5 1 o.s 1 5 1 0.5 1 0.5 1 0.5 1 821) 1 5 1 0.25 1 M108 2600E 500N 495741 5410666 107 4 2.5 1 0.25 1 5 10 70 3 20 1 0.5 1 0.5 1 24 1 0.5 1 2 3 0.5 1 1670 2 5 1 1.2 1 M109 2600E 475N 495726 5410650 61 2 2.5 1 0.25 1 21 42 263 13 30 2 0.5 1 4 8 .2 2 0.5 1 4 7 0.5 1 1680 2 5 1 6.9 6 M110 2600E 450N 495713 5410623 29 1 2.5 1 0.6 2 15 30 226 11 220 15 0.5 1 4 8 40 2 0.5 1 3 5 0.5 1 1090 1 5 1 1.6 1 M111 2600E 425N 495698 5410601 42 2 2.5 1 0.25 1 12 24 133 7 30 2 0.5 1 2 4 43 2 0.5 1 3 5 0.5 1 1770 2 5 1 2 2 M112 2600E 400N 495681 5410579 90 3 2.5 1 0.25 1 22 44 125 6 30 2 0.5 1 4 8 32 1 0.5 1 7 12 0.5 1 1360 2 5 1 4 .9 4 r·.'l 3 2600E .JON 49W5:5 <>-t . ~ ~8 I 2.5 1 O.2~ 1 1 2 29 1 5 1 0.5 0.5 1 1..5 1 0.5 1 0.5 1 0.5 1 10,10 1 15 1 0.25 1 M114 2600E 300N 495622 5410499 75 3 2.5 1 1.3 5 229 458 104 5 160 11 0.5 1 54 108 80 4 0.5 1 44 73 0.5 1 730 1 5 1 61.1 53 M115 2600E 250N 495584 5410458 91 3 2.5 1 0.25 1 11 22 139 7 5 1 0.5 1 2 4 61 3 0.5 1 3 5 0.5 1 1230 1 5 1 3.6 3 M116 2600E 200N 495562 5410423 29 1 2.5 1 0.25 1 16 32 348 17 30 2 0.5 1 3 6 53 2 0.5 1 4 7 0.5 1 1290 1 5 1 3.3 3 .r.l117 2600E 15rN 495528 541031'13 14 1 2.5 1 0.25 1 7 14 107 5 50 3 0.5 1 1 2 10 1 0.5 1 2 3 0.5 1 630 1 5 1 1.5 1 M118 2600E 100N 495499 5410347 42 2 2.5 1 0.25 1 13 26 136 7 30 2 0.5 1 3 6 64 3 0.5 1 3 5 0.5 1 1130 1 5 1 4.9 4 M119 2600E 50N 495471 5410297 87 3 2.5 1 0.25 1 64 128 92 5 5 1 0.5 1 13 26 41 2 0.5 1 1. 23 0.5 1 1170 1 5 1 19.7 17 M120 2800E 200N 495767 5410311 76 3 2.5 1 0.25 1 71 142 13 2 10 1 0.5 1 15 30 68 3 0.5 1 15 25 0.5 1 800 1 5 1 49.6 43 M121 2800E 250N 495795 5410352 75 3 2.5 1 0.25 1 32 64 99 5 20 1 0.5 1 6 12 43 2 0.5 1 8 13 0.5 1 1300 1 5 1 9 8 M122 2250E 150N 495278 5410551 65 2 2.5 1 0.25 1 10 20 201 10 20 1 0.5 1 2 4 50 2 0.5 1 3 5 0.5 1 1330 1 5 1 4.3 4 M123 2350E 475N 495513 5410753 90 3 2.5 1 0.25 1 62 124 50 2 20 1 0.5 1 12 24 32 1 0.5 1 15 25 0.5 1 1100 1 5 1 12.1 11 M124 2350E 450N 495506 5410729 49 2 2.5 1 0.25 1 5 10 28 1 60 4 0.5 1 0.5 1 41 2 0.5 1 2 3 0.5 1 1330 1 5 1 1.4 1 M1 25 2350E 425N 495484 541 0709 71 3 2.5 1 0.25 1 18 36 21 1 20 1 0.5 1 3 6 13 1 0.5 1 5 8 0.5 1 760 1 5 1 4.2 4 M1 26 2350E 400N 495467 5410666 86 3 2.5 1 0.25 1 46 92 122 6 20 1 0.5 1 9 18 55 3 0.5 1 11 18 0.5 1 1260 1 5 1 11 .3 10 M127 2350E 375N 495452 5410659 38 1 2.5 1 0.25 1 5 10 199 10 30 2 0.5 1 0.5 1 21 1 0.5 1 1 2 0.5 1 1040 1 5 1 2 2 M1 28 2350E 350N 495448 5410643 76 3 2.5 1 0.25 1 26 52 86 4 5 1 0.5 1 5 10 46 2 0.5 1 5 8 0.5 1 950 1 5 1 9.1 8 M129 2350E 300N 495417 5410596 75 3 2.5 1 0.25 1 25 50 51 3 20 1 0.5 1 5 10 32 1 0.5 1 7 12 0.5 1 870 1 5 1 9.1 8 M130 2350E 250N 495388 5410561 21 1 2.5 1 0.25 1 7 14 162 6 20 1 0.5 1 1 2 69 3 0.5 1 2 3 0.5 1 1090 1 5 1 2.7 2 M131 2350E 200N 495360 5410522 56 2 2.5 1 0.25 1 5 10 106 5 40 3 0.5 1 1 2 43 2 0.5 1 1 2 0.5 1 1530 2 5 1 1.2 1 M132 2350E 150N 495324 5410484 57 2 2.5 1 0.5 2 10 20 116 6 80 5 0.5 1 2 4 29 1 0.5 1 2 3 0.5 1 660 1 5 1 3 3

Peat Samples (n'"10)

IANALYTE Itlne Istation IEa.Gng INOithlng IMij IM9R~MO I MOR'! Nb INbRRlNii I NdRRjNI INJRRjpb IPbRRlpd IPdRRIPr IpiRRIRb I RbRRlSb ISbRRlsm ISmRiJSn ISnRRISr Isi'RRITe IteRRlfh IThRRI

