Metalliferous Mineral Deposits of the Cascade Range in Oregon
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Geology of the Northern Part of the Southeast Three Sisters
AN ABSTRACT OF THE THESIS OF Karl C. Wozniak for the degree of Master of Science the Department cf Geology presented on February 8, 1982 Title: Geology of the Northern Part of the Southeast Three Sisters Quadrangle, Oregon Redacted for Privacy Abstract approved: E. M. Taylorc--_, The northern part of the Southeast Three Sisters quadrangle strad- dles the crest of the central High Cascades of Oregon. The area is covered by Pleistocene and Holocene volcanic and volcaniclastic rocks that were extruded from a number of composite cones, shield volcanoes, and cinder cones. The principal eruptive centers include Sphinx Butte, The Wife, The Husband, and South Sister volcanoes. Sphinx Butte, The Wife, and The Husband are typical High Cascade shield and composite vol- canoes whose compositions are limited to basalt and basaltic andesite. South Sister is a complex composite volcano composed of a diverse assem- blage of rocks. In contrast with earlier studies, the present investi- gation finds that South Sister is not a simple accumulation of andesite and dacite lavas; nor does the eruptive sequence display obvious evolu- tionary trends or late stage divergence to basalt and rhyolite. Rather, the field relations indicate that magmas of diverse composition have been extruded from South Sister vents throughout the lifespan of this volcano. The compositional variation at South Sister is. atypical of the Oregon High Cascade platform. This variation, however, represents part of a continued pattern of late Pliocene and Pleistocene magmatic diver- sity in a local region that includes Middle Sister, South Sister, and Broken Top volcanoes. Regional and local geologic constraints combined with chemical and petrographic criteria indicate that a local subcrustal process probably produced the magmas extruded fromSouth Sister, whereas a regional subcrustal process probably producedthe magmas extruded from Sphinx Butte, The Wife, and The Husband. -
DOGAMI MP-13, Index to the Ore Bin, 1950-1974
- "'0 Q) .,. > Q) 0::: ......... M I NDE X r- .... Q) � 0 � .,. TO T H E :> 0 Q) c 0 Q) u .,. � 0 R E BI N 1950 -1974 Miscellaneous Paper 13 (Revised) STA TE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRI ES STATE OF OREGON DEPARTMEN T OF GEOLOGY AND MINERAL IN DUSTRIES 1069 State Office Building, Portland, Oregon 9720 1 Miscellaneous Paper 13 REVISED INDEX TO TH E ORE BIN 1950 - 1974 GOVERNING BOARD R. W. deWeese, Portland, Chairman Leeanne MacColl, Portland H. Lyle Van Gordon, Grants Pass STATE GEOLOGIST R. E. Corcoran 1975 Index to The ORE BIN 1950 - 1974 This index to The ORE BIN includes work done by Margaret C. Lewis for the first Miscellaneous Paper 13 covering 1950 through 1969. Additional entries from that period have been made and published material from 1970 through 1974 has been indexed by Nora T. Mussotto. Carol S. Brookhyser edited the material and prepared the camera copy. The index consists of two sections: author index and subject irdex. In both, each entry includes date and page numbers of publication. To simplify preparation and use of the index, only senior authors• names are used throughout. AUTHOR* INDEX TO The ORE BIN 1950 - 1974 A ALLEN, J. E. 1962 High Cascades graben and the "mythinterpretation" of Mount Multnomah fslbs.] (Feb. 1962: 22) 1974 Catlin Gabel lava tubes (Sept. 1974:149-155) ALLISON, I. S. 1952 Dr . Ethel Sanborn, an appreciation (Nov. 1952: 73-74) 1962 Geomorphology, role of weathering fslbs .] (Feb. 1962:19} APPLEGATE, S. P. 1968 Fossil sand shcrk (Feb. -
LATE TERTIARY CLIMATIC CHANGES in OREGON by EDWINT
