DOCSLIB.ORG

City of Rocks National Reserve Geologic Resources Inventory Report

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

National Park Service U.S. Department of the Interior Natural Resource Program Center City of Rocks National Reserve Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2010/191 THIS PAGE: View from East Ridge to the east overlooking City of Rocks National Reserve. Features called “panholes” result from weathering processes and are found atop some of the granite exposures within the reserve. Panholes, such as this one, can fill with water following rains. ON THE COVER: Stripe Rock is one of numerous granite exposures in City of Rocks National Reserve. The large number and distribution of these features led emigrants to christen the area a “City of Rocks.” National Park Service photographs by Wallace Keck. City of Rocks National Reserve Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2010/191 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 April 2010 U.S. Department of the Interior National Park Service Natural Resource Program Center Ft. Collins, Colorado The National Park Service, Natural Resource Program Center publishes a range of reports that address natural resource topics of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. This report received informal peer review by subject-matter experts who were not directly involved in the collection, analysis, or reporting of the data. Views, statements, findings, conclusions, recommendations, and data in this report are those of the author(s) and do not necessarily reflect views and policies of the National Park Service, U.S. Department of the Interior. Mention of trade names or commercial products does not constitute endorsement or recommendation for use by the National Park Service. Printed copies of this report are produced in a limited quantity and they are only available as long as the supply lasts. This report is available from the Geologic Resources Inventory website (http://www.nature.nps.gov/geology/inventory/gre_publications.cfm) and the Natural Resource Publications Management website (http://www.nature.nps.gov/publications/ NRPM). Please cite this publication as: Thornberry-Ehrlich, T. 2010. City of Rocks National Reserve: geologic resources inventory report. Natural Resource Report NPS/NRPC/GRD/NRR—2010/191. National Park Service, Ft. Collins, Colorado. NPS 003/102081, April 2010 ii NPS Geologic Resources Division Contents List of Figures ................................................................................................................ iv Executive Summary ....................................................................................................... v Acknowledgements ...................................................................................................... vi Credits ........................................................................................................................................................................ vi Introduction ................................................................................................................... 1 Purpose of the Geologic Resources Inventory ............................................................................................................... 1 Park Setting ................................................................................................................................................................. 1 Geologic Setting .......................................................................................................................................................... 1 Geologic Issues .............................................................................................................. 5 Erosion and Slope Processes ......................................................................................................................................... 5 Joints and Fragile Features ........................................................................................................................................... 6 Recreational Demands ................................................................................................................................................. 6 Mine-Related Issues and Disturbed Lands ..................................................................................................................... 7 Water Issues ................................................................................................................................................................ 7 Wind Erosion ............................................................................................................................................................... 7 Seismicity ..................................................................................................................................................................... 8 Volcanism .................................................................................................................................................................... 8 General Geology and Research..................................................................................................................................... 8 Geologic Features and Processes ................................................................................ 11 Introduction ............................................................................................................................................................... 11 Joint Sets ................................................................................................................................................................... 11 Landform Types and Geomorphological Evolution ...................................................................................................... 11 Weathering Processes ................................................................................................................................................ 13 Historical Connections with Geology .......................................................................................................................... 14 Albion Mountains Metamorphic Core Complex .......................................................................................................... 14 Basin-and-Range Features and Almo Fault .................................................................................................................. 15 Map Unit Properties .................................................................................................... 25 Map Units within City of Rocks National Reserve ........................................................................................................ 25 Geologic History .......................................................................................................... 29 Precambrian (prior to 542 million years ago) ............................................................................................................... 29 Paleozoic Era (542 to 251 million years ago) ............................................................................................................... 29 Mesozoic Era (251 to 65.5 million years ago) .............................................................................................................. 29 Cenozoic Era (65.5 million years ago until today) ........................................................................................................ 30 Glossary ........................................................................................................................ 35 Literature Cited ............................................................................................................ 39 Appendix A: Overview of Digital Geologic Data ....................................................... 43 Appendix B: Scoping Meeting Participants ................................................................ 45 Attachment 1: Geologic Resources Inventory Products CD CIRO Geologic Resources Inventory Report iii List of Figures Figure 1. Maps of City of Rocks National Reserve and the surrounding area .....................................................................3 Figure 2. Rockfalls are a potential geologic hazard throughout City of Rocks National Reserve ........................................ 10 Figure 3. These photos illustrate the use of restoration projects to restore disturbed areas .............................................. 10 Figure 4. Three mechanisms by which joints form in granitic rocks ................................................................................. 16 Figure 5. Aerial image of the central area of City of Rocks National Reserve ...................................................................
Recommended publications
  • 2448, Raft River Mountains Fault