M045 1950E 725N 495282 54111 82 33 1 2.5 1 0.25 1 11 22 63 3 400 27 0.5 1 3 6 17 1 0.5 1 3 5 0.5 1 860 1 5 1 1.5 1 M057 2050E 500N 495257 5410940 48 2 2.5 1 0.25 1 27 54 243 12 260 19 0.5 1 7 14 81 4 0.5 1 7 12 0.5 1 1240 1 5 1 6.2 5 MOn 2250E 575N 495473 5410909 10 1 2.5 1 0.25 1 13 26 143 7 90 6 0.5 1 3 6 37 2 0.5 1 4 7 0.5 1 980 1 5 1 0.9 1 M078 2250E 550N 495458 5410880 23 1 2.5 1 0.25 1 27 54 202 10 140 10 0.5 1 6 12 37 2 O.S 1 7 12 0.5 1 1090 1 5 1 3.3 3 M079 2250E 525N 495446 5410852 13 1 2.5 1 0.25 1 5 10 44 2 150 10 0.5 1 1 2 13 1 0.5 1 2 3 0.5 1 690 1 5 1 1.5 1 M084 2250E 400N 495377 5410750 10 1 2.5 1 0.25 1 7 14 11 2 6 50 3 0.5 1 1 2 9 1 0.5 1 2 3 0.5 1 540 1 5 1 0.6 1 M103 2600E 650N 495821 5410818 18 1 2.5 1 0.25 1 7 14 135 7 100 7 0.5 1 2 4 19 1 0.5 1 2 3 0.5 1 760 1 5 1 0.25 1 M107 2600E 525N 495758 5410692 13 1 2.5 1 0.25 1 3 6 135 7 30 2 0.5 1 0.5 1 5 1 0.5 1 0.5 1 0.5 1 820 1 5 1 0.25 1 M113 2600E 350N 495655 5410543 16 1 2.5 1 0.25 1 1 2 29 1 5 1 0 5 1 0.5 1 2.5 1 0.5 1 0.5 1 0.5 1 1000 1 5 1 0.25 1 M117 2600E 150N 495528 5410383 14 1 2.5 1 0.25 1 7 14 107 5 50 3 0.5 1 1 2 10 1 0.5 1 2 3 0.5 1 630 1 5 1 1.5 1

MAD83 Zone 17 IANALYTI: IUne Station I Eastlng [Northing rl ni{R tn ITIRR 'U URR :W WRR Y IYRR IYb IYbRR IZn 17nRR 7 . IZrRR TREERR +SrRR Moo1 1800E 725N 495147 5411260 1.5 1 0.25 1 2 1 0.5 1 17 1 2 1 10 1 2.5 1 11 7 Moo2 1800E 675N 495122 5411208 1.5 1 0.25 1 6 2 0.5 1 51 3 6 3 10 1 2.5 1 23 10 MOO3 1800E 625N 495103 5411163 1.5 1 0.25 1 1 1 0.5 1 28 2 3 1 10 1 2.5 1 14 8 M004 1800E 575N 495086 5411128 1.5 1 0.25 1 14 5 0.5 1 22 1 4 2 10 1 2.5 1 12 8 M005 1800E 550N 495073 5411107 1.5 1 0.25 1 4 1 0.5 1 37 2 5 2 10 1 2.5 1 19 10 MOO6 1800E 525N 495064 5411084 1.5 1 0.25 1 10 4 0.5 1 29 2 5 2 10 1 2.5 1 14 8 M007 1800E SOON 495048 5411062 1.5 1 0.25 1 7 3 0.5 1 77 5 17 7 10 1 2.5 1 38 8 MOOS 1800E 475N 495040 5411031 1.5 1 0.25 1 6 2 0.5 1 31 2 7 3 10 1 2.5 1 16 8 MOO9 1800E 450N 495028 5411011 1.5 1 0.25 1 7 3 0.5 1 39 2 7 3 10 1 2.5 1 17 8 M010 1800E 425N 495025 5410992 1.5 1 0.25 1 5 2 0.5 1 101 6 21 9 10 1 2.5 1 67 6 M011 1800E 375N 495002 5410947 1.5 1 0.25 1 5 2 0.5 1 51 3 14 6 20 2 2.5 1 24 9 M012 1800E 325N 494976 5410906 1.5 1 0.25 1 6 2 0.5 1 24 2 6 3 10 1 2.5 1 14 8 M013 1850E 375N 495025 5410904 1.5 1 0.25 1 5 2 0.5 1 55 3 17 7 10 1 2.5 1 28 7 M014 1850E 425N 495052 5410946 1.5 1 0.25 1 6 2 0.5 1 57 4 10 4 10 1 2.5 1 22 8 M015 1850E 450N 495065 5410994 1.5 1 0.25 1 1 1 0.5 1 38 2 5 2 10 1 2.5 1 16 8 M016 1850E 475N 495075 5411013 1.5 1 0.25 1 8 3 0.5 1 29 2 8 3 10 1 2.5 1 15 11 M017 1850E SOON 495086 5411031 1.5 1 0.25 1 6 2 0.5 1 25 2 2 1 10 1 2.5 1 15 10 M01 8 1850E 525N 495117 5411055 1.5 1 0.25 1 4 1 0.5 1 26 2 2 1 10 1 2.5 1 15 10 M019 1850E 550N 495122 5411071 6 4 0.25 1 4 1 0.5 1 40 3 3 1 10 1 9 4 43 7 M020 1850E 575N 495137 5411086 11 7 0.25 1 20 7 0.5 1 54 3 4 2 10 1 12 5 335 7 M021 18SOE 625N 495163 54111 26 7 5 0.25 1 18 6 0.5 1 26 2 2 1 10 1 8 3 27 7 M022 1850E 675N 495195 5411177 6 4 0.25 1 2 1 0.5 1 24 2 2 1 10 1 2.5 1 17 9 M023 1850E 725N 495225 5411210 15 10 0.25 1 1 1 0.5 1 37 2 3 1 10 1 8 3 80 6 M024 1900E 725N 495245 5411201 7 5 0.25 1 9 3 0.5 1 30 2 3 1 10 1 6 2 27 8 M025 1900E 675N 495221 5411159 1.5 1 0.25 1 4 1 0.5 1 25 2 2 1 10 1 7 3 43 7 M026 1900E 625N 495187 5411112 1.5 1 0.25 1 5 2 0.5 1 29 2 2 1 10 1 6 2 42 7 M027 1900E 575N 495166 5411077 1.5 1 0.25 1 3 1 0.5 1 33 2 2 1 10 1 7 3 46 8 M028 1900E 550N 495159 5411042 1.5 1 0.25 1 5 2 0.5 1 30 2 3 1 10 1 2.5 1 21 10 M029 1900E 525N 495143 5411032 1.5 1 0.25 1 5 2 0.5 1 36 2 3 1 10 1 6 2 36 9 M030 1900E SOON 495143 5411014 7 5 0.25 1 38 14 0.5 1 49 3 6 3 10 1 6 2 25 10 M031 1900E SOON 495140 5411014 1.5 1 0.25 1 33 12 0.5 1 28 2 5 2 10 1 2.5 1 14 9 M032 1900E 475N 4951 25 5410986 1.5 1 0.25 1 4 1 0.5 1 7 1 1 1 1600 160 2.5 1 10 4 M033 1900E 450N 495107 5410964 1.5 1 0.25 1 21 8 0.5 1 21 1 2 1 10 1 2.5 1 10 8 M034 1900E 425N 495106 5410939 1.5 1 0.25 1 7 3 0.5 1 28 2 4 2 10 1 2.5 1 13 9 M035 1900E 375N 495078 5410894 1.5 1 0.25 1 3 1 0.5 1 54 3 5 2 10 1 2.5 1 34 9 M036 1950E 425N 495135 5410931 1.5 1 0.25 1 28 10 0.5 1 36 2 4 2 20 2 2.5 1 33 7 M037 1950E 450N 495134 5410944 1.5 1 0.25 1 19 7 0.5 1 13 1 3 1 10 1 2.5 1 10 9 M038 1950E 475N 495160 5410969 5 3 0.25 1 19 7 0.5 1 33 2 2 1 10 1 7 3 54 7 M039 1950E SOON 495178 5410984 1.5 1 0.25 1 14 5 0.5 1 23 1 4 2 10 1 2.5 1 12 8 M040 1950E 525N 495187 5411010 8 5 0.25 1 13 5 0.5 1 27 2 3 1 70 7 9 4 25 7 M041 19SOE 5SON 495199 5411033 16 11 0.25 1 14 5 0.5 1 40 3 3 1 10 1 10 4 150 5 M042 1950E 575N 495211 5411048 1.5 1 0.25 1 11 4 0.5 1 30 2 2 1 10 1 5 2 27 10 M043 1950E 625N 495233 5411094 1.5 1 0.25 1 5 2 0.5 1 19 1 3 1 10 1 2.5 1 11 8 M044 1950E 675N 495259 5411141 1.5 1 0.25 1 3 1 0.5 1 27 2 2 1 10 1 7 3 41 7 IM045 1950E '7'25N 49,1128 ... 5411 "82 15 10 0.25 1 17 6 0.5 1 3S 2 6 3 ~ 28 25 1 64 3 M046 2000E 725N 495320 5411160 12 8 0.25 1 36 13 0.5 1 83 5 10 4 410 41 11 4 764 5 M047 2000E 675N 495301 5411109 20 13 0.25 1 15 5 1 2 50 3 4 2 90 9 11 4 309 7 M048 2000E 625N 495275 5411068 1.5 1 0.25 1 7 3 0.5 1 15 1 3 1 10 1 7 3 11 7

