Pdf) That Provides an Overview of the Earthquake, the Tsunami Warning Timeline, and Recommendations for Future Response

Total Page:16

File Type:pdf, Size:1020Kb

Pdf) That Provides an Overview of the Earthquake, the Tsunami Warning Timeline, and Recommendations for Future Response G E O L O G Y F A N O D T N M I E N M E T R R A A L P I E N D D U N S O T G R E I R E S O 1937 Oregon Department of Geology and Mineral Industries Volume 67, Number 1, Fall 2006 3 Recent geologic history of the upper White River valley 7 Response to 1998 debris fl ow in the upper White River valley 11 USGS debris fl ow fl ume at H. J. Andrews Experimental Forest 15 Field trip guide to the geology of the Lower Crooked River Basin 25 MLRR Program 2005 Mined Land Reclamation Awards Also in this issue: Agency News Recent DOGAMI publications Recent dissertations & theses related to Oregon geology Oregon seismicity in 2005 TO OUR READERS — Welcome back! From the State Geologist: In this issue of Oregon Geology, we play catch-up since our last issue of Fall 2004 by publish- ing a set of articles that have been languishing for some time and by summarizing recent agency activities. We want to continue to publish articles on Oregon's unique geology, but we can't do it without your submissions! See page 35 for contributor guidelines. — Vicki S. McConnell Agency News you can view online Oregon stratigraphy, rock type, and Geologic Mapping Section rock property theme maps on topographic and shaded Our first priority remains completion of the statewide digi- relief backdrops. tal compilation map, now in its third year. To this end, we The Oregon Geologic Map Advisory Committee has have completed and released the second version of the advised DOGAMI and its partners to complete mapping of Oregon Geologic Data Compilation. OGDC-2 incorporates the Southern portion of the state, including the Klamath a digital and spatial database for northeast and southeast Falls, Medford, and Cape Blanco 1:250,000 scale quad- Oregon with the central portion of the state being added rangles. This compilation will incorporate new mapping to the compilation in winter 2006. We anticipate this proj- by DOGAMI in the Klamath Basin and Grants Pass areas. ect and the final digital model to be our primary mapping The Southern Willamette Valley was previously defined by product, with completion by 2010. A subset of the Oregon the Committee as a multi-year, multi-quadrangle project Geologic Data Compilation from the first two years is also in 2004 but was only partially funded by USGS. We now now available to view on our website, http://www.oregon- propose to map up to four quads in the area. South coast geology.com (Figure 1, page 13). Using data from OGDC-2, urban areas were identified as high priority for mapping (Continued on page 13) Mineral Land Regulation and Reclamation Program: 229 Broadalbin OREGON GEOLOGY Street SW, Albany 97321-2246, phone (541) 967-2039, FAX (541) 967- (ISSN 0164-3304) 2075. Gary W. Lynch, Assistant Director of Regulation. VOLUME 67, NUMBER 1 FALL 2006 The Nature of the Northwest Information Center: Suite 177, 800 NE Published in Spring and Fall by the Oregon Department of Geology and Mineral Industries on its web Oregon St. # 5, Portland, OR 97232-2162, phone (503) 872-2750, FAX site http://www.oregongeology.com. (Volumes 1 through 40 were entitled The Ore Bin.) (971) 673-1562. Internet: http://www.naturenw.org Governing Board Donald J. Haines, Manager. Donald A. Haagensen, Chair . .Lake Oswego Permission is granted to reprint information contained herein. Steve Macnab. Bend Credit given to the Oregon Department of Geology and Mineral In- Barbara P. Seymour . .Oceanside dustries for compiling this information will be appreciated. Vera Simonton . .Pendleton State Geologist . Vicki S. McConnell Cover photo Assistant Director . .Don Lewis The White River Bridge on Oregon Route 35, east of Editor . Deb Schueller Mount Hood, after the debris flow events of early No- Main Office: Suite 965, 800 NE Oregon Street # 28, Portland vember 2006. Note the blue-jacketed person standing 97232, phone (971) 673-1555, FAX (971) 673-1562. in the channel near the center of the bridge span. The Internet: http://www.oregongeology.com debris deposit is roughly 4–6 m high on the upslope Baker City Field Office: 1510 Campbell Street, Baker City 97814, phone side of the bridge. Debris completely filled the chan- (541) 523-3133, FAX (541) 523-5992. nel and overtopped the bridge deck, so total debris Mark L. Ferns, Geologist, Eastern Oregon Section Leader. flow depth reached more than 6 m. [Route 35 was Coastal Field Office: 313 SW Second Street, Suite D, Newport 97365, re-opened December 9, 2006.] phone (541) 574-6642, FAX (541) 265-5241. Jonathan C. Allan, Geologist, Coastal Section Leader. Photo contributed by William J. Burns, DOGAMI. Grants Pass Field Office: 5375 Monument Drive, Grants Pass 97526, phone (541) 476-2496, FAX (541) 474-3158. Thomas J. Wiley, Geologist, Southwest Oregon Section Leader. 