Open File Report 80-4. Bibliography of Geothermal Resource
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Geologic Map of the Simcoe Mountains Volcanic Field, Main Central Segment, Yakama Nation, Washington by Wes Hildreth and Judy Fierstein
Prepared in Cooperation with the Water Resources Program of the Yakama Nation Geologic Map of the Simcoe Mountains Volcanic Field, Main Central Segment, Yakama Nation, Washington By Wes Hildreth and Judy Fierstein Pamphlet to accompany Scientific Investigations Map 3315 Photograph showing Mount Adams andesitic stratovolcano and Signal Peak mafic shield volcano viewed westward from near Mill Creek Guard Station. Low-relief rocky meadows and modest forested ridges marked by scattered cinder cones and shields are common landforms in Simcoe Mountains volcanic field. Mount Adams (elevation: 12,276 ft; 3,742 m) is centered 50 km west and 2.8 km higher than foreground meadow (elevation: 2,950 ft.; 900 m); its eruptions began ~520 ka, its upper cone was built in late Pleistocene, and several eruptions have taken place in the Holocene. Signal Peak (elevation: 5,100 ft; 1,555 m), 20 km west of camera, is one of largest and highest eruptive centers in Simcoe Mountains volcanic field; short-lived shield, built around 3.7 Ma, is seven times older than Mount Adams. 2015 U.S. Department of the Interior U.S. Geological Survey Contents Introductory Overview for Non-Geologists ...............................................................................................1 Introduction.....................................................................................................................................................2 Physiography, Environment, Boundary Surveys, and Access ......................................................6 Previous Geologic -
Flood Basalts and Glacier Floods—Roadside Geology
u 0 by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 WASHINGTON STATE DEPARTMENTOF Natural Resources Jennifer M. Belcher - Commissioner of Public Lands Kaleen Cottingham - Supervisor FLOOD BASALTS AND GLACIER FLOODS: Roadside Geology of Parts of Walla Walla, Franklin, and Columbia Counties, Washington by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 Kaleen Cottingham - Supervisor Division of Geology and Earth Resources WASHINGTON DEPARTMENT OF NATURAL RESOURCES Jennifer M. Belcher-Commissio11er of Public Lands Kaleeo Cottingham-Supervisor DMSION OF GEOLOGY AND EARTH RESOURCES Raymond Lasmanis-State Geologist J. Eric Schuster-Assistant State Geologist William S. Lingley, Jr.-Assistant State Geologist This report is available from: Publications Washington Department of Natural Resources Division of Geology and Earth Resources P.O. Box 47007 Olympia, WA 98504-7007 Price $ 3.24 Tax (WA residents only) ~ Total $ 3.50 Mail orders must be prepaid: please add $1.00 to each order for postage and handling. Make checks payable to the Department of Natural Resources. Front Cover: Palouse Falls (56 m high) in the canyon of the Palouse River. Printed oo recycled paper Printed io the United States of America Contents 1 General geology of southeastern Washington 1 Magnetic polarity 2 Geologic time 2 Columbia River Basalt Group 2 Tectonic features 5 Quaternary sedimentation 6 Road log 7 Further reading 7 Acknowledgments 8 Part 1 - Walla Walla to Palouse Falls (69.0 miles) 21 Part 2 - Palouse Falls to Lower Monumental Dam (27.0 miles) 26 Part 3 - Lower Monumental Dam to Ice Harbor Dam (38.7 miles) 33 Part 4 - Ice Harbor Dam to Wallula Gap (26.7 mi les) 38 Part 5 - Wallula Gap to Walla Walla (42.0 miles) 44 References cited ILLUSTRATIONS I Figure 1. -
Anthropological Study of Yakama Tribe
