The Missoula Flood
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Hay Creek WSC Assessment.Pdf
Gilliam County Hay Creek/Scott Canyon Watershed Assessment • i Hay Creek / Scott Canyon Watershed Assessment Prepared by the Gilliam County Natural Resources Department for the Hay Creek/Scott Canyon Working Group Principal Author: Sue Greer, Contract Watershed Assessment Staff with assistance from: Susie Anderson, Watershed Coordinator, Gilliam-East John Day Watershed Council George Meyers, SWCD Watershed Technical Specialist June, 2003 Gilliam County Hay Creek/Scott Canyon Watershed Assessment • ii Hay Creek & Scott Canyon Watershed Gilliam County, Oregon Scott Canyon Highway 19 N Highway 206 Hay Creek Watershed Scott Canyon Watershed Stream Flow County Roads State Highways Condon Gilliam County Hay Creek/Scott Canyon Watershed Assessment • iii TABLE OF CONTENTS CHAPTER 1 – INTRODUCTION Goals and Objectives of Hay Creek / Scott Canyon Working Group. 1 Agencies & Jurisdictions. 2 Legislation and Management Plans . 4 CHAPTER 2 – WATERSHED OVERVIEW Watershed Description. 5 Ecoregions . 6 Land Ownership . 7 Land Use . 7 Noxious & Invasive Weeds . 8 Fish & Wildlife . 9 Population . 9 Climate & Precipitation . 9 Vegetation Zones . 11 Soils . 12 CHAPTER 3 – HISTORICAL CONDITIONS Historical Timeline. 16 Introduction . 17 Geology. 17 Climate . 18 Vegetation. 18 Native American Use. 19 Presence of Fish & Wildlife. 20 Natural Disturbance Patterns . 20 Settlement . 21 Livestock & Farming . 22 Roads & Rails. 23 City Water Supply. 23 CHAPTER 4 – CHANNEL HABITAT TYPES & CHANNEL MORPHOLOGY Introduction . 25 Methods . 25 Potential of Restoration basis CHTs. 26 CHT Description & Analysis . 27 Fish Barriers. 29 CHAPTER 5 – HYDROLOGY & WATER USE Introduction . 31 History . 31 Peak Stream Flows . 32 Water Rights . 32 Ground Water. 33 Road Density . 34 Gilliam County Hay Creek/Scott Canyon Watershed Assessment • iv CHAPTER 6 – SEDIMENT SOURCES Introduction . -
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. -
Surficial Geologic Map of the Lenore Quadrangle, Nez Perce County, Idaho
IDAHO GEOLOGICAL SURVEY DIGITAL WEB MAP 14 MOSCOW-BOISE-POCATELLO OTHBERG, BRECKENRIDGE, AND WEISZ Disclaimer: This Digital Web Map is an informal report and may be revised and formally published at a later time. Its content and format S URFICIAL G EOLOGIC M AP OF THE L ENORE Q UADRANGLE, N EZ P ERCE C OUNTY, I DAHO may not conform to agency standards. Kurt L. Othberg, Roy M. Breckenridge, and Daniel W. Weisz 2003 Qac CORRELATION OF MAP UNITS Qls Qls Qcb Qcb Surficial Latah Columbia River QTlbr Deposits Formation Basalt Qls m Qac Qam Qoam Qas Qac HOLOCENE QTlbr Qad Qls Qcb Qcg Qm 13,000 years Qad Qag QUATERNARY PLEISTOCENE QTlbr QTlbr Qac Qls QTlbr Qac PLIOCENE TERTIARY Qac Tl Tcb MIOCENE Qcb QTlbr INTRODUCTION Qcg Colluvium from granitic and metamorphic rocks (Holocene and Pleistocene)— Primarily poorly sorted muddy gravel composed of angular and subangular pebbles, cobbles, and boulders in a matrix of sand, silt, and clay. Emplaced The surficial geologic map of the Lenore quadrangle identifies earth materials by gravity movements in Bedrock Creek canyon where there are outcrops on the surface and in the shallow subsurface. It is intended for those interested of pre-Tertiary granitic rocks and quartzite. Includes local debris-flow deposits in the area's natural resources, urban and rural growth, and private and and isolated rock outcrops. Includes colluvium and debris-flow deposits Qac public land development. The information relates to assessing diverse QTlbr from the upslope basalt section, and areas of thin loess (typically less than conditions and activities, such as slope stability, construction design, sewage 5 feet). -
Washington Geology