2 OREGON GEOLOGY, VOLUME 67, NUMBER 1, FALL 2006 Recent geologic history of the upper White River valley, Oregon by Thomas G. DeRoo, Mount Hood National Forest Headquarters, 16400 Champion Way, Sandy, OR 97055 About 12,000 years ago two major clastic flows from the Old Maid erup- landscape-shaping processes were tive period partially filled the upper waning in the upper White River val- valley with large amounts of loose ley (Figures 1 and 2): a glacier from volcanic material, forming a deposi- the last major ice age had either melt- tional surface that extended roughly Mt. Hood ed entirely or retreated substantially, to the entrance to the narrow White and the Polallie eruptive period had River canyon, about 850 m in eleva- ended. The White River was adjusting tion. At least one lahar reached Tygh to the lahar deposits and pyroclastic- Valley and covered the valley floor upper White flow deposits that partially filled the there (Cameron and Pringle, 1987). River valley valley. For most of the next 12,000 The loose material in the upper years the White River valley was prob- valley eroded rapidly. Runoff from ably free of major geologic changes. intense rainstorms cut large gullies in The river and slope processes devel- the more steeply sloped fill material oped a relatively stable valley that in the upper valley. Most of the sedi- was forested up to at least 1675 m ment was transported by debris flows elevation (Scott, 1995) and probably that deposited coarser-sized particles Figure 1. Study area location. The yellow resembled other major river valleys of above 1030 m elevation. Subsequent polygon outlines the upper White River the region. flood events and debris flows contin- valley. The white line transecting the poly- About 220 years ago a remarkable ued building an alluvial fill or fan that gon is Oregon Route 35. change occurred. Lahars and pyro- (Continued on page 5) Figure 2. Looking down the White River Glacier from 2440 m elevation. Three subparallel drainages that converge at the head of the alluvial fan are visible in the upper half of the photo. (9-10-98 photo) OREGON GEOLOGY, VOLUME 67, NUMBER 1, FALL 2006 3 Released July 14, 2006: RECENT DOGAMI PUBLICATIONS The following individually released publications comprise the USGS STATEMAP 2002 deliverable (originally bundled together as Open-file report Publications are available from: Nature of the Northwest, 800 O-03-11): • Preliminary geologic map of the Eugene East and Eugene West NE Oregon St., #5, Portland, OR 97232, [email protected], (503) quadrangles, Lane county, Oregon, by Ian P. Madin and Robert B. 872-2750; or from the DOGAMI field offices in Baker City, Murray. Open-file report O-06-17. 1 CD, $10. 1510 Campbell Street, (541) 523-3133, and Grants Pass, 5375 • Preliminary geologic map of the Gold Hill and Rogue River 7.5 Monument Drive, (541) 476-2496. For online purchasing, go minute quadrangles, Jackson and Josephine counties, Oregon, by Thomas J. Wiley. Open-file report O-06-18. 1 CD, $10. to http://www.naturenw.org, select “Store” and “Maps and • Geology of the Upper Grande Ronde River Basin, Union county, Reports” and use the short identification of the publication Oregon, by Mark L. Ferns, Vicki S. McConnell, Ian P. Madin, and Jenda (e.g., RMS-1) for a search. A. Johnson. Open-file report O-06-19. 1 CD, $10. • Preliminary geologic map of the Service Buttes, Echo, Nolin, Look online (http://www.oregongeology.com) for: Barnhart, and Pendleton 7.5 minute quadrangles (west to east), Umatilla County, Oregon [map only; no text], by Vicki S. McConnell. • All Ore Bin and Oregon Geology past issues− Open-file report O-06-20. 1 CD, $10. http://www.oregongeology.com/sub/quarpub/OrGeo.htm The following individually released publications comprise the USGS • All Geologic Map Series (GMS) maps− STATEMAP 2003 deliverable: http://www.oregongeology.com/sub/publications/GMS/gms.htm • Oregon statewide geologic map data: A pilot project where digi- • Oregon Geologic Data Compilation (OGDC) interactive map− tal techniques changed the geologic map compilation process http://www.oregongeology.com/sub/ogdc/index.htm and product, by Mark L. Ferns, Ronald P. Geitgey, Margaret D. Jenks, Lina Ma, Ian P. Madin, Vicki S. McConnell, and Paul E. Staub. Open-file report O-06-03. 1 CD, $10. (Complete data set for northeast Oregon Released February 17, 2006: released as OGDC-1, July 12, 2005.) • Geoanalytical information layer for Oregon (GILO) -- Release 1, • Preliminary geologic map of the Wimer and McConville Peaks northeast Oregon, by Mark L. Ferns and Vicki S. McConnell. GILO rel. 7.5 minute quadrangles, Jackson and Josephine counties, Or- 1. 1 CD, $10. egon, by Thomas J. Wiley. Open-file report O-06-05.