    2448, Raft River Mountains Fault

    2448, RAFT RIVER MOUNTAINS FAULT Structure number: 2448. Comments: Hecker's (1993) fault number 6-17. Structure name: Raft River Mountains fault. Comments: Synopsis: Poorly understood middle to late Pleistocene(?) fault in the Raft River Mountains. The fault is in both Utah and Idaho. Date of compilation: 10/99. Compiler and affiliation: Bill D. Black (Utah Geological Survey) and Suzanne Hecker (U.S. Geological Survey). State: Utah. County: Box Elder. 1° x 2° sheet: Brigham City. Province: Basin and Range. Reliability of location: Poor. Comments: Mapped by Compton (1972) and Doelling (1980). Mapping from Doelling (1980). Geologic setting: North-trending normal fault near the Utah-Idaho border along the northeast side of the Raft River Mountains. The Raft River Mountains have a core of Precambrian metamorphic rocks and trend east-west, similar to the Uinta Mountains. Northern slopes of the mountains drain into the Snake River and are considered part of the Snake River Plain, rather than the Great Basin. Sense of movement: N. Comments: Dip: No data. Comments: Dip direction: E. Geomorphic expression: Faulted alluvium. Age of faulted deposits: Middle to late Pleistocene(?). Paleoseismology studies: None. Timing of most recent paleoevent: (4) Middle and late Quaternary (<750 ka). Comments: Recurrence interval: No data. Comments: Slip rate: Unknown, probably <0.2 mm/yr. Comments: Length: End to end (km): 2 Cumulative trace (km): 2 Average strike (azimuth): N1°E REFERENCES Compton, R.R., 1972, Geologic map of the Yost quadrangle, Box Elder County, Utah and Cassia County, Idaho: U.S. Geological Survey Miscellaneous Investigations Series Map I-672, scale 1:31,680.
  • Timan-Pechora Basin Province, Russia, 2008

    Timan-Pechora Basin Province, Russia, 2008

    Assessment of Undiscovered Oil and Gas Resources of the Timan-Pechora Basin Province, Russia, 2008 40°E 45°E 50°E 55°E 60°E 65°E 70°E Using a geology-based assessment methodology, the 70°N U.S. Geological Survey (USGS) estimated means of 1.6 billion barrels of undiscovered oil and 9 trillion cubic feet of natural gas north of the Arctic Circle in the Timan- BARENTS Pechora Basin Province of Russia. SEA KARA SEA Introduction The U.S. Geological Survey (USGS) recently assessed PAY-KHOY RIDGE the undiscovered oil and gas potential of the Timan-Pechora Basin Province in Russia as part of the USGS Circum-Arctic NORTHWEST Arctic Circle IZHMA Oil and Gas Resource Appraisal program. Geologically, A DEPRESSION the Timan-Pechora Basin Province is a triangular-shaped AU MAIN BASIN PLATFORM AU cratonic block bounded by the northeast-southwest trend- 65°N ing Ural Mountains and the northwest-southeast trending Timan Ridge. The northern boundary is shared with the BASINS AU South Barents Sea Province (fig. 1). The Timan-Pechora A’ Basin Province has a long history of oil and gas exploration S IN TA and production. The first field was discovered in 1930 and, N U O after 75 years of exploration, more than 230 fields have been TIMAN RIDGE M discovered and more than 5,400 wells have been drilled. This L A R has resulted in the discovery of more than 16 billion barrels U of oil and 40 trillion cubic feet of gas. Several studies have presented geological summaries FOREDEEP RUSSIA of the Timan-Pechora Basin Province and the potential for its remaining oil and gas resources (for example, Ulmishek, 1982; Lindquist, 1999; Ulmishek, 2000).
  • Research Natural Areas on National Forest System Lands in Idaho, Montana, Nevada, Utah, and Western Wyoming: a Guidebook for Scientists, Managers, and Educators

