3D Cartographic Animation: Visualizing Disaster on the Columbia River
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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. -
Gilliam County Emergency Management
Gilliam County Multi-Jurisdictional Natural Hazards Mitigation Plan Prepared for: Gilliam County, Arlington, Condon, and Lonerock © 2013, University of Oregon’s Community Service Center Photos: Oregon State Archives Gilliam County Multi-jurisdictional Natural Hazards Mitigation Plan Report for: Gilliam County City of Arlington City of Condon City of Lonerock 221 South Oregon Street Condon, Oregon 97823 Prepared by: University of Oregon’s Community Service Center: Resource Assistance to Rural Environments & Oregon Partnership for Disaster Resilience 1209 University of Oregon Eugene, Oregon 97403-1209 January 2013 (This page intentionally left blank) Special Thanks & Acknowledgements GilliAm County developed this NaturAl HazArds MitigAtion PlAn through A regionAl pArtnership funded by the Federal Emergency MAnAgement Agency’s Pre-DisAster MitigAtion Competitive GrAnt ProgrAm. FEMA AwArded the Mid-ColumbiA Gorge Region grAnt to support the update of naturAl hazArd mitigAtion plAns for eight counties in the region. The region’s plAnning process utilized A four-phased plAnning process, plAn templAtes And plAn development support provided by Resource AssistAnce for RurAl Environments (RARE) and the Oregon PArtnership for DisAster Resilience (OPDR) At the University of Oregon’s Community Service Center. This project would not have been possible without technicAl And financiAl support provided by the Mid-ColumbiA Council of Governments. Regional partners include: • Mid-ColumbiA Council of Governments • Oregon MilitAry DepArtment – Office of Emergency -
Giga Flood Chapter 8
Lake Allison In Oregon’s Willamette Valley during the largest Lake Missoula Flood the “GigaFlood” (Map by Rick Thompson) Revised Second Edition Copyright © 2015 Rick Thompson All rights reserved. No part of this book may be reproduced or transmitted in any form, or by any means, electronic or mechanical, including photocopying, recording, or by any information storage and retrieval system, without written permission from the publisher. Printed in the United States Published by LMF Publishing Cover photograph: Willamette Falls, Rick Thompson Cover design: Rick Thompson ISBN 978-0-9890840-2-4 LMF Publishing P.O. Box 33056 Portland, OR 97292 GigaFlood The Largest of the Lake Missoula Floods In Northwest Oregon and Southwest Washington Revised Second Edition by Rick Thompson LMF Publishing Portland, OR Table of Contents Foreword..........................................................................9 Preface............................................................................11 Acknowledgements........................................................12 Introduction: The GigaFlood Story................................13 Chapter 1: The Ice Age..................................................17 Chapter 2: Ice Sheets and Ice Lobes..............................21 Chapter 3: The Lake Missoula Floods...........................29 Chapter 4: Discovering the Floods.................................35 Chapter 5: The Channeled Scablands.............................47 Chapter 6: Water Gaps...................................................67 Chapter -
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]. -
A PALEOCLIMATIC and PALEOHYDROLOGIC RECONSTRUCTION of PLEISTOCENE FOSSIL LAKE, OREGON by © 2010 Julie Beth Retrum B.A., Univers
A PALEOCLIMATIC AND PALEOHYDROLOGIC RECONSTRUCTION OF PLEISTOCENE FOSSIL LAKE, OREGON By © 2010 Julie Beth Retrum B.A., University of Minnesota Morris, 2001 M.S., The University of Kansas, 2004 Submitted to the Department of Geology and the Faculty of the Graduate School of The University of Kansas in partial fulfillment of the requirements for the degree of Doctor of Philosophy _____________________________________ Luis A González, Co-Chair _____________________________________ Stephen T. Hasiotis, Co-Chair _____________________________________ William C. Johnson _____________________________________ Jennifer A. Roberts _____________________________________ Gregory A. Ludvigson Date Submitted: _______________________ The dissertation committee for Julie Beth Retrum certifies that this is the approved version of the following dissertation: A PALEOCLIMATIC AND PALEOHYDROLOGIC RECONSTRUCTION OF PLEISTOCENE FOSSIL LAKE, OREGON Committee: _____________________________________ Luis A González, Co-Chair _____________________________________ Stephen T. Hasiotis, Co-Chair _____________________________________ William C. Johnson _____________________________________ Jennifer A. Roberts _____________________________________ Gregory A. Ludvigson Date Submitted: _______________________ ii ABSTRACT Julie B. Retrum, Ph.D. Department of Geology, September 2010 University of Kansas Fossil Lake, Oregon, is a Pleistocene lacustrine basin (~ 650–13 ka) in the northwestern part of the Great Basin best known for its abundant and diverse vertebrate assemblage. -
