Chapter 85. the Example of the Lake Missoula Flood
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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 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]. -
1. Geologic Background
Ice Age Floods Study of Alternatives Background section d BACKGROUND 1. Geologic Background n recent geological history, portions of the United States have been the site of several Imassive flooding events caused by the abrupt drainage of glacial lakes. The most dramatic of these are the Ice Age Floods, which covered parts of Montana, Idaho, Washington, and Oregon. For a better understanding of the Floods, perhaps a good place to start is to first look at the geological and climatic changes that led up to these cataclysmic floods. NPS Photo Today’s travelers to the Northwest are witnesses Generally accepted scientific evidence extinct 65 million years ago, and about to a story that puzzled geologists for years. indicates that the earth is around 4.5 to 20 million years ago, in late Cenozoic 4.6 billion years old. Glaciation can be Era, the Pacific Northwest started to look traced all the way back to the Proterozoic much as it does today, with its Era, approximately 2.3 billion years ago, mountains, valleys, and shorelines. when the earth was covered with ice. Near the end of the Proterozoic Era, Ice Ages have occurred sporadically summary between 850 and 600 million years ago, throughout the earth’s history, although his section presents a brief overview of the rock records indicate another global they represent a relatively small part of TGlacial Lake Missoula Floods story, two of the glaciation period. geologic time. Many of the still visible key people involved with discovering the Floods effects of the great ice sheets that and the glacial lake from which the Floods About 200 million years ago the Atlantic periodically covered parts of North originated, and events that led up to the initiation Ocean began to open up and the America were produced during the last of the Ice Age Floods Alternatives Study. -
Websites Maps Ice Age Floods
Maps Websites NOVA—Mystery of the Megaflood Glacial Lake Allison in Oregon’s Willamette Valley http://www.pbs.org/wgbh/nova/megaflood/ at the Height of the Lake Missoula Flood Explore the Channeled Scablands through an Reference Map interactive map, read an interview with geologist, The Ice Age Floods caused massive dams that Ice Age take a quiz, visit the teacher's guide, and more. forced water to temporarily pool into lakes throughout the Northwest. This map shows the Ice Age Floods Institute Floods most recent theories on the boundaries and depths http://www.iceagefloodsinstitute.org/ of Lake Allison, the glacial lake that was located in The Ice Age Flood Institute is a non-profit the Willamette Valley. organization of citizens throughout Montana, Idaho, Washington, and Oregon committed to tell the Ice Age Floods in the Pacific Northwest story of the Channeled Scablands. Reference Map Produced by the Ice Age Floods Institute, this map University of Wisconsin, Green Bay— shows clear evidence of the nearly unimaginable Channeled Scablands: Overview floods that scoured channels throughout the http://www4.uwsp.edu/geo/projects/geoweb/ Northwest contributing to the unique geological participants/dutch/vtrips/scablands0.htm formations seen throughout the states of Montana, Field trip pages follow the floodwaters of Glacial Idaho, Washington, and Oregon. Lake Missoula. Lots of pictures & some nice maps. CVO Website - Glacial Lake Missoula Lake Missoula Flood Path from Missoula, Montana http://vulcan.wr.usgs.gov/Glossary/Glaciers/Ic to Portland, Oregon eSheets/description_lake_missoula.html Reference Map US Geological Survey web site, with information Paired with smaller versions of the panorama and links about Glacial Lake Missoula. -
Geology Data Package for the Single-Shell Tank Waste Management Areas at the Hanford Site