    Research Natural Areas on National Forest System Lands in Idaho, Montana, Nevada, Utah, and Western Wyoming: a Guidebook for Scientists, Managers, and Educators

    USDA United States Department of Agriculture Research Natural Areas on Forest Service National Forest System Lands Rocky Mountain Research Station in Idaho, Montana, Nevada, General Technical Report RMRS-CTR-69 Utah, and Western Wyoming: February 2001 A Guidebook for Scientists, Managers, and E'ducators Angela G. Evenden Melinda Moeur J. Stephen Shelly Shannon F. Kimball Charles A. Wellner Abstract Evenden, Angela G.; Moeur, Melinda; Shelly, J. Stephen; Kimball, Shannon F.; Wellner, Charles A. 2001. Research Natural Areas on National Forest System Lands in Idaho, Montana, Nevada, Utah, and Western Wyoming: A Guidebook for Scientists, Managers, and Educators. Gen. Tech. Rep. RMRS-GTR-69. Ogden, UT: U.S. Departmentof Agriculture, Forest Service, Rocky Mountain Research Station. 84 p. This guidebook is intended to familiarize land resource managers, scientists, educators, and others with Research Natural Areas (RNAs) managed by the USDA Forest Service in the Northern Rocky Mountains and lntermountain West. This guidebook facilitates broader recognitionand use of these valuable natural areas by describing the RNA network, past and current research and monitoring, management, and how to use RNAs. About The Authors Angela G. Evenden is biological inventory and monitoring project leader with the National Park Service -NorthernColorado Plateau Network in Moab, UT. She was formerly the Natural Areas Program Manager for the Rocky Mountain Research Station, Northern Region and lntermountain Region of the USDA Forest Service. Melinda Moeur is Research Forester with the USDA Forest Service, Rocky Mountain ResearchStation in Moscow, ID, and one of four Research Natural Areas Coordinators from the Rocky Mountain Research Station. J. Stephen Shelly is Regional Botanist and Research Natural Areas Coordinator with the USDA Forest Service, Northern Region Headquarters Office in Missoula, MT.
  • High Resolution Adobe PDF

    High Resolution Adobe PDF

    115°20'0"W 115°0'0"W 114°40'0"W 114°20'0"W PISTOL LAKE " CHINOOK MOUNTAIN ARTILLERY DOME SLIDEROCK RIDGE FALCONBERRY PEAK ROCK CREEK SHELDON PEAK Red Butte "Grouse Creek Peak WHITE GOAWTh iMte OVaUlleNyT MAoIuNntain LITTLE SOLDIER MOUNTAIN N FD " N FD 6 8 8 T d Parker Mountain 6 Greyhound Mountain r R a k i e " " 5 2 l e 0 1 0 r 0 0 il 1 C l i a 1 n r o Big Soldier Mountain a o e pi r n Morehead Mountain T Pinyon Peak L White MoSunletain g Deer Rd " T " HONEYMOON LAKE " " BIG SOLDIER MOUNTAIN SOLDIER CREEK GREYHOUND MOUNTAIN PINYON PEAK CASTO SHERMAN PEAK CHALLIS CREEK LAKES TWIN PEAKS PATS CREEK Lo FRANK CHURCH - RIVER OF NO RETURN WILDERNESS o n Sherman Peak C Mayfield Peak Corkscrew Mountain r " d e " " R ek ls R l d a Mosquito Flat Reservoir F r e Langer Peak rl g T g k a Ruffneck Peak " ac d D P R d " k R Blue Bunch Mo"untain d e M e k R ill C r e Bear Valley Mountain k e e htmile r " e ig C r E C en r C re d ave Estes Mountain e G ar B e k " R BLUE BUNCH MOUNTAIN d CAPE HORN LAKES LANGER PEAK KNAPP LAKES MOUNT JORDAN l Forest CUSTER ELEVENMILE CREEK BAYHORRSaEm sLhAorKn EMountaiBn AYHORSE Nat De Rd Keysto"ne Mountain velop Road 579 d R " Cabin Creek Peak Red Mountain rk Cape Horn MounCtaaipne Horn Lake #1 o Bay d " Bald Mountain F hors R " " e e Cr 2 d e eek 8 R " nk Rd 5 in Ya d a a nt o ou Lucky B R S A L M O N - C H A L L I S N Fo S p M y o 1 C d Bachelor Mountain R q l " u e 2 5 a e d v y 19 p R Bonanza Peak a B"ald Mountain e d e w Nf 045 D w R R N t " s H s H C d " e sf r e o Basin Butte r 0 t U ' o r e F a n e 0 l t 21 t
  • Andalusite, 0.5 to 1 Meter ANDALUSITE Across, and This Grades Into a Zone of Andalusite Al2sio5 Crystals in the Slate (Snelgrove Et Al., 1944)