NA083 Zone 17 ANALYTE Une Station Eating Northing TI TIRR TI TIRR U URR W WRR Y YRR Yb YbRR Zn ZnRR Zr ZrRR TREERR I MgRR+CaRR+SrftR M049 2000E 575N 495259 5411019 1.5 1 0.25 1 9 3 0.5 1 29 2 4 2 10 1 2.5 1 14 9 M050 2000E 550N 495239 5410986 1.5 1 0.25 1 10 4 0.5 1 20 1 I, 2 10 1 2.5 1 12 7 M051 2000E 525N 495235 5410979 1.5 1 0.25 1 11 4 0.5 1 16 1 3 1 10 1 2.5 1 10 7 M052 2000E 500N 495219 5410955 1.5 1 0.25 1 11 I, 0.5 1 18 1 I, 2 10 1 2.5 1 12 7 M053 2000E 475N 495213 5410936 1.5 1 0.25 1 15 5 0.5 1 30 2 5 2 50 5 2.5 1 15 6 M054 2000E 450N 495195 5410910 1.5 1 0.25 1 11 I, 0.5 1 16 1 5 2 10 1 2.5 1 12 9 MOSS 2000E 425N 495190 5410885 4 3 0.25 1 4 1 0.5 1 39 2 5 2 50 5 11 4 34 7 M056 2050E 4SON 495232 5410904 4 3 0.25 1 41 15 0.5 1 110 7 10 I, 260 26 2.5 1 359 5 M057 2050E SOON 495267 6410940 9 6 0.25 , 46 16 0.6 1 116 7 13 5 670 67 2.6 1 163 6 M058 2050E 550N 495301 5410965 1.5 1 0.25 1 135 48 0.5 1 57 4 7 3 130 13 2.5 1 236 6 M059 2050E SOON 495333 5410994 5 3 0.25 1 18 6 0.5 1 21 1 3 1 10 1 7 3 12 7 M060 2100E 600N 495349 5410995 17 11 0.25 1 115 41 0.5 1 74 5 6 3 470 47 2.5 1 89 3 M061 2100E SOON 495352 5410996 12 8 0.25 1 89 32 0.5 1 68 4 6 3 260 26 2.5 1 82 3 M062 2100E 550N 495333 5410957 1.5 1 0.25 1 28 10 0.5 1 28 2 3 1 660 68 2.5 1 23 3 M063 2100E 500N 495306 5410905 1.5 1 0.25 1 6 2 0.5 1 21 1 3 1 60 6 2.5 1 27 6 M064 2100E 4SON 495277 5410864 68 59 0.25 1 52 19 0.5 1 155 10 14 6 410 41 29 12 1456 5 M065 2100E 400N 495251 5410820 5 3 0.25 1 13 5 0.5 1 36 2 4 2 90 9 2.5 1 136 6 M066 2150E 500N 495349 541 0681 6 4 0.25 1 5 2 0.5 1 17 1 I, 2 30 3 2.5 1 11 8 M067 2350E 500N 495514 5410783 4 3 0.25 1 10 4 0.5 1 94 6 9 4 10 1 11 4 458 7 M068 2350E 525N 495530 5410803 1.5 1 0.25 1 7 3 0.5 1 16 1 4 2 10 1 2.5 1 11 7 M069 2350E 5SON 495541 5410822 1.5 1 0.25 1 12 4 0.5 1 24 2 5 2 10 1 6 2 13 7 M070 2350E 575N 495548 5410850 1.5 1 0.25 1 5 2 0.5 1 58 4 17 7 10 1 2.5 1 56 6 M071 2350E SOON 495562 5410872 1.5 1 0.25 1 4 1 0.5 1 220 14 49 20 30 3 8 3 1016 4 M072 2350E 625N 495578 5410911 59 39 0.25 1 10 4 0.5 1 119 7 11 5 300 30 49 20 777 4 M073 2350E 650N 495588 5410930 1.5 1 0.25 1 3 1 0.5 1 22 1 I, 2 10 1 2.5 1 61 5 M074 2250E 650N 495514 5410965 1.5 1 0.25 1 6 2 0.5 1 57 4 9 4 40 4 8 3 275 4 M075 2250E 625N 495490 5410935 1.5 1 0.25 1 3 1 0.5 1 39 2 9 4 10 1 2.5 1 110 5 M076 2250E SOON 495488 5410922 1.5 1 0.25 1 4 1 0.5 1 38 2 8 3 70 7 2.5 1 101 4 IMQ"? 2250E 575N 49/i04',3 6410909 1.6 1 0.25 1 20 7 0.5 1 49 3 7 3 90 9 2.5 1 74 3 1 M078 2250E 550N 495458 5410880 6 4 0.25 1 68 21 0.5 1 69 4 9 • 130 13 2.5 1 148 3 M07S 2250E 52&H 49'-'«6 5410852 16 11 0.2~ 1 12 4 0.6 1 36 2 8 3 670 67 2E: 1 34 3 MOSO 2250E 500N 495436 5410832 43 29 0.25 1 10 4 0.5 1 69 4 10 4 340 34 13 5 386 4 M081 2250E 475N 495424 5410810 1.5 1 0.25 1 3 1 0.5 1 25 2 4 2 40 4 2.5 1 141 5 MOS2 2250E 450N 495410 5410786 1.5 1 0.25 1 9 3 0.5 1 23 1 4 2 120 12 2.5 1 89 4 M083 2250E 425N 495390 5410764 1.5 1 0.25 1 11 4 0.5 1 22 1 5 2 90 9 2.5 1 61 4 IMOM 2250E 400N 495377 6410750 7 6 0.25 1 10 4 0.5 1 30 2 5 2 500 50 2.5 1 39 3 M085 2250E 375N 495364 5410720 1.5 1 0.25 1 14 5 0.5 1 63 4 13 5 270 27 2.5 1 176 3 M086 2250E 350N 495346 5410693 1.5 1 0.25 1 5 2 0.5 1 32 2 6 3 220 22 2.5 1 150 4 M087 2250E 300N 495323 5410657 1.5 1 0.25 1 15 5 0.5 1 86 5 12 5 10 1 7 3 384 4 M068 2250E 250N 495308 5410621 1.5 1 0.25 1 4 1 0.5 1 22 1 5 2 10 1 2.5 1 33 4 MOS9 2250E 200N 495276 5410562 1.5 1 0.25 1 3 1 0.5 1 17 1 5 2 90 9 2.5 1 45 4 M090 2250E 200N 495280 5410560 1.5 1 0.25 1 4 1 0.5 1 16 1 4 2 150 15 2.5 1 53 4 M091 2800E 300N 495821 5410410 1.5 1 0.25 1 6 2 0.5 1 69 4 5 2 10 1 29 12 458 6 M092 2800E 350N 495846 5410451 4 3 0.25 1 20 7 0.5 1 47 3 3 1 40 4 19 8 359 5 M093 2800E 400N 495873 5410493 1.5 1 0.25 1 4 1 0.5 1 32 2 11 5 10 1 2.5 1 82 6 M094 2800E 425N 495890 5410506 1.5 1 0.25 1 2 1 0.5 1 40 3 12 5 10 1 2.5 1 89 4 M095 2800E 450N 495903 5410523 1.5 1 0.25 1 2 1 0.5 1 34 2 9 4 10 1 2.5 1 65 5 M096 2800E 475N 495919 5410547 1.5 1 0.25 1 12 4 0.5 1 68 4 12 5 10 1 2.5 1 244 6

