1. Geologic Background
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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). -
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. -
Sculpted by Floods Learning Resource Guide Overview
Sculpted by Floods Learning Resource Guide Overview: KSPS’s Sculpted by Floods tells the story of the ice age floods in the Pacific Northwest. It is a story of the earth's power, scientific discovery and human nature - one touted by enthusiasts as the greatest story left untold. During the last ice age, floods flowing with ten times the volume of all the world's current rivers combined inundated the Northwest. What they left behind was a unique landscape that citizens of the Pacific Northwest call home. Subjects: Earth Science, Geology, History, Pacific Northwest History Grade Levels: 6-8 Materials: Lesson handouts, laptops/computers Learning Guide Objectives: Define the following vocabulary terms and use them orally and in writing: glacier, flood, cataracts, landform, canyon, dam. Analyze how floods can create landforms and shape a region’s landscape, using the Missoula Floods as a case study. Next Generation Science Standards MS-ESS2-2. Construct an explanation based on evidence for how geoscience processes have changed Earth’s surface at varying time and spatial scales. Washington State History Standards EALR 4: HISTORY: 3.1. Understands the physical characteristics, cultural characteristics, and location of places, regions, and spatial patterns on the Earth’s surface Common Core English Language Arts Anchor & Literacy in History/Social Studies Standards CCSS.ELA-LITERACY.CCRA.R.7. Integrate and evaluate content presented in diverse media and formats, including visually and quantitatively, as well as in words. CCSS.ELA-LITERACY.CCRA.W.4. Produce clear and coherent writing in which the development, organization, and style are appropriate to task, purpose, and audience. -
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. -
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. -
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. -
Chapter 85. the Example of the Lake Missoula Flood
Chapter 85 The Example of the Lake Missoula Flood As already noted, uniformitarian hypotheses rarely, if ever, can be supported by extensive geological evidence. Part of this is due to the nature of the features, since they originated in the past. The same charge could be leveled against Flood explanations. However, geomorphological evidence for the Retreating Stage of the Flood is strong, as this ebook shows. Whereas uniformitarian scientists have to invent speculative secondary hypotheses to salvage their paradigm in the light of conflicting evidence, the Flood paradigm does not need to invent secondary hypotheses, because the evidence is consistent with the paradigm. Furthermore, the Flood paradigm has an example of how a well-substantiated catastrophic flood at the peak of the Ice Age created a water and wind gap.1 The Lake Missoula flood (earlier called the Spokane or the Bretz flood) demonstrates catastrophic floods can easily produce water and wind gaps. Figure 85.1. Glacial Lake Missoula as shown on a kiosk sign at Lake Pend Oreille. 1 Oard, M.J., 2004. The Missoula Flood Controversy and the Genesis Flood, Creation Research Society Monograph No. 13, Chino Valley, AZ. The Lake Missoula Flood One of the largest lakes ever ponded by an ice dam was glacial Lake Missoula (Figure 85.1). After this lake deepened to 2,000 feet (610 m) at the dam site in northern Idaho, the bursting ice dam initiated one of the largest floods on earth, except that described in Genesis. Glacial Lake Missoula contained 540 mi3 (2,210 km3) of water and emptied in two days. -
The Man of Scorn