    Andalusite, 0.5 to 1 Meter ANDALUSITE Across, and This Grades Into a Zone of Andalusite Al2sio5 Crystals in the Slate (Snelgrove Et Al., 1944)

    echelon pegmatites passes into a vein of fine- grained (10 to 30 mm) andalusite, 0.5 to 1 meter ANDALUSITE across, and this grades into a zone of andalusite Al2SiO5 crystals in the slate (Snelgrove et al., 1944). 2. Champion mine: As euhedral crystals to 5 cm One of three polymorphs of Al2SiO5 (the other two are kyanite and sillimanite), andalusite is partially altered to muscovite in quartz. On the primarily a constituent of medium-grade 36th level drift, 45 meters east of Number 7 shaft metamorphic rocks derived from shales. Also, it station: A body of massive andalusite in quartzite occurs very much less commonly as a constituent with chalcopyrite and muscovite, adjacent to a of a few rare pegmatites, some quartz veins, and large quartz vein localized along contact between aluminous hydrothermal replacement deposits. It Negaunee Iron Formation and Goodrich Quartzite is often strongly altered to muscovite. Northern (Babcock, 1966a, b). 3. Republic mine: With co- Peninsula. existing sillimanite in rocks adjacent to fayalitic Negaunee Iron Formation (olivine) (Haase and Klein, 1978). Also in a vein with beryl 300 paces east and 75 north of the western ¼ post of section 17, T46N, R29W. FROM: Robinson, G.W., 2004 Mineralogy of Michigan by E.W. Heinrich updated and revised: published by A.E. Seaman Mineral Museum, Houghton, MI, 252p. Figure 35: Andalusite crystals to 3 cm, coated with muscovite in quartz, from the Champion mine, Champion, Marquette County. A. E. Seaman Mineral Museum specimen No. DM 14850, Jeffrey Scovil photograph. Iron County: SW ¼ SE ¼ section 20, T42N, R3W, Lake Mary quadrangle: Found as 1 cm poikiloblasts in the Michigamme Slate with garnet, staurolite, sillimanite, and sericite (Bayley, 1959).
  • Metamorphic and Metasomatic Kyanite-Bearing Mineral

    Metamorphic and Metasomatic Kyanite-Bearing Mineral

    Metamorphic and Metasomatic Kyanite-Bearing Mineral Assemblages of Thassos Island (Rhodope, Greece) Alexandre Tarantola, Panagiotis Voudouris, Aurélien Eglinger, Christophe Scheffer, Kimberly Trebus, Marie Bitte, Benjamin Rondeau, Constantinos Mavrogonatos, Ian Graham, Marius Etienne, et al. To cite this version: Alexandre Tarantola, Panagiotis Voudouris, Aurélien Eglinger, Christophe Scheffer, Kimberly Tre- bus, et al.. Metamorphic and Metasomatic Kyanite-Bearing Mineral Assemblages of Thassos Island (Rhodope, Greece). Minerals, MDPI, 2019, 10.3390/min9040252. hal-02932247 HAL Id: hal-02932247 https://hal.archives-ouvertes.fr/hal-02932247 Submitted on 7 Sep 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. minerals Article Metamorphic and Metasomatic Kyanite-Bearing Mineral Assemblages of Thassos Island (Rhodope, Greece) Alexandre Tarantola 1,* , Panagiotis Voudouris 2 , Aurélien Eglinger 1, Christophe Scheffer 1,3, Kimberly Trebus 1, Marie Bitte 1, Benjamin Rondeau 4 , Constantinos Mavrogonatos 2 , Ian Graham 5, Marius Etienne 1 and Chantal Peiffert
  • Notice Concerning Copyright Restrictions