1 Anthropological Study of Yakama Tribe: Traditional Resource Harvest Sites West of the Crest of the Cascades Mountains in Washington State and below the Cascades of the Columbia River Eugene Hunn Department of Anthropology Box 353100 University of Washington Seattle, WA 98195-3100 [email protected] for State of Washington Department of Fish and Wildlife WDFW contract # 38030449 preliminary draft October 11, 2003 2 Table of Contents Acknowledgements 4 Executive Summary 5 Map 1 5f 1. Goals and scope of this report 6 2. Defining the relevant Indian groups 7 2.1. How Sahaptin names for Indian groups are formed 7 2.2. The Yakama Nation 8 Table 1: Yakama signatory tribes and bands 8 Table 2: Yakama headmen and chiefs 8-9 2.3. Who are the ―Klickitat‖? 10 2.4. Who are the ―Cascade Indians‖? 11 2.5. Who are the ―Cowlitz‖/Taitnapam? 11 2.6. The Plateau/Northwest Coast cultural divide: Treaty lines versus cultural 12 divides 2.6.1. The Handbook of North American Indians: Northwest Coast versus 13 Plateau 2.7. Conclusions 14 3. Historical questions 15 3.1. A brief summary of early Euroamerican influences in the region 15 3.2. How did Sahaptin-speakers end up west of the Cascade crest? 17 Map 2 18f 3.3. James Teit‘s hypothesis 18 3.4. Melville Jacobs‘s counter argument 19 4. The Taitnapam 21 4.1. Taitnapam sources 21 4.2. Taitnapam affiliations 22 4.3. Taitnapam territory 23 4.3.1. Jim Yoke and Lewy Costima on Taitnapam territory 24 4.4. -
Characterization of Ecoregions of Idaho
1 0 . C o l u m b i a P l a t e a u 1 3 . C e n t r a l B a s i n a n d R a n g e Ecoregion 10 is an arid grassland and sagebrush steppe that is surrounded by moister, predominantly forested, mountainous ecoregions. It is Ecoregion 13 is internally-drained and composed of north-trending, fault-block ranges and intervening, drier basins. It is vast and includes parts underlain by thick basalt. In the east, where precipitation is greater, deep loess soils have been extensively cultivated for wheat. of Nevada, Utah, California, and Idaho. In Idaho, sagebrush grassland, saltbush–greasewood, mountain brush, and woodland occur; forests are absent unlike in the cooler, wetter, more rugged Ecoregion 19. Grazing is widespread. Cropland is less common than in Ecoregions 12 and 80. Ecoregions of Idaho The unforested hills and plateaus of the Dissected Loess Uplands ecoregion are cut by the canyons of Ecoregion 10l and are disjunct. 10f Pure grasslands dominate lower elevations. Mountain brush grows on higher, moister sites. Grazing and farming have eliminated The arid Shadscale-Dominated Saline Basins ecoregion is nearly flat, internally-drained, and has light-colored alkaline soils that are Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and America into 15 ecological regions. Level II divides the continent into 52 regions Literature Cited: much of the original plant cover. Nevertheless, Ecoregion 10f is not as suited to farming as Ecoregions 10h and 10j because it has thinner soils. -
Historical and Current Forest and Range Landscapes in the Interior
United States Department of Historical and Current Forest Agriculture Forest Service and Range Landscapes in the Pacific Northwest Research Station United States Interior Columbia River Basin Department of the Interior and Portions of the Klamath Bureau of Land Management General Technical and Great Basins Report PNW-GTR-458 September 1999 Part 1: Linking Vegetation Patterns and Landscape Vulnerability to Potential Insect and Pathogen Disturbances Authors PAUL F. HESSBURG is a research plant pathologist and R. BRION SALTER is a GIS analyst, Pacific Northwest Research Station, Forestry Sciences Laboratory, 1133 N. Western Avenue, Wenatchee, WA 98801; BRADLEY G. SMITH is a quantitative ecologist, Pacific Northwest Region, Deschutes National Forest, 1645 Highway 20 E., Bend, OR 97701; SCOTT D. KREITER is a GIS analyst, Wenatchee, WA; CRAIG A. MILLER is a geographer, Wenatchee, WA; CECILIA H. McNICOLL was a plant ecol- ogist, Intermountain Research Station, Fire Sciences Laboratory, and is currently at Pike and San Isabel National Forests, Leadville Ranger District, Leadville, CO 80461; and WENDEL J. HANN was the regional ecologist, Northern Region, Intermountain Fire Sciences Laboratory, and is currently the National Landscape Ecologist stationed at White River National Forest, Dillon Ranger District, Silverthorne, CO 80498. Historical and Current Forest and Range Landscapes in the Interior Columbia River Basin and Portions of the Klamath and Great Basins Part 1: Linking Vegetation Patterns and Landscape Vulnerability to Potential Insect and Pathogen Disturbances Paul F. Hessburg, Bradley G. Smith, Scott D. Kreiter, Craig A. Miller, R. Brion Salter, Cecilia H. McNicoll, and Wendel J. Hann Interior Columbia Basin Ecosystem Management Project: Scientific Assessment Thomas M. -