JULY 1978 VOLUME 6 - NUMBER 3 A PLBLICATION OF THE DEPARTMENT OF NATURAL RESOURCES WASHINGTON GEOWGIC NEWSLETTER BERT L.COLE COMMISSIONER OF PUBLIC LANDS RALPH A BESWICK, Supervisor VAUGHN E. LIVINGSTON,JR.,State Geologist DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGY AND EARTH RESOURCES DEPARTMENT Of NATURAL RESOURCES, DIVISION OF GEOLOGY AND EARTH RESOURCES, OLYMPIA, WASHINGTON, 98504 LOCATION MAP : DIVISION OF GEOLOGY AND EARTH RESOURCES DEPT. SOCIAL AND HEALTH SERVICES t ~ i~L f ...J ~ i ,...... N g a: ~ ~OGY ANO EARTH <t tt RESOURCES D u -, t STATE CAPITOL ... TACOMA S~TILE- IDEPT. HIGHWAYS CITY CENTER FREEWAY EXIT PORTLA~ STATE CAPITOL EXIT Vaughn E. (Ted) Livingston, Jr., Supervisor Geologic Staff J. Eric Schuster, Assistant Supervisor Minerals and Energy Geologists Land Use Geologists Carl McFarland James G. Rigby Allen J. Fiksdal Keith L. Stoffel Clint Milne Glennda B. Tucker Kurt L. 0th berg Gerald W. Thorsen Wayne S. Moen Ellis R. Vonheeder Pamela Palmer Weldon W. Rau Charles W. Walker Regulations and Operations Surface Mined Land Reclamation and Oil and Gos Conservation Act Donald M. Ford, Assistant Supervisor Publications: Library: Laboratory: Secretaries: Loura Broy Connie Manson Arnold W. Bowman Patricia Ames Keith Ikerd Cherie Dunwoody Wonda Walker Kim Summers Pamela Whitlock Mailing address: Deportment of Natural Resources Division of Geology and Earth Resou rces Olympia, WA 98504 (206) 753-6183 ORIGIN OF THE GRAND COULEE AND DRY FALLS by Ted Livingston Washington State hos many interesting geo original terrain until in the Grand Coulee area it was logic features. Among the more outstanding dre the completely buried. During the course of these erup Grand Coulee and Dry Falls . -
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. -
The Cordilleran Ice Sheet 3 4 Derek B
1 2 The cordilleran ice sheet 3 4 Derek B. Booth1, Kathy Goetz Troost1, John J. Clague2 and Richard B. Waitt3 5 6 1 Departments of Civil & Environmental Engineering and Earth & Space Sciences, University of Washington, 7 Box 352700, Seattle, WA 98195, USA (206)543-7923 Fax (206)685-3836. 8 2 Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada 9 3 U.S. Geological Survey, Cascade Volcano Observatory, Vancouver, WA, USA 10 11 12 Introduction techniques yield crude but consistent chronologies of local 13 and regional sequences of alternating glacial and nonglacial 14 The Cordilleran ice sheet, the smaller of two great continental deposits. These dates secure correlations of many widely 15 ice sheets that covered North America during Quaternary scattered exposures of lithologically similar deposits and 16 glacial periods, extended from the mountains of coastal south show clear differences among others. 17 and southeast Alaska, along the Coast Mountains of British Besides improvements in geochronology and paleoenvi- 18 Columbia, and into northern Washington and northwestern ronmental reconstruction (i.e. glacial geology), glaciology 19 Montana (Fig. 1). To the west its extent would have been provides quantitative tools for reconstructing and analyzing 20 limited by declining topography and the Pacific Ocean; to the any ice sheet with geologic data to constrain its physical form 21 east, it likely coalesced at times with the western margin of and history. Parts of the Cordilleran ice sheet, especially 22 the Laurentide ice sheet to form a continuous ice sheet over its southwestern margin during the last glaciation, are well 23 4,000 km wide. -
Megaflood Adventure Section 3