    Notice Concerning Copyright Restrictions

    NOTICE CONCERNING COPYRIGHT RESTRICTIONS This document may contain copyrighted materials. These materials have been made available for use in research, teaching, and private study, but may not be used for any commercial purpose. Users may not otherwise copy, reproduce, retransmit, distribute, publish, commercially exploit or otherwise transfer any material. The copyright law of the United States (Title 17, United States Code) governs the making of photocopies or other reproductions of copyrighted material. Under certain conditions specified in the law, libraries and archives are authorized to furnish a photocopy or other reproduction. One of these specific conditions is that the photocopy or reproduction is not to be "used for any purpose other than private study, scholarship, or research." If a user makes a request for, or later uses, a photocopy or reproduction for purposes in excess of "fair use," that user may be liable for copyright infringement. This institution reserves the right to refuse to accept a copying order if, in its judgment, fulfillment of the order would involve violation of copyright law. Geothermal Resources Council, TRANSACTIONS Vol. 4, September 1980 SUBSURFACE GEOLOGY OF THE RAFT RIVER GEOTHERMAL AREA, IDAHO H. R. Covington U.S. Geological Survey Box 25046, Denver Federal Center Denver, CO 80225 ABSTRACT . northward onto the Snake River Plain and is flanked on the east by the Sublette and Black Pine The Raft River Valley occupies an upper Mountains, on the west by the Jim Sage and Cenozoic structural basin filled with nearly Cotterel Mountains and on the south by the Raft 1,600 m of fluvial silt, sand, and gravel.
  • Geologic Section of the Black Range at Kingston, New Mexico

    Geologic Section of the Black Range at Kingston, New Mexico

    BULLETIN 33 Geologic Section of the Black Range at Kingston, New Mexico BY FREDERICK J. KUELLMER Structure and stratigraphy of the Black Range, detailed petrology of igneous rocks, and general guides to ore exploration 1954 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Eugene Callaghan, Director THE REGENTS MEMBERS EX OFFICIO The Honorable Edwin L. Mechem ..............................Governor of New Mexico Tom Wiley ................................................ Superintendent of Public Instruction APPOINTED MEMBERS Robert W. Botts .............................................................................. Albuquerque Holm O. Bursum, Jr ................................................................................ Socorro Thomas M. Cramer ...............................................................................Carlsbad Frank C. DiLuzio .............................................................................Los Alamos A. A. Kemnitz ...........................................................................................Hobbs Contents Page ABSTRACT ......................................................... …………………………………… 1 INTRODUCTION ........................................................................................................3 ACKNOWLEDGMENTS .............................................................................................4
  • Part 629 – Glossary of Landform and Geologic Terms

    Part 629 – Glossary of Landform and Geologic Terms

    Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition.
  • GSA TODAY Conference, P

    GSA TODAY Conference, P

    Vol. 10, No. 2 February 2000 INSIDE • GSA and Subaru, p. 10 • Terrane Accretion Penrose GSA TODAY Conference, p. 11 A Publication of the Geological Society of America • 1999 Presidential Address, p. 24 Continental Growth, Preservation, and Modification in Southern Africa R. W. Carlson, F. R. Boyd, S. B. Shirey, P. E. Janney, Carnegie Institution of Washington, 5241 Broad Branch Road, N.W., Washington, D.C. 20015, USA, [email protected] T. L. Grove, S. A. Bowring, M. D. Schmitz, J. C. Dann, Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA D. R. Bell, J. J. Gurney, S. H. Richardson, M. Tredoux, A. H. Menzies, Department of Geological Sciences, University of Cape Town, Rondebosch 7700, South Africa D. G. Pearson, Department of Geological Sciences, Durham University, South Road, Durham, DH1 3LE, UK R. J. Hart, Schonland Research Center, University of Witwater- srand, P.O. Box 3, Wits 2050, South Africa A. H. Wilson, Department of Geology, University of Natal, Durban, South Africa D. Moser, Geology and Geophysics Department, University of Utah, Salt Lake City, UT 84112-0111, USA ABSTRACT To understand the origin, modification, and preserva- tion of continents on Earth, a multidisciplinary study is examining the crust and upper mantle of southern Africa. Xenoliths of the mantle brought to the surface by kimber- lites show that the mantle beneath the Archean Kaapvaal Figure 2. Bouguer gravity image (courtesy of South African Council for Geosciences) craton is mostly melt-depleted peridotite with melt extrac- across Vredefort impact structure, South Africa. Color scale is in relative units repre- senting total gravity variation of 90 mgal across area of figure.