Final Environmental Impact Statement and Proposed Land-Use Plan Amendments for the Boardman to Hemingway Transmission Line Proje
B2H Final EIS and Proposed LUP Amendments Appendix H—Visual Resources Supporting Data Appendix H VISUAL RESOURCES SUPPORTING DATA This appendix includes the following: Appendix H1 – Visual Analysis Unit Descriptions - Visual Analysis Unit Descriptions Table - Change in Cultural Modification to the Scenic Quality Rating Units Appendix H2 – Contrast Rating Worksheets - Baker Field Office Visual Contrast Rating Worksheets* - Malheur Field Office Visual Contrast Rating Worksheets* - Owyhee Field Office Visual Contrast Rating Worksheets* - Additional Visual Contrast Rating Worksheets Appendix H3 – Photo Simulations - Photo Simulations from Visual Resource Report 1 - Additional Photo Simulations *NOTE: For the Final Environmental Impact Statement, additional route variations have been analyzed. As a result, certain routes analyzed for the Draft Environmental Impact Statement have been renamed. They are as follows: Proposed Action changed to Applicant’s Proposed Action Alternative Burnt River Alternative to Flagstaff A – Burnt River Alternative Flagstaff Hill to Flagstaff A Alternative Double Mountain Alternative to Variation S5-B2 H-1 This page intentionally left blank. B2H Final EIS and Proposed LUP Amendments Appendix H1—Visual Analysis Unit Descriptions Appendix H1 VISUAL ANALYSIS UNIT DESCRIPTIONS The Visual Analysis Unit (VAU) descriptions are provided in Table H1-1, which includes an overall description of each VAU within the B2H Project area for visual resources. The descriptions of the units include information about the landforms, topography, water, and vegetation within the units, as well as other features and information. The VAUs are identified by two digits, followed by three numbers, and a unit name. The two digits represent the BLM field office or resource area in which the unit is located (BR=Border Resource Area; CE=Central Oregon Resource Area; BA=Baker Resource Area; MA=Malheur Resource Area; OW=Owyhee Field Office; FR=Four Rivers Field Office). -
Summary of the Columbia Plateau Regional Aquifer-System Analysis, Washington, Oregon, and Idaho
SUMMARY OF THE COLUMBIA PLATEAU REGIONAL AQUIFER-SYSTEM ANALYSIS, WASHINGTON, OREGON, AND IDAHO PROFESSIONAL PAPER 1413-A USGS tience for a changing world Availability of Publications of the U.S. Geological Survey Order U.S. Geological Survey (USGS) publications from the Documents. Check or money order must be payable to the offices listed below. Detailed ordering instructions, along with Superintendent of Documents. Order by mail from prices of the last offerings, are given in the current-year issues of the catalog "New Publications of the U.S. Geological Superintendent of Documents Survey." Government Printing Office Washington, DC 20402 Books, Maps, and Other Publications Information Periodicals By Mail Many Information Periodicals products are available through Books, maps, and other publications are available by mail the systems or formats listed below: from Printed Products USGS Information Services Box 25286, Federal Center Printed copies of the Minerals Yearbook and the Mineral Com Denver, CO 80225 modity Summaries can be ordered from the Superintendent of Publications include Professional Papers, Bulletins, Water- Documents, Government Printing Office (address above). Supply Papers, Techniques of Water-Resources Investigations, Printed copies of Metal Industry Indicators and Mineral Indus Circulars, Fact Sheets, publications of general interest, single try Surveys can be ordered from the Center for Disease Control copies of permanent USGS catalogs, and topographic and and Prevention, National Institute for Occupational Safety and thematic maps. Health, Pittsburgh Research Center, P.O. Box 18070, Pitts burgh, PA 15236-0070. Over the Counter Mines FaxBack: Return fax service Books, maps, and other publications of the U.S. Geological Survey are available over the counter at the following USGS 1. -
Primitive Magmas at Five Cascade Volcanic Fields 413
