stripping benefication rpt galway twp · 2017. 1. 16. · county rare earth-potassic mica study...

RECEIVED OCT L 7 lOO~ '(L

GeOScIeNce ASSESSMENT OFFIce

Bulk Sample Project Amphibolite Gneiss Contact Mica Studies

Claims 1249338 & 1249345 Study D.N.Webster I Earth Resources Property

South-West Galway Township Peterborough County. Southeastern Ontario

by

Frederick T, Archibald, B,Sc,Geologist October 20, 2006

Table of Contents

Title Section Page #

Summary .:Introduction Property Description & Access Topography & Vegetation History of Area General GeoJogy Geological Table of Formations 2004 Bulk Sampling - Geological Program 2005 Bulk Sampling - Geological Program 2006 Bulk Sampling and Diamond DJilling Program Thin Section Results Results and Specifics of 2005 Sampling Program Conclusions & Recommendations

.£ertificateof .Qualifications

Appendix

1 .... 3

4 6 7 9 11 12 14 15 16 1.7 18

·20

Location Plan of Bulk Sampling (Pits and trench locations) . Expense .. BreakdowrLSpecifics

Location Plan Trench I Pit 3 - CGG Samples .Beneficiation- Assay Summary CGG Series

Chart 1 £hart 2 Chart 3 13 pages

I

Peterborough. County Rare Earth-Potassic Mica Study

Summary -

The rare-earth industry is growing and as technology-intensive uses increase so does the demand for rare earth elements (AMR Technologies Inc, Apr.200S). Rare earths are used in glass, catalysts, magnets, ceramics, phosphors, and metallurg,ical adaptations. A study was performed to bulk sample the biotite mica bearing amphibolites to observe size ratios and percentages. The biotite micas have an affinity of being potassic rich and occurring with certain rare-earth elements.

A preliminary study was started on a seventy meter wide olivineepidote rich brecciated amphibolite in 2003 to find any potential for rare earths or econonomically viable potassium concentrations or other viable commodities on claim 1249345 and claim 1249338; and completed in the beginning of 2004. A follow-up program of backhoe trenching and bulk sampling was done from four areas along a faulted- amphibolite I alkalic syenite contact in south-west Galway Township to confirm mica grades and size distributions. The olivine rich breccia zone lies along a sheared contact between amphibolite units to the south and anorthosite-amphibolite units to the north. Although this unit can be upwards of 110 meters in width, the breccia rich sections are narrower. All of the units generally dip 45 to 85 to the south. The potassic rich bands, generally coinciding or in contact with biotite and amphibolite gneiss units which surround the Volturno Lake Granodiorite Batholith Complex, are generally averaging twenty-five to one-hundred metres in width. Along the contact is a brecciated-mylonitic zone of potassic rich amphibolite (biotite rich) and a brecciated epidote I olivine calcium-carbonate syenite-granite.

A rare-earth spectrum of analysis was done and significant zirconium (Zr02) assays were observed. Xenotime is a phosphate with similar structure to ZrSi04 and could be associated with scheelite (tungsten) scarn and U30a-bearing material. Other than potassic rich micas with K20 ratios as high as 4.5% within this area, no other viable minerals were observed in this area

2 Rare-earth mineralogy has indicated that the zone of interest is within

a metasomatic / mylonitic! skarn type carbonatite which occurs at the contact with amphibolites and potassic-alkalic granites / syenites! pegmatites. In most likelihood the carbonatites (carbonate rich magmatic rocks associated with explosive volcanism within major faults) and monazite (alkalic granites and high-grade metamorphic rocks) are intercalated and associated with both calc-alkalic marbles and dolomitic marbles.

The biotite mica bulk sample percentages averaged 19.0% to 62.50/0 biotite mica with an affinity for potassic rich material which can be used as an additive for agricultural! farming uses. Drillhole data indicates that these zones occur within amphibolite gneiss contact areas with dolomitic and calcitic marbles; and that they occur in amounts between 5.0% mica to 70.00/0 mica down to depths averaging between 17.0 meters and 29.0 meters in depth. The mica conrtent decreases with depth with decrease in both weathering and metamorphic alteration.

The total cost for this program, (consisting of diamond drilling, trenching, and benefication of samples), was $29,868.50 which included backhoe excavation within four sites ($10,308.50) , beneficiation! assaying of samples ($11,760.00), and field mapping and bulk sampling ($5,400.00). Selective samples were combined for bulk sample tests. This program was performed in the Fall of 2005 and in the Spring of 2006; the last phase of field bulk sampling done from June 13, 2006 to June 24, 2006. The pits and trenches were photographed and filled and levelled back to normal after sampling was performed. This work was performed for Earth Resources

Ltd. ; owner of the property.

3 Introduction-

This report contains the studies of a mylonitic breccia unit which parallels the outer-core contact area, made up of biotite rich amphibolites, surrounding the Volturno Lake Alkalic Batholith Complex. Much work has been done on the neighbouring Anstruther Granite Batholith and Cheddar Syenite Batholith, this being the most southerly of the known alkalic syenite-granite batholith complexes. Further south, the area is overlain by limestone capping and not much is known about these areas and if there are other granitic batholith structures.

This work has been carried out by F.T.Archibald Consulting Ltd., an independent consulting geologist firm. F.T.Archibald has worked and is presently working on numerous geological sub-contracting projects in the area as an independent agent for development of various commodities. This report is done for Earth Resources Ltd.; owner of the property.

The Lands for Life exists in Cavendish Township to the east, and although this area is not in contention, Lands for Life is already planning to expand within the Crown Land areas in the north section of Cavendish Township. This area in particular lies to the west of a recreational-reserve area designated at the western limits of the Kawarta Highlands Land for Life designation.

The purpose of this program has been to focus on the potassic rich areas within a epidote-olivine-apatite rich heterolithic breccia zone. Studies of the fragments show that they are in actuality stretched conglomeritic xenoliths with mylonitic fabric and are considered upper mantle facies fragments. Previous programs performed on this zone were done to indicate potential for diamonds and potassic-rich aggregates for agricultural (soil additive) uses. This program was performed to analyze the percentages of biotite micas within the contact areas of the amphibolitebearing areas surrounding the Volturno Granite Batholith within Galway and Harvey Townships.

4 Property Description and Access-

The central section of the property is located within the southern and eastern portions of Galway Township, and along the west side of Cavendish Township. These townships are located in southern Ontario between Lindsay and Peterborough. The property consists of unpatented mining claims and patented concessions. The property is located approximately one hundred and seventy kilometers northeast of Toronto, or about thirty kilometers northeast of the town of Bobcaygeon. The claims can be accessed by cottage roads to Crystal Lake via Crystal Lake Road (from the northwest and south) and Bass Lake (from the southwest) via Bass Lake Road. Crystal Lake Road is about 14.0 kilometres north of Bobcaygeon (on Highway #36) and extends about 13.2 kilometres to the west edge of the property. Bass Lake is accessible via two points, 11.0 kilometers north of Bobcaygeon to Bass Lane (Fire Route #402), or 2.0 kilometres east to Bass Lake Road. The Bass Lane route is taken for approximately 4.0 kilometres to the west edge of the property, and the Bass Lake Road route is taken for approximately 13.0 kilometres to the south boundary of the property respectively. The property can also be accessed from Fire Access Route 108 (in Cavendish Township) which is intersected by Highway #507 and due west for some 13.2 kilometres to the property. Fire Access Route #108 is some nine kilometers north of Flynn's Comers along Highway #507. The property is also accessed by the Loom Lake Forest Access Road which is some nine to twelve kilometers west of Highway #507 (at a point immediately south of Catchacoma Lake and lying along the Harvey-Cavendish Township boundary.

These claims are located in the Southeastern Ontario Mining District within the Peterborough District. Ministry of Natural Resources for this area, including Aggregate Mining permits, is under the Minden jurisdiction.