OCTOBZB,1930 MONTHLY WEATHER REVIEW 406 squd-line turbulence, but only when the center of de- up by mountain barriers into isolated streams that produce prasion has passed south of Colorado. This type of pres- thunderstorms, only when there has been a previous sure distribution occurs more frequently in spring than in inipor ta tion of relatively moist air. any other season of the year, but no season is free from it. But a vigorous southward flow of cold air over the Other types of pressure distribution produce thunder- plains States reaches New Mexico with a well-defined storms in this region, but only the types illustrated cold front moving southwestward, along which decided produce squall-line storms in that portion of New Mexico squall-line phenomena often occurs. lying east of the continental divide. The mountain ranges of central New Mexico mark The cold front, with its squall-line phenomena, as the western limit of this type of squall line, so that over known in the eastern half of the United States, can not the larger portion of New Mexico importations of cold take shape in the mountainous region of the Southwest, air are only in the form of narrow streams following the where the front of an advancing cold current is broken topographic depressions. LATE TERTIARY CLIMATIC CHANGES IN OREGON By EDWINT. HOD~E,Professor of Geology [University of Oregon] Evidence is presented in this paper of five climatic For instance, near the city of The Dalles subangular, changes in Oregon beginning in late Pliocene time and st,riated glacial erratics are abundant. -
Metalliferous Mineral Deposits of the Cascade Range in Oregon
UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Bulletin 893 METALLIFEROUS MINERAL DEPOSITS OF THE CASCADE RANGE IN OREGON BY EUGENE CALLAGHAN AND A. F. BUDDINGTON Prepared in cooperation with the STATE MINING BOARD OF OREGON UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1938 For sale by the Superintendent of Documents, Washington, D.C. ------ Price 1.25 CONTENTS Page Abstract__. ..................................................... 1 Introduction ^..................................................... 3 Field work and acknowledgments..__---___-____.__..._.___.__._. 3 Previous work. .___________ ________________________________ 4 Surface features^ .:...-............ ____________..___..__.__.___ 6 Climate and vegetation__.___________________________________ 7 Accessibility- ________--___-___-___----_-___-__________________ 7 Geology. _ ___.-----_-----_----------------------------_--___---_-_ 7 General features.--------_-_----___----__----___--_-_,_____.___ 7 Sedimentary rocks of the Rogue River and Bear Creek Valleys._-__- 10 Black lavas of the western margin of the Cascade Range-_-__-_-_-__ 1C Gray andesitic lavas and associated rocks of the Western Cascades._ 11 General features-_---_--_--------_--------..----_--_------__ 11 Basalt -_-i__---___-_---__---_-___--___--._________-___ 12 Labradorite andesite (basaltic andesite)__.__________________ 13 Normal andesite_-________________________________________ 13 Rhyolite-_________________________________________________ -
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. -
D:\NWR\Wpdocs\= SOURCE ATLAS ===\Description and References
U. S. OBSIDIAN SOURCE CATALOG # WWW.SOURCECATALOG.COM OREGON OBSIDIAN SOURCES The prominent landform in the center of the image above is the lower plateau of the Obsidian Cliffs unit, one of Oregon’s most intensively-utilized prehistoric sources of glass. The photo was taken facing west from the summit of the Middle Sister, Oregon High Cascades. OBSIDIAN CLIFFS ALTERNATE NAMES: North Sister, Obsidian Ridge, Three Sisters. LOCATION - COUNTY: Lane. ACCESS AND OWNERSHIP: Three Sisters Wilderness Area; special permit required for entry to plateau area. Access limited by snow in winter months. GEOLOGIC BACKGROUND/SETTING: Mapped as part of unit Qr (rhyodacite and dacite) by Taylor et al. 1987. ARCHAEOLOGICAL SIGNIFICANCE: Trace element studies of obsidian artifacts from archaeological sites in Oregon, Washington, and British Columbia indicate that this source is one of the most significant ones in Oregon. ACKNOWLEDGMENTS: Jon Silvermoon. REFERENCES Anttonen, Gary J. 1972 Trace Elements in High Cascade Volcanic Rocks, Three Sisters Area, Oregon. Unpublished Ph.D. Dissertation, Department of Geology, Stanford University, Palo Alto, California. Baxter, Paul W., Thomas J. Connolly, and Craig E. Skinner 2015 Obsidian Use in the Willamette Valley and Adