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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. -
Interior Columbia Basin Mollusk Species of Special Concern
Deixis l-4 consultants INTERIOR COLUMl3lA BASIN MOLLUSK SPECIES OF SPECIAL CONCERN cryptomasfix magnidenfata (Pilsbly, 1940), x7.5 FINAL REPORT Contract #43-OEOO-4-9112 Prepared for: INTERIOR COLUMBIA BASIN ECOSYSTEM MANAGEMENT PROJECT 112 East Poplar Street Walla Walla, WA 99362 TERRENCE J. FREST EDWARD J. JOHANNES January 15, 1995 2517 NE 65th Street Seattle, WA 98115-7125 ‘(206) 527-6764 INTERIOR COLUMBIA BASIN MOLLUSK SPECIES OF SPECIAL CONCERN Terrence J. Frest & Edward J. Johannes Deixis Consultants 2517 NE 65th Street Seattle, WA 98115-7125 (206) 527-6764 January 15,1995 i Each shell, each crawling insect holds a rank important in the plan of Him who framed This scale of beings; holds a rank, which lost Would break the chain and leave behind a gap Which Nature’s self wcuid rue. -Stiiiingfieet, quoted in Tryon (1882) The fast word in ignorance is the man who says of an animal or plant: “what good is it?” If the land mechanism as a whole is good, then every part is good, whether we understand it or not. if the biota in the course of eons has built something we like but do not understand, then who but a fool would discard seemingly useless parts? To keep every cog and wheel is the first rule of intelligent tinkering. -Aido Leopold Put the information you have uncovered to beneficial use. -Anonymous: fortune cookie from China Garden restaurant, Seattle, WA in this “business first” society that we have developed (and that we maintain), the promulgators and pragmatic apologists who favor a “single crop” approach, to enable a continuous “harvest” from the natural system that we have decimated in the name of profits, jobs, etc., are fairfy easy to find. -
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. -
Washington Geology Released Since [Project Chief: W
·- July 1983 Volume 11 Number 3 Washington Geologic Newsletter · . Lovitt mine, near Wenatchee, Chelan County, Washington, 1977. Photo by Jack Jansons BRIAN J . BOYLE COMMISSIONER OF PUBLIC LANDS ART STEARNS, Supervisor RAYMOND LASMANIS, State Geologist DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGY AND EARTH RESOURCES Marlin Woy - To Porllond n Exit IOs·• [" GEOLOGY ANO /. t Roctl)11onl•t ... Solllh EARTH ~CES i..-<-....<....<c.L..'-'-! !! 0 I u Sound .. C 'Entrance- Moll Elf!H~~• · 0Poulsot\S. Mortin\ s,. : ••••• ,Porklno .....~ :....... ----. ........... .................... • • • • •• • • • • Coll•o• Z ·········o····· ... 4224 6th Ave. S.E., Lacey, Washington in Albortson• MAILING ADDRESS: Department of Natural Resources Division of Geology and Earth Resources Olympia, WA 98504 (206) 459-6372 Field office address: Department of Natural Resources Division of Geology and Earth Resources Spokane County Agricultural Center N. 222 Havana Spokane, WA 99202 ( 509) 458-2038 Lauta Btay, Editor The Washington Geologic Newsletter, a quarterly report of geologlc articles, Ts published by the Division of Geology and Earth Resources, Department of Natural Resources. The newsletter is free upon request. The division also publishes bulletins, information circulars, and geologic maps. A list of these publicatiOflS will be sent upon request. .. THE WENATCHEE GOLD RUSH by Bonnie Bunning* INTRODUCTION from the D ''reef" between 1949 and 1967. For a long time the ore was shipped directly to the Tacoma smelter On March 4, 19831 when Breakwater Resources LLd. where a substantial credit for the siliceous ores (used as and Asamera Minerals, Inc., made their exciting gold find flux in the smelter) helped make t he mine profitable. In public, companies and individuals from Canada and the 1961, Day Mines, Inc., and Lovitt Mining Co. -
Dry Falls Visitor Center Due to the Fact That Many Travelers Saw These Unusual Landforms in the Landscape As They Drove the Coulee Corridor
Interactive Design Approach IMMERSIVE Theater Topo Model The design approach for the exhibits is closely integrated with the Seating architecture. The layering of massive, linear building walls pro- for 50-60 EXHIBIT vides a direction for the design and layout of exhibit components. Gallery Real ‘Today’ erratic OUTDOOR Terrace Building walls are cut open at strategic points to accommodate WITH EXhibits specific exhibits and to allow for circulation. Smaller, wall-panel exhibits are used for supports and dividers. Equipment ‘Volcanic ‘Ice Age Floods’ Room Period’ Approaching the center, visitors are forced to walk around a mas- sive erratic – these huge boulders are seemingly deposited directly Gallery Animal Modelled erratic Lava flow overhead Freestanding time line animal cutouts on the path to the front door. The displaced rock serves as a strong Welcome in floor icon of the violent events that occurred during the Ice Age Floods. Through the Visitor Center’s front doors, visitors are startled to see another massive erratic precariously wedged overhead between W M Retail / cafe the two parallel building walls. Just out of reach it makes an un- usual photo opportunity for visitors who puzzle over how the rock terrace stays in place. From an interpretive standpoint, it is important to Outdoor Classroom realize no actual erratics are present in the Sun Lakes-Dry Falls with Amphitheater State Park landscape. During the floods, water was moving too quickly for erratics to be deposited at Dry Falls - they were car- ried downstream and deposited in the Quincy and Pasco basins many miles away. However, the results of the visioning workshop determined that erratics are an important and exciting flood fea- ture to display at the Dry Falls Visitor Center due to the fact that many travelers saw these unusual landforms in the landscape as they drove the Coulee Corridor. -
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]. -
Walla Walla Subbasin Assessment
Walla Walla Subbasin Assessment General Overview Components Prepared by: Walla Walla Basin Watershed Council Version 2: April 2004 Note: This document was not reviewed or approved by the Subbasin Planning Team, subbasin plan leads, co-managers, or subbasin technical staff. 1 Introduction History and Description of Planning Entity The organization for developing the Walla Walla River Subbasin Plan was comprised of the lead agencies, subcontractors, the Planning Team, the Technical Team, and other governmental and non-governmental organizations that will provide local input. The role of each member group is described below. Lead Agencies and Co-Lead Agency The lead agency for the Oregon portion of the Walla Walla subbasin was the Walla Walla Basin Watershed Council, with the Walla Walla Watershed Foundation serving as its fiscal agent. The co-lead entity for the Washington portion of the subbasin was Walla Walla County. The responsibility of co-leads was to oversee and initiate the planning process and ensure that it was an open and inclusive and there was proper outreach to and input from subbasin stakeholders. Subcontractors The Co-lead entities subcontracted with consultant(s) to perform the following functions: (1) facilitation assistance, (2) public involvement assistance, and (3) report preparation including technical assistance. The consultants’ roles were to facilitate and assist with the coordination of Technical and Planning Team and Working Group meetings. The consultants worked closely with the Technical and Planning Teams and the Working Group, and compiled, edited, and wrote (as appropriate) various sections of all draft and final versions of the assessment, inventory, and management plan components of the subbasin plan. -
Chapter 7. Parks and Recreation Element
1 Chapter 7. Parks and Recreation Element 2 7.1. Introduction 3 Parks, recreational facilities, and open space are generally considered beneficial resources and 4 essential contributors to a community’s quality of life. Located within the County are a number 5 of different types of parks and recreational facilities. 6 The County has not traditionally served as a provider of park and recreation facilities. Local 7 cities, private agencies, federal agencies, and schools have an established history of furnishing 8 these services. 9 The purpose of this element is to evaluate parks and recreation facilities in the County and to 10 develop goals and policies that guide management and coordination of them. 11 7.1.1. Applicable Growth Management Act Goals 12 GMA planning goals that are applicable to the Parks and Recreation Element include the 13 following: 14 . Open space and recreation. Retain open space, enhance recreational opportunities, conserve 15 fish and wildlife habitat, increase access to natural resource lands and water, and develop 16 parks and recreation facilities (Revised Code of Washington [RCW] 36.70A.020(9)). 17 . Public facilities and services. Ensure that those public facilities and services necessary to 18 support development shall be adequate to serve the development at the time the development 19 is available for occupancy and use without decreasing current service levels below locally 20 established minimum standards (RCW 36.70A.020(12)). 21 . Historic preservation. Identify and encourage the preservation of lands, sites, and structures 22 that have historical or archaeological significance (RCW 36.70A.020(13)). 23 Goals described in the Shoreline Management Act (SMA) also support the Parks and Recreation 24 Element. -
INTERIOR/GEOLOGICAL SURVEY USGS· INF -72- 2 !R I) - Electric City-Grand Coulee, Washington the CHANNELED SCABLANDS of EASTERN WASHINGTON
9 INTERIOR/GEOLOGICAL SURVEY USGS· INF -72- 2 !R I) - Electric City-Grand Coulee, Washington THE CHANNELED SCABLANDS OF EASTERN WASHINGTON - The Geologic Story of the Spokane Flood- '(( U.S. GOVERNMENT PRINTING OFFICE , 1976 0 -208-172 F'or sale by the uperint.endent. of Documents, .S. Government Printing Office Washington, D.. 20402- Pric~ 70 cents Lock No. 024 - 001-02507- I nL nlog o. I 19.2: W27/6/974 There is n minimum charge of $1.00 for each mail order A trave ler enterin g th e tal f W as hington fro m th e Eas t crosses a flat-to-rolling country sid o f deep, fertil so il commonly sown with w heat. ontinuing wes twa rd , he abruptly nters a d eply scar red land o f bare bl a k ro k ut by labyrin thine ca nyons and chann el , plunge pools and ro k bas in s, ca ca de and ca tara t ledges, and di playi ng ragged buttes and li ffs, alcoves, im men e gravel bars, and giant ripple marks. Th e traveler has reached the starkly sceni " Chan neled cab lands," and this d ramatic hange in th e landscape may well ca use him to w onder " w hat happ n d here? " Th e answ er- th e grea te t fl ood documented by man. This publica tion, summari zin g th e equence of geologic events that culminated in th e so-call ed ''Spokan Fl ood," w as prepar d in res ponse to a ge neral int re t in geology and a particul ar interes t in th e o ri gin of th e Scab land o ften ex pre sed by th ose ross in g th e State of W as hington. -
THE SPOKANE AQUIFER, WASHINGTON: Its Geologic Origin
THE SPOKANE AQUIFER, WASHINGTON: Its Geologic Origin and Water-Bearing and Water-Quality Characteristics Cover: Aerial view of the Spokane Flood sweep ing southwesterly across the study area (outlined in red) and vicinity. THE SPOKANE AQUIFER, WASHINGTON: Its Geologic Origin and Water-Bearing and Water-Quality Characteristics By Dee Molenaar U.S. GEOLOGICAL SURVEY WATER-SUPPLY PAPER 2265 DEPARTMENT OF THE INTERIOR DONALD PAULHODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE: 1988 For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 Library of Congress Cataloging in Publication Data Molenaar, Dee. The Spokane aquifer, Washington. (U.S. Geological Survey water-supply paper; 2265) Bibliography: p. Supt.ofDocs.no. : 119.13:2265 1. Aquifers Washington (State) Spokane Region. I. Title. II. Series. GB1199.3.W2M651987 553.7'9'0979737 84-600259 PREFACE: WHY THIS REPORT WAS WRITTEN This report was prepared to provide a non The description of the Spokane aquifer technical description and understanding of the includes the geologic story behind its origin Spokane aquifer, one of the world's most pro and its part in the Spokane Valley's hydrologic ductive water-bearing formations. Because the setting. Discussed are the relation among pre aquifer also has a most fascinating geologic ori cipitation over the area (mostly in the head gin, a discussion of the geologic story of the waters of the Spokane River basin), the flow of Spokane area is presented. This should enhance the Spokane River, and the movement of the reader's appreciation of the natural proces water to, through, and from the aquifer. -