Township

Galway Galway

5

The claim group surveyed is listed as follows: Claim Number

1249345 1249338

# Unjts(20hect.each)

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The length of the operating season is twelve months of the year with peak seasons being in early Spring and Fall. Timbering is presently going on in the area and timber roads are kept open by both snowmobiling and timbering.

Power is available in close proximity to the property to the west, south and north. The plant will most likely use propane heating on-site. Local manpower is available as is heavy machinery. Parts and fabrications are available in Peterborough which is some fifty kilometres to the southeast.

The property has several paved highways on all sides, and has local containerized trucks of all sizes which can ship to the local markets.

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6 Topography & Vegetation- s~

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The vegetation ranges from dense bush to wide open areas of mature to semi-mature birch,maple,white pine, spruce and cedar. In several of the areas, specifically on neighbouring patented lots, the coniferous trees have been logged off within the past few years. Birch and maple hardwoods are found on the higher ridge areas and within extensive sand and gravel deposits. Coniferous trees tend to occupy the lower swampy areas of the property. Approximately thirty to forty percent of the property is at lower elevation and covered by varying thicknesses of overburden.

The terrain is generally rolling to flat with overburden thickness· varying from a few centimetres to tens of metres. Overburden depth was generally greatest in swamp-covered fault areas and erosional gouges left by glaciation. The effect of glaciation is a series of whalesback ridges which are highly scoured and scarped along their northern faces. The geological units of greater resistance tend to be higher and less weathered, hence being outcrops. A total of five to ten percent of the claims are outcropped, and less than forty percent of the property has bedrock exposure. In most cases the bedrock is less than a few metres in depth below the overburden cover.

The area over the mid-eastern section of the gabbro complex has been recently logged by a timber company from the Minden area (selective cutting).

7 History otArea-

Uranium mineralization was discovered in Galway and Cavendish Townships in 1950. Also during this period two quartz vein systems on the claims were trenched and investigated for unknown commodities; one of which is up to 8.0 meters in width.

From 1975 to 1977, Bright (OGS) mapped Cavendish Township. The Ontario Department of Mines had previously mapped the northwest section of Galway Township, and no mapping had been done in the areas of the marble complexes. Previously, Galway Township was known for iron, silver, and uranium exploration. The only active mining presently is for limestone slabs used for landscaping purposes.

In the mid 1970's (1975-1977), another program of renewed vermiculite exploration occurred in Cavendish Township by Goshawk Mines Ltd. and Insulite Development Corporation. This work was abandoned as it was located in close proximity to cottages on Catchacoma Lake.

In the early 1970's, Goshawk Resources Inc. and Insulite Development Corp. located and tried to develop a vermiculite deposit in Cavendish Township. This zone wraps around the west contact with the Anstruther Granite Batholith.

In the 1980's and up until 1996, Teck Corporation /Breakwater Resources Ltd. I St.Joe Gold Explorations explored for zinc in the northern sections of Cavendish and Galway Townships in the vicinities of Salmon Lake and Solerno Lake respectively. This was curtailed due to the close proximity to the cottagers on Solerno Lake.

In 2000-2001, Lydia Diamonds located a diamond-bearing lamproite dyke system in the Wolf Lake areas of Tudor-Grimsthorpe Township. This was follow-up work from a till sampling program in which a northeasterly trending fault system was followed within an amphibolitic- mafic metavolcanic system which is in contact with a gabbro intrusive pluton. Diamonds have been reported from this dyke system.

8 In 2001 and 2002, two limestone quarries (Mervin Johnson Quarry

and Jeff Parnell Quarry) have been operating under two mining leases in Galway and Cavendish Townships respectively. During the same period the Preston Quarry was operating a syenite traprock quarry in Cavendish Township.

In 2003 and 2004, studies were performed for indications of diamond potential within several sections of the deep-seated carbonatite related fault systems. Potassic rich amphibolites along the contact areas of the alkalic granite-anorthosite complexes were also studied for their potassic aggregate potential for use as agricultural additives.

In the Fall of 2005 and the Spring of 2006, a study of four areas within this claim block (claims 1249345 and 1249338)was studyied for its mica potential; in specific its potassium (K203) potential. Potassium in naturally weathered material can be added to soils as a non-toxic and natural fertillizer (as a triple-mix additive) without otgher additives.

9 General Geology-

The area covered by the claims is underlain by carbonate-rich metasediments of marble and diopside (Grenville Province of the Precambrian Shield), carbonated biotite-schists (metasediments), amphibole-rich metasediments, intrusive amphibolite schist, syenite I syenite-gneiss intrusions, pegmatite intrusions, quartz monzonite, and crystalline limestones. These rocks are of mid Proterozoic age (1280-1300 Ma). Bands of altered biotite or amphibolite rich rock can be observed in areas of intense deformation and shearing.

The structural geology of the Grenville Province is Complex and is dominated by large-scale regional fold structures that have been folded and re-folded by tectonism, high-grade metamorphism, and intrusive activity.

A period of major orogenic deformation occurred pre 1300 Ma when the volcanic and sedimentary rocks were deposited on the basement rocks. Felsic Intrusions dating 1240 to 1270 Ma indicates a mid Proterozoic orogenic period as most of the orogenic period occurred between 1220 to 1160 Ma period. During the Grenville Orogeny, rock units around the Anstruther Batholith and Volturno Lake Batholith were metamorphosed and deformed into flow-folds situated around the rim of the felsic-alkali batholiths.

The area was glaciated during the Pleistocene. In areas where geological trend is in a north-south direction the rocks have been scoured. cleanly and little to no glacial till has been deposited. In areas where the geological trends are east-west, there is some glacial till deposited at the bases of hills and at the edge of valleys where there are catch-basins. In some cases there is 1 .0 to 3.0 metres of glacial till which is deposited intermittently (generally within the east-west valleys.

The potassic rich biotite-bearing zones are situated generally in contact with gneissic shears or amphibolite shears. Phlogopite, tremolite,

10 and biotite hydrothermally alter to chlorite. In most cases it appears that talc and serpentinite are negligible.

The bedrock in the southern portion of Galway Township generally. appears to dip steeply (45 to 85 degrees) southeasterly and strikes northeasterly. This is in contrast to the flat-lying bedding found within the deposits to the east and south of Catchacoma Lake in Cavendish Township. Weathering increases with depth where the dip steepens. In some areas close to shears and faults the dip is crenulated and flow banded. Intense folding is located in several zones rimming the granite (syenite-alaskite) structures.

Geological mapping has located several parallel bands of biotitebearing marble which diverge and converge around intrusive alkalic complexes consisting of syenite, granite, and alakites . The biotite gene-rally weathers to chlorite or the iron rich facies. It is thought that some of the zones are actually the same but are divided by dyke systems of syenite granite, quartz monzonite, and pegmatite. Generally, the zones are continuous except where block-faulted by northeasterly trending faults. Several of these faults have been mapped either by topographical controls or geological inconsistencies between the close-spaced trenches. The major faults in the area are northeasterly trending.