NAD83 Zone 17 ANAlYTE Une station Eastlng Northing n nRR n nRR U URR W WRR Y YRR Vb YbRR Zn ZnRR lr lrRR TREERR ~MQRR+CaRR+SrRR M097 2800E SOON 495923 5410578 1.5 1 0.25 1 3 1 0.5 1 37 2 10 4 10 1 2.5 1 96 4 M008 2800E 525N 495943 5410586 1.5 1 0.25 1 3 1 0.5 1 14 1 3 1 10 1 2.5 1 26 6 M099 2800E 550N 495939 5410622 1.5 1 0.25 1 3 1 0.5 1 38 2 8 3 10 1 2.5 1 115 6 M100 2800E 575N 495938 5410649 1.5 1 0.25 1 2 1 0.5 1 43 3 11 5 10 1 2.5 1 80 3 M101 2800E 600N 495966 5410665 1.5 1 0.25 1 6 2 0.5 1 48 3 9 4 10 1 2.5 1 168 7 M102 2800E 650N 495981 5410709 1.5 1 0.25 1 4 1 0.5 1 25 2 3 1 10 1 6 2 71 5 1,.103 2600E bi>oiN 495821 5410818 1.5 1 0.25 1 3 1 0.5 1 24 2 3 1 170 17 2.5 1 40 2 M104 2600E 800N 495803 5410758 1.5 1 0.25 1 15 5 0.5 1 32 2 3 1 10 1 8 2 161 6 M1 05 2800E 575N 495779 5410739 1.5 1 0.25 1 2 1 0.5 1 23 1 5 2 10 1 2.5 1 31 5 M106 2600E 550N 495772 541071 5 1.5 1 0.25 1 3 1 0.5 1 21 1 5 2 10 1 2.5 1 54 8 IM101 "..oDE fi25N 495758 5410\$92 1.6 1 0.25 1 8 3 0.5 1 7 1 O.S 1 420 42 2.5 1 18 3 M108 2600E SOON 495741 5410666 1.5 1 0.25 1 3 1 0.5 1 19 1 4 2 10 1 2.5 1 25 7 M109 2600E 475N 495726 5410650 1.5 1 0.25 1 10 4 0.5 1 31 2 7 3 120 12 2.5 1 115 6 M110 2600E 450N 495713 5410623 1.5 1 0.25 1 295 105 0.5 1 35 2 8 3 150 15 2.5 1 96 4 M111 2600E 425N 495698 5410601 1.5 1 0.25 1 19 7 0.5 1 23 1 5 2 50 5 2.5 1 63 5 M112 2600E 400N 495681 5410579 1.5 1 0.25 1 6 2 0.5 1 38 2 3 1 10 1 7 3 105 6 1'.l '13 ~!I()E .151'''' 49511" 5<'10f 3 1.5 1 n .;; 1 3 1 0.'" 1 5 1 1 1 bOO 6<- 2.~ 1 '1 3 M114 2600E 300N 495622 5410499 114 76 0.25 1 16 6 0.5 1 143 9 12 5 220 22 71 28 1252 5 M11 5 2600E 250N 495584 5410458 1.5 1 0.25 1 7 3 0.5 1 19 1 3 1 10 1 2.5 1 51 6 M116 2600E 200N 495562 5410423 1.5 1 0.25 1 3 1 0.5 1 32 2 9 4 150 15 2.5 1 94 4 1'.1117 2600E 1 SON 49&628 5410383 1 1 0.25 1 15 5 0.5 1 33 2 4 2 490 ..• 1.lI 2.5 1 11 2 M118 2600E 100N 495499 5410347 1.5 1 0.25 1 3 1 0.5 1 33 2 9 4 180 18 2.5 1 80 4 M11 9 2600E SON 495471 5410297 41 27 0.25 1 16 6 0.5 1 43 3 4 2 60 6 18 7 31 2 6 M120 2800E 200N 495767 5410311 25 17 0.25 1 12 4 0.5 1 44 3 4 2 10 1 39 16 354 5 M121 2800E 250N 495795 5410352 1.5 1 0.25 1 5 2 0.5 1 39 2 6 3 40 4 2.5 1 165 6 M1 22 2250E 150N 495278 5410551 1.5 1 0.25 1 10 4 0.5 1 15 1 4 2 60 6 2.5 1 61 5 M123 2350E 475N 495513 5410753 1.5 1 0.25 1 4 1 0.5 1 49 3 3 1 30 3 14 6 282 6 M1 24 2350E 450N 495506 5410729 1.5 1 0.25 1 2 1 0.5 1 26 2 8 3 10 1 2.5 1 31 5 M125 2350E 425N 495484 5410709 1.5 1 0.25 1 1 1 0.5 1 27 2 2 1 10 1 8 3 78 5 M126 2350E 400N 495467 5410666 11 7 0.25 1 24 9 0.5 1 39 2 4 2 10 1 16 6 21 5 6 M127 2350E 375N 495452 5410659 1.5 1 0.25 1 3 1 0.5 1 15 1 4 2 40 4 2.5 1 25 4 M1 28 2350E 350N 495448 5410643 1.5 1 0.25 1 7 3 0.5 1 24 2 3 1 60 6 8 3 117 5 M129 2350E 300N 495417 5410596 5 3 0.25 1 14 5 0.5 1 33 2 3 1 10 1 12 5 112 5 M130 2350E 250N 495388 5410561 1.5 1 0.25 1 5 2 0.5 1 15 1 5 2 110 11 2.5 1 39 4 M131 2350E 200N 495360 5410522 1.5 1 0.25 1 5 2 0.5 1 14 1 3 1 60 6 2.5 1 29 5 M132 2350E 150N 495324 5410484 1.5 1 0.25 1 12 4 0.5 1 14 1 3 1 250 25 2.5 1 55 4