Washington State Geology - Fire and Ice Trip
Washington State Geology - Fire and Ice Trip General Links “Fire and Ice” by Robert Frost http://www.poetryfoundation.org/poem/173527 Geologictimepics (Summarizing Washington State’s Geology in 19 photo out-takes) https://geologictimepics.com/2017/09/01/summarizing-washington-state-geology-in-19-photo- out-takes/ Glossary of Geological Volcanic Terms https://volcanoes.usgs.gov/vsc/glossary/ Ice Age Floods in the Pacific Northwest (map) https://iafi.org/iafi/wp-content/uploads/IAF-PacNW-Map.png Missoula Floods https://www.opb.org/television/programs/ofg/episodes/1001/ Northwest Origins - An Introduction to the Geologic History of Washington State http://www.burkemuseum.org/static/geo_history_wa/ Volcano Hazards Program: Cascades Volcano Observatory http://volcanoes.usgs.gov/observatories/cvo/ Mount Saint Helens 360 Degree View of Mount St. Helens from Crater Rim http://mountsthelens.com/360-degree-view.html Mount St. Helens History http://mountsthelens.com/history-1.html Mount St. Helens National Volcanic Monument https://www.fs.usda.gov/recarea/giffordpinchot/recarea/?recid=34143 Mount St. Helens (USGS - 2 websites) https://volcanoes.usgs.gov/volcanoes/st_helens/ https://volcanoes.usgs.gov/volcanoes/st_helens/st_helens_geo_hist_106.html Ape Caves Ape Caves - Map and Guide... http://mountsthelens.com/ape-caves.html Ape Cave Interpretive Site https://www.fs.usda.gov/recarea/giffordpinchot/recarea/?recid=40393 Ape Caves: Washington Trails Association https://www.wta.org/go-hiking/hikes/ape-cave Get Outside in a Cave https://www.visitmtsthelens.com/things-cowlitz-county/mt-st-helens-ape-caves/ -
Mcnary National Wildlife Refuge U.S
McNary National Wildlife Refuge U.S. Fish & Wildlife Service McNary National Wildlife Refuge Comprehensive Conservation Plan / Comprehensive Conservation Plan Management Direction Management Direction Mid-Columbia National Wildlife Refuge Complex 64 Maple Street Burbank, WA 99323 Phone 509/546 8300 Refuge Information 1 800/344 WILD December 2008 The mission of the U.S. Fish and Wildlife Service is working with others to conserve, protect, and enhance fish, wildlife, and plants and their habitats for the continuing benefit of the American people. All photos ©C and G Bartlett Photography Dec. 2008 Vision for the McNary National Wildlife Refuge Stretching along the bend in the middle Columbia River where the waters of the Snake and Walla Walla Rivers join the Columbia, the McNary National Wildlife Refuge links a network of diverse habitats stretching dozens of miles from Richland, Washington, to the Wallula Gap and beyond. The Refuge’s shrub-steppe, basalt cliff, riparian, river islands and aquatic habitats will be managed to fulfill the needs of native fish, wildlife, and plants. By actively restoring habitat, controlling exotic species, and enhancing existing habitats and resources, the Refuge will serve as an anchor for biodiversity and a model for habitat restoration and land management. Just as the Columbia River is an important corridor for the transportation of people and goods, it is also an important natural corridor for migratory birds and fish, including endangered salmon and steelhead stocks. Food, rest and sanctuary will be provided for large concentrations of migratory and wintering waterfowl and shorebirds using the Refuges each year. Extensive corridors of riparian and floodplain habitat will be restored and enhanced for nesting and migrating neo-tropical songbirds.