11 Geological Table of Formations

PhanerozQjc- Cenozojc- peat, marl, sand and gravel (glaciofluvial) Paleozoic- Ordovician (middle) (458-478 Ma)

-80bcaygeon Formation Limestone -Gull River Formation Limestone

(trilobite and gastropod interlaces) -Shadow Lake Formation Limestone

Precambrian- P[oterozoic-1160-1220Ma Carbonatite Suite-Pegmatite

Carbonatite Granite

Syenite Diorite-Gabbro

Alaskite Suite- Felsic Intrusive (gneisses) 1240-1270Ma Diorite Suite- Felsic Intrusive(granodiorite gneiss)

Mafic Inrusive (gabbro gneiss) Trondhjemite Suite- Medium Intrusive(moozonite gneiss)

Medium Intrusive(granite gneiss) Medium Intrusive(granodiorite gneiss) Mafic Intrusive(diorite gneiss)

Nepheline Suite-Alkalic Syenite Intrusive(potassic syenite gneiss) Nepheline Syenite Intrusive Mafic Alkalic Intrusive(nepheline gabbro)

Anorthosite Suite- Mafic Intrusive (gabbro gneiss) Calcareous Metasedimentary Suite-

Calcitic Marble (gneissic to massive) Dolomitic Marble(gneissic to massive) Amphibolitic mudstone-greywacke

Calcitic-siliceous mudstone-greywacke Siliceous Metasedimentary Suite-

gneissic greywacke gneissic arkose

Metavolcanic Rocks-Andesite-Dacite Suite-Felsic Metavolcanics (gneissic) Rusty-graphitic-pyritic-pyrrhotitic

Tonalite Gneiss Basement Rock Suite

(After- S.B.Lumbers 2000, Ontario Geological Survey

12 2004 Geological - Sampling Program-

The biotite-rich amphibolite zones have been extended northeasterly through severa~ Townships which include: Harvey Township, Gatway Township, Cavendish Township, and Glamorgan Township. Iron content in the rocks appears to increase to the northeast. Observations of the nepheHne syenites within these befts show an iron content to high for commercial mining operations (with exception of the Blue Mountain nepheline syenite which is presently being mined near Nephton,Ontario).

One zone in particular, a brecciated zone with increased amounts of potassic-apatite-olivine-epidote, has become of interest for its rare earths and potassium potential.

The biotite- rich gneissic syenite to gneissic amphibolite units are associated with the Volturno Lake Batholith Intrusive ,some ten by seventeen kilometers in diameter, is an oblong structure with a granodiorite core and a granite outer-core. All units are surrounded by amphibole gneiss and biotite gneiss rocks.

The biotite bands are generally associated with highly sheared calcitic to dolomitic marbles which are in close assoctation with syenites (atkaH feldspar rich) and amphibolite units. There is also a relationship between nepheline syenite marble and carbonatite marble which is probably predominantly nepheHne syenite with a lesser degree nepheline pyroxenite. Only one thin band of pyroxenite has been observed during the geological mapping program.

Generally there are two deformation belts which converge in the central sections and split where the Anstruther Batholith and the Voltumo Lake Batholith meet. These zones dip 45 degrees northwesterly to vertical (mainly steeply dipping northwesterly).

13 -There are -several-major-cross-cutting -faults -trending -north~south and

northwest-southeast; the most significant being the Bass Lake-Nogies Creek Fault and the Otter Lake-Loom Lake Fault.

--It-appears-that-the highest -amounts -of- biotite-is -associated -with steeply dipping or crenulated-banded syenitic contacts.- Where there is a shallow dip, the marbles appear to be mainly crystalline and only surficially

.. weathered; The marble-units along the-west edges-of the AnstrutherVoltumo Lake Batholiths are steeply dipping (southeasterly and northwesterly).

14

2005-Geological--Sampling -Program The potassic rich amphibolitic rock shows a three-directional

cleavage pattern and high-heat I high fluid type alteration. Samples have . -been sent-to Lakefield Labs·for further microscope work.

The samples are generally 11.0 to 62.0 percent Si02 composition which increases with the increase in AI203 composition.

Heavy mineral assays have shown elevations in the following minerals within these zones which ring around the south contact of a gabbro I anorthosite I granite intrusive structure. These are:

Cu,Zn,La,Ce,Nd,Cr Some of these elements are expected to be higher than normal as

they occur along shear-fault deformation zones. The iron content appears. to be higher than normal within similar neighbouring structures. The potassium content is related directly to the biotite mica mineralization which appears to be generally unweathered and unaffected by the hydrometamorphic alteration processes.

Observation of the material sluiced indicates that there is very little clay alteration and material breaks up readily with water as the rock is generally super-hydrated. The rock is made up of granite I pegmatite inclusions (migmatic) within biotite-rich amphibolitic rock. This unit has been traced across the property for at least 2400 meters before it pinches out to the east and to the west; priobaly due to cross-faulting structures along Nogies Creek to the west and to the east side of claim 1249345.

15 2006 Bulk Sample and Diamond Drilling Program-

A series of eight trenches, one which consisted of a large pit dug down to 5.5 meters in depth, was trenched and mapped with channel samples dug from the sides and the base of the trenches and pits (iephotographs). Five of the trenches were dug on claim 1249345 and three of the trenches were dug on claim 1249335.

Triple A Resources Ltd. were hired to perform beneficiation tests for mica on the samples from the months of February, 2006 through to and including October of 2006. Triple A Resources has been carying out beneficiation tests for mica (vermiculite) for Regis Resources Inc. and has been doing so for the past four years (in specific for assessment work compilations). Samples CGG-1 through CGG-2.9 inclusive were evaluated from Pit 31 Trench 3 for the purposes of this report. Other samples from other trenches are ongoing and are not part of the costs included in this report.

Triple A Resources Ltd. performed some 175.0 meters of diamond drilling (SO core size) in four vertical holes using a II Prospector "diamond drill. Two of these holes were performed on claim 1249338 and two holes on claim 1249345. Water monitors were placed in the holes after obtaining the cores and the geological information. The core is stored in Buckhorn, Ontario.

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16 Thin Section- Microscope Results

El. Archibald Consulting Ud.

Name Amphibolite-Granite Metasomatite - metamorphosed scam undergoing fluid percolation

Composition 70% diopside (clinopyroxene) altered biotite amphibolite eclogitic garnet (G-1 type) clinopyroxene apatite magnetite chromite

17 Specifics & Results of 2006 Bulk Sampling Program-

Four areas were bulk sampled with the use of a Cat 320LC model backhoe excavator; one on claim 1249338 and three areas on claim 1249345. Material was excavated and representative samples taken before the pits and trenches were filled and back-filled (See- Photos of

excavations). The sampling was performed in October and November of 2005 and finished from June 13 to June 24 of 2006. Beneficiation was performed in the months of May and June of 2006 by Triple A Resources Ltd. In each of the areas a two-tonne sample of material was piled for future use, although the trenches and pits were filled in to what they were previous to excavation. In each case the samples were sent in as representative concentrates. Several samples were beneficiated to observe heavy mineral concentrates under binocular microscopes.

18

Conclusions-The claim group is essentially underlain by metasomatic and

intercalated calcitic marbles, dolomitic marbles, syenitic marbles, and nepheline syenites which lie along the east flank of a biotite rich amphibolite unit that surrounds the Volturno Lake Granodiorite Complex. These units have been intruded by potassic granites (alaskites) and syenites and by amphibolitic-biotitic gabbro units.

Samples were run for diamond potential and only one sample indicated eclogitic garnets and olivine; both indicators of diamonds although the samples are from upper mantle and are of no importance. Garnets are of the almandine garnet variety were most abundant and are of no importance. The eclogitic garnets were diagnosed as crustal arid not deepseated magma source, and the olivine crystal was Fe-rich and confirmed not indicative of diamond origin.

Samples have been run for chemical composition tests and there is low potassic content within the mica minerals which are of biotite composition. Samples tested for potassic potential and generally average less than 3.20/0 K20. Values are too low to be of economic importance.

Samples were run for fibrous content as amphibolite rocks are known for their fiber content. No asbestos.(crysotile) or tremolite fibres were observed in any of the four areas sampled.

Tests have been done on the rare earths and semi-precious mineral potential and is anomalous in the elements (in order of significance): zinc, strontium, zirconium (the most significant being the latter).

Rare-earth mineralogy has indicated that the zone of interest is within a metasomatic / mylonitic I skarn type carbonatite which occurs at the contact with amphibolites and potassic-alkalic granites / syenites I pegmatites. In most likelihood the carbonatites (carbonate rich magmatic rocks associated with explosive volcanism within major faults) and monazite (alkalic granites and high-grade metamorphic rocks) are intercalated and associated with both calc-alkalic marbles and dolomitic

19 marbles.

