ORIGIN and MEANING of the GEOGRAPHIC NAME PALOUSE in Eastern Washington and Western Idaho, North of the Snake and Clearwater
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Washington Division of Geology and Earth Resources Open File Report
RECONNAISSANCE SURFICIAL GEOLOGIC MAPPING OF THE LATE CENOZOIC SEDIMENTS OF THE COLUMBIA BASIN, WASHINGTON by James G. Rigby and Kurt Othberg with contributions from Newell Campbell Larry Hanson Eugene Kiver Dale Stradling Gary Webster Open File Report 79-3 September 1979 State of Washington Department of Natural Resources Division of Geology and Earth Resources Olympia, Washington CONTENTS Introduction Objectives Study Area Regional Setting 1 Mapping Procedure 4 Sample Collection 8 Description of Map Units 8 Pre-Miocene Rocks 8 Columbia River Basalt, Yakima Basalt Subgroup 9 Ellensburg Formation 9 Gravels of the Ancestral Columbia River 13 Ringold Formation 15 Thorp Gravel 17 Gravel of Terrace Remnants 19 Tieton Andesite 23 Palouse Formation and Other Loess Deposits 23 Glacial Deposits 25 Catastrophic Flood Deposits 28 Background and previous work 30 Description and interpretation of flood deposits 35 Distinctive geomorphic features 38 Terraces and other features of undetermined origin 40 Post-Pleistocene Deposits 43 Landslide Deposits 44 Alluvium 45 Alluvial Fan Deposits 45 Older Alluvial Fan Deposits 45 Colluvium 46 Sand Dunes 46 Mirna Mounds and Other Periglacial(?) Patterned Ground 47 Structural Geology 48 Southwest Quadrant 48 Toppenish Ridge 49 Ah tanum Ridge 52 Horse Heaven Hills 52 East Selah Fault 53 Northern Saddle Mountains and Smyrna Bench 54 Selah Butte Area 57 Miscellaneous Areas 58 Northwest Quadrant 58 Kittitas Valley 58 Beebe Terrace Disturbance 59 Winesap Lineament 60 Northeast Quadrant 60 Southeast Quadrant 61 Recommendations 62 Stratigraphy 62 Structure 63 Summary 64 References Cited 66 Appendix A - Tephrochronology and identification of collected datable materials 82 Appendix B - Description of field mapping units 88 Northeast Quadrant 89 Northwest Quadrant 90 Southwest Quadrant 91 Southeast Quadrant 92 ii ILLUSTRATIONS Figure 1. -
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. -
Palouse River Tributaries Subbasin Assessment and TMDL
Palouse River Tributaries Subbasin Assessment and TMDL Idaho Department of Environmental Quality January 2005 This Page Intentionally Left Blank. Palouse River Tributaries Subbasin Assessment and TMDL January 2005 Prepared by: Robert D. Henderson Lewiston Regional Office Idaho Department of Environmental Quality 1118 F. Street Lewiston, ID 83501 This Page Intentionally Left Blank. Palouse River Tributaries Subbasin Assessment and TMDL January 2005 Acknowledgments Completing this Subbasin Assessment and TMDL would not have been possible without the support of the following individuals and organizations: • Mark Shumar • Alan Monek • Brock Morgan • Barbara Anderson • Dennis Meier • Palouse River Watershed Advisory Group • Tom Dechert • Cary Myler • Jason Fales • William Kelly • John Cardwell • Ken Clark • Bill Dansart • Richard Lee • John Gravelle • Marti Bridges • Daniel Stewart Thank you! Cover photo by Robert D. Henderson i Palouse River Tributaries Subbasin Assessment and TMDL January 2005 This Page Intentionally Left Blank. ii Palouse River Tributaries Subbasin Assessment and TMDL January 2005 Table of Contents Abbreviations, Acronyms, and Symbols .......................................................xiii Executive Summary........................................................................................xvii Subbasin at a Glance .................................................................................................xvii Key Findings ............................................................................................................. -
Power System