Recommended publications
  • Environmental Assessment Mt. Hood
    Forest Service PaCiflC Northwest Region Environmental Assessment Mt. Hood National Forest a: USDA Forest Service nagement White River National Wild and Scenic River Environmental Assessment Deciding Officials: Mike Edrington, Forest Supervisor Mt. Hood National Forest 2955 N.W. Division Gresham, OR 97030 James L. Hancock, District Manager Prineville District: Bureau of Land Management 185 E. 4th Street Prineville, OR 97754 For Further Information: Diana L. Ross Mt. Hood National Forest Bear Springs Ranger District (503) 328-6211 Berry Phelps Bureau of Land Management Prineville District Office (503) 447-4115 TABLE OF CONTENTS Chapter I : Need for the Proposal ....... , ..................... , II l-l Introduction ............................................. 1-I PurposeandNeed ....................................... l-l The Decisions Needed. ................................... l-l Background ............................................. l-l Legislation ........................................... I-l Planning Mandate ..................................... I-2 Summary of the Resource Assessment ..................... I-6 Issues ................................................. l-8 Existing Plans, Policies, and Agreements ...................... l-l 5 US Forest Service ..................................... l-15 Bureau of Land Management ............................ I-l 5 US Fish and Wildlife Service ............................. I-l 5 Conferated Tribes of the Warm Springs Reservation of Oregon . I-l 6 Land Conservation and Development and County
    [Show full text]
  • Analysis of 1997–2008 Groundwater Level Changes in the Upper Deschutes Basin, Central Oregon
    Prepared in cooperation with the Oregon Water Resources Department Analysis of 1997–2008 Groundwater Level Changes in the Upper Deschutes Basin, Central Oregon Scientific Investigations Report 2013–5092 U.S. Department of the Interior U.S. Geological Survey Cover: Upper Left: Irrigation diversion dam on the Deschutes River in Bend, Oregon, May 2002. Upper Right: Groundwater-fed wetland between Cultus Lake and Crane Prairie Reservoir, August 2012. Lower Left: Headwater spring feeding Fall River, Oregon, May 2002. Lower right: Strata of the Deschutes Formation and overlying lavas exposed along the Crooked River, May 2002. All photographs taken by Marshall Gannett, U.S. Geological Survey. Analysis of 1997–2008 Groundwater Level Changes in the Upper Deschutes Basin, Central Oregon By Marshall W. Gannett and Kenneth E. Lite, Jr. Prepared in cooperation with the Oregon Water Resources Department Scientific Investigations Report 2013–5092 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2013 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S.