Gingko Petrifed Forest Vantage, Washington Petrifcation is a process where trees and wood are turned to stone. The trees are buried and protected from natural forces, transforming the wood to solid rock over huge amounts of time. Most of the wood you see at Gingko is from the Missoula Floods, so you can see how the trees looked 13,000 years ago! Take the The Trees of Stone Interpretive Trail 2 miles west of the Visitor Center. On the trail you’ll see lots of fossils, erratics, and petrifed logs. Pick your favorite thing and draw it! BONUS: Gingko Petrifed Forest has its own Junior Ranger program. Complete it to earn another badge! Palouse Falls State Park Lacrosse, Washington Long before the foods, tectonic forces stressed the basalt bedrock and opened deep fractures. The megafoods took advantage of these weakened areas and used them to change the course of the river. Palouse Falls has many of these cracks in the canyon walls. How many can you fnd? Columbia River Gorge NationalCascade Locks,Scenic Oregon Area Ev en t ho ug h t h e lan ds ca pe loo ks di˛ er en t fr o m t he par k s in W as hin gt o n an d M o n t an a, t he I ce Ag e FloodsTumbl a es along types o f w a terf a lls! Cascade car v ed o u t t his s pec t acu lar g o r ge, t oo . As yserif o u’res orock e dri steps. -
Washington's Channeled Scabland
t\D l'llrl,. \·· ~. r~rn1 ,uR\fEY Ut,l\n . .. ,Y:ltate" tit1Washington ALBEIT D. ROSEWNI, Governor Department of Conservation EARL COE, Dlnctor DIVISION OF MINES AND GEOLOGY MARSHALL T. HUNTTING, Supervisor Bulletin No. 45 WASHINGTON'S CHANNELED SCABLAND By J HARLEN BRETZ 9TAT• PIUHTIHO PLANT ~ OLYMPIA, WASH., 1"511 State of Washington ALBERT D. ROSELLINI, Governor Department of Conservation EARL COE, Director DIVISION OF MINES AND GEOLOGY MARSHALL T. HUNTTING, Supervisor Bulletin No. 45 WASHINGTON'S CHANNELED SCABLAND By .T HARLEN BRETZ l•or sate by Department or Conservation, Olympia, Washington. Price, 50 cents. FOREWORD Most travelers who have driven through eastern Washington have seen a geologic and scenic feature that is unique-nothing like it is to be found anywhere else in the world. This is the Channeled Scab land, a gigantic series of deeply cut channels in the erosion-resistant Columbia River basalt, the rock that covers most of the east-central and southeastern part of the state. Grand Coulee, with its spectac ular Dry Falls, is one of the most widely known features of this ex tensive set of dry channels. Many thousands of travelers must have wondered how this Chan neled Scabland came into being, and many geologists also have speculated as to its origin. Several geologists have published papers outlining their theories of the scabland's origin, but the geologist who has made the most thorough study of the problem and has ex amined the whole area and all the evidence having a bearing on the problem is Dr. J Harlen Bretz. Dr. -
Geologic Map of the Twin Falls 30 X 60 Minute Quadrangle, Idaho
Geologic Map of the Twin Falls 30 x 60 Minute Quadrangle, Idaho Compiled and Mapped by Kurt L. Othberg, John D. Kauffman, Virginia S. Gillerman, and Dean L. Garwood 2012 Idaho Geological Survey Third Floor, Morrill Hall University of Idaho Geologic Map 49 Moscow, Idaho 83843-3014 2012 Geologic Map of the Twin Falls 30 x 60 Minute Quadrangle, Idaho Compiled and Mapped by Kurt L. Othberg, John D. Kauffman, Virginia S. Gillerman, and Dean L. Garwood INTRODUCTION 43˚ 115˚ The geology in the 1:100,000-scale Twin Falls 30 x 23 13 18 7 8 25 60 minute quadrangle is based on field work conduct- ed by the authors from 2002 through 2005, previous 24 17 14 16 19 20 26 1:24,000-scale maps published by the Idaho Geological Survey, mapping by other researchers, and compilation 11 10 from previous work. Mapping sources are identified 9 15 12 6 in Figures 1 and 2. The geologic mapping was funded in part by the STATEMAP and EDMAP components 5 1 2 22 21 of the U.S. Geological Survey’s National Cooperative 4 3 42˚ 30' Geologic Mapping Program (Figure 1). We recognize 114˚ that small map units in the Snake River Canyon are dif- 1. Bonnichsen and Godchaux, 1995a 15. Kauffman and Othberg, 2005a ficult to identify at this map scale and we direct readers 2. Bonnichsen and Godchaux, 16. Kauffman and Othberg, 2005b to the 1:24,000-scale geologic maps shown in Figure 1. 1995b; Othberg and others, 2005 17. Kauffman and others, 2005a 3. -