A rare-earth spectrum of analysis was done and significant zirconium (Zr02) assays were observed. Values averaging 0.03% to 0.21% Zr02 (zirconium silica oxide) were observed but these values are insignificant to have market potential.

Bulk sample concentrates were beneficiated and average biotite mica contents ranged from 19.0% content to 62.5% content. These concentrates can be concentrated further by Humphrey Spiral (wet separation) technique up to 86% to 920/0 concentrates, or by air winnowing (dry separation) up to 50% to 65% concentrates. The size distribution of the majority of the mica ranges from -4 mesh to + 45 mesh (more specifically between -8 mesh and +20 mesh sizes.

Diamond drilling indicates that the mica contents are high to depths down to 17.0 meters and 29.0 meters; after which the mica content decreases with the lack of surficial weathering and with decrease in metamorphic alteration. Drilling indicated mica amounts as low as 5.0% mica and as high as 70.00/0 mica; the higher mica contents occuring along steeply dipping fault or shear zone contacts.

October 20, 2006 Concord, Ontario F.T. Archibald, B.Sc. Geologist, P.Geo.#1052

20

Certificate of Qualifications 1. I am an independent consulting mineral exploration geologist. and

have been engaged in the geological profession continuously since graduation in 1978.

2. I have particular experience in exploring for diamonds, gold, base metals, and other precious and industrial minerals. I have been a management consultant directly involved in the discovery and developmentof several gold and vermiculite deposits.

3. I am a graduate of Carleton University (B.Sc. 1978) in Geology

4. I am a registered P.Geo. under OGO Permit #618

5. I have practised as P.Geo. under Professional Engineers and Geoscientists of Newfoundland (Class A).

6. I am a registered P .Geo. under APGO Permit #1052

7. I am qualified for writing reports under the National Instrument 43-101.

8. My knowledge of the Galway Township area has been carried on as an independent consultant for several clients since 1999.

9. My most recent visit to the property was in October of 2006

10. This report is addressed to the Assessment Office of the Ministry of Northern Development & Mines and is provided for exclusive use by the owner of the claim herein.

11. I have been given no stock and only consulting fees as consideration and act solely as an agent for Earth Resources and David Webster.

October 20, 2006 Concord, Ontario

Q\c~ F.T.A~B.SC. Geologist, B.Sc.P.Geo.

2005-2006 Work Breakdown Claims 1249338 & 1249338

Earth Resources Ltd. Property

A)Bulk Sampling and Backhoe Excavation programs 2005

October 10-31 inclusive

2006

April 19 to 24 inclusive

May 13 to 17 inclusive

June 13 to 24 inclusive

B) Expenditure Breakdown

Bulk Sampling - 12 days @ $450/day each ----------------

(April 19-24, May 13-16)

$ 5,400.00

travel I mob I demob. 4800 km X 0.50 per km.(equiv. room & board)

-------------------- $ 2,400.00

60 days beneficiating samples Triple A Resources

@ $5,880.00 per month -------------------- $11,760.00

Excavator Trenching Cat 320EL (83.5 hr @ $120Ihr)------------ $10,308.50

TOTAL EXPENDITURES on claim 1249345/1249338----- $ 29,868.50

Expenditure on claim 1249338------ $6790.70 Expenditure on claim 1249345------$23,077.80

Ci 0_

~ -o

! -

----- CREEl<

CLAIM 1249345 CONt 2 LOT 15

-------- GALWAY TW5P •. o 5.0 10.0 I~.O

METERS

, Bulk Pit [Specimens

Benefi.ci.ati.on' Sampling. Galway (Webster) Trenching

C.lalm 12493450 eGG Series Trench-Pit #3

Sample # Interval Sampled Channel Width (m) % Mica Highest %Size (meters) (mesh)

CGG1-LlNE A 0-5.0N 5.0 46.5 -20+45 CGG2 5.0-10.0N 5.0 36.5 -20+60 CGG5 10.0-15.0N 5.0 45.0 -20+45 CGG6 15.0-20.0N 5.0 33.5 -8+60 CGG7 20.0-25.0N 5.0 32.5 -20+60 CGG8 25.0-30.0N 5.0 46.0 -20+45 CGG9 30.0-35.0N 5.0 41.0 -20+45 CGG10 35.0-40.0N 5.0 43.0 -20+60 CGG11 40.0-45.0N 5.0 24.0 -20+60 CGG12 45.0-50.0N 5.0 48.5 -20+45 CGG13 SO.O-SS.ON 5.0 41.5 -20+45 CGG14 55.0-60.0N 5.0 43.5 -20+45 CGG15 60.0-65.0N 5.0 41.0 -20+45 CGG16-LlNE B 65.0-70.0N 5.0 62.5 -8+60 CGG17 70.0-75.0N 5.0 32.0 -8+45 CGG18 75.0-80.0N 5.0 51.0 -8+60 CGG19 aO.0-a5.0N 5.0 40.0 -20+60 CGG20 85.0-90.0N 5.0 40.5 -20+45 CGG21 90.0-95.0N 5.0 47.0 -20+45 CGG22 95.0-100N 5.0 49.0 -20+60 CGG23 1 00.0-105 .ON 5.0 57.0 -20+60 CGG24 105.0-110.0N 5.0 38.5 -20+60 CGG27 110.0-115.0N 5.0 29.5 -20+60 CGG28 11S.0-120.0N 5.0 19.0 -20+60 CGG29 120.0-125.0N 5.0 26.5 -20+60

2

Trench 6 @ old beaver damlhouse (Z series East) 06-153 06-154 06-155 100 kg. of bulk material

Trench 7 06-156 06-157 06-15S 06-t59"

Trench"S

0-5.0N "5.0N-10.0N 10.0N-15.0N t5. ON:.ZO. ON"

06-160 0-5.0N 06-161" 5.ON~10~ON

5.0 5.0 5.0 5.0

5.0 5.0"

2.5m depth 2.0m depth 2.3m depth Z.3m depth-

3.0m depth 3". Om depth

20.0 m. length

Bulk Pit /Specimens Benetlclation J Samp_ling

Galway (Webster) Trenching Claims 1.249338 &. 1.2.49345

Trench 1@ Road- 17T0696977- 4947752 3.0m d~pth 0-3. Om depth 0-3. Om depth . 0-3. Om depth 3.0-5.0m depth 3.0-5. Om depth

06-128 06-129 06-130 06-131 06-132 06-133 06-134

12.98-17.08 17.08-20.08 20.08-22.58 22.58-25.08 17.08-20.08 20.08-22.58 22.58-25.08

4.1 3.0 2.5 2.5 3.0 2.5 2.5 3.0-5.0m depth- 20.1 m length

Trench 2 06-135 06-136 06-137 06-138 06-139 06-140 06-141 06-142 06-143 06-144 06-145 06-146-

5.0N-8.0N 3.0 8.0N-11.0N 3.0 27.0N-31.5N 4.5 31.5N-36.0N 4.5 53.0N-60.0N 7.0 60.0N-67.0N 7.0 67.0N-70.0N 3.0 73.30N-77.30N 4.0 77.30N-81.30N 4.0 81.30N-84.30N 3.0 84.30N-86.30N 2.0 118.0N:'124.0N 6.0

3.5m d~pth 3.5m depth 4.0m depth 4.0m depth 3.0m depth 3.0m depth 2.2m depth 2.2m depth 5.0m depth 5.0m depth 3.0m depth 4.0m depth- 51'.0 m length

PitlTrench-3 @ 8E corner-17T0697757- 4949041 (Z series)- 1'20 kg. material-bulk Pit 12.0m X 12.0m excavated to 5.0 m depth and stockpiled-30%frag.

Trench 4 06-144A 06-145A 06-147 06-148 06-149 06-146A 06-150 06-151

IrenCh'S

0-5.0N 5.0 5.0N-10.0N 5.0 31.0N-34.0N 3.0 34.0N-36.5N 2.5 36.5N-39.0N 2.5 39.0N-41.0N 3.0 124.40N-127.0N 2.6 127.0N-130.0N 3.0

2.3m depth 1.5m depth 3.0m depth 4.0m depth 4.0m depth 4.0m depth 3.0m depth 3.0m depth-

06-152 bulk pile (bluish-green amphibolitic carbonatite)

26.6 m length

· , Webster Biotite-Mica Borehole Data

Claims 1249338 & 1249345

V06-01 17T 4949347N-0697943E 29.0 ft { a.84 m}- (water tabte· at 4.90 m depth). Drilled July 26, 2006

0-19.0m- Dolomitic Marble- green to purple mica rich (biotite) 65% to 70% mica content, calcite rich seams, pyrite rich coarse disseminated

19.0-20.0m- Dolomitic Marble with mica rich seams - purple colour

20.0.0-29.0m- Dolomitic Marble- massive and equigranular

29.0-45.0m- Dolomitic Marble- equigranular and massive

45.0m - End of Hole

biotite mica content 0-20.0m (averaging 65%-70% mica content)

V06-02 17T 4949034N-0697793E big pit -29.0 feet .(8.84 -mdepth)~ water -table ·at 7.92 -mdepth} Drilled July 27, 2006

0-23.0m- Dolomitic Marble- purple to green mica bands averaging 8% to 12% mjca content (75% to 80% jn bands)

23.0-24m- Amphibolite Schist- weathered purple to green mica rich (70% mica content)

24.0-29.0m- Dolomitic Marble- purple to green mica bands averaging 8% to 12% mjca content (75% to 80% in bands

29.0-4S.0m- Dolomitic Marble- equigranular and massive

4S.0m- End of Hole

biotite mica rich from 0 to 29.0 m depth averaging 8% to 12% content

0-17.0

o ~ :-2.. t: ~-:. /.'; L'" -

17T 4948533N-0697~90E .25.0 ft .. (7.-62.m.depth} -.(water ·table·at ·6.71-m -depth) Drilled August 4, 2006

Calc-Alkaline Marble- mica averaging 5% to 8% content

17.0-25.0- Amphibolite with calcite bands, greenish grey colour banded at 80 _ degrees to core axis

25.0m-40.0m- Amphibolite- massive and equigranular amphibolite gneiss

40.0m - End of Hole

biotite mica content up to 5% to 8% content down to 17.0 m depth)

V06-04 17T 4948170N-0697323E 29;.O-ft-( ·8 .. 84 .m)- {water -table ·at.5.50 .mdepth} Drilled August 7, 2006

0-13.0m- Amphibolite $chlst- highly schistose, banded at 70 to 80 degrees to core axis, with aggolomUic marble bands at 45 degrees to core axis

13.0-29.0m- Amphibolite- green to purple mica bands averaging 1/2 inch to 3/4 inch thick, banded at 80 degrees to core axis

29.0-45.0m- Amphibolite- mica content decreasing with depth to competent amphibolite gneiss

45.0m - End of Hole

biotite mica rich down to 29.0m depth (60% to 13.0 m depth and 20% from 13.0 to 29.0m depth)

Sample number 2823 grams

fractions +4 -4+8 -8+20 -20+45 ·45 +60 -60 fraction weights g 696 724 ·731 368 95 207 weightrung - 200 200 200 50 ----after exfoliation. g -- 162 152 172 36 ---wasteg -- 162 131 122 30 ---mica. g - 0 20 49 6 -moist. or lost % - 19 24 14 28 -weight % 24.6 25.6 25.8 13 3.3 7.4 mica % - +0 10 24.5 12 ---total mica % of -- -complete sample


+4 - 4+8 - 8+20 -20 +45 - 45 +60 - 60 fractions

fraction weights g 730 480 548 393 133 440

weight rung - 200 200 200 100 --after exfoliation. g - 164 164 170 92 -wasteg --- 164 144 144 77 --mica.g - sign 19 26 14 -moist. or lost % - 18 18 15 8 ---weight % 26.7 17.6 20.1 14.4 4.8 16.1

mica% - +0 9.5 13 14

total mica % of complete - -sample

--.-


fractions +4 -4+8 ·8+20 -20+45 -40+60 -60


weight run g -- 200 200 200 50 ---after exfoliation g -- 160 146 152 45 -wasteg - 160 136 134 37 -micag - Sign 10 18 7 ---moist. or lost % - 20 27 24 10 -weight % 40.5 15 18.8 .12 3.2 16.9

mica % - +0 6 9 14 -total mica % of complete - --sample

Sample number 2821 erams

fractions +4 -4 +8 -8 +20 -20 +45 -45 +60 -60


weight rung - 200 200 200 SO ---after exfoliation g - 163 142 157 35 -wasteg - 163 130 120 27 --micag - sign 10 36 8 -moist. or lost % - 18.5 29 21.5 7.5 -weight % 30.2 20.7 26.2 12 3.3 7.2

mica % - +0 5 18 16 -total mica % of complete ~-- --sample

, -.

fractions +4 +8. ~8 +20 -20 +45 -45 +60 -60 I

fraction weights g -- 1020 1534 541 105 151

weight rung --- 200 200 200 50 ---after exfoliation g --- 195 186 191 46 -wasteg -- 195 171 144 37 ~

micag -- sign 15 . 47 7 --moisture or lost % -- 2.5 9.3 4.5 8 -weight % ---- 28.6 43.1 15.2 2.9 4.2

mica % ---- +0 7.5 23.5 14 --,

total mica % of complete -- --sample


fractions +4 -4+8 -8 +20 -20+45 -45 +60 -60

fraction weights g 649 744 996. 510 156 391

weight run g - 200 200 200 100 -after exfoliation g -- 132 139 161 78 -

waste g - 125 119 139 69 -

micag - 7 20 22 9

moisture or lost % - 34 30.5 19.5 22 ---weight % 18.8 21.5 28.9. 14.7 4.5 11.3

mica % --~ 3.5 10 11 9 -total mica % of complete - --sample

Sanmle number eGG 7 3055 grams

fraction +4 -4+8 ~8 "20 -20 +45 -45 +60 -60 fraction weights g 753 583 697 500 143 371

weight rung - 200 200 200 100 --after exfoliation g - 178 155 165 82 -wasteg -- 178 135 138 69 --micag -- Sign 13 26 13 -moisture or lost % - 12.3 22.5 17.5 18 --weight % 24.6 19 22.8 16.3 4.6 12.1

mica % - +0 6.5 13 13 ---total mica % of complete ---- ----sample

Sample number CC'J(J8

fraction +4 -4+8 -8 +20 -20 +45 -45 +60 -60

fraction weight g 397 757 1260 707 163 248

weight nm g - 200 200 200 100 --after exfoliation g - 196 195 186 94 -wasteg - 196 174 141 82 -micag -- sign 21 45 12 -moisture or lost % --- 2 4 7 6 ---weight % 11.2 21.4 35.6 20 4.6 7

mica % --- +0 12 22 12 -total mica % of complete - --sample

-.~

Sample number CGG9 3245 grams

fractions +4 -4+8 -8 +20 -20 +45 -45 +60 -60 fraction weights g 888 761 942 654 82 161 weightnmg ---- 200 200 200 50 -after exfoliation g -- 193 193 187 47 --waste g -- 193 174 145 39 --micag - SIgn 16 42 6 --moisture or lost % - 3.5 3.5 6.5 6 -weight % 27.4 23.4 29 20.l 2.5 4.9 mica % --- +0 8 21 12 -total mica % of complete ---- -sample