    [Show full text]
  • Analysis of 1997–2008 Groundwater Level Changes in the Upper Deschutes Basin, Central Oregon
    Prepared in cooperation with the Oregon Water Resources Department Analysis of 1997–2008 Groundwater Level Changes in the Upper Deschutes Basin, Central Oregon Scientific Investigations Report 2013–5092 U.S. Department of the Interior U.S. Geological Survey Cover: Upper Left: Irrigation diversion dam on the Deschutes River in Bend, Oregon, May 2002. Upper Right: Groundwater-fed wetland between Cultus Lake and Crane Prairie Reservoir, August 2012. Lower Left: Headwater spring feeding Fall River, Oregon, May 2002. Lower right: Strata of the Deschutes Formation and overlying lavas exposed along the Crooked River, May 2002. All photographs taken by Marshall Gannett, U.S. Geological Survey. Analysis of 1997–2008 Groundwater Level Changes in the Upper Deschutes Basin, Central Oregon By Marshall W. Gannett and Kenneth E. Lite, Jr. Prepared in cooperation with the Oregon Water Resources Department Scientific Investigations Report 2013–5092 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2013 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S.
    [Show full text]
  • Lower White River Wilderness Area Brochure
    LOWER WHITE RIVER The United States Congress designated the Low- er White River Wilderness in 2009 and it now has a total of 2,806 acres. All of this wilderness is lo- cated in Oregon and is managed by the Bureau of Land Management and the U.S. Forest Service. The White River rises in the high Cascades in western Wasco County, in the Mount Hood Na- tional Forest on the southeast flank of Mount Hood. The headwaters are just below White River Glacier in White River Canyon. Additions to the Mount Hood Wilderness protect upper por- tions of the river, while the Lower White River Wilderness, southeast of the majestic Mount Hood Wilderness and east of highway 26, protect a segment of lower White River stretch. Be sure to contact the BLM’s Prineville District or the Mt. Hood National Forest for the latest con- ditions and access to the spectacular Lower White River Wilderness Area! LOWER WHITE RIVER WILDERNESS s 0.5 ·0 •·0.5 1 Mile 0.5 0 0.5 1 Kilometer Surface m"""''o..- and lond OW!IOI8tip lo oubjact ID ongoing chango. Contacl the BLM Plilovillo Diotrict ollico for furlhor infonnotion. LEGEND Administered Land c::::J Lower White River/White River Forest Service Collector c==J US Forest Service Wilderness Boundary Road Number Bureau of Land Management BLM Lower White River 270 Forest Service Local c==J Wilderness Road Number 490A c:::::J State US Forest Service Forest Service - White Riwr Wilderness Trail Numbe - Warm Springs Indian State Highway Reservation - Existing Wild and Scenic River Paved Road c==J Private or Other No warnonty lo modo by tho Bureou or Land Uon_.ont 00 lo lho oocuraoy, noiobil~ or oomplatanooa of u- - for ;..-.al or Other Road aggregate ...., wllh olhor dlda.
    [Show full text]
  • United States Department of the Interior Geological Survey
    UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Bibliographies and location maps of publications on aeromagnetic and aeroradiometric surveys for the states west of approximately 104° longitude (exclusive of Hawaii and Alaska) by Patricia L. Hill Open-File Report 91-370-A 1991 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards. TABLE OF CONTENTS Page General Information.................................................... 2 Arizona................................................................ 4 California............................................................. 18 Colorado............................................................... 41 Idaho.................................................................. 54 Montana................................................................ 67 Nevada................................................................. 80 New Mexico ............................................................. 101 Oregon................................................................. 113 Utah................................................................... 122 Washington............................................................. 135 Wyoming................................................................ 145 Western Area DOE-NURE .................................................. 153 rev. 3-1-91 GENERAL INFORMATION FOR THE AEROMAGNETIC AND AERORADIOMETRIC INDEXES Bibliographies and location maps of selected publications containing aeromagnetic
    [Show full text]
  • Comprehensive Plan
