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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. -
Josephine County, Oregon, Historical Society Document Oregonłs
Finding fossils in Oregon is not so much a question of Places to see fossils: where to look for them as where not to look. Fossils are rare John Day Fossil Beds National Monument in the High Lava Plains and High Cascades, but even there, , _ Contains a 40-million year record of plant and animal life . ·� � .11�'!]�:-.: some of the lakes are famous for their fossils. Many of the ill the John Day Basill ill central Oregon near the towns of .• .� . ' · sedimentary rocks in eastern Oregon contain fossil leaves or · ,,����<:l. · . ' · •· Dayville' Fossil, and Mitchell. The Cant Ranch Visitor ; ' " ' ' j ' .- � bones. Leaffossils are especially abundant in the - Center at Sheep Rock on Highway 19 includes museum : ,· .,, 1 • , .. rocks at the far side of the athletic · exhibits of fossils. Open every day 8:30-5. For general l· · . ., ;: . · : field at Wheeler High School ,...,..;� information, contact John Day Fossil Beds National . -- - ' '· in the town of Fossil. Monument, 420 West Main St., John Day, OR 97845, ' l-, Although it is rare to phone (503) 575-0721. find a complete Oregon Museum of Science and Industry animal fossil, a 1945 SE Water Ave., Portland, OR 97214. Open Thurs. & search of river Fri. 9:30-9; Sat. through Wed. 9:30-7(sumrner hours); beds may turn . l 9:30-5(rest of year), phone (503) 797-4000 up c h1ps or Condon Museum, University of Oregon even teeth. In Pacific Hall, Eugene, OR 97403. Open only by western appointment, phone (503) 346-4577. Oregon, the ' . ; Douglas County Museum of History and sedimentary ' r Natural History rocks that are 1 primarily off1-5 at exit 123 at Roseburg (PO Box 1550, Roseburg, marine in OR 97470). -
Paleontology and Stratigraphy of Eocene Rocks at Pulali Point, Jefferson County, Eastern Olympic Peninsula, Washington
PALEONTOLOGY AND STRATIGRAPHY OF EOCENE ROCKS AT PULALI POINT, JEFFERSON COUNTY, EASTERN OLYMPIC PENINSULA, WASHINGTON by RICHARD L. SQUIRES, JAMES L. GOEDERT, and KEITH L. KALER WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES REPORT OF INVESTIGATIONS 31 1992 ., WASHINGTON STATE DEPARTMENT OF Natural Resources Brian Boyle • Commhstoner of Public Lands An Steo_r0$ - Superv1sor Division ol Geology and Earth Resources Raymond Lcmnanls. State Geologlsl PALEONTOLOGY AND STRATIGRAPHY OF EOCENE ROCKS AT PULALI POINT, JEFFERSON COUNTY, EASTERN OLYMPIC PENINSULA, WASHINGTON by RICHARD L. SQUIRES, JAMES L. GOEDERT, AND KEITH L. KALER WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES REPORT OF INVESTIGATIONS 31 1992 W>.SHING'TON STAT1r OEPARTMDIT or Natural Resources 8ncll) Bov,. · COmmmioner ot Pu!xk: tancb M $i.atni; S\lp$1'WOJ' DtY!llcn 01 Gtology ahCS £artti ~ Raymond l.mlMn.:I ~Geologist Cover: From left, ?Falsifusus marysvillensis; Pachycrommium clarki; large bivalve, Veneri cardia hornii s.s.; Delectopecten cf. D. vancouverensis sanjuanensis; Turritella uvasana hendoni. These specimens are shown at 150 percent of the dimensions on Plates 1 and 3. Use of trade, product, or firm names in this report is for descriptive purposes only and does not consitute endorsement by the Washington Division of Geology and Earth Resources. 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 $ 1.85 Tax (Stale residenl.t only) .15 Total $ 2.00 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. -
Szabo Janos.Indd
