gtilo-2 geothermal information layer for oregon ds...geothermal information layer for oregon —...

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GEOTHERMAL INFORMATION LAYER FOR OREGON — RELEASE 2 2012 35.1°C (95.18°F) – 121°C (249.8°F) low-temperature well ≤18.3°C (64.9°F) low-temperature well 20.1°C (68.18°F) – 35°C (95°F) low-temperature well 18.31°C (64.9°F) – 20°C (68°F) low-temperature well Temperature not available or reported 35.1°C (95.18°F) – 99°C (210.2°F) thermal spring ≤18.3°C (64.9°F) thermal spring 20.1°C (68.18°F) – 35°C (95°F) thermal spring 18.31°C (64.9°F) – 20°C (68°F) thermal spring Spring temperature not available 35.1°C (95.18°F) – 121°C (249.8°F) geothermal prospect well ≤18.3°C (64.9°F) geothermal prospect well 20.1°C (68.18°F) – 35°C (95°F) geothermal prospect well 18.31°C (64.9°F) – 20°C (68°F) geothermal prospect well Temperature not available or reported 182.9°C (361.22°F) – 294°C (561.2°F) geothermal well ≤47.2°C (116.96°F) geothermal well 107.2°C (224.96°F) – 182.8°C (361.04°F) geothermal well 47.3°C (117.14°F) – 107.1°C (224.78°F) geothermal well Temperature not available or reported Geothermal Wells (maximum temperature reported) EXPLANATION OF MAP UNITS Thermal Springs (maximum temperature reported) Low-Temperature Wells (maximum temperature reported) Geothermal Prospect Wells (maximum temperature reported) INTRODUCTION The Geothermal Information Layer for Oregon (GTILO) is the Oregon Department of Geology and Mineral Industries (DOGAMI) geospatial database system that currently stores and manages Oregon's geothermal resource information. In this release of GTILO (GTILO-Release 2), there are two Esri shapfiles called GTILO-2_Geothermalspring_database and GTILO-2_Geothermalwell_database. A brief description of the data each shapefile contains is provided below. This map displays these data and shows those areas in Oregon that either have been investigated for geothermal resource potential or show potential for a geo- thermal resource. Please read each shapefile’s metadata and visit http://www.oregongeology.org for addi- tion details. GTILO-2_Geothermalspring_database: Hot and Warm Springs There are 690 points on this map that represent Oregon’s thermal springs. These springs are produced by the emergence of geothermally heated groundwater and defined in most cases as those having tempera- tures greater than 20°C (68°F), or a minimum temperature of 10°C (50°F) above mean annual air tem- perature. This database also lists springs with temperature information listed only as “warm” or “hot” and springs having temperatures greater than 18.3°C (65°F) information. Understand that there is no univer- sally accepted definition of a thermal spring. A characteristic of thermal springs in Oregon is that they usually represent a group of affiliated springs. In previous studies, it was customary to count each spring group but not every spring in that group. Where possible, we counted each spring in a group but only when several spring locations, which would have been otherwise included in a group, were separately shown on a U.S. Geological Survey 1:24,000-scale quad- rangle map or indicated in some other previous studies. GTILO-2_Geothermalwell_database: Low-Temperature Wells There are 4,344 points shown on this map that represent various types of low-temperature wells (e.g., domestic/irrigation/other water supply wells) throughout Oregon. Low-temperature wells are defined as those wells within which there is water in the borehole having a temperature greater than 18.3°C (65°F) or a minimum temperature of slightly less than 10°C above mean annual air temperature, and wells that are at least 60 ft (18.3 m) deep. Understand that there is no universally accepted definition for a low- temperature well, in terms of the temperature of the water that it contains or depth that it was drilled. Water temperature is reported by the driller; the means by which it was acquired is entirely unknown. Geothermal Prospect Wells There are 1,019 points on this map that represent geothermal prospect wells in Oregon. A geothermal prospect well is defined as any well drilled as a geophysical test well, seismic shot hole, mineral explora- tion drilling, core drilling, or temperature gradient test well, less than 2,000 ft (667 m) in depth, and drilled in prospecting for geothermal resources. Geothermal Wells Sixty-six boreholes were drilled as geothermal wells for producing geothermal resources and includes any geothermal re-injection wells. Data Sources The data depicted on this map