397 The Canadian M ine ralo g i st Vol. 35, pp. 397423 (1997) PRIMITIVEMAGMAS AT FIVECASCADE VOLCANIC FIELDS: MELTSFROM HOT, HETEROGENEOUS SUB.ARC MANTLE CHARLES R. BACONI, PEGGY E. BRUGGMAN, ROBERT L. CHRISTIANSEN, MICHAEL A. CLYNNE" JULIE M. DONNELLY-NOLAN ANDWES HILDRETH U.S.Geological Survey, 345 Mitdl.efield Road" Mmlo Parh Califurnia94025-3591,U.SA. ABSTRACT Major and trace elementconcenftations, including REE by isotopedilution, and Sr, Nd, Pb, and O isotoperatios have been determinedfor 38 mafic lavasfrom the Mount Adams,Crater Lake, Mount ShastaMedicine Lake, and Lassenvolcanic flelds, in the Cascadearc, northwestempart of the United States.Many of the sampleshave a high Mg# tl@Mg/(Mg + FeD > 601and Ni content(>140 ppm) suchthat we considerthem to be primitive. We rccognlzerhree end-member p:,jmillrve magma groups in the Cascades,characterized mainly by their trace-elementand alkali-metal abundances:(1) High-alumina olivine tholeiite (HAOT) hastrace element abundaaces similarto N-MORB, exceptfor slightly elevatedLllE, andhas Eu/Eu* > 1. (2) Arc basalt andbasaltic andesite have notably higher L/lE contents,generally have higher SiO2contents, are more oxidized andhave higher Cr for a given Ni abundancethan HAOT. Theselavas show relative depletioninl/F.i4 havelowerl/ftEE andhigherl,ftEEthan HAOT, andhave smallerEulEu* (0.94-1.06).(3) Alkali basaltfrom the Simcoevolcanic field eastof Mount Adamsreprcsents the third end-membr, which contributesan intraplate geochemicalsigpature to magna compositions.Notable geochemical featuresamong -
GEOLOGIC MAP of the MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE of SOUTHERN WASHINGTON by Wes Hildreth and Judy Fierstein
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-2460 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE OF SOUTHERN WASHINGTON By Wes Hildreth and Judy Fierstein When I climbed Mount Adams {17-18 August 1945] about 1950 m (6400') most of the landscape is mantled I think I found the answer to the question of why men by dense forests and huckleberry thickets. Ten radial stake everything to reach these peaks, yet obtain no glaciers and the summit icecap today cover only about visible reward for their exhaustion... Man's greatest 2.5 percent (16 km2) of the cone, but in latest Pleis experience-the one that brings supreme exultation tocene time (25-11 ka) as much as 80 percent of Mount is spiritual, not physical. It is the catching of some Adams was under ice. The volcano is drained radially vision of the universe and translating it into a poem by numerous tributaries of the Klickitat, White Salmon, or work of art ... Lewis, and Cis pus Rivers (figs. 1, 2), all of which ulti William 0. Douglas mately flow into the Columbia. Most of Mount Adams and a vast area west of it are Of Men and Mountains administered by the U.S. Forest Service, which has long had the dual charge of protecting the Wilderness Area and of providing a network of logging roads almost INTRODUCTION everywhere else. The northeast quadrant of the moun One of the dominating peaks of the Pacific North tain, however, lies within a part of the Yakima Indian west, Mount Adams, stands astride the Cascade crest, Reservation that is open solely to enrolled members of towering 3 km above the surrounding valleys. -
Iron Horse State Park Master Plan Addendum Iron Horse Palouse – Malden to Idaho Border
MASTER PLAN IRON HORSE STATE PARK MASTER PLAN ADDENDUM IRON HORSE PALOUSE – MALDEN TO IDAHO BORDER WASHINGTON STATE PARKS AND RECREATION COMMISSION Approved March 27, 2014 TABLE OF CONTENTS CHAPTER 1: INTRODUCTION ......................................................................................................................... 1 PURPOSE ................................................................................................................................................... 1 STUDY AREA .............................................................................................................................................. 1 RECREATION USE ...................................................................................................................................... 3 RECREATION SERVICE AREA ...................................................................................................................... 3 CHAPTER 2: EXISTING CONDITIONS .............................................................................................................. 5 STUDY APPROACH ..................................................................................................................................... 5 LAND OWNERSHIP .................................................................................................................................... 5 EXISTING BRIDGES ..................................................................................................................................... 5 REMOVED BRIDGES -