Lake Missoula and Its Floods by Kendall L
Society for Range Management Lake Missoula and Its Floods By Kendall L. Johnson he city of Spokane lies astride the Spokane River, out of the earth over previous untold centuries. The winds some 40 miles from its origination near Coeur created dune-like deposits of variable orientation and depth d’Alene, Idaho. The convention center and that today make up fertile farmland in southeastern hotel, site of the 65th annual meeting of SRM, are Washington and adjacent Idaho. Bretz’s Flood followed the Tlocated right along the river, creating a beautiful and even path of the many earlier fl oods and recreated the effects over idyllic setting. These qualities make it even harder to imagine thousands of square miles in the Columbia Basin. These can a long-ago day when a miles-wide wall of water, measuring briefl y be considered in four major categories: 1) the chan- as much as 500 feet high, bore down on this site. Hours neled scablands, 2) the river canyon, 3) the Grand Coulee, before, a great ice dam on glacial Lake Missoula (present-day and 4) Lake Lewis. Clark Fork River) had failed. The dam was as much as 2,500 feet in height, impounded a lake up to 2,000 feet deep, The Channeled Scablands extended east in the intermontane valleys for 200 miles, and The enormous depth of the advancing front of water, covered some 3,000 square miles. It probably contained over 500 cubic miles of water, approximating half the volume of measured in the several hundreds of feet, moving at speeds Lake Michigan. -
This File Was Created by Scanning the Printed Publication
This file was created by scanning the printed publication. Text errors identified by the software have been corrected; however, some errors may remain. Editors SHARON E. CLARKE is a geographer and GIS analyst, Department of Forest Science, Oregon State University, Corvallis, OR 97331; and SANDRA A. BRYCE is a biogeographer, Dynamac Corporation, Environmental Protection Agency, National Health and Environmental Effects Research Laboratory, Western Ecology Division, Corvallis, OR 97333. This document is a product of cooperative research between the U.S. Department of Agriculture, Forest Service; the Forest Science De- partment, Oregon State University; and the U.S. Environmental Protection Agency. Cover Artwork Cover artwork was designed and produced by John Ivie. Abstract Clarke, Sharon E.; Bryce, Sandra A., eds. 1997. Hierarchical subdivisions of the Columbia Plateau and Blue Mountains ecoregions, Oregon and Washington. Gen. Tech. Rep. PNW-GTR-395. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 114 p. This document presents two spatial scales of a hierarchical, ecoregional framework and provides a connection to both larger and smaller scale ecological classifications. The two spatial scales are subregions (1:250,000) and landscape-level ecoregions (1:100,000), or Level IV and Level V ecoregions. Level IV ecoregions were developed by the Environmental Protection Agency because the resolution of national-scale ecoregions provided insufficient detail to meet the needs of state agencies for estab- lishing biocriteria, reference sites, and attainability goals for water-quality regulation. For this project, two ecoregions—the Columbia Plateau and the Blue Mountains— were subdivided into more detailed Level IV ecoregions. -
Quaternary Studies Near Summer Lake, Oregon Friends of the Pleistocene Ninth Annual Pacific Northwest Cell Field Trip September 28-30, 2001
Quaternary Studies near Summer Lake, Oregon Friends of the Pleistocene Ninth Annual Pacific Northwest Cell Field Trip September 28-30, 2001 springs, bars, bays, shorelines, fault, dunes, etc. volcanic ashes and lake-level proxies in lake sediments N Ana River Fault N Paisley Caves Pluvial Lake Chewaucan Slide Mountain pluvial shorelines Quaternary Studies near Summer Lake, Oregon Friends of the Pleistocene Ninth Annual Pacific Northwest Cell Field Trip September 28-30, 2001 Rob Negrini, Silvio Pezzopane and Tom Badger, Editors Trip Leaders Rob Negrini, California State University, Bakersfield, CA Silvio Pezzopane, United States Geological Survey, Denver, CO Rob Langridge, Institute of Geological and Nuclear Sciences, Lower Hutt, New Zealand Ray Weldon, University of Oregon, Eugene, OR Marty St. Louis, Oregon Department of Fish and Wildlife, Summer Lake, Oregon Daniel Erbes, Bureau of Land Management, Carson City, Nevada Glenn Berger, Desert Research Institute, University of Nevada, Reno, NV Manuel Palacios-Fest, Terra Nostra Earth Sciences Research, Tucson, Arizona Peter Wigand, California State University, Bakersfield, CA Nick Foit, Washington State University, Pullman, WA Steve Kuehn, Washington State University, Pullman, WA Andrei Sarna-Wojcicki, United States Geological Survey, Menlo Park, CA Cynthia Gardner, USGS, Cascades Volcano Observatory, Vancouver, WA Rick Conrey, Washington State University, Pullman, WA Duane Champion, United States Geological Survey, Menlo Park, CA Michael Qulliam, California State University, Bakersfield, -