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. -
1 Reply to Comments 1 We Would Like to Thank the Three Anonymous
1 Reply to comments 2 We would like to thank the three anonymous reviewers and Marco Jorge for their comments. We are 3 particularly pleased that three of the four reviews thought it was an important paper that should be 4 published, and their constructive criticisms have really helped to improve it. We are disappointed that 5 reviewer #2 thinks that we cannot extract information and meaning from the geomorphological 6 signature of tunnel valleys. But we strongly disagree with this view and our argument is laid out below. 7 That they ignore a large body of literature spanning many disciplines that has shown the importance of 8 geomorphology for investigating landforms genesis we find rather perplexing. The reviewer comments 9 are in black and our replies and revisions in blue. 10 - Stephen Livingstone and Chris Clark 11 12 Short Comment by Marco Jorge 13 INTRODUCTION 14 L80-84 (statement of objective): Consider rephrasing sentence (perhaps revise whole paragraph). 15 Suggest to remove “To rectify this” (to correct this error), because it is about the lack of data rather 16 than error. Scale -> geographic scale; Pattern -> spatial arrangement; Rectify “. .mapping of the size, 17 shape, pattern and [spatial] distribution to better understand spatial properties. .” L84: “constitution” 18 -> Composition? 19 We have replaced “to rectify this” with “Based on previous studies and the availability of DEMs, we 20 are now able to undertake…” (as suggested by reviewer #3), changed “pattern” to “spatial 21 arrangement” and “constitutes” to “is”. 22 Reword the rationale for study area selection; e.g., that the landforms can be mapped from a DEM is 23 unrelated to the study area. -
Bibliography of PHYSI~AL LIMNOLOGY
STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF SHORE EROSION DIVISION OF GEOLOGICAL SURVEY REPORT OF INVESTIGATIONS NO. 25 (CONTRIBUTION NO. 4 LAKE ERIE GEOLOGICAL RESEARCH PROGRAM) Bibliography Of PHYSI~AL LIMNOLOGY 1781 ••••1954 COLUMBUS 1955 STATE OF OHIO Frank J. Lausche, Governor DEPAR 1MENT OF NATURAL RESOURCES A. W. Marion, Director NATURAL RESOURCES COMMISSION George Wenger, Chairman John A. Slipher, Bryce Browning, Vice Chairman Secretary C. D. Blubaugh Dr. John L. Rich Dr. C. L. Dow Milton Ronsheim A. W. Marion Dean L. L. Rummell DIVISION OF GEOLOGICAL SURVEY John H. Melvin, Chief DIVIS ION OF SHORE EROSION F . 0 , Kugle , Chief STATE OF OHIO Frank J. Lausche, Governor DEPARTMENT OF NATURAL RESOURCES A. W. Marion, Director DIVISION OF SHORE EROSION F. 0. Kugel, Chief DIVISION OF GEOLOGICAL SURVEY John H. Melvin, Chief REPORT OF INVESTIGATIONS NO. 2 5 (CONTRIBUTION NO. 4 LAKE ERIE GEOLOGICAL RESEARCH PROGRAM) BIBLIOGRAPHY OF PHYSICAL LIMNOLOGY 1781 .... 1954 By James L. Verber This publication is a cooperative project of the Division of Shore Erosion and The Division of Geological Survey. The research upon which the publication is based has been sponsored chiefly by t the Division of Shore Erosion. i COLUMBUS, 1955 I Blank Page t:;ONTENTS Page INTRODUCTION •••••••••• v Organization of the Index • v Suggestions on using the Index vi ABBREVIATIONS • vii BmLIOGRAPHY 1 INDEX and ALPHABETICAL LIST OF LAKES CITED 45 ADDENDUM WITH INDEX . • . 54 iii Blank Page INTBODU~TION The Bibliography of Physical Limnology, 1781- their assistance in preparing the manuscript for publica- 1953, contains both a bibliography and subject index tion.