FRAGMENTA PALAEONTOLOGICA HUNGARICA Volume 34 Budapest, 2017 pp. 9–48 Gastropods of the Lower Jurassic Hierlatz Limestone Formation, part 3. New pleurotomarioideans from the fauna of Hierlatz Alpe (Hallstatt, Austria) János Szabó Department of Palaeontology and Geology, Hungarian Natural History Museum, H-1083 Budapest, Ludovika tér 2, Hungary. E-mail: [email protected] Abstract – Th is paper adds sixteen pleurotomarioidean species to the fauna from the type local- ity area of the Lower Jurassic Hierlatz Limestone Formation (Hallstatt, Austria). Majority of these species are unknown from former publications; only one species has already been recognised from the Bakony Mts (Hungary). Most of the species belong or are related to the genus Pleurotomaria or Laevitomaria but two new genera are also established besides eleven new species: Neorotomaria n. gen., Granulizona n. gen., Pleurotomaria nodulocostulata n. sp., Pleurotomaria wiesberghausensis n. sp., Pleurotomaria nodulocincta n. sp., Pleurotomaria seminodosa n. sp., Pleurotomaria indistincta n. sp., Pleurotomaria nongradata n. sp., Pleurotomaria? homoruspira n. sp., Pleurotomaria? laponya n. sp., Neo- rotomaria obertraunensis n. sp., Neorotomaria subgradata n. sp. and Granulizona mandli n. sp. With 145 fi gures. Key words – Granulizona, Hierlatz Limestone, Jurassic, Laevitomaria, Neorotomaria, Pleurotomaria INTRODUCTION Th is paper is dedicated to those taxa from the unpublished parts of museum collections, which represent the “modern” slit-bearing gastropods in the Early Jurassic faunas of the Hierlatz Alpe. Most of the recognised species are identifi ed as Pleurotomaria Defrance, 1826 (Pleurotomariidae) but several species have so extreme morphology that their assignments to this genus remain uncertain until better material is available; some others need new genera to accommodate them. -
The Columbia River Gorge: Its Geologic History Interpreted from the Columbia River Highway by IRA A
VOLUMB 2 NUMBBI3 NOVBMBBR, 1916 . THE .MINERAL · RESOURCES OF OREGON ' PuLhaLed Monthly By The Oregon Bureau of Mines and Geology Mitchell Point tunnel and viaduct, Columbia River Hi~hway The .. Asenstrasse'' of America The Columbia River Gorge: its Geologic History Interpreted from the Columbia River Highway By IRA A. WILLIAMS 130 Pages 77 Illustrations Entered aa oeoond cl,... matter at Corvallis, Ore., on Feb. 10, l9lt, accordintt to tbe Act or Auc. :U, 1912. .,.,._ ;t ' OREGON BUREAU OF MINES AND GEOLOGY COMMISSION On1cm or THm Co><M188ION AND ExmBIT OREGON BUILDING, PORTLAND, OREGON Orncm or TBm DtBIICTOR CORVALLIS, OREGON .,~ 1 AMDJ WITHY COMBE, Governor HENDY M. PABKB, Director C OMMISSION ABTBUB M. SWARTLEY, Mining Engineer H. N. LAWRill:, Port.land IRA A. WILLIAMS, Geologist W. C. FELLOWS, Sumpter 1. F . REDDY, Grants Pass 1. L. WooD. Albany R. M. BIITT8, Cornucopia P. L. CAI<PBELL, Eugene W 1. KEBR. Corvallis ........ Volume 2 Number 3 ~f. November Issue {...j .· -~ of the MINERAL RESOURCES OF OREGON Published by The Oregon Bureau of Mines and Geology ~•, ;: · CONTAINING The Columbia River Gorge: its Geologic History l Interpreted from the Columbia River Highway t. By IRA A. WILLIAMS 130 Pages 77 Illustrations 1916 ILLUSTRATIONS Mitchell Point t unnel and v iaduct Beacon Rock from Columbia River (photo by Gifford & Prentiss) front cover Highway .. 72 Geologic map of Columbia river gorge. 3 Beacon Rock, near view . ....... 73 East P ortland and Mt. Hood . 1 3 Mt. Hamilton and Table mountain .. 75 Inclined volcanic ejecta, Mt. Tabor. 19 Eagle creek tuff-conglomerate west of Lava cliff along Sandy river. -