Sample number COOlO 3159 grams

fractions +4 -4+8 -8 +20 -20 +45 -45 +60 -60 fraction weights g 551 734 1025 487 123 253 weight run -- 200 200 200 100 --after exfoliation g - 148 151 157 78 -waste g - 148 135 118 62 ---micag - sign 15 39 16 -moisture or lost % --- 26 24.5 21.5 22 --weight % 17.4 23.2 32.4 15.4 3.8 8

mica % -- +0 7.5 19.5 16 --total mica % of complete -- --sample

Sample number CGGll 3508 grams

fractions +4 -4+8 -8 +20 -20+45 -45 +60 -60 fraction weights g 197 880 1531 635 113 150 weight nm -- 200 200 200 50 ""-

after exfoliation g - 196 196 192 47 -waste g - 196 187 168 43 -micag - SIgn 9 23 4 --moisture or lost % - 2 2 4 6 --weight % 5.6 25.1 43.6 18 3.2 4.2

mica % - +0 4.5 11.5 8 -

total mica % of complete -- -sample


fractions +4 -4+8 -8+20 -20 +45 -45 +60 -60

fraction weight g 145 677 1403 716 166 274

weight rung -- 200 200 200 100 -after exfoliation g -- 197 193 188 94 -wasteg - 197 166 143 80 --micag - SIgn 24 45 14 ---moisture or lost % - 1.5 3.5 6 6 -

weight % 4.3 20 41.6 21.2 4.9 8.1

mica % - +0 12 22.5 14 -total mica % of complete - -sample

Sample number Cool3 3348 grams

fractions +4 -4+8 -8+20 -20 +45 -45 +60 --60 fraction weights g 90 674 1450 730 150 255 weight rung - 200 200 200 100 --after exfoliation g -- 197 197 191 96 -wasteg - 197 190 158 81 -micag - SIgn 10 43 15 -moisture or lost % - 1.5 1.5 4.5 4 --weigbt% 2.7 20 43 21.8 4.4 7.6

mica % - +0 5 21.5 15 --total mica % of complete --sample


fractions +4 4+8 -8 +20 -20+45 -45+60 -60


weight rung - 200 200 200 SO --after exfoliation g -- 196 198 188 46 --wasteg -- 194 181 145 39 -micag - 1 15 43 7 -moisture or lost % - 2 1 21.5 14 --weight % 11.2 31 33.3 153 3.4 5.9

mica % --- 0.5 7.5 21.5 14 ---total mica % of complete -- -sample

Sample number COOlS 3517 grams

fractions +4 -4+8 -8+20 ·20+45 -45 +60 -60


weight rung --- 200 200 200 100 --after exfoliation g - 186 161 179 81 -waste g -- 183 148 127 69 -micag -- 4 12 42 12 -moisture or lost % -- 7 19.5 10.5 19 --weight % 16.1 23.3 33.6 14.2 4 6.8

mica % - 2 6 21 12 -total mica % of complete -- -sample


fractions +4 -4 +8 -8+20 -20 +45 -45+60 -60


weight rung - 200 200 200 100 ---after elCfoliation g - 176 137 145 71 -waste g - 176 95 90 56 -micag - sign 40 55 15 -moisture or lost % - 12 31 27.5 29 --weight % 10.4 19.2 37.2 19.9 4.3 8.6

mica % -- +0 20 27.5 15 -total mica % of complete --- --sample

Sample number eGG17 3461 grams

fractions +4 -4+8 -8 +20 -20+45 -45 +60 -60


weight rung --- 200 200 200 200 ---after exfoliation g -- 198 195 195 196 -wasteg -- 194 169 172 184 -lDlcag - 3 26 23 12 --moisture or lost % -- I 2.5 2.5 2 -weight % 4.1 15.6 31.6 27.2 9.3 11.8

mica % -- 1.5 13 11.5 6 ---total mica % of complete - ----sample


fractions +4 -4+8 ·8 +20 -20 +45 -45 +60 -60


weight rung -- 200 200 200 100 --after exfoliation g - 174 170 170 75 -wasteg -- 169 145 124 60 -micag - 1 25 46 15 --moisture or lost % - 13 15 15 15 -weight % 14.1 20 38 16 4.1 7.8

mica % - 0.5 12.5 23 15 -total mica % of complete - --sample

Sample number CGG19 3420 gram~

fractions +4 -4+8 -8t20 -20+45 45+60 -60 fraction weights g 405 711 1297 611 134 262 weight run g -- 200 200 200 100 --after exfoliation g --- 197 194 190 90 --wasteg - 195 182 158 77 ---rmcag - 1 12 . 32 13 --moisture or lost % - 1.5 3 , 5 10 -weight % 11.8 20.7 38 . 17.8 3.9 7.6

mica % - .5 6 16 13 -total mica % of complete --

. sample

Sample number CGG20 3184 srrams

fractions +4 -4+8 -8+20 -20 +45 -45 +60 -60 fraction weights g 303 964 109$ 478 117 213 weight run g --- 200 200 200 50 --after exfoliation g - 197 194 189 47 --waste g - 197 181 149 40 .--

, micag - sign 13 , 40 7 -moisture or lost % ~ 1.5 3 5.5 6 -weight % 9.5 30.3 34A: 15 3.6 6.6

, mica % - +0 6.5 20 14 -total mica % of complete - --, sample

Sam}:!le number GRADE

fractions

fraction weights g

weight rung -after exfoliation g

wasteg

micag

moisture or lost %

weight %

mica %

total mica % of complete sample

Sample number

fractions

fraction weights g

weight rung

after exfoliation g

wasteg

micag

moisture or lost %

weight %

mica %


CGG19 1 1 arqe

+4

405

--------11.8

--

CGG20

+4

303

----

----9.5

--

3420 grams l - Jq. , _ ..

nuero· _. Sm2 L 3 tled3 . 4

-4+8 -8 +20 -20 +45 ~45 +60 -60

711 1297 6Il 134 262

200 200 200 100 ---197 194 190 90 -195 182 158 77 -1 12 32 13 -1.5 3 5 10 ~--

20.7 38 17.8 3.9 7.6

.5 6 16 13 -

Yield 6.5 to 7.0

3184 grams

-4+8 -8 +20 -20 +45 -45 +UO -60

964 1096 478 117 213

200 200 200 50 --197 194 189 47 ---197 181 149 40 -sign 13 40 7 --1.5 3 5.5 6 -30.3 34.4 15 ·3.6· 6.6

+0- 6.5 20 14 --"

-

Sample number COO21 3631 grams

fractions +4 -4+8 -8 +20 -20 +45 -4S +60 -60


weight rung - 200 200 200 50 -after exfoliation g -- 196 192 189 48 -wasteg - 196 169 146 41 -micag - sign 23 43 7 -moisture or lost % --- 2 4 5.5 4 -weight % 19.6 27.9 31.4 14.5 2.5 3.9

mica % - +0 11.5 21.5 14 . -total mica % of complete --- -sample


fractions +4 -4+8 -8+20 -20+45 -45+60 -60


weight rung -- 200 200 200 50 -after exfoliation g - 193 192 183 46 -waste g - 193 172 141 37 -micag - sign . 20 42 9 -moisture or lost % - 3.5 4 8.5 8 ---weigbt% 14 20.6 34 18.3 3.7 8.6

mica % - +0 10 21 18 --total mica % of complete --- -sample


fractions +4 -4+8 -8+20 -20+45 -45 +60 -60


weight run g - 200 200 200 100 -after exfoliation g - 138 129 154 80 --wasteg --- 138 109 108 56 -D'llcag - sign 20 46 24 -moisture or lost % - 31 35.5 23 20 ---weight % 24.2 22.4 28.4 14.9 35