are attributed partly to the following sources: See the metadata files for more detailed source information. Data Access Free access to data used in GTILO—Release 2 can be obtained at http://repository.usgin.org/collection. Please contact the Nature of the Northwest Information Center to purchase GTILO—Release 2. Understand that these data are provided “as-is” without warranty of any kind, including, but not limited to, the implied warranties of merchantability and fitness for a particular purpose. The user assumes all responsibility for the accuracy and suitability of these data for a specific application. In no event will the Oregon Department of Geology and Mineral Industries be liable for any damages, including lost profits, lost savings, or other incidental or consequential damages arising from the use of or inability to use the data. Geo-Heat Center Western States Geothermal Databases CD-ROM. Geothermal Areas Database of the U.S. Geothermal information from the United States Geological Survey (USGS) online database. Southern Methodist University (SMU) Geothermal Laboratory online database. Great Basin Center for Geothermal Research, University of Nevada, Reno, online database. University of Idaho, Department of Geological Sciences, Moscow, Idaho. United States Geological Survey Geographic Names Information System and National Hydrography Dataset. DOGAMI Mineral Land Reclamation and Regulation program, Albany, Oregon, files of geothermal prospect permits and geothermal well permits. Oregon Water Resources Division (OWRD) water well database. DOGAMI unpublished and published geothermal reports, maps, and databases, accuracy of which varies according to the original source(s). 124°0'0''W 123°0'0''W 122°0'0''W 121°0'0''W 120°0'0''W 119°0'0''W 118°0'0''W 117°0'0''W 124°0'0''W 125°0'0''W 123°0'0''W 122°0'0''W 121°0'0''W 120°0'0''W 119°0'0''W 118°0'0''W 117°0'0''W 42°0'0''N 43°0'0''N 44°0'0''N 45°0'0''N 46°0'0''N 42°0'0''N 43°0'0''N 44°0'0''N 45°0'0''N 46°0'0''N Map Projection Information: Projection: Lambert Conformal Conic Units: International Feet Central Meridian: -121.00 Standard Parallel: 1: 43.00 Standard Parallel: 2: 45.5 Latitude of Oregon: 42.00 Datum: North American 1983 For copies of this publication contact: Nature of the Northwest Information Center 800 NE Oregon Street, #28, Ste. 965 Portland, Oregon 97232 telephone (971) 673-2331 http://www.natureNW.org GTILO—Release 2 compiled by Clark A. Niewendorp, Tracy R. Ricker, Kelley W. Rabjohns, and Shane H. Brodie Oregon Department of Geology and Mineral Industries 2012 10 20 30 40 50 KILOMETERS SCALE 1:500 000 0 1 0 0 1 20 30 40 MILES O R E G O N D E P A R T M E N T O F G E O L O G Y A N D M I N E R A L I N D U S T R I E S 1 9 3 7 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES www.OregonGeology.org Larry Givens, Governing Board Chair Vicki S. McConnell, Director and State Geologist Andree V. Pollock, Assistant Director, Geologic Survey and Services Rachel R. Lyles Smith, Project Operations Manager Ian P. Madin, Chief Scientist NOTICE This map cannot serve as a substitute for site-specific investigations by qualified practitioners. Site-specific data may give results that differ from those shown on the map. The views and conclusions contained in this document are those of the authors. GEOTHERMAL INFORMATION LAYER FOR OREGON — RELEASE 2 (GTILO — Release 2) By Clark A. Niewendorp, Tracy R. Ricker, Kelley W. Rabjohns, and Shane H. Brodie PLATE 1 LEGEND Interstate freeway U.S. highway State highway 5 99 62 County boundary City/town 10 0 Bend Eugene Ashland Klamath Falls Ontario Paisley Lakeview Adel Burns Salem Portland The Dalles Madras Hermiston Pendleton La Grande Baker City Albany Roseburg Fields LANE WASHINGTON MULTNOMAH YAMHILL DOUGLAS CURRY BAKER JOSEPHINE KLAMATH COOS DESCHUTES CROOK HARNEY LAKE MALHEUR UNION UMATILLA WALLOWA GRANT LINN WASCO SHERMAN HOOD RIVER GILLIAM MORROW CLACKAMAS JEFFERSON WHEELER TILLAMOOK LINCOLN BENTON POLK COLUMBIA CLATSOP JACKSON Marion 5 84 5 84 5 84 101 101 101 95 95 97 395 20 20 97 197 199 20 20 26 30 53 6 202 47 18 18 22 22 99W 99W 223 223 99E 221 47 211 26 26 35 22 58 126 138 138 99 38 42 227 62 62 66 140 99 140 31 140 26 26 26 395 395 395 97 19 206 19 218 74 74 207 244 204 11 82 3 86 30 205 395 X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 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Page 1: GTILO-2 Geothermal Information Layer for Oregon DS...GEOTHERMAL INFORMATION LAYER FOR OREGON — RELEASE 2 2012 35.1°C (95.18°F) – 121°C (249.8°F) low-temperature well ≤18.3°C