Volume 12, 1946 1946 INDNX to GEOLOGIC,\L F::EWS-L1'l'l'er Volume 12 Compiled by John Eliot Allen, and 1!:1-Iart If
G&lLOGICAL SOCIETY NEWS LETTER Volume 12, 1946 1946 INDNX to GEOLOGIC,\L f::EWS-L1'l'l'ER Volume 12 Compiled by John Eliot Allen, and 1!:1-iart If.. Baldwin ·~----------------------------- Subject Index Annual Fanquet Address: J. E. Allen, pp. 36-37 Annual Banquet Photo: O. E. Stanley, opposite p. 44 Annual Banquet Speaker, Dr. L. W. Staples: E. !!. Baldwin, ·p.38 Annual Picnic: J. E. Allen, pp. 88-89 Annual Picnic l'hoto: o. E. Stanley, opposite p. 108 Annual Report, Histoz•ical Committee: 0, E. Stanley, p. 27 " • Library Committee: M. Hughes, p. 33 '' " Museum Committee: J. C. Stevens, pp. 4C-41 " " Research Committee: E, 11. Baldwin, pp. 41-42 " " Secretary: · A. Henley, p. 28 " " Treasurer: H. M. Stockwell, p. 32 • " Trip Committee: II. B. Schminky, p. 33 Bauxite field trip: R. S. Mason, p. 49 Bend trip, hiehlights of the: u. Shepard, p. 78 Ily-Laws of the G, S. O. C.: pp. 96-102 Climate and post-e-lacial fore&t succession in the Oregon Cascades by H. P. Ilan- sen--A reviev.: J. E. Allen, pp. 104-105 Columbia Gorge, fossil ¥:cods of the: G. F. Beck, pp. 46-47 Committee Appointments, 1946: J, E. Allen, p. 27 Composition of ocean water--reprint: p. 59 Condon, Thomas, en Oregon pioneer: E. C, ~cCornack, pp. 69-72, 82-84; preamble by W. C. Adams, p. 69 Condon, History of the Liberty ship SS Thomas: S. E. S., p. 15 Constitution, preamble: J. E. Allen, p. 96 Sarthquake--'pertial reprint from Ore-Bin; p. 60 Eastern Oregon, Geologist's weekend in ; W. -
Historic Columbia River Highway: Oral History August 2009 6
HHHIIISSSTTTOOORRRIIICCC CCCOOOLLLUUUMMMBBBIIIAAA RRRIIIVVVEEERRR HHHIIIGGGHHHWWWAAAYYY OOORRRAAALLL HHHIIISSSTTTOOORRRYYY FFFiiinnnaaalll RRReeepppooorrrttt SSSRRR 555000000---222666111 HISTORIC COLUMBIA RIVER HIGHWAY ORAL HISTORY Final Report SR 500-261 by Robert W. Hadlow, Ph.D., ODOT Senior Historian Amanda Joy Pietz, ODOT Research and Hannah Kullberg and Sara Morrissey, ODOT Interns Kristen Stallman, ODOT Scenic Area Coordinator Myra Sperley, ODOT Research Linda Dodds, Historian for Oregon Department of Transportation Research Section 200 Hawthorne Ave. SE, Suite B-240 Salem OR 97301-5192 August 2009 Technical Report Documentation Page 1. Report No. 2. Government Accession No. 3. Recipient’s Catalog No. OR-RD-10-03 4. Title and Subtitle 5. Report Date Historic Columbia River Highway: Oral History August 2009 6. Performing Organization Code 7. Author(s) 8. Performing Organization Report No. Robert W. Hadlow, Ph.D., ODOT Senior Historian; Amanda Joy Pietz, ODOT Research; and Hannah Kullberg and Sara Morrissey, ODOT Interns ; Kristen Stallman, ODOT Scenic Area Coordinator; Myra Sperley, ODOT Research; and Linda Dodds, Historian 9. Performing Organization Name and Address 10. Work Unit No. (TRAIS) Oregon Department of Transportation Research Section 11. Contract or Grant No. 200 Hawthorne Ave. SE, Suite B-240 Salem, OR 97301-5192 SR 500-261 12. Sponsoring Agency Name and Address 13. Type of Report and Period Covered Oregon Department of Transportation Final Report Research Section 200 Hawthorne Ave. SE, Suite B-240 Salem, OR 97301-5192 14. Sponsoring Agency Code 15. Supplementary Notes 16. Abstract The Historic Columbia River Highway: Oral History Project compliments a larger effort in Oregon to reconnect abandoned sections of the Historic Columbia River Highway. -