Peat Samples (n-10)

,ANALYfE IUne ,statIOn ,fasting INOrthing In IfiRR In InRR ,0 10RR IW IWRR 19 IVRR IVb IVbRRjzn ,znRR jzr ItrRRlfREeRR IMjRR+caRR+SrRR

M045 1950E 125N 495282 5411182 15 10 0.25 1 17 6 0.5 1 36 2 6 3 280 28 2.5 1 64 3 M057 2050E SOON 495257 5410940 9 6 0.25 1 46 16 0.5 1 116 7 13 5 670 67 2.5 1 163 5 M077 2250E 575N 495473 5410909 1.5 1 0.25 1 20 7 0.5 1 49 3 7 3 90 9 2.5 1 74 3 M078 2250E 550N 495458 5410860 6 4 0.25 1 58 21 0.5 1 69 4 9 4 130 13 2.5 1 148 3 M079 2250E 525N 495446 5410852 16 11 0.25 1 12 4 0.5 1 38 2 8 3 670 67 2.5 1 34 3 M084 2250E 400N 495377 5410750 7 5 0.25 1 10 4 0.5 1 30 2 5 2 500 50 2.5 1 39 3 M103 2600E 650N 495821 5410818 1.5 1 0.25 1 3 1 0.5 1 24 2 3 1 170 17 2.5 1 40 2 M107 2600E 525N 495758 5410692 1.5 1 0.25 1 8 3 0.5 1 7 1 0.5 1 420 42 2.5 1 18 3 M113 2600E 350N 495655 5410543 1.5 1 0.25 1 3 1 0.5 1 5 1 1 1 680 66 2.5 1 12 3 M117 2600E 150N 495528 5410383 1.5 1 0.25 1 15 5 0.5 1 33 2 4 2 490 49 2.5 1 41 2

APPENDIX IV

Bubble Plots of Analyzed Data

•

TRES OR RESOURCES 1- SURVEY 2006 - AgRR 494800 mE 495000 mE 495200 mE 495400 mE 495600 mE 495800 mE 496000 mE 496200 mE

AgRR ~ 15.00 z N E 0 + + + + + 0 8 3 ~ N z ~

-t~ '" ~ z a E 0 + + + 0

0

3 0

~ z 10.00 ~

'" # ~ z 0 CD

E

+/ 0 0 +

+ 0 7.50 0 'V

3 '" z

0 • 10

~ Z 0 5.00 m

E 0 + + + 0

0

3 0 <0

Z 0 • 10

'" 2.50 ~ z 0 ... E 0 + + + + 0

0

3 0

1.00

.... z

0

Z-units : • 10

0 10 1015 494800 mE mE

mE 0 7.51010

0 5 10 7.5 Plot Projection: 0 2.510 5

0 200 400 HAD 83, Zone 17 1 to 2.5

Samples (n=132) Meters

'3eochemistry plots by: lAount Morgan Resources Ltd., Ninni e Manitoba

TRE OR RESOURCES MMI- SURVEY 2006 - AuRR 494800 mE 495400 mE 495600 mE 495800 mE 496000 mE 496200 mE

AuRR ~ 26.00 z I\)

E + + + + + 8 8

3 ~ N z ~

wf~ ~ z

§ E

+ + + 8 3 ~ z ~

~ 15.00 z 0 0>

E 0 0 + + 0 0

3 0:>

Z 0

~

I 10.00

~ z 0 0>

E + + + 8 7.50

0

3 0 <D

Z 0 ; I()

5.00

~ z 0 ... 2.50

E + + + + 8 0

3 0

0.00

.. z

0

Z-units : ; I()

0 15 to 26

010 to 15

0 7.5 to 10 Plot Projection: 0 5 to 7.5 0 200 400 HAD 83, Zone 17 0 2.5 to 5 Samples (n=132) 0 0 to 2.5 Meters