PNNL-15955 Geology Data Package for the Single-Shell Tank Waste Management Areas at the Hanford Site S. P. Reidel M. A. Chamness January 2007 Prepared for CH2M HILL Hanford Group, Inc., and the U.S. Department of Energy under Contract DE-AC05-76RL01830 PNNL-15955 Geology Data Package for the Single-Shell Tank Waste Management Areas at the Hanford Site S. P. Reidel M. A. Chamness January 2007 Prepared for CH2M HILL Hanford Group, Inc., and the U.S. Department of Energy under Contract DE-AC05-76RL01830 Pacific Northwest National Laboratory Richland, Washington 99352 Foreword This data package discusses the geology of the single-shell tank (SST) farms and the geologic history of the area. The purpose of this report is to provide the most recent geologic information available for the SST farms. This report builds upon previous reports on the tank farm geology and Integrated Disposal Facility geology with information available after those reports were published. Both metric and English units of measurement are used in this document. However, English units are used for descriptions and discussions of drilling activities and samples because that is the system of units used by drillers to measure and report depths and well construction details. To convert feet to meters, multiply by 0.3048; to convert inches to centimeters, multiply by 2.54; to convert meters to feet, multiply by 3.28. iii Acknowledgments The authors acknowledge Frederick M. Mann at CH2M HILL Hanford Group, Inc. (Richland, Washington) for providing project funding and technical guidance. We also greatly appreciate the technical reviews provided by Ann Tallman and Dave Myers and Mike Connelly (both of CH2M HILL), Marc Wood (Fluor Hanford, Inc., Richland, Washington), and Bob Bryce (Pacific Northwest National Laboratory). -
The Cheney–Palouse Tract of Washington's Channeled Scablands
The Cheney–Palouse Tract of Washington’s Channeled Scablands SPRAGUE 231 e k LINCOLN SPOKANE C r a b C r e COUNTY SPRAGUE COUNTY 90 395 23 RITZVILLE o u t h F o e S r k k WHITMAN C ADAMS r a a COUNTY b k L COUNTY C r e e e u water g 261 flow r a direction S p 26 127 r Map Area u PINE o During the last ice age, a lobe of the Cordilleran Ice Sheet formed an This map shows the CITY ice dam that blocked a major valley in what is now western topographic evidence of c LAMONT Montana, creating Glacial Lake Missoula. Between 15,000 and the Missoula Floods on a s 13,000 years ago the ice began to recede and the lake portion of the Channeled S periodically breached the ice dam. These breaches Scablands in eastern Washington L created an estimated 40 catastrophic floods that known as the Cheney–Palouse L e I flowed westward during this time period. k scabland tract. Smooth, linear H k These ice-age floods, also known as the a features are former channels of the L L c Missoula Floods, swept across what is floods, while the more textured land U k K now eastern Washington and c adjacent to the pathways was higher in A o o R R onward to the Pacific Ocean elevation, and was thus unaffected by the A r K along the Columbia River flooding. d corridor. The floods scoured e the landscape on a massive Flooded areas were often scoured down to b scale, leaving behind bedrock, as can be seen east of Sprague Lake scarred terrain known and the Karakul Hills. -
The Lake Missoula Floods and the Channeled Scabland Author(S): J
The Lake Missoula Floods and the Channeled Scabland Author(s): J. Harlen Bretz Source: The Journal of Geology, Vol. 77, No. 5 (Sep., 1969), pp. 505-543 Published by: The University of Chicago Press Stable URL: http://www.jstor.org/stable/30062250 . Accessed: 15/01/2015 10:22 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The University of Chicago Press is collaborating with JSTOR to digitize, preserve and extend access to The Journal of Geology. http://www.jstor.org This content downloaded from 128.193.164.203 on Thu, 15 Jan 2015 10:22:29 AM All use subject to JSTOR Terms and Conditions THE LAKE MISSOULA FLOODS AND THE CHANNELED SCABLAND1 J HARLEN BRETZ Department of the Geophysical Sciences, University of Chicago ABSTRACT This paper reviews the outstanding evidence for (1) repeated catastrophic outbursts of Montana's glacially dammed Lake Missoula, (2) consequent overwhelming in many places of the preglacial divide along the northern margin of the Columbia Plateau in Washington, (3) remaking of the plateau's preglacial drainage pattern into an anastomosing complex of floodwater channels (Channeled Scabland) locally eroded hundreds of feet into underlying basalt, (4) convergence of these flood-born rivers into the Columbia Valley at least as far as Portland, Oregon, and (5) deposition of a huge delta at Portland. -
The Stonecutter and the Missoula
