Greeting Cards, Postcards, Notepads, Magnets and More
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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). -
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. -
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. -
Oregon State Parks
iocuN OR I Hi ,tP7x OREGON STATE PARKS HISTORY 1917-1963 \STATE/ COMPILED by CHESTER H. ARMSTRONG JULY I. 1965 The actual date of the i is less than thirty years ag older, supported by a few o were an innovation as so lit The Oregon parks system o beautification advocated b: Governors, the early State ] neers. The records reveal out areas, made favorable were generous with their Roy A. Klein, State Highk& ary 29, 1932, as a leader wl The state parks system thought of highway beauti many highway users who h who could not well afford t] In the park story we fii the many influential people complete, it is necessary to thought or trend in the idea the thought of highway be, may see and follow the trai present state narks system. In the preparation of th $ been examined. It was neck ing to property acquisitions deeds and agreements. as tln records of the Parks Divisik Excellent information h; State Parks and Recreatioi A Public Relations Office. As many etbers. I Preface The actual date of the founding of the Oregon State Parks System is less than thirty years ago but the fundamental principles are much older, supported by a few of the leading park people of that time. They were an innovation as so little had been done by any state in the Union. The Oregon parks system owes its beginning to the thought of highway beautification advocated by many leaders of the state, including the Governors, the early State Highway Commissioners and Highway Engi- neers. -
OFR 2004-7, a Self-Guided Tour of the Geology of the Columbia River
A Self-Guided Tour of the Geology of the Columbia River Gorge— Portland Airport to Skamania Lodge, RESOURCES Stevenson, Washington by David K. Norman and Jaretta M. Roloff WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Open File Report 2004-7 March 2004 NATURAL trip location DISCLAIMER Neither the State of Washington, nor any agency thereof, nor any of their em- ployees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any informa- tion, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or other- wise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the State of Washington or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the State of Washington or any agency thereof. WASHINGTON DEPARTMENT OF NATURAL RESOURCES Doug Sutherland—Commissioner of Public Lands DIVISION OF GEOLOGY AND EARTH RESOURCES Ron Teissere—State Geologist David K. Norman—Assistant State Geologist Washington Department of Natural Resources Division of Geology and Earth Resources PO Box 47007 Olympia, WA 98504-7007 Phone: 360-902-1450 Fax: 360-902-1785 E-mail: [email protected] Website: http://www.dnr.wa.gov/geology/ Cover photo: Looking east up the Columbia River Gorge from the Women’s Forum Overlook. Crown Point and its Vista House are visible on top of the cliff on the right side of the river. -
Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington
Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington Scientific Investigations Report 2017–5022–N U.S. Department of the Interior U.S. Geological Survey Cover. Palouse Falls, Washington. The Palouse River originates in Idaho and flows westward before it enters the Snake River near Lyons Ferry, Washington. About 10 kilometers north of this confluence, the river has eroded through the Wanapum Basalt and upper portion of the Grande Ronde Basalt to produce Palouse Falls, where the river drops 60 meters (198 feet) into the plunge pool below. The river’s course was created during the cataclysmic Missoula floods of the Pleistocene as ice dams along the Clark Fork River in Idaho periodically broke and reformed. These events released water from Glacial Lake Missoula, with the resulting floods into Washington creating the Channeled Scablands and Glacial Lake Lewis. Palouse Falls was created by headward erosion of these floodwaters as they spilled over the basalt into the Snake River. After the last of the floodwaters receded, the Palouse River began to follow the scabland channel it resides in today. Photograph by Stephen P. Reidel. Field-Trip Guide to the Vents, Dikes, Stratigraphy, and Structure of the Columbia River Basalt Group, Eastern Oregon and Southeastern Washington By Victor E. Camp, Stephen P. Reidel, Martin E. Ross, Richard J. Brown, and Stephen Self Scientific Investigations Report 2017–5022–N U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. -
Columbia River Gorge National Scenic Area This Report Contains the Best Available Information at the Time of Publication
Schedule of Proposed Action (SOPA) 10/01/2019 to 12/31/2019 Columbia River Gorge National Scenic Area This report contains the best available information at the time of publication. Questions may be directed to the Project Contact. Expected Project Name Project Purpose Planning Status Decision Implementation Project Contact R6 - Pacific Northwest Region, Regionwide (excluding Projects occurring in more than one Region) Regional Aquatic Restoration - Wildlife, Fish, Rare plants In Progress: Expected:11/2019 11/2019 James Capurso Project - Watershed management Objection Period Legal Notice 503-808-2847 EA 07/13/2019 [email protected] *UPDATED* Description: The USFS is proposing a suite of aquatic restoration activities for Region 6 to address ongoing needs, all of which have completed consultation, including activities such as fish passage restoration, wood placement, and other restoration activities. Web Link: http://www.fs.usda.gov/project/?project=53001 Location: UNIT - R6 - Pacific Northwest Region All Units. STATE - Oregon, Washington. COUNTY - Adams, Asotin, Benton, Chelan, Clallam, Clark, Columbia, Cowlitz, Douglas, Ferry, Franklin, Garfield, Grant, Grays Harbor, Island, Jefferson, King, Kitsap, Kittitas, Klickitat, Lewis, Lincoln, Mason, Okanogan, Pacific, Pend Oreille, Pierce, San Juan, Skagit, Skamania, Snohomish, Spokane, Stevens, Thurston, Wahkiakum, Walla Walla, Whatcom, Whitman, Yakima, Baker, Benton, Clackamas, Clatsop, Columbia, Coos, Crook, Curry, Deschutes, Douglas, Gilliam, Grant, Harney, Hood River, Jackson, Jefferson, -
Ralph I. Gifford Photographs, Circa 1910S - 1947
Guide to the Ralph I. Gifford Photographs, circa 1910s - 1947 Title Ralph I. Gifford Photographs (P 218-SG 2) Dates circa 1910s - 1947 (inclusive) 1935-1947 (bulk) Creator Gifford, Ralph I. Summary The Ralph I. Gifford Photographs consist of images taken by Gifford throughout Oregon, primarily during the 1930s and 1940s. The photographs depict many Oregon landmarks and scenes, including the Oregon Coast, Crater Lake, Mount Hood, the Wallowa Mountains, and the Snake River Canyon. The collection includes numerous images of sport fishing as well as several photographs of Native Americans. Ralph Gifford was the son of Benjamin A. Gifford and took over his father©s Portland photography business around 1920. In 1936, Ralph became the first photographer of the newly established Travel and Information Department of the Oregon State Highway Department, a position he held until his death in 1947. Quantity 2.5 cubic feet, including 2089 photographs (17 boxes, including 2 oversize boxes, and 1 map folder) Restrictions on Access Collection is open for research. Oregon State University Libraries, University Archives 121 The Valley Library Oregon State University Corvallis, OR 97331-4501 Phone: 541-737-2165 Email: [email protected] Web: http://osulibrary.oregonstate.edu/archives Finding aid prepared by Lawrence A. Landis; updated by Elizabeth Nielsen, 2011. Funding for encoding this finding aid was provided through a grant awarded by the National Endowment for the Humanities. PDF Created May 28, 2013 Guide to the Ralph I. Gifford Photographs, circa 1910s - 1947 Page 2 of 31 Biographical Note Born in Portland, Ralph I. Gifford (1894-1947) worked in his father©s (Benjamin A.