3eochemistry plots by: Wount Morgan Resources Ltd., Mnni e Manitoba

TRES OR RESOURCES MMI-M SURVEY 2006 -CdRR 494800 mE 495400 mE 495600 mE 495800 mE 496000 mE 496200 mE CdRR

01 14.00 ~ z ;;; E 0

+ + + + + 0

8 3 ~ N z

~

~~ 12.00

01 ~

Z 0 E 0

+ + + 0 10.00 § 3 z

~

01 ~

z 7.50 E

+ + 8 3 00 z 0

~

01 ... 5.00 0 z '" E 0

+ + + 0 0

3 0

'" z 0

~ 2.50

z E + + + + 0

3 0 1.00 " z 0 Z-units :

~

0 12 to 14

mE 495000 mE 0 10 to 12

0 7.5 to 10 Plot Projection: 0 5 to 7.5

0 200 400 HAD 83, Zone 17 0 2.5 to 5 Samples (n=132) 1 to 2.5

Meters 3eochemistry plots by: Wount Morgan Resources Ltd., Ninni e Manitoba

TRES OR RESOURCES MMI-M SURVEY 2006 -CeRR 494800 mE 495400 mE 495600 mE 495800 mE 496000 mE 496200 mE

CeRR

1: ~ 204.00 z ~ E 0 + + + + + 0

0

3 0

N ~ z ;

wf~ '"

'" ~ z 0

E 0 + + + 0

0

3 0

S! z ;

'"

'" ~ z 0 CD

E 0 100.00

0 + + 0 0

3 0:>

Z 0

~

~ z ~ E

+ + + 8 0

3 50.00 0 CD

Z 0

~

~ 25.00

z 0 .... E

+0 0 10.00 + + + + 0 0

3 5.00 0

1.00 C!

z ; 0 Z-units : '"

0 0100 to 204

494800 mE 495000 mE 495200 mE 495400 mE 495600 mE 495800 mE 496000 mE 496200 mE 0 50 to 100

° 25 to 50 Plot Projection: 0 10 to 25 0 200 400 NAD 83, Zone 17 0 5 to 10 Samples (n=132) 1 to 5 Meters

'3eochemistry plots by: lAount Morgan Resources Ltd., Ninni e Manitoba

TRES OR RESOURCES MMI-M SURVEY 2006 -CuRR 494800 mE 495200 mE 495400 mE 495600 mE 495800 mE 496000 mE 496200 mE CuRR

r.n 11 .00 ~ z '" E 0

+ + + + + 0

8 3 ~ N z

~ wfE r.n ~

Z 0 E 0 8.00 + + + 0

§ 3 z

~

~ 6.00 z

E + 0 + 3 0

00 z 0 ; '"

~ 4.00

0 z '" E + + + 8 0 3 0 <0 Z 0 ; '" 2.00

~ z ~ E + + + + 8 0

3 0 0.00 .... z 0 Z-units:

~

081011

494800 mE 495000 mE 495200 mE 0610 8

o 410 6

Plot Projection: 0 210 4

0 200 400 NAD 83, Zone 17 o 010 2


3eochemistry plots by: lAount Morgan Resources Ltd., Ninni e Manitoba

TRES OR RESOURCES M 1-

z E g N

Z E

§

~

Z E

8 ~

~

z E

§ ~

494800 mE

+

+ +

I + +

+ +

'3eochemistry plots by: lAount Morgan Resources Ltd.,

!....:=-_~Il...l Ninni e Manitoba

495400 mE

+

o 200

Meters

SURV Y 2006 - Mg+Ca+SrRR 495600 mE 495800 mE 496000 mE

+ + +

+ +

+

400

496200 mE

+

+

+

+

+

496200

Plot Projection: NAD 83, Zone 17 Samples (n=132)

'" g 3 z

§ 3 z

~ o 0> o o 3 z

~ al o o 3 Z

~ o .. g 3 Z

Mg+Ca+SrRR 11.00

10.00

8.00

6.00

4.00

2.00 Z-units:

0101011

o 81010

o 610 8 o 410 6 o 210 4

TRES OR RESOURCES MMI-M SURVEY 2006 - Pb R 494800 mE 495000 mE 495200 mE 495400 mE 495600 mE 495800 mE 496000 mE 496200 mE PbRR

! 27.00

z ~ E 0

+ + + + + 0

8 3 ;::! N z

~ wf-m ! z 0 20.00 E + + + 8 § 3 z

~

! 15.00

z 0 co

E 0

8 + + 0

3 co z 0

~ 10.00

! z 0

0> E 0

+ + + 0 7.00 0 3 0 co Z 0

~ 4.00

'" ~ z E + + + + 0 3 0 0.00 C!; z

Z-units:

~

020t027

494800 mE 495000 mE 496000 015 to 20

o 10 to 15 Plot Projection: 0 7 to 10

0 200 400 NAD 83, Zone 17 0 4to 7 Samples (n=132) Oto 4

Meters

3eochemistry plots by: Wount Morgan Resources Ltd., Ninni e Manitoba

TRES OR RESOU C SM I-M SURV Y2006 -Ti R 494800 mE 495000 mE 495200 mE 495400 mE 495600 mE 495800 mE 496000 mE 496200 mE TiRR

U1 76.00 .... -z

N E 0 + + + + + 0

0

3 0

N N

Z ~

;:

wf-~ '"

~ -z 0

E 0 + + + 0

0

3 0

~ z

50.00 ;: '"

U1

~ Z 0 Q)

E 0 0 + + 0 0

3 <Xl

Z 0

;: '"

U1 25.00 ~ z

0 0>

E 0 + + + 0

0

3 0 <0

Z 0

;: '"

U1 10.00 ~ 0

z .... 5.00

E 0 + + + + 0

0

3 0

1.00

.... z

0

Z-units: ;: '"

o 50 to 76 494800 mE 495000 mE 495200 mE 495400 mE 496000 mE 496200 mE 025 to 50

0 10 to 25 Plot Projection: 0 5 to 10

0 200 400 HAD 83, Zone 17 1 to 5



TRES OR RESOURCES MMI SURVEY 2006 ZnRR 494800 mE 495000 mE 495200 mE 495400 mE 495600 mE 495800 mE 496000 mE 496200 mE ZnRR

~ 160.00 z N E 0 + + + + + 0

g 3 ~ N z • wf-m on

'" ~ z

8 E

+ + + 0 0

3 0

~ z ~

100.00

~ z 0 (I)

E

g 0 + + 0

3 co

z 0

~

~ 50.00 z 0 C>

E + + + g 0

3 0 co

Z 0 • on

25.00

I; 0

~ z 0

10.00 • E + + + + 8 5.00

0 0

3 0.00 ....