Geologic Map of the Lacamas Creek Quadrangle, Clark County, Washington
Geologic Map of the Lacamas Creek Quadrangle, Clark County, Washington By Russell C. Evarts Pamphlet to accompany Scientific Investigations Map 2924 2006 U.S. Department of the Interior U.S. Geological Survey INTRODUCTION PREVIOUS GEOLOGIC INVESTIGATIONS GEOGRAPHIC AND GEOLOGIC SETTING Previous geologic mapping in the Lacamas Creek area, generally carried out as part of broad The Lacamas Creek 7.5' quadrangle is in regional reconnaissance investigations, established southwestern Washington, approximately 25 km the basic stratigraphic framework and distribution of northeast of Portland, Oregon, along the eastern geologic units in the quadrangle. Trimble (1963) margin of the Portland Basin, which is part of the mapped and described the geology of the map area at Puget-Willamette Lowland that separates the Cascade a scale of 1:62,500 as part of a general geologic Range from the Oregon Coast Range (fig. 1). Since investigation of the Portland metropolitan area. late Eocene time, the Cascade Range has been the Working simultaneously but independently, locus of an episodically active volcanic arc associated Mundorff (1964) mapped the area of the Lacamas with underthrusting of oceanic lithosphere beneath Creek quadrangle for a water-resources evaluation of the North American continent along the Cascadia Clark County. He published a 1:48,000-scale Subduction Zone. Lava flows that erupted early in the geologic map and provided detailed descriptions of history of the arc underlie the eastern half of the the basin-fill deposits. Lacamas Creek quadrangle, forming a dissected Swanson and others (1993) updated terrain, with elevations as high as 2050 ft (625 m), Mundorff’s Clark County work as part of an that slopes irregularly but steeply to the southwest. -
Three Main Types of Rocks on the Planet and in Oregon Lesson to Grow
Lesson to Grow Three Main Types of Rocks on the Planet and in Oregon Description: This lesson builds on the student readings found Grade Level: 4-10 in Oregon’s Ancient Geology. There are three main types of rocks in the world and all are found here Essential Skills: 3, 9 in Oregon. In this lesson, students learn what the NGSS: 4-ESS2-1, 5-ESS3-1 three main types of rocks are and identify geologic events in our region that could have created these CCSS: RI.4.7, W.4.7, W.4.8 rocks. Social Sciences: 6.11, 6.12, Background: 6.13, 6.14, 7.8., 7.9, 7.10, 7.13, 1) The three student geology readings can be 8.10, HS.14, HS.15 downloaded and printed from the online lesson, Math: MP.5 Oregon’s Ancient Natural History - Time: 2-3 class periods 2) The geologic events described in these readings were capable of forming one or more of the Materials: three types of rocks on the planet - sedimentary, Student reading sheets from metamorphic, or igneous. Oregon’s Ancient Natural History online 3) All rocks on earth are formed as either igneous, sedimentary or metamorphic rocks. The diagram AITC Library Resources: to the right shows how the rocks on earth are changed from one rock type to another. Cycling Back to Nature: Soils Alive This changing of rock types is called the “Rock Cycle”. A copy of this Rock Cycle image The Soul of Soil can be downloaded from the Geology Resources section. More Lessons: Earth as an Apple and Soil Directions: Conservation Note: Prior to this lesson, students should have received a copy of the three-part readings Water Filtering and Soil on Oregon’s Ancient Geology (Columbia Basalts, Missoula Floods, and Fire & Ice) and had Soil Horizons & Below our Feet time to read the material and discuss it with their class. -
Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington
Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington Scientific Investigations Report 2017–5022–N U.S. Department of the Interior U.S. Geological Survey Cover. Palouse Falls, Washington. The Palouse River originates in Idaho and flows westward before it enters the Snake River near Lyons Ferry, Washington. About 10 kilometers north of this confluence, the river has eroded through the Wanapum Basalt and upper portion of the Grande Ronde Basalt to produce Palouse Falls, where the river drops 60 meters (198 feet) into the plunge pool below. The river’s course was created during the cataclysmic Missoula floods of the Pleistocene as ice dams along the Clark Fork River in Idaho periodically broke and reformed. These events released water from Glacial Lake Missoula, with the resulting floods into Washington creating the Channeled Scablands and Glacial Lake Lewis. Palouse Falls was created by headward erosion of these floodwaters as they spilled over the basalt into the Snake River. After the last of the floodwaters receded, the Palouse River began to follow the scabland channel it resides in today. Photograph by Stephen P. Reidel. Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington By Victor E. Camp, Stephen P. Reidel, Martin E. Ross, Richard J. Brown, and Stephen Self Scientific Investigations Report 2017–5022–N U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S.