GEOTHERMAL INFORMATION LAYER FOR OREGON — RELEASE 22012

35.1°C (95.18°F) – 121°C (249.8°F) low-temperature well

≤18.3°C (64.9°F) low-temperature well

20.1°C (68.18°F) – 35°C (95°F) low-temperature well

18.31°C (64.9°F) – 20°C (68°F) low-temperature well

Temperature not available or reported

35.1°C (95.18°F) – 99°C (210.2°F) thermal spring

≤18.3°C (64.9°F) thermal spring

20.1°C (68.18°F) – 35°C (95°F) thermal spring

18.31°C (64.9°F) – 20°C (68°F) thermal spring

Spring temperature not available

35.1°C (95.18°F) – 121°C (249.8°F) geothermal prospect well

≤18.3°C (64.9°F) geothermal prospect well

20.1°C (68.18°F) – 35°C (95°F) geothermal prospect well

18.31°C (64.9°F) – 20°C (68°F) geothermal prospect well

Temperature not available or reported

182.9°C (361.22°F) – 294°C (561.2°F) geothermal well

≤47.2°C (116.96°F) geothermal well

107.2°C (224.96°F) – 182.8°C (361.04°F) geothermal well

47.3°C (117.14°F) – 107.1°C (224.78°F) geothermal well

Temperature not available or reported

Geothermal Wells(maximum temperature reported)

EXPLANATION OF MAP UNITS

Thermal Springs(maximum temperature reported)

Low-Temperature Wells(maximum temperature reported)

Geothermal Prospect Wells(maximum temperature reported)

INTRODUCTION

The Geothermal Information Layer for Oregon (GTILO) is the Oregon Department of Geology and Mineral Industries (DOGAMI) geospatial database system that currently stores and manages Oregon's geothermal resource information. In this release of GTILO (GTILO-Release 2), there are two Esri shapfiles called GTILO-2_Geothermalspring_database and GTILO-2_Geothermalwell_database. A brief description of the data each shapefile contains is provided below. This map displays these data and shows those areas in Oregon that either have been investigated for geothermal resource potential or show potential for a geo-thermal resource. Please read each shapefile’s metadata and visit http://www.oregongeology.org for addi-tion details.

GTILO-2_Geothermalspring_database:

Hot and Warm SpringsThere are 690 points on this map that represent Oregon’s thermal springs. These springs are produced by the emergence of geothermally heated groundwater and defined in most cases as those having tempera-tures greater than 20°C (68°F), or a minimum temperature of 10°C (50°F) above mean annual air tem-perature. This database also lists springs with temperature information listed only as “warm” or “hot” and springs having temperatures greater than 18.3°C (65°F) information. Understand that there is no univer-sally accepted definition of a thermal spring.

A characteristic of thermal springs in Oregon is that they usually represent a group of affiliated springs. In previous studies, it was customary to count each spring group but not every spring in that group. Where possible, we counted each spring in a group but only when several spring locations, which would have been otherwise included in a group, were separately shown on a U.S. Geological Survey 1:24,000-scale quad-rangle map or indicated in some other previous studies.

GTILO-2_Geothermalwell_database:

Low-Temperature WellsThere are 4,344 points shown on this map that represent various types of low-temperature wells (e.g., domestic/irrigation/other water supply wells) throughout Oregon. Low-temperature wells are defined as those wells within which there is water in the borehole having a temperature greater than 18.3°C (65°F) or a minimum temperature of slightly less than 10°C above mean annual air temperature, and wells that are at least 60 ft (18.3 m) deep. Understand that there is no universally accepted definition for a low-temperature well, in terms of the temperature of the water that it contains or depth that it was drilled. Water temperature is reported by the driller; the means by which it was acquired is entirely unknown.