z 0

Z-units : • on

010010160 495200 mE

496000 mE 496200 mE 0 5010100

0 2510 50 Plot Projection: 0 1010 25 0 200 400 HAD 83, Zone 17 0 510 10 Samples (n=132) 010 5 Meters

3eochemistry plots by: Wount Morgan Resources Ltd., Ninni e Manitoba

TRES OR RESOURCES MMI-M SURVEY 2006 -~reeRR 494800 mE 495000 mE 495200 mE 495400 mE 495600 mE 495800 mE 496000 mE 496200 mE I: reeRR

'" 1454.00 ~ z ;;; E

+ + + + + 8 8 3 ~ M z ;:

wf-~ 1250.00 '"

~ z

§ E

+ + + a

3 1000.00

a ~

Z ~

~ Z a 750.00 '"

E

+ 8 8 + 3

co

Z a ;: '"

'" 500.00 ~ z a '"

E a + + + a

a

3 a co

Z a

~ 250.00

~ z a .. E a + + + + a 8 3

v

z 9.00 a

Z-units : ~

o 1,250 to 1,454 mE 495000 mE 495200 mE o 1,000 to 1,250

0 750 to 1,000 Plot Projection: 0 500 to 750 0 200 400 HAD 83, Zone 17 0 250 to 500 Samples (n=132) 9 to 250 Meters


To: Tres-Or Resources Ltd 1934 - 131 Street WHITE ROCK BC V4A 7R7 V4A 7R7

P.O. No. Project No. No. Of Samples Date Submitted Report Compfises

DEFAULT 70 Nov 25,2005 Pages 1 to 9

Certificate of Analysis Work Order: 086701

(Inclusive of Cover Sheet)

Distribution of unused material:

70 Soils

Certified By

Date: Dec 14,2005

Stuart Lam Operations Manager

Report Footer:

ISO 9002 REGISTERED ISO 17025 Accredited for Specific Tests. see No. 456

L. N. R. = Listed not received n.a. = Not applicable

I.S. = Insufficient Sample = No result

*INF = Composition of this sample makes detection impossible by this method

M after a result denotes ppb to ppm conversion. % denotes ppm to % conversion

Subject to SGS General Terms and Conditions

The data reported on this certificate of analysis represanls the sample submitted to SGS Minerals Services. Reproduction of this analytical report. in full or in part. is prohibited without prior written approval.

SGS Canada Inc. Mineral Services 1885 Leslie Street Toronto ON M3B 2M3 t(416) 445-5755 f(416) 445-4152 WWW.sgS.ca .. -.. -............•• -.. ~-...... - .......................... .

E'-nt Method Oet.LiIn.

Page 2 of9

The data repoI1ed on this certificate of analysis represents the sample submitted to SGS Minerals Services. Reproduction of this analytical report, in full or in part, is prohibited withOut prior wtiItIIn approval.

SGS Canada Inc. Mineral Services 1685 Leslie Street Toronto ON M3B 2M3 t(416)445-5755 f(416)445-4152 www.sgs.ca

_ot _____ .. _l

SG$ Element M8thocI Det.Um.

1

iM052 lM053~· /M054----

Final: .. ······-AgT

MMI-M~ 1\

As: MMI-M5;

10 PPB

1

The data reported on this certificate of analysis represents the sample submitted to SGS Minerals Services. Reproduction of this analytical report, in full or in part, is prohibited without prior wriHen approval.

SGS Canada Inc. Mineral Services 1885 Leslie Street Toronto ON M3B 2M3 1(416) 445-5755 1(416) 445-4152

Page 3 of9

_ .. _----.. -1

Element Method Det.Um. Units

~~f::~·· !M047~-·· f~~'"-·'

iM048 ,',. "~<.-

The data reported on this certificate or analysis represents the sample submitted to SGS Minerals Se!vices. Reproduction of this analytical report, in full or in part. is prOhibited without prior written approval.

SGS Canada Inc. f(416) 445-4152 www.sgs.ca

- .. --___ .. _1

Element Method DeWm. Units

M049

! : Page 50f9

The dam repol1ed on this certificate of analysis represents the sample submitted to SGS Minerals Services. Reproduction of this analytical report, in full or in part, is prohibilBd without prior written approval.

SGS Canada Inc. Mineral Services 1885 Leslie Street Toronto ON M38 2M3 t(416) 445-5755 f(416) 445-4152 www.sgs.ca

- .. --_____ 1

Element Method Det.Um. Units e-.. --.. ··· .. · ~~~~ ......... _ .............. ..

~;~ .. 004

~{1F 1M018 IM019 .. ····· IMci20 . lM021'" ~ ... ~,,-.... -..... iM022 ~~-~~-.-...

1M023 '-4024· .. · lMo25 iMo26 IM027" i·,_~_·_w .. iM028

lM02S' 1M030 iMOl:;" IM032 (-~-.-- .. ~. '" ~

~~.~~ .... lM034 IM03S····

~~~~ ..................... . IM03S· .. .. lMo39 E~§: iM041

l'JI.~~ ..... iM043

iM044

iM.~~. IM048 iMii47" . iM04e ... ,

F ! . 08670'1 Page 6 of9

The data reported on this certificate of analysis represents the sample submitted to SGS Minerals Services. Reproduction of this ana/ytical report, in full or in part, is prohibited without prior writ1en approval.

SGS Canada Inc. f(416) 445-4152 www.sgs.ca

- .. --___ ... _1

iM070 ~D;:;PMOO1~ FOupM013· .~ .. >.-"~-".-<.-."'

t!?up.~~~~ t!?~~_ MO~~~. i*OupM049

f:~~~~1

086701 Page 7 of9

The data ~ on this certificate of analysis represents the sample submitted to SGS Minerals ServiCes. Reproduction of this analytical report, in fuU or in part, is prohibited without prior written approval.

SGS Canada inc. Mineral Services 1885 Leslie Street Toronto ON M3B 2M3 t(416) 445-5755 f(416) 445-4152 www.ags.cs

- .. --___ .. _1

a-nt MattIod Det.1Im. Units r-----

~~-O~-1 iM002 1------- - --------

~-t.AOOO-

~~~

1M042 Icw~~~, ___ "

iM043

~-~----iM045 1" .... _ .. -. ....

jM046 iM047-jM04S-

PageS of9

The data repor1e<l on this certificate of analysis represents the sample submitted to SGS Minerals Services. Reproduction of this analytical report, in full or in part. is prohibited without prior written approval.