WashingtonHistory.org THE STONECUTTER & THE MISSOULA FLOOD ERRATICS By Nathan Reynolds COLUMBIA The Magazine of Northwest History, Spring 2006: Vol. 20, No. 1 In 1884 a local stonecutter installed a granite cornerstone in the new Catholic church under construction in Vancouver, Washington. The origin of this block of stone has presented something of a mystery. Was it mined from the only vein of granite in the area, which lay at some distance and several thousand feet in elevation, or was it somehow obtained from a source much closer at hand? An examination of competing geological theories and information provided by local residents helps to solve this puzzle. On the first day of November 1879, Victor Zepherinus Barthelemy filed a homestead claim in the LaCamas area of Washington Territory, about 15 miles east of Fort Vancouver. He, his wife, and two sons lived in a 300-square-foot cabin that Barthelemy had built in October of that year. The family had only recently traveled to the area from Ohio, where both sons were born and Barthelemy had been raised. Relatives on his wife’s side of the family had already homesteaded in the LaCamas area; Barthelemy selected a parcel immediately adjacent to theirs. Although he was raised in the United States, Barthelemy had been born in France in late 1841 or early 1842 and emigrated with his family to the United States in 1849. On November 7, 1854, Victor’s father, John Barthelemy, received United States citizenship in the common court of Montgomery County, Ohio. As John’s minor son, Victor also was granted citizenship. -
Chronology of Missoula Flood Deposits at the Coyote Canyon Mammoth Site, Washington State, USA
quaternary Article Chronology of Missoula Flood Deposits at the Coyote Canyon Mammoth Site, Washington State, USA George V. Last 1,2,* and Tammy M. Rittenour 3 1 Mid-Columbia Basin Old Natural Education Sciences (MCBONES) Research Center Foundation, Kennewick, WA 99338, USA 2 School of the Environment, Washington State University—Tri-Cities, Richland, WA 99354, USA 3 Department of Geosciences, Utah State University, Logan, UT 84322, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-509-946-8050 Abstract: Late Pleistocene outburst megafloods, mostly from glacial Lake Missoula, hydraulically ponded behind downstream constrictions in the Columbia River in southeastern Washington State, USA. Optically stimulated luminescence (OSL) ages for flood deposits from the Coyote Canyon Mammoth Site, located in a high (315–320 m asl) distal portion of the transient lake, indicate that at least seven floods ponded high enough to inundate the area during the period 20.9 ± 2.6 ka to 16.3 ± 2.8 ka. This is consistent with a radiocarbon age of about 17.4 ± 0.2 ka cal BP from the middle of the flood sequence. OSL ages from loess deposits overlying a paleosol at the top of the flood sequence range from 14.0 ± 2.3 ka to 10.9 ± 2.0 ka, suggesting a hiatus of about 2.3 thousand years. These datasets are consistent with current understanding that multiple late Pleistocene megafloods occurred between 20 ka and 14 ka and that earlier floods produced higher flood stages than later ones. The lack of flood deposits in the Coyote Canyon area younger than 16 ka supports the hypothesis that younger megafloods did not hydraulically pond in the Pasco Basin above about 230 m asl. -
Vol63-No1-A03.Pdf (7.976Mb)
Quaternary Science Journal GEOZON SCIENCE MEDIA Volume 63 / Number 1 / 2014 / 44-59 / DOI 10.3285/eg.63.1.03 ISSN 0424-7116 E&G www.quaternary-science.net Ice-Rafted Erratics and Bergmounds from Pleistocene Outburst Floods, Rattlesnake Mountain, Washington, USA Bruce N. Bjornstad How to cite: Bjornstad, B. N. (2014): Ice-Rafted Erratics and Bergmounds from Pleistocene Outburst Floods, Rattlesnake Mountain, Washing- ton, USA. – E&G Quaternary Science Journal, 63 (1): 44–59. DOI: 10.3285/eg.63.1.03 Abstract: Exotic ice-rafted debris from the breakup of ice-dammed glacial lakes Missoula and Columbia is common in slackwater areas along the 1,100-km route for outburst floods in the northwestern US. A detailed analysis was performed at Rattlesnake Mountain, which lay beyond the limit of the former ice sheet, where an exceptionally high concentration of ice-rafted debris exists midway along the floods’ path. Here floodwaters temporarily rose to 380 m elevation (forming short-lived Lake Lewis) behind the first substantial hydraulic constriction for the outburst floods near Wallula Gap. Within the 60 km2 study area more than 2,100 erratic isolates and clusters, as well as bergmounds were recorded. Three quarters of erratic boulders are of an exotic granitic composition, which stand in stark contrast to dark Columbia River basalt, the sole bedrock in the region. Other exotics include Proterozoic quartzite and argillite as well as gneiss, diorite, schist and gabbro, all once in direct contact with the Cordilleran Ice Sheet to the north. Most ice-rafted debris is concentrated between 200 and 300 m elevation.