Geothermal Prospect WellsThere are 1,019 points on this map that represent geothermal prospect wells in Oregon. A geothermal prospect well is defined as any well drilled as a geophysical test well, seismic shot hole, mineral explora-tion drilling, core drilling, or temperature gradient test well, less than 2,000 ft (667 m) in depth, and drilled in prospecting for geothermal resources.

Geothermal WellsSixty-six boreholes were drilled as geothermal wells for producing geothermal resources and includes any geothermal re-injection wells.

Data Sources

The data depicted on this map are attributed partly to the following sources:

See the metadata files for more detailed source information.

Data Access

Free access to data used in GTILO—Release 2 can be obtained at http://repository.usgin.org/collection. Please contact the Nature of the Northwest Information Center to purchase GTILO—Release 2.

Understand that these data are provided “as-is” without warranty of any kind, including, but not limited to, the implied warranties of merchantability and fitness for a particular purpose. The user assumes all responsibility for the accuracy and suitability of these data for a specific application. In no event will the Oregon Department of Geology and Mineral Industries be liable for any damages, including lost profits, lost savings, or other incidental or consequential damages arising from the use of or inability to use the data.

• Geo-Heat Center Western States Geothermal Databases CD-ROM. • Geothermal Areas Database of the U.S. • Geothermal information from the United States Geological Survey (USGS) online database. • Southern Methodist University (SMU) Geothermal Laboratory online database.• Great Basin Center for Geothermal Research, University of Nevada, Reno, online database. • University of Idaho, Department of Geological Sciences, Moscow, Idaho. • United States Geological Survey Geographic Names Information System and National Hydrography

Dataset. • DOGAMI Mineral Land Reclamation and Regulation program, Albany, Oregon, files of geothermal

prospect permits and geothermal well permits. • Oregon Water Resources Division (OWRD) water well database. • DOGAMI unpublished and published geothermal reports, maps, and databases, accuracy of which

varies according to the original source(s).

124°0'0''W 123°0'0''W 122°0'0''W 121°0'0''W 120°0'0''W 119°0'0''W 118°0'0''W 117°0'0''W

124°0'0''W125°0'0''W 123°0'0''W 122°0'0''W 121°0'0''W 120°0'0''W 119°0'0''W 118°0'0''W 117°0'0''W

42°0'0''N

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Map Projection Information:Projection: Lambert Conformal ConicUnits: International FeetCentral Meridian: -121.00Standard Parallel: 1: 43.00Standard Parallel: 2: 45.5Latitude of Oregon: 42.00Datum: North American 1983

For copies of this publication contact:Nature of the Northwest Information Center

800 NE Oregon Street, #28, Ste. 965Portland, Oregon 97232

telephone (971) 673-2331http://www.natureNW.org

GTILO—Release 2 compiled by Clark A. Niewendorp,Tracy R. Ricker, Kelley W. Rabjohns, and Shane H. Brodie Oregon Department of Geology and Mineral Industries201210 20 30 40 50 KILOMETERS

SCALE 1:500 00001001 20 30 40 MILES

OR

EG

ON

DE

PA

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ENT O F GE O L O G Y A NDM IN

ER

AL

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US

TR

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1937

STATE OF OREGONDEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIESwww.OregonGeology.orgLarry Givens, Governing Board ChairVicki S. McConnell, Director and State GeologistAndree V. Pollock, Assistant Director, Geologic Survey and ServicesRachel R. Lyles Smith, Project Operations Manager Ian P. Madin, Chief Scientist

NOTICE

This map cannot serve as a substitute for site-specific investigations by qualified practitioners. Site-specific data may give results that differ from those shown on the map.

The views and conclusions contained in this document are those of the authors.

GEOTHERMAL INFORMATION LAYER FOR OREGON — RELEASE 2

(GTILO — Release 2)

By Clark A. Niewendorp, Tracy R. Ricker, Kelley W. Rabjohns, and Shane H. Brodie

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