Land Use Variation on Mid-Columbia Plateau Upland and Lowland Archaeology Sites
Central Washington University ScholarWorks@CWU All Master's Theses Master's Theses Spring 2016 Land Use Variation on Mid-Columbia Plateau Upland and Lowland Archaeology Sites Cathy J. Anderson Central Washington University, [email protected] Follow this and additional works at: https://digitalcommons.cwu.edu/etd Part of the Anthropology Commons, and the Geography Commons Recommended Citation Anderson, Cathy J., "Land Use Variation on Mid-Columbia Plateau Upland and Lowland Archaeology Sites" (2016). All Master's Theses. 385. https://digitalcommons.cwu.edu/etd/385 This Thesis is brought to you for free and open access by the Master's Theses at ScholarWorks@CWU. It has been accepted for inclusion in All Master's Theses by an authorized administrator of ScholarWorks@CWU. For more information, please contact [email protected]. LAND USE VARIATION ON MID-COLUMBIA PLATEAU UPLAND AND LOWLAND ARCHAEOLOGY SITES A Thesis Presented to The Graduate Faculty Central Washington University In Partial Fulfillment of the Requirements for the Degree Master of Science Resource Management By Cathy Jean Anderson June 2016 i CENTRAL WASHINGTON UNIVERSITY Graduate Studies We here by approve the thesis of Cathy Jean Anderson Candidate for the degree of Master of Science APPROVED FOR THE GRADUATE FACULTY ______________ __________________________________________ Dr. Patrick T. McCutcheon, Committee Chair ______________ __________________________________________ Dr. Steven Hackenberger ______________ __________________________________________ Dr. Craig S. Revels ______________ __________________________________________ Dr. Kevin Archer, Dean of Graduate Studies ii ABSTRACT LAND USE VARIATION ON MID-COLUMBIA PLATEAU UPLAND AND LOWLAND ARCHAEOLOGY SITES by Cathy Jean Anderson June 9, 2016 Investigators of the Mid-Plateau archaeological record have interpreted artifact deposits in their environmental settings as evidence of human land use labeled as site types. -
IC-62, Heat Flow Studies in the Steamboat Mountain-Lemei Rock
,. \\ :\ .J ~\ .... 7 \; t,6 i u2 W~~fnffl:RY u.no C ';I, .... DEPARTMENT OF NATURAL RESOURCES i n BERT L. COLE, Commissioner of Public Lands ; RALPH A. BESWICK Supervisor I: s DIVISION OF GEOLOGY AND EARTH RESOURCES VAUGHN E. LIVINGSTON, JR., State Geologist INFORMATION CIRCULAR 62 HEAT FLOW STUDIES IN THE STEAMBOAT MOUNTAIN-LEMEI ROCK AREA, SKAMANIA COUNTY, WASHINGTON BY J. ERIC SCHUSTER, DAVID D. BLACKWELL, PAUL E. HAMMOND, and MARSHALL T. HUNTTING Final report to the NATIONAL SCIENCE FOUNDATION on sponsored proiect AER75 ... 02747 1978 STATE OF WASHINGTON DEPARTMENT OF NATURAL RESOURCES BERT L COLE, Commissioner of Public Lands RALPH A. BESWICK Supervisor DIVISION OF GEOLOGY AND EARTH RESOURCES VAUGHN E. LIVINGSTON, JR., State Geologist INFORMATION CIRCULAR WA He<1.t iluw 33.J. -7 stu.diei::,; ln the .M6 t> i Stean, l:on. t --- bJ. ~uu,i ta i u-.Lem~ i 1970 Jiuck d.rea, Skaina11ia Cuunt),, W a i'ii1 i u ~ton HEAT FLOW STUDIES IN THE STEAMBOAT MOUNTAIN-LEMEI ROCK AREA, SKAMANIA COUNTY, WASHINGTON BY J. ERIC SCHUSTER, DAVID D. BLACKWELL, PAUL E. HAMMOND, and MARSHALL T. HUNTTING Final report to the NATIONAL SC !ENCE FOUNDATION on sponsored project AER75-02747 1978 CONTENTS Abstract ................. , . .. .. .. .. .. .. .. .. .. 1 Introduction ..................................................................... , • . 2 Acknowledgments • • • • • • . • • . • . • • . • . • . • . • . • . • • • • • • . • • • • . • . 3 Geo logy • . • • • • • • . • • • • • • . • • . • • . • . • . • • . • . 4 Genera I features ............................