SGS Canada Inc. «416) 445-4152 www.sgs.ca -_.--. ------- - .. _---_ .. ---)

! : Page 9 of9

~~P"M02S" "--'''-,-'''''-'''' roup M037 ,---"'''''-'''''''' , oupM049

t§~~M~i""

The data reported on this certiIicate of analysis represents the sample submitted to SGS Minerals Services, Reproduction of thill analytical report, in full or in part, ill prohibited without prior written approval,

SGS Canada Inc, Mineral Services 1885 Leslie Street Toronto ON M3B 2M3 t(416) 445-5755 1(416) 445-4152 WWW,sgS,C8 "",--"-----"''''-,,,'-""" '"

- ...... - __ - .. _1

To: Tres-Or Resources Ltd 1934 - 131 Street WHITE ROCK BC V4A 7R7 V4A 7R7

P.O. No. Project No. No. Of Samples Date Submitted Report Compiises

DEFAULT 63 Nov 25,2005 Pages 1 to 9

Certificate of Analysis Work Order: 086702

Date: Dec 13, 2005

(Inclusive of Cover Sheet)

Distribution of unused material:

63 Soils

Report Footer:

Certified By

ISO 9002 REGISTERED

Stuart Lam Operations Manager

ISO 17025 Accredited for Specific Tests. see No. 456

l.N.R. = listed not received n.a. = Not applicable

I.S. = Insufficient Sample = No result

"I N F = Composition of this sample makes detection impossible by this method

M after a result denotes ppb to ppm conversion, % denotes ppm to % conversion

Subject to SGS General Terms and Conditions

The data reported on this certifica1e of analysiS represents the sample submitted to SGS Minerals Services. Reproduction of this analytical report, in full or in part, is prohibited without prior written approval.

SGS Canada Inc. Mineral Services 1665 leslie Street Toronto ON M3B 2M3 1(416) 445-5755 '(416) 445-4152 WWW.sgs.ca

IMOge" /Moli:;"IM09S"'" iM09S"

iM100" ! ... " ...... . iM101 t>,.<--.~.-~.""

iM102 !-"-"-.,,. iM103 1'''''--IM104

!M10S'

iM112 ( ..... "._-iM113 1··· .. ·_·· .. ;M114 !M11"S' iM.~i~: iM117

iM118

The data repor1ed on this certifiQlte of analySis represents the sample submitted to SGS Minerals Services. Reproduction of this analytical report, in full or in part, is prohibited without prior written approval.

SGS Canada Inc. .."." ....... f( .. :.4." .. 1 .. 6.> 445-4152 WWW.sgs.ca _ot _____ ._)

Element Method Dat.Um. Units

The dala reported on this certificate of analysis represents the sample submitted to SGS Minerals Services. Reproduction of this analytical report, in full or in part, is prohibited without prior written approval.

SGS Canada Inc. Mineral Services 1885 Leslie Street TOlOnlD ON M3B 2M3 t(416) 445-5755 1(416) 445-4152

- .. --___ .. _1

a-nt Method Det.Um. Units

7

88 _ ~,,~""""' .. ,,' , .. , ....... " . IMOSS ~pi~: 1M091

~~~~:~: 094

F

The data reported on this certificate of analysis represents the sample submitted to SGS Minerals S8IVices. Reproduction of this analytical report, in full or in part, is prohibited without prior written approval.

Page 4 of9

SGS Canada Inc. f(416) 445-4152 WWW.sgs.ca

Element Method DatUm.

Units ""'""""""""""""""""1

f~~~"""-~~-",," "--"-,, """"""--=~:.~~:~: ". !M121

Page 5 of9

The data repor1ed on this certificate of analysis represents the sample submitted to SGS Minerels Services. Reproduction of this analytical report, in full or in part, is prohibited without prior written approval.

SG5 Canada Inc. MineraiServices 1885 Leslie Street Toronto ON M3B 2M3 t(416) 445-5755 f(416) 445-4152 WWW.sgs.ca "-"""".""" .. ~" .. """""""."""" """"""

Element Method Det.Um.

"",1"

···········1 I ·············t

o·,t", __ , i

··t .+ 1

Final:

<1

The data repot1ed on this certificate of analysis represents the semple submitted to SGS Minerels SeIVices. Reproduction of this analytical report, in fuH or in part, is prohibited without prior written approval.

Page 6 of9

SGS Canada Inc. MineralServices 1885 Leslie Street Toronto ONM3B2M3 t(416)445-5755 f(416)445-4152 WWW.sgs.ca

Element Method Det.Llm. Units

The data reported on this certifICate of analysis represents the sample submitted to SGS Minerals Services. Reproduction of this analytical report. in full or in part. is prohibited without prior written approval.

SGS Canada Inc ......... + .... M .... i.ne .....• ra.1 S&IVices 1885 Leslie Street Toronto ON M3B 2M3 1(416) «5-5755 f(416) 445-4152 www.sgs.cs

- .. --___ .. _1

Element Method Det.LIm. Units

~1if r~:""''''''''''''''''''

7

JM097 .. 'M09S' M099

oM100 L

!~~.~J .. iM102 j_"" __ '_"'" ·'c

I~~~~ .. IM104

t~Z .. ~".~~-'''''.

l~.~.~! ........ iM108

iM109 l-"~~·-·'~"~·~··· .

!M110

1M111" ,~~.~~~o_~· ... iM112 L ......... · iM113 1··· .... _ .. · iM114

1M115 iM116 !M117 .... ~!.1.8 ..

The data reported on this certificate of analysis represents the sampte submitted to SGS Minerals Services. Reproduction of this analytical report, in full or In part, is prohibited without prior writlBn approval.

PageS of9

SGS Canada Inc. Mineral Services 1885 Leslie Street Toronto ON M3B 2M3 t(416) 445-5755 1(416) 445-4152 WWW.sgS.C8

Element Method Det.Um. Units

i~D:~~ iM120 c·_··_·,···,,_·,,·,,·"'· !M121

iM122 t~---·

oup M071

PD~PMo83'" ;--_._. __ .---- -..

rOup M095 I .. ----·~-«~'-' .. '-"'~"' l*oupM107

~oUP-M119' l~'~,"-ff~' ~"n" ~~.""

r.[).':I!:,.M131

Page 9 of9

The data reported on this certificate of analysis represents the sample submitted to SGS Minerals Services_ Reproduction of this analytical report, in full or in part, is prohibited without prior written approval.

SGS Canada Inc. Mineral Services 1885 Leslie Street Toronto ON M3S 2M3 t(416) 445-5755 f(416) 445-4152 www.sgs.ca _.r ___ I __ 4e_1

assessment report on geochemical survey on claims … · 2017-01-16 · geoscience assessment...

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