mica % -- +0 10 23 24 -total mica % of complete - -sample


fractions +4 -4+8 -8 +20 -20 +45 -45 +60 -60


weight rung - 200 200 200 50 -after exfoliation g - 145 150 161 35 --wasteg - 141 130 132 27 --micag -- 3 17 29 7 -moisture or lost % - 27.5 25 19 30 -weight % 23.5 20.1 29.3 13.7 3.7 9.3

mica % - 1.5 8.5 14.5 14 -total mica % of complete sample

Sample number COO27 2281 grams

fractions +4 -4+8 -8 +20 -20+45 -45 +60 -60


weight run g -- 200 200 200 50 -after exfoliation g - ]94 193 189 45 -wasteg -- 194 184 164 39 -micag - sign 10 25 6 -moisture or lost % -- .. 3.5 5.5 10 .J --weight % 14.6 24.6 29.8 18.7 4.6 7.4

mica % - +0 5 12.5 12 -total mica % of complete ---sample


fractions +4 -4+8 -8 +20 -20 +45 -45 +60 -60


weight run g - 200 200 200 50 -after exfoliation g - 196 197 191 48 -waste g - 196 189 175 42 -micag - SIgn 6 16 4 -moisture or lost % - 2 1.5 4.5 4 --weight % 18.2 22.2 26.2 19.7 5 9

mica % -- +0 3 8 8 --total mica % of complete - ----sample


fractions +4 -4+8 -8+20 -20+45 -45 +60 -60


weight rung - 200 200 200 50 -after exfoliation g - 198 198 192 47 -wasteg - 198 191 166 41 -,

micag - sign 7 26 5 -moisture or lost % - 1 1 4 6 --weight % 8.3 28 33.2 : 20.3 4.2 6.9

mica % - +0 3.5 13 10 --total. mica % of complete -- --sample

fractions

fraction weights g

weight run g

after exfoliation g ,

wasteg

micag

moisture or lost % ,

weight %

mica % ,


-,I. ...

1106488 Ontario Limited oIa

.1:li$3:[·]il~1 SAND Be GRAVEL ,

P.O. Box 100, Buckhorn,Ontario KOL 1JO (705) 657-9311 Office (705) 657-9627 Fax E-Mail: [email protected]

. We~J;g~:buckhornsandgravel.com

~.<. F~T. Archibald

'>/0 Cio F.T. Archibald Consulting >::. 668 Milway Ave., :.,' .:... ..' . :"':, Unit #16,·,' •

·.:<:Concord, Ontario L4K 3V6

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GST: #89777

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Comment: Payment In Full Upon Job Completion. 2% over 30 days.

Sold By:

INVOICE 'p "., .. -

Invoice No.:

Date:

Page: '.

. Re: Order No.

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27848

Oct 19, 2006

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1106488 Ontario Limited o/a

SAND & GRAVEL

p.o. Box 100, Buckhorn, Ontario KOL lJO (705) 657-9311 Office (705) 657-9627 Fax E-Mail: [email protected] Wets~~~bPuckhornsandgravel.com

F.T. Archibald

'c/o F.T. Archibald Consulting ,,668 Milway Ave.; ,

Unit #16 C~ncord, Ontario L4K 3V6 'c

GST:#89777

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, Invoice No.:

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Page:

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Ship to:,

F.T. Archibald "RE: GALWAY 2005

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Comment: Payment In Full Upon Job Completion. 2% over 30 days,

Sold By:

27849

Oct 10, 2006

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1106488 Ontario Umited o/a

l:llrij3:[·]il~1 SAND & GRAVEL

P.O. Box 100, Buckhorn, Ontario KOL 1JO

(705) 657-9311 Office (705) 657-9627 Fax E-Mail: [email protected]

WeS~HfO:buckhornsa!ldgravel.com

F.T. Archibald··

clo F.T. Archibald Consulting 668 Milway Ave.; .

• '·.c Unit #16 . . ",

• Concord, Ontario L4K 3V6

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GST: #89777

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Comment: Payment In Full Upon Job Completion. 2% over 30 days.

Sold By:

INVOICE

Invoice No.: 27853

Date:

Page:

Re: Order No.

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PHONE: _______________________ __

PHONE: ______________ _

ORDER INFORMATION

MATERIAL __ J_a..---;--:H_t_CU_Lt...;../...:....·c C=.' ____ _

QUANTITY ___ --'.I_~=-1==D~~. ________ _

REQUESTED DATE ------7''-:--7-1''''-------PRICE QUOUD __ BY _-""Z=-:.~1"__f.:....r-_ .. ____ _ DATE ORDER TAKEN _______________ _