HISTORY AND CURRENT STATUS OF THE ELECTRICITY INFRASTRUCTURE IN THE PACIFIC NORTHWEST Kevin Schneider Ph.D., P.E. Chair, Seattle Chapter of the IEEE PES IEEE PES SCHOLARSHIP PLUS INITIATIVE 2 Washington State PES Scholars • Patrick Berg, Seattle University • Parichehr Karimi, University of • Zachary Burrows, Eastern Washington Washington UiUnivers ity • TiTravis Kinney, WhitWashington Sta te UiUnivers ity • Erin Clement, University of Washington • Allan Koski, Eastern Washington University • Anastasia Corman, University of • Kyle Lindgren, University of Washington, Washington • John Martinsen, Washington State • Gwendolyn Crabtree, Washington State University University • Melissa Martinsen, University of • David Dearing, Washington State Washington University • JthJonathan NhiNyhuis, SttlSeattle PifiPacific UiUnivers ity • Terra Donley, Gonzaga University Derek Jared Pisinger, Washington State Gowrylow, Seattle University University • Sanel Hirkic, Washington State University • Douglas Rapier, Washington State • Nathan Hirsch, Eastern Washington University University • Chris Rusnak, Washington State University • John Hofman, Washington State • Kaiwen Sun, University of Washington University • Joshua Wu, Seattle University • • Tracy Yuan, University of Washington 3 OVERVIEW Part 1: The Current Status of the Electricity Infrastructure in the Pacific North west Part 2: How the Current System Evolved Over Time Part 3: Current Challenges and the Path Forward Part 4: Concluding Comments PART 1:: THE CURRENT STATUS OF THE ELECTRICITY INFRASTRUCTURE -
Syllable Structure in Umatilla Sahaptin* Tymoteusz Alan Chrzanowski
Syllable Structure in Umatilla Sahaptin* Tymoteusz Alan Chrzanowski A thesis submitted in partial fulfillment of the requirements for the degree of Bachelor of Arts in Linguistics Swarthmore College December 2018 Abstract Umatilla Sahaptin is a Shaptian language spoken in North-Eastern Oregon by the Umatilla tribe. While it has some documentation, such as a dictionary and sketch grammar, there are still acknowledged gaps in the literature. The purpose of this thesis is to fill one of those gaps with a description of syllable structure. To do this I compare data gathered from speakers of Umatilla with published accounts of sylla ble structure in the mutually intelligible sister language Yakima. After establishing what is meant by syllable structure and what is known about Yakima, I discuss the data I gathered. Using word list and sentence elicitations, stories, poems, and songs I conclude that Umatilla syllable structure is very similar to Yakima's, with some differences, namely in maximal margins, minimal words, and licensing of sonority sequence defying clusters. 'I would like to thank my consultants, Thomas Morningowl and Mildred Quaemptes, since it was their time and knowledge that made this work possible at all. I would also like to thank the Confederated Tribes of the Umatilla, for the privilege of working with the tribe, specifically the Language Program, the Education Commission, and the Board of Trustees. In particular I would like to thank Modesta Minthorn, for her help and guidance through the process of securing per mission for my work and scheduling time to do it. I would also like to thank the Eugene M. -
Washington Grain Train
How does the Washington Grain Train generate revenues? Washington Usage fees for grain cars are generated on the BNSF Railroad based on a combination of mileage traveled and number of days on that railroad (time and mileage). The further the car travels Grain Train and the longer it is on a particular railroad, the more money the car earns. The shuttle service between grain elevators and the barge terminal in Wallula use a different system. A car use fee per trip was June 2011 established for the shuttle service based on estimates of time and mileage. One car use fee was established for shipments on the PV Hooper rail line, and another for the BLMR. These fees are deposited directly into accounts managed by each of the three Grain Train Revolving Fund (Washington State-Owned Cars) port districts. These funds are used for grain car maintenance, car tracking, and Dollars in millions eventual car replacement (based on a 20- $1.4 year depreciation schedule). A portion of $1.2 these fees are also set aside and used as $1.0 a “reserve” fund that is periodically tapped for fleet expansion. $0.8 Once the reserve fund has grown large $0.6 enough to purchase rail cars and there is $0.4 a demonstrated need for additional cars, WSDOT can instruct the port districts to $0.2 send funds to a rail car sales firm selected $0 by WSDOT. This firm then delivers the cars 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010 to Washington for rehabilitation and then Twenty nine additional grain hopper rail cars were purchased in 2010. -
2017-2022 Comprehensive Scheme of Harbor Improvements – Port of Clarkston
Port of Clarkston 2017 – 2022 Harbor Improvements Comprehensive Scheme of PORT OF CLARKSTON COMPREHENSIVE SCHEME OF HARBOR IMPROVEMENTS (COMPREHENSIVE SCHEME) 2017 - 2022 Contributions by: Port of Clarkston Board of Commissioners Rick Davis, District 1, Chair Wayne Tippett, District 2 Marvin L. Jackson, District 3 Port Staff Wanda Keefer, Manager Jennifer Bly, Port Auditor Belinda Campbell, Economic Development Assistant Steve Pearson, Maintenance Lead Justin Turner, Maintenance Staff 849 Port Way Clarkston, WA 99403 (509) 758-5272 Port of Clarkston Comprehensive Scheme of Harbor Improvements Page i Port of Clarkston Comprehensive Scheme TABLE OF CONTENTS Page Title Page Cover Page i Table of Contents ii Introduction Mission of the Port 1 The Comprehensive Scheme of Harbor Improvements 2 History of Washington Ports 2 General Powers 3 Transportation 3 Economic Development 4 The Port of Clarkston 4 Characteristics of Asotin County 4 Port Properties 6 Port Planning Documents 8 Asotin Marina 10 Goals, Policies and Objectives for Port Development 12 Economic Development Initiatives 18 Preface 18 Industrial and Commercial Infrastructure 19 A – Development Overview 19 B -- Recent Development 20 Transportation Infrastructure 21 A -- Marine Related 21 B -- Non-Marine Related 22 Communications /Security Infrastructure 22 A -- Telecommunications 22 B -- Port Security System 23 Recreation and Tourism 23 Capacity Building and Other Broader Economic Development Initiatives 24 Planned Improvements 26 Near Term Recommendations 26 Medium Term Recommendations -
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. -
Top 26 Trails in Grant County 2020
and 12 Watchable Wildlife Units For more information, please contact: Grant County Tourism Commission P.O. Box 37, Ephrata, WA 98823 509.765.7888 • 800.992.6234 In Grant County, Washington TourGrantCounty.com TOP TRAILS Grant County has some of the most scenic and pristine vistas, hiking trails and outdoor 26 recreational opportunities in Washington State. and 12 Watchable Wildlife Units Grant County is known for its varied landscapes on a high desert plateau with coulees, lakes, in Grant County Washington reservoirs, sand dunes, canals, rivers, creeks, and other waterways. These diverse ecosystems Grant County Tourism Commission For Additional copies please contact: support a remarkable variety of fish and PO Box 37 Jerry T. Gingrich wildlife species that contribute to the economic, Ephrata, Washington 98837 Grant County Tourism Commission recreational and cultural life of the County. www.tourgrantcounty.com Grant County Courthouse PO Box 37 Ephrata, WA 98837 No part of this book may be reproduced in (509) 754-2011, Ext. 2931 any form, or by any electronic, mechanical, or other means, without permission in For more information on writing from the Grant County Tourism Grant County accommodations Commission. www.tourgrantcounty.com © 2019, Grant County Tourism Commission Second printing, 10m Trails copy and photographs Book, map and cover design by: provided by: Denise Adam Graphic Design Cameron Smith, Lisa Laughlin, J. Kemble, Veradale, WA 99037 Shawn Cardwell, Mark Amara, (509) 891-0873 Emry Dinman, Harley Price, [email protected] Sebastian Moraga and Madison White Printed by: Rewriting and editing by: Mark Amara Pressworks 2717 N. Perry Street Watchable Wildlife copy and Spokane, Washington 99207 photographs provided by: (509) 462-7627 Washington Department of [email protected] Fish and Wildlife Photograph by Lisa Laughlin CONTENTS CONTENTS Grant County Trails and Hiking Grant County Watchable Wildlife Viewing Upper Grand Coulee Area 1. -
Appendix a Data Compilation
APPENDIX A DATA COMPILATION Table of Contents A-1 Bibliography A-2 Non-GIS Data Directory A-3 GIS Data Directory APPENDIX A-1 BIBLIOGRAPHY Spokane Watershed Bibliography Appendix A1 1. Adema, G. W. Bedrock Depth and Morphology of the Rathdrum Prairie, Idaho: University of Idaho; c1999. 67 pages. Notes: Master of Science Thesis 2. Adema, G. W.; K.F.Sprenke., and R.M. Breckenridge. Bed Morphology of the Spokane Valley/Rathdrum Prairie Aquifer from a Detailed Gravity Survey [abstract]. Geological Society of America. 1998; 30(6). 3. Ader, M. J. Hydrogeology of the Green Bluff Plateau Spokane County. Washington State Department of Ecology, Shorelands and Water Resources Program; 1996; Open File Technical Information Report 96-03. 27 pages. 4. Allen, D. R. Latah Creek, Washington, Watershed: 1995-1996 Water Year Water Quality Assessment [abstract]. Inland Northwest Water Resources Conference, Program and Abstracts; 1997. 5. Amerigian, C.; J. Toth, and S.P. Reidel. Paleomagnetism of the Columbia River Basalt Group [abstract]. Geological Society of America Abstracts With Programs. 1987; 19(6):354. 6. Ames, K. C.; N.P. Matson.; D.M. Suzuki., and P.B. Sak. Inventory, Characterization, and Water Quality of Springs, Seeps, and Streams near Midnite Mine, Stevens County, Washington. U.S. Geological Survey; 1996; U.S. Geological Survey Open-File Report 96-115. 53 pages. 7. Anderson, A. M.; K. Bloudek.; P.O. Hyde; O. O'Connor, and N. Ogren. Evaluation of Urban Runoff Treatment in Swales. Spokane, Washington: Gonzaga University, School of Engineering, Center for Engineering Design; 1996; Senior Design Project 95-5. 44 pages. 8. -
Palouse River and Coulee City Rail Line
Palouse River and Coulee City Rail Line Palouse River and Coulee City Rail Line For More Information: Mike Rowswell WSDOT State Rail and Marine Office [email protected] 360-705-7900 360-705-7930 www.wsdot.wa.gov/rail www.wsdot.wa.gov/projects/rail/PCC_Acquisition/ WSDOT State Rail and Marine Office The Palouse River and Coulee PO Box 47407 City (PCC) rail line is the state’s Olympia, WA 98504-7407 longest short-line freight rail system and spans four counties in eastern Washington. In 2007, the Washington State Department of Transportation (WSDOT) completed the purchase of this rail line to save it from abandonment. January 2008 Palouse River and Coulee City Rail Line What is the Palouse River and Coulee City deteriorated over time. After attempting to develop Who is going to operate these lines? (PCC) Rail Line? business for a number of years, Watco finally WSDOT is working with local governments to discuss considered abandoning the lines because they As part of the purchase agreement, Watco will formation of an intergovernmental entity to govern were not profitable. In making that determination, the three branches. When such an entity is formed, it The former Palouse River and Coulee City (PCC) continue to operate the PV Hooper Branch under a Watco cited the expensive maintenance conditions will assume responsibility for the former PCC system. rail line is a 300-mile short-line freight rail system lease signed with the state in November 2004 and mentioned above, increased competition from the WSDOT will continue to oversee rehabilitation work that provides direct rail service to shippers, modified in 2007.