    Deschutes County Transportation System Plan 2010 - 2030 Adopted by Ordinance 2012-005 August 6, 2012 By The Deschutes County Board of Commissioners EXHIBIT C ORDINANCE 2012-005 Page 1 of 268 TABLE OF CONTENTS Executive Summary ...................................................................................................... 10 Chapter One Introduction ...................................................................................................................................30 1.1 Geographic Setting .......................................................................................................30 1.2 Transportation Planning ..............................................................................................31 Goal 12 .....................................................................................................................31 Transportation Planning Rule (TPR) ..................................................................31 TPR Requirements for Deschutes County ......................................................33 1.3 Major Changes Since the Adoption of the 1998 Plan ...........................................35 Regional Growth and Destination Resorts ......................................................35 Urban Growth and County Coordination .......................................................36 Public Transportation ...........................................................................................36 Financial Impacts ....................................................................................................37
    [Show full text]
  • The Geology and Hydrothermal Alteration of the Bear Creek Butte Area, Crook County, Central Oregon
    Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 1986 The geology and hydrothermal alteration of the Bear Creek Butte area, Crook County, central Oregon Richard Matthew Wilkening Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geology Commons, Hydrology Commons, and the Mineral Physics Commons Let us know how access to this document benefits ou.y Recommended Citation Wilkening, Richard Matthew, "The geology and hydrothermal alteration of the Bear Creek Butte area, Crook County, central Oregon" (1986). Dissertations and Theses. Paper 3656. https://doi.org/10.15760/etd.5542 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. AN ABSTRACT OF THE THESIS OF Richard Matthew Wilkening for the Masters of Science in Geology presented April, 24, 1986. Title: The Geology and Hydrothermal Alteration of the Bear Creek Butte area, Crook County, Central Oregon: APPROVED BY THE MEMBERS OF THE THESIS COMMITTEE: ummings, Chairman Dr. Robert O. Van Atta The Eocene Clarno Formation, the Oligocene John Day Formation and basalts of the High Lava Plains are exposed in the Bear Creek Butte area in Central Oregon. In this area the Clarno Formation can be divided into a lower sequence composed of intermediate lava flows with intercalated mudf lows and volcaniclastic sediments and an upper sequence of rhyolite and basalt flows and felsic ruffs. Separating the two units is a well developed 2 saprolite.
    [Show full text]
  • Field Guides
    Downloaded from fieldguides.gsapubs.org on May 6, 2011 Field Guides Paleogene calderas of central and eastern Oregon: Eruptive sources of widespread tuffs in the John Day and Clarno Formations Jason D. McClaughry, Mark L. Ferns, Martin J. Streck, Karyn A. Patridge and Caroline L. Gordon Field Guides 2009;15;407-434 doi: 10.1130/2009.fld015(20) Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Field Guides Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. Notes © 2009 Geological Society of America Downloaded from fieldguides.gsapubs.org on May 6, 2011 The Geological Society of America Field Guide 15 2009 Paleogene calderas of central and eastern Oregon: Eruptive sources of widespread tuffs in the John Day and Clarno Formations Jason D.
    [Show full text]
  • Geologic Framework of the Regional Ground-Water Flow System in the Upper Deschutes Basin, Oregon
    Cover photographs: Top: Steelhead Falls on the Deschutes River near Crooked River Ranch, Oregon. Middle: Crooked River Canyon at Crooked River Ranch, Oregon. Bottom: North and Middle Sister with a wheel-line irrigation system in the foreground near Sisters, Oregon. (Photographs by Rodney R. Caldwell, U.S. Geological Survey.) U.S. Department of the Interior U.S. Geological Survey Geologic Framework of the Regional Ground-Water Flow System in the Upper Deschutes Basin, Oregon By KENNETH E. LITE JR. and MARSHALL W. GANNETT Water-Resources Investigations Report 02–4015 Prepared in cooperation with Oregon Water Resources Department; Cities of Bend, Redmond, and Sisters; Deschutes and Jefferson Counties; The Confederated Tribes of the Warm Springs Reservation of Oregon; and U.S. Environmental Protection Agency Portland, Oregon 2002 U. S. DEPARTMENT OF THE INTERIOR GALE A. NORTON, Secretary U.S. GEOLOGICAL SURVEY CHARLES G. GROAT, Director The use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. For additional information: Copies of this report may be purchased from: District Chief U.S. Geological Survey USGS Information Services 10615 S.E. Cherry Blossom Dr. Box 25286 Portland, OR 97216-3103 Denver, CO 80225-0286 E-mail: [email protected] Telephone: 1-888-ASK-USGS Internet: http://or.water.usgs.gov Suggested citation: Lite, K.E., Jr., and Gannett, M.W., 2002, Geologic framework of the regional ground-water flow system in the upper Deschutes Basin, Oregon: U.S. Geological Survey Water-Resources Investigations Report 02–4015, p.