Lewis and Clark at Fort Clatsop: a Winter of Environmental Discomfort and Cultural Misunderstandings
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 7-9-1997 Lewis and Clark at Fort Clatsop: A winter of Environmental Discomfort and Cultural Misunderstandings Kirk Alan Garrison Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Diplomatic History Commons, and the United States History Commons Let us know how access to this document benefits ou.y Recommended Citation Garrison, Kirk Alan, "Lewis and Clark at Fort Clatsop: A winter of Environmental Discomfort and Cultural Misunderstandings" (1997). Dissertations and Theses. Paper 5394. https://doi.org/10.15760/etd.7267 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]. THESIS APPROVAL The abstract and thesis of Kirk Alan Garrison for the Master of Arts in History were presented July 9, 1997, and accepted by the thesis committee and the department. COMMITTEE APPROVALS: r DEPARTMENT APPROVAL: Go~do~ B. Dodds, Chair Department of History ********************************************************************* ACCEPTED FOR PORTLAND STATE UNIVERSITY BY THE LIBRARY on L?/M;< ABSTRACT An abstract of the thesis of Kirk Alan Garrison for the Master of Arts in History, presented 9 July 1997. Title: Lewis and Clark at Fort Clatsop: A Winter of Environmental Discomfort and Cultural Misunderstandings. I\1embers of the Lewis and Clark expedition did not like the 1805-1806 winter they spent at Fort Clatsop near the mouth of the Columbia River among the Lower Chinookan Indians, for two reasons. -
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. -
The Evolving Landscape of the Columbia River Gorge
The Evolving Landscape of the Columbia River Gorge Jim E. O’Connor Carleton Watkins, photographer, OHS neg., OrHi A reprint from the Oregon Historical Quarterly Special Issue Dissecting the Columbia: Lewis and Clark West of the Divide William L. Lang, guest editor Volume , Number Fall the journal of record for oregon history Jim E. O’Connor The Evolving Landscape of the Columbia River Gorge Lewis and Clark and Cataclysms on the Columbia ravelers retracing lewis and clark’s journey to the Pacific over the past two hundred years have witnessed tre- mendous change to the Columbia River Gorge and its pri- mary feature, the Columbia River. Dams, reservoirs, timber Tharvest, altered fisheries, transportation infrastructure, and growth and shrinkage of communities have transformed the river and valley. This radically different geography of human use and habitation is commonly contrasted with the sometimes romantic view of a prior time provided both by early nineteenth-century chroniclers and present-day critics of the modern condition — an ecotopia of plentiful and perpetual resources sustaining a stable culture from time immemorial. Reality is more com- plicated. Certainly the human-caused changes to the Columbia River and the gorge since Lewis and Clark have been profound; but the geologic his- tory of immense floods, landslides, and volcanic eruptions that occurred before their journey had equally, if not more, acute effects on landscapes and societies of the gorge. In many ways, the Lewis and Clark Expedi- tion can be viewed as a hinge point for the Columbia River, the changes engineered to the river and its valley in the two hundred years since their visit mirrored by tremendous changes geologically engendered in the thousands of years before. -
Notes from the Gulf on Fossils Eocene of The