  • Boise Caldwell Nampa Idaho Falls Pocatello Twin Falls

    d R t y S e s h t m 4 a N R N ver Rd Old Spiral awai Riv n Ri 95 W Hanley Av Waw er Dow '( Hwy d R d Rd -.128 12 r R e Coeur d’Alene Lewiston y Snake River '(95 t se et 0 0.5 1.0 mi d u 0 1 2 mi R 95 m '( H a y s y R a a Wawaw l N l ai River l Nez Perce County Lewiston Rd t n e N A e B Levee t Historical Society Museum Clearwater River N o D St Park 12 3A o '( Rd E Margaret Av t ill S K l Bridge St S Pioneer D d M o ik ll R 6 e i y c 12 h 12 t B 52 t M a t Park yp a '(+,2 S Kiwanis S 5 ass ,+ n P l 5 +, W t Coeur d'Alene a r h o t t t Bridge S n Park M S t BRITISH COLUMBIA o 9 a Lapwai Rd S s n i n n Memorial i Golf Club g h v S p a t t Ramsey e t a i M h A e S Elm t St 6 D City m t r c Park 5 h t Magrath n e a t 1 7th Av r t A v Hall t Pakowki o 8 i P.O. Locomotive e 4 S v S N 1 St. Mary v R +, G 3 3 Clarkson +, h 36 41 o Lake Lewis-Clark h t Park +, +, e t 879 G ALBERTA 3 d Reservoir k -.
  • Engineering Geology in Washington, Volume I Washington Diviaion of Geology and Euth Resources Bulletin 78

    Engineering Geology in Washington, Volume I Washington Diviaion of Geology and Euth Resources Bulletin 78

    ENGINEERING GEOLOGY IN WASHINGTON Volume I RICHARD W. GALSTER, Chairman Centennial Volume Committee Washington State Section, Association of Engineering Geologists WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES BULLETIN 78 1989 Prepared in cooperation with the Washington State Section of the A~ociation or Engineering Geologists ''WNatural ASHINGTON STATE Resources DEPARTMENT OF Brian Boyle • Commlssloner 01 Public Lands Ari Stearns - Sup,,rvuor Division of Geology and Earth Resources Raymond LcumanJs. Slate Geologist The use of brand or trade names in this publication is for pur­ poses of identification only and does not constitute endorsement by the Washington Division of Geology and Earth Resources or the Association of Engineering Geologists. This report is for sale (as the set of two volumes only) by: Publications Washington Department of Natural Resources Division of Geology and Earth Resources Mail Stop PY-12 Olympia, WA 98504 Price $ 27.83 Tax 2.17 Total $ 30.00 Mail orders must be prepaid; please add $1.00 to each order for postage and handling. Make checks or money orders payable to the Department of Natural Resources. This publication is printed on acid-free paper. Printed in the United States of America. ii VOLUME I DEDICATION . ................ .. .. ...... ............ .......................... X FOREWORD ........... .. ............ ................... ..... ................. xii LIST OF AUTHORS ............................................................. xiv INTRODUCTION Engineering Geology in Washington: Introduction Richard W. Galster, Howard A. Coombs, and Howard H. Waldron ................... 3 PART I: ENGINEERING GEOLOGY AND ITS PRACTICE IN WASHINGTON Geologic Factors Affecting Engineered Facilities Richard W. Galster, Chapter Editor Geologic Factors Affecting Engineered Facilities: Introduction Richard W. Galster ................. ... ...................................... 17 Geotechnical Properties of Geologic Materials Jon W. Koloski, Sigmund D. Schwarz, and Donald W.