    [Show full text]
  • White River Watershed Assessment
    5/25/2004 White River Watershed Assessment White River Watershed Assessment Prepared by Wasco County Soil and Water Conservation District For White River Watershed Council Principal Authors: Karen Lamson Jennifer Shannon Clark, Wasco County Soil and Water Conservation District The Dalles OR. Walkin’plow near Pine Grove from Chaff in the Wind, published by Friends of Maupin Library Copies of the White River Watershed Assessment are available in electronic or paper format from [email protected], or by contacting Wasco County SWCD at 2325 River Road, Suite 3, The Dalles OR 97058 or (541) 296-6178 x119. 1 5/25/2004 White River Watershed Assessment 2 5/25/2004 White River Watershed Assessment Introduction This Assessment has been undertaken by the White River Watershed Council, in partnership with the Wasco County Soil and Water Conservation District. The purpose of the Assessment is to provide a description of conditions and trends in the White River Watershed relevant to conservation of its natural resources. The objective is to discover where natural resources or processes are working, and where they need to be restored, particularly in regards to fish habitat and water quality. The term “watershed” describes an area of land that drains downslope to the lowest point. A watershed consists of a network of drainage pathways that can be underground, or on the surface. These pathways converge into a stream and river system as the water moves downstream. The White River Watershed includes all of the waters that drain into the White River, between its headwaters on the flanks of Mt.
    [Show full text]
  • Oregon Natural Areas Plan
    Portland State University PDXScholar Institute for Natural Resources Publications Institute for Natural Resources - Portland 2010 Oregon Natural Areas Plan Oregon Natural Heritage Advisory Council Let us know how access to this document benefits ouy . Follow this and additional works at: http://pdxscholar.library.pdx.edu/naturalresources_pub Part of the Natural Resources and Conservation Commons, and the Sustainability Commons Citation Details Oregon Natural Heritage Advisory Council. 2010. Oregon Natural Areas Plan. Oregon Biodiversity Information Center, Institute for Natural Resources – Portland, Portland State University, Portland, OR. 198pp. This Technical Report is brought to you for free and open access. It has been accepted for inclusion in Institute for Natural Resources Publications by an authorized administrator of PDXScholar. For more information, please contact [email protected]. Oregon Natural Areas Plan 2010 Natural Heritage Advisory Council to the State Land Board State Land Board Kate Brown Ted Kulongoski Ted Wheeler Secretary of State Governor State Treasurer Natural Heritage Advisory Council Voting Members Richard Brown Robert Chandler Stuart Garrett Charles Carter Alan Dickman Cathy Macdonald Ex-Officio Members Agriculture Director: Katy Coba, represented by Rebecca Currin Fish and Wildlife Director: Roy Elicker, represented by Holly Michaels Forestry Director: Marvin Brown, represented by Andrew Yost Higher Education Chancellor: George Pernsteiner, represented by Scott Heppell Parks and Recreation Director: Tim Wood,
    [Show full text]
  • Geology of Oregon Orr Orr.Pdf
    Fifth Edition Geology of Oregon Elizabeth L. Orr William N. Orr University of Oregon Cover: Ripple-marked sand dunes on the Oregon Coast resemble a gigantic fingerprint (photo by Gary Tepfer). Copyright ® 1964 by Ewart M. Baldwin Copyright ® 1976, 1981, 1992, 2000 by Kendall/Hunt Publishing Company ISBN 0-7872-6608-6 All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, without the prior written permission of the copyright owner. Printed in the United States of America 10 98765432 Table of Contents Introduction 1 History of geologic study in Oregon 9 Blue Mountains 21 Klamath Mountains 51 Basin and Range 79 High Lava Plains 103 Deschutes-Columbia Plateau 121 Cascade Mountains 141 Coast Range 167 Willamette Valley 203 Bibliography 223 Glossary 245 Index 251 iii Dedicated to the graduates Acknowledgments Between the fourth and fifth editions of Geology of Oregon, the importance of global tectonics to the state has been ingrained even deeper. Riding on the leading edge of the moving North American plate, Oregon reflects the underlying mecha- nism of the plate collision boundary in virtually all aspects of its geology. In the seven years since the fourth edition was written, an irregular but continuing drumbeat of earthquakes reminds us of the forces beneath our feet and the need to prepare for catastrophic changes be they quakes, volcanoes, tsunamis, floods, or massive earth movements. Most profound is the discovery of irrefutable evidence that these catastrophes have been visited on the state quite regularly over the past few thousands of years as well as the absolute surety that similar disasters will oc- cur in the near and distant future.
    [Show full text]