By Jeff Reich The Man of Scorn f I asked you where the world’s largest waterfall is located, how would you reply? Would it be Inga or Kisangani Falls, both located in the Congo, or Niagara Falls, or Imaybe Victoria Falls located on the Zambezi River in Zimbabwe? Well, those are some great answers. But would you believe it is located in central Washington State in America? “What?” you might exclaim. But it is true. The only problem is, this falls has not had water running over it for centuries; thus the reason for its name — Dry Falls. Here is what Wikipedia tells us: As stated, it is around 400 feet high which at one point was estimated to “Dry Falls is a 3.5 mile long scalloped and over 3 miles long, which makes it have been up to 1,000 feet deep! More precipice in central Washington on the almost fi ve times the width of Niagara than 2,000 square miles of central opposite side of the Upper Grand Cou- Falls and over twice as high. What must Washington State were scrubbed bare, lee from the Columbia River, and at the the falls have looked like with its full forming what is called “the scablands.” head of the Lower Grand Coulee. At fi ve volume of water thundering over it? It And nearly 1,000 square miles of the times the width of Niagara, Dry Falls would have shaken the ground for miles scablands contain gravel deposits from is thought to be the greatest known around. -
Geomorphic and Sedimentological History of the Central Lake Agassiz Basin
Electronic Capture, 2008 The PDF file from which this document was printed was generated by scanning an original copy of the publication. Because the capture method used was 'Searchable Image (Exact)', it was not possible to proofread the resulting file to remove errors resulting from the capture process. Users should therefore verify critical information in an original copy of the publication. Recommended citation: J.T. Teller, L.H. Thorleifson, G. Matile and W.C. Brisbin, 1996. Sedimentology, Geomorphology and History of the Central Lake Agassiz Basin Field Trip Guidebook B2; Geological Association of CanadalMineralogical Association of Canada Annual Meeting, Winnipeg, Manitoba, May 27-29, 1996. © 1996: This book, orportions ofit, may not be reproduced in any form without written permission ofthe Geological Association ofCanada, Winnipeg Section. Additional copies can be purchased from the Geological Association of Canada, Winnipeg Section. Details are given on the back cover. SEDIMENTOLOGY, GEOMORPHOLOGY, AND HISTORY OF THE CENTRAL LAKE AGASSIZ BASIN TABLE OF CONTENTS The Winnipeg Area 1 General Introduction to Lake Agassiz 4 DAY 1: Winnipeg to Delta Marsh Field Station 6 STOP 1: Delta Marsh Field Station. ...................... .. 10 DAY2: Delta Marsh Field Station to Brandon to Bruxelles, Return En Route to Next Stop 14 STOP 2: Campbell Beach Ridge at Arden 14 En Route to Next Stop 18 STOP 3: Distal Sediments of Assiniboine Fan-Delta 18 En Route to Next Stop 19 STOP 4: Flood Gravels at Head of Assiniboine Fan-Delta 24 En Route to Next Stop 24 STOP 5: Stott Buffalo Jump and Assiniboine Spillway - LUNCH 28 En Route to Next Stop 28 STOP 6: Spruce Woods 29 En Route to Next Stop 31 STOP 7: Bruxelles Glaciotectonic Cut 34 STOP 8: Pembina Spillway View 34 DAY 3: Delta Marsh Field Station to Latimer Gully to Winnipeg En Route to Next Stop 36 STOP 9: Distal Fan Sediment , 36 STOP 10: Valley Fill Sediments (Latimer Gully) 36 STOP 11: Deep Basin Landforms of Lake Agassiz 42 References Cited 49 Appendix "Review of Lake Agassiz history" (L.H. -
The Missoula Flood
THE MISSOULA FLOOD Dry Falls in Grand Coulee, Washington, was the largest waterfall in the world during the Missoula Flood. Height of falls is 385 ft [117 m]. Flood waters were actually about 260 ft deep [80 m] above the top of the falls, so a more appropriate name might be Dry Cataract. KEENAN LEE DEPARTMENT OF GEOLOGY AND GEOLOGICAL ENGINEERING COLORADO SCHOOL OF MINES GOLDEN COLORADO 80401 2009 The Missoula Flood 2 CONTENTS Page OVERVIEW 2 THE GLACIAL DAM 3 LAKE MISSOULA 5 THE DAM FAILURE 6 THE MISSOULA FLOOD ABOVE THE ICE DAM 6 Catastrophic Flood Features in Eddy Narrows 6 Catastrophic Flood Features in Perma Narrows 7 Catastrophic Flood Features at Camas Prairie 9 THE MISSOULA FLOOD BELOW THE ICE DAM 13 Rathdrum Prairie and Spokane 13 Cheny – Palouse Scablands 14 Grand Coulee 15 Wallula Gap and Columbia River Gorge 15 Portland to the Pacific Ocean 16 MULTIPLE MISSOULA FLOODS 17 AGE OF MISSOULA FLOODS 18 SOME REFERENCES 19 OVERVIEW About 15 000 years ago in latest Pleistocene time, glaciers from the Cordilleran ice sheet in Canada advanced southward and dammed two rivers, the Columbia River and one of its major tributaries, the Clark Fork River [Fig. 1]. One lobe of the ice sheet dammed the Columbia River, creating Lake Columbia and diverting the Columbia River into the Grand Coulee. Another lobe of the ice sheet advanced southward down the Purcell Trench to the present Lake Pend Oreille in Idaho and dammed the Clark Fork River. This created an enormous Lake Missoula, with a volume of water greater than that of Lake Erie and Lake Ontario combined [530 mi3 or 2200 km3]. -