If you do not need this report after it has served your purpose, please return it to the Geological Survey, using the official mailing label at the end UNITED STATES DEPARTMENT OF THE INTERIOR NOTES ON FOSSILS FROM THE EOCENE OF THE GULF PROVINCE GEOLOGICAL SURVEY PROFESSIONAL PAPER 193— B UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Professional Paper 193—B NOTES ON FOSSILS FROM THE EOCENE OF THE GULF PROVINCE I. THE ANNELID GENUS TUBULOSTIUM II. THE GASTROPOD FAMILIES GASSIDIDAE, FIGIDAE, AND BUGGINIDAE BY JULIA GARDNER Shorter contributions to general geology, 1938-39 (Pages 17-44) UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1939 For sale by the Superintendent of Documents, Washington, D. C. - ------ Price 10 cents CONTENTS Page Abstract._______________________________________________________________________.._____.__..___.____ 17 Introduction. _________________________________________________________________________________________________ 17 I. The annelid genus Tubulostium- _______-__________________________--____-_-_-__-____-______-_-__----__-_--__-_ 17 II. The gastropod families Cassididae, Ficidae, and Buccinidae_ ______________________________________________________ 21 Index____ _-_-__-_--___-___________________________________________.--___--__----_----_--------------_——,-- 43 ILLUSTRATIONS Page PLATES 6-8. Annelids and gastropods from the Eocene of the Gulf provmce_______--_--_____-__---__--___-_--_-__-___- 39 FIGURE 1. Tubulostium horatianum Gardner, n. sp., cross section of tube______________________________________________ 19 2. Tubulostium leptostoma (Gabb), cross section of tube._____________________-___-_-_____----__-_-_-__--__-- 20 3. Map showing distribution of Galeodea. ________________________-_-___-_______---_-_-_---_--_--------_-_- 22 4. Map showing distribution of Priscoficus (Priscoficus) _______-__________-________________-__-_-_--_-_------ 29 5. -
Marine Gastropods from the Pogibshi Formation (Alaska) and Their Paleobiogeographical Significance
Andean Geology 47 (3): 559-576. September, 2020 Andean Geology doi: 10.5027/andgeoV47n3-3278 www.andeangeology.cl Early Jurassic (middle Hettangian) marine gastropods from the Pogibshi Formation (Alaska) and their paleobiogeographical significance *Mariel Ferrari1, Robert B. Blodgett2, Montana S. Hodges3, Christopher L. Hodges3 1 Instituto Patagónico de Geología y Paleontología, IPGP (CCT CONICET-CENPAT), Boulevard Alte. Brown 2915, (9120) Puerto Madryn, Provincia de Chubut, Argentina. [email protected] 2 Blodgett and Associates, LLC, 2821 Kingfisher Drive, Anchorage, Alaska 99502, USA. [email protected] 3 California State University Sacramento, 6000 J Street, Sacramento, California 95819, USA. [email protected]; [email protected] * Corresponding author: [email protected] ABSTRACT. A middle Hettangian marine gastropod assemblage is reported from the Kenai Peninsula of south-central Alaska supplying new paleontological evidence of this group in Lower Jurassic rocks of North America. Pleurotomaria pogibshiensis sp. nov. is described from the middle Hettangian marine succession informally known as Pogibshi formation, being the first occurrence of the genus in the Kenai Peninsula and the oldest occurrence of the genus in present-day Alaska and North America. One species of the genus Lithotrochus, namely Lithotrochus humboldtii (von Buch), is also reported for the first time from the Kenai Peninsula. Lithotrochus has been considered as endemic to South America for a time range from the early Sinemurian