DIRECTIONS

~~~m[3[! P.O. BOX 100 rfA"f0 (tJrcx... ~ LiJ A BUCKHORN, ONTARIO

KOL lJO (70S) 657-9311

I DELIVERY INVOICE NO. : I INVOICE DATE: .Lv. / 2OJP6 J 7. 7t tonnes @ C It Delivery Charge

SUB TOTAL

7% G.S.T. (89777 3073 RT) 8% P.S.T. (on aggregate only) INVOICE TOTAL

TERMS

PAYMENT IN FULL UPON DELIVERY UNLESS ARRANGED

Interest will be charged at the rate of 2% per month on All accounts outstanding over 30 days.

-----....::~'""r~:-:;o-..... f!;9---It.'+---,-r------~ ~." ....... ALL accounts over 60 days will be put into collection

-------f).L~::::--;,:::,;yz~-.:=01.::=J.-..!:~~~~'-.,-::...~~...;..;..-::·.~-"!.3!r-, ~~··~~..,l.i ;:) <~f ~~~~~~~~~~~ over private property, ~ur trucks

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ADDITIONAL INFORMATION

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do so at customer risk.

CUSTOMER: _________________ _

PAYMENT INFORMATION I Received $ __ .....--__ -,--___ ---,= ____ _

cash cheque ...

Received by ______________ _

PIHX • AGGR £GAn UPORl GOLD· flU

,';

. . . . '. .......

;- .

...... . .. ' -

. :-.'~'

.... .... .'.

~:!:~[3~~~~'l1~rn m ADDRESS: ---:Crr1;/O:;--jhh;~1:;;lD:>~:::---(ttfraiJ7A.iT"".f ".rM":;' ·dt20.......--

PHONE: ______________ _ PHONE: ______________ _

MATERIAL __ ~...!:0<::!... ...... ::::..y_,t_;_I..:::C1"I::::::..:L:::· .-.:...(:::~~ ____ _

QUANTrrY ________ ~I=Lo~~~. __________ __ REQUESTED DATE -----r--::-r..,--------PRICE QUOTED BY _.!:J_7_~.=.:~ f:....;r-~,. ____ _

DATE ORDER TAKEN --_________ _

DIRECTIONS I

ADDITIONAL INfORMATION

WHrT£ - CUSTOMER YEllOW - INVOla

.. ~: .... . ' . .- . .... : .' ',' .....

P':!r:1r.tmr:n .. P.O. BOX 100 ~ ..:J o~.:2 -.::JLlJt.t.Ji!.IL:U.!I BUCKHORN, ONTARIO

KOL lJO (70S) 657-9311

I DELIVERY INVOICE NO. : I INVOICE DATE: L / ).&t9h I4:Mtonnes~ It "'-:-' ____ _

Delivery Charge _',-'--____ _

SUB TOTAL 7% G.S.T. (89777 3073 RT) 8% P.S.T. (on aggregate only) INVOICE TOTAL

TERMS I PAYMENT IN fULL UPON DELIVERY UNLESS

ARRANGED Interest will be charged at the rate of 2% per month on ALL accounts outstanding over 30 days. ALL accounts over 60 days will be put into collection - NO EXCEPTIONS. If required to drive over private property, our trucks do so at customer risk.

CUSTOMER: _____________ _

PAYMENT INFORMATION

Received $--=~--~-----;;::=;;o.----cash cheque iIIIl

Received by ______________ _

I OFFICE USE ONLY ____ INV. # ------1 . 1# 3 lit DATE ~

PINK - AGGREGATI REPORT GOLD- flU

. .... ".

' .. : .. ... ......... .

.. ...... :- '. ""'.-.. ' ','-:.

'.;

.' .' ,.

NOTRE NUMERO / OUR NUMBER

DATE

A /i - A~

VENDU A / SOLD TO '£T /-Irr!u fl-r1 / J (hnSu jl~b UVRE A / SHIP TO ~J y,'rl/r:J (-j )c1=>Jbu~ .~~ ./

, ~I

ADRESSE / ADDRESS ADRESSE/ADD:~ __ L . (') P. (hI 7:2. I

I

( t<..:(! k hoo"\, ()/\ --= MO l-rro .J

,;..~t -+i X'/n .... 'u 4 ,.g /J. fJd J.:::1C10() I ( N° D·ENR. DE TAXE IVENDEUR FAB CONDITIONS

IVIA TAX REG. NO. SALESPERSON FOB TERMS

QUANTITE DESCRIPTION

PRIX MONTANT QUANTITY PRICE AMOUNT

II ..... I ( :(')(k~\J WI' nQ ~PP3 £5(£ ocJ

U

I

TPS/GST ,q,~) 00

TVP/PST I~ TOTAL S'(3( II .-

C Blueline' DeB 176 FACTURE - INVOICE

VENDU A I SOLD TO

ADRESSE I ADDRESS

N° D'ENR. DE TAXE TAX REG. NO.

QUANTITE . QUANTITY

[;1 Blueline· DCB 176

NOTRE NUMERO lOUR NUMBER 113205 DATE :funt' J6.lloOlo COMMANDE DU CLIENT I CUSTOMER'S ORDER

VENDEUR SALESPERSON

DESCRIPTION

UVRE A I SHIP TO

Ll f .r-?

( ~j-l;/~g J--e~ \..../ \.. J

FACTURE -INVOICE

\>f-) ,1) ~ \ \ t) -'S\S~£ 6'6 f '0 ~

£OL IJO

PRIX MONTANT PRICE AMOUNT

~Sdt7 -

TPS/GST l5'g~ -TVP/PST

TOTAL )n~ -

VENDU A I SOLD TO

ADRESSE I ADDRESS

N" D'ENR. DE TAXE TAX REG. NO.

QUANTITE QUANTITY

o Blueline' DCB 176

j\

NOTRE NUMERO lOUR NUMBER

DATE

VENOEUR SALESPERSON

DESCRIPTION

--~./ Of\c\u t;nd It-~

~

........--..... \ ~ 1_\n:I1

1./ '-../'"

1

113206

LIVRE A I SHIP TO

FAB FOB

5; ti

I

FACTURE - INVOICE


.. -

-qjfj -I

5"t~ '- --TPS/GST

TVP/PST

TOTAL l5j~~ t- ,.

.... . .

VENDU A I SOLD TO

ADRESSE I ADDRESS

N" D'ENR. DE TAXE TAX REG. NO.

9UANTlTE QUANTITY

[.1 Blueline' DeB 176

-~/ rUCI<:

... ~

NOTRE NUMERO lOUR NUMBER 113210 .-

DATE (!/c.1. /O,tPOO& COMMANDE DU CUENT I CUSTOMER'S ORDER

VENDEUR SALESPERSON

DESCRIPTION

UVAE A I SHIP TO

j::" X .oc£l)"C'

4C{(J i3 - ~ r (}(?;;( ,;ly-OcJ. ft, ,

!J 7 y'{) K#:

,.2 I C; 11(,;..

---".----tJ9'7! /(n.

FACTURE - INVOICE


~ ,70 i9t/co\ -,(0 7() 15"33 ~

--f---..--I-'"

~_71 7C

TPS/GST b[{O~ 7~ TVP/PST

TOTAL D09f 4)

SOUTH

101

......

AMPHIBOLITE GNEISSIC

o &.0

METERS

PLATE 68

101 '101

~I 06,130 06;'28 ~O;:"';28~:s,-_____ ~

NEPH.-AMPHIB.-MARBL 'MICA RICH

DIP 65 SOUTH

,10.0

AMPHIBOLITE GNEISIC

2006

12493385""

TRENCH I

,

PLATE 69

r.'b ... 0 ,

~ ~

SOUTH :..o~ NORTH ~ ..

~. r.'b

- 0 o~

~4! c; ot-I41 ... 0 • 01140 ot-I4I /

V' 06-138 - - - .. --..... '\. .. IMII ~ :$II; / oe-I4I - 1-

"""- OIlaa os-m 06-138 ! ./ ot-I4I ! "1 -

III t-

G~N i III - ~ , MICA i III CRYSTALLIN RICH ~ APf'PHIBOLITIC CARBONATITE 1&1 C[ ..J

MARBLE MARBLE CARBONATITE t:: :J: I RICH ti s.z MICA RICH III z CRYST. ~

It: CRYST. -MARBLE

, ..J

i 0 ..J GREEN MICA ,-'" ('>, -

MARBLE It: MARBLE AMPHIB.-SYENITE MARB.

~ f!! CRYSTALLINE to GNEISSIC AMPHIBOLITE MARBLE GNEISSIC MARBLE CRYSTALLINE MARBLE ~ ,

(1 ,

~ GNEISSIC MICA RICH VUGS DIP 70 SOUTH

It: RED-GREEN MICA LAYERS :i: 0 . MARBLE ~ C[

,

2006

J I , ~24g33a

0 5.0 10.0 METERS

TRENCH 2

-~(hp\) 0. ~:-d/

') PLATE 70

~~ "" ,~... :--- ,.-..... ':'," ,

NORTH sqUTH .... ~

-,/ - • --,. CJ&.I4C ........ •

7 ... B'

II\1II I,", - IlGII "'" ()6.147 ()6.14I ~ .. .. -nil .. ~ \-.. •• ~c

-; ./"" HIlI • I I .

041-180 (I6;.UI1 CEDAR.U .... -c::::. , .......... --~" ~'- ..

• .

"MICA RICH biotite mica rich GNEISSIC RED-PURPLE IRON RI

AMPHIBOLlTIC MARBLE GN SYENITE-AMPHIBOLITE GNEISS AMPHIBOLITE CRYSTALLINE MARBLE CALC.CARB. CRYSTALLINE MARBLE AMPHIBOLITIC MARBLE MARBLE

DIP 65 SOUTH

V SERIES CLAIM 1249345

.

TRENCH # 4 1 J , 0 11.0 10.0

MEmtS

CQ 1<1 (II . ~'-1 '-'\,GI'--I"\l

PLATE 71 ,

SOUTH SWQmp NORTH ..... lIOII .. 7GII ~ - ... 100II

II' MIll 01118 - - IMIII IlOl III ~7 " 118 ..... "- 08-111 I-I

lIOM ...... O&-IM ell! IITnlIW.\ • J ~ , , 1

17TOU8219, 4949412 8PS 17T06tU0741

't_ .a

2, 0c ~". ,...... J

-\ .. :1 ' ',; : "," .

"

SYENITE MICA CARBONATITE MICA RICH GNEISSIC AMPHIB. MARBLE GNEIS AMPHIBOLITE GNEISSIC OLIVINE AMPHIBOlITrE BRECCIA GNEISSIC AMPHIBOLITE

AMPHIB. Attf'H CARBONAT

-

-

I ,

0 11.0 10.0 METERS CLAIM 1249345

TRENCH 7 20~ROGRAM to ",01 ~i\(~ .1 ~

" - - --. - -- -. .- --. .. - - . ~-"---

stripping benefication rpt galway twp · 2017. 1. 16. · county rare earth-potassic mica study...

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