Article in Press
ARTICLE IN PRESS Quaternary Science Reviews 24 (2005) 1533–1541 Correspondence$ Fresh arguments against the Shaw megaflood hypothesis. that the Lake Agassiz flood was the ‘‘largest in the last A reply to comments by David Sharpe on ‘‘Paleohy- 100,000 years’’ refers to a different publication (Clarke draulics of the last outburst flood from glacial Lake et al., 2003). We agree that, in terms of peak discharge, Agassiz and the 8200 BP cold event’’ both the Missoula floods (e.g., Clarke et al., 1984; O’Connor and Baker, 1992) and the Altay event (Baker et al., 1993) were indeed larger (roughly 17 Sv for Missoula and 418 Sv for Altay) but the released water 1. The megaflood hypothesis volume was a small fraction of that released from glacial Lake Agassiz (Table 1). Furthermore, the focus of We disagree with the premise underlying most of Clarke et al. (2003) was on abrupt climate change David Sharpe’s comments, namely that the Shaw triggered by freshwater injection to the North Atlantic subglacial megaflood hypothesis enjoys sufficient main- Ocean at 8200 BP: Freshwater volume rather than peak streamacceptance that we were negligent in failing to flood discharge is the relevant measure of flood cite it. Although the literature on Shavian megafloods magnitude for activation of this climate switch. Sharpe’s has grown over the past decade, it is less clear that the comment that ‘‘improved knowledge of additional flood ideas have gained ground. As a recent datum, Benn and terrains is important in assessing the impact of specific Evans (2005) assert that ‘‘most Quaternary scientists outburst floods on rapid climate change’’ seems to miss give little or no credence to the [Shaw] megaflood the point that flood intensity, which controls the interpretation, and it conflicts with an overwhelming geomorphic imprint, is only a second-order influence body of modern research on past and present ice sheet on the climate impact. -
8-Ton Rock Centerpiece of New Museum Exhibit
8-ton rock centerpiece of new museum exhibit • PERRY BACKUS [email protected] May 12, 2020 Ravalli County Museum Board member Dennis Moore helps Donaldson Brothers employees Vern Weidow and Mark Jessop set an 8-ton glacial rock into place on the museum grounds. By mid-June, the rock will become the centerpiece of a new permanent exhibit about Glacial Lake Missoula and its impact on the Bitterroot Valley. Ravalli County Museum Executive Director Tamar Stanley and museum board member Dennis Moore stand next to the newly delivered 8-ton boulder that will serve as the museum's new permanent exhibit that explains a portion of the natural history of the Bitterroot Valley. To fully understand the significance of Ravalli County Museum’s newest exhibit, visitors will need to come armed with imagination and a willingness to look skyward. The 8-ton rock that was carefully lowered into place on the museum’s lawn Monday is there to take them on a journey thousands of years back in time. The first thing they might do is look toward the towering Bitterroot Range just west of Hamilton. It was once home to the huge boulder that geologists call a glacial erratic. It found its way to the valley floor through the upheaval caused by glaciers more than 15,000 years ago. And then for thousands of years more, its home was the bottom of the massive Glacial Lake Missoula. To get an idea of the depth of the lake that would have covered Hamilton back then, visitors can lift their eyes to the top of the museum’s cupola and then imagine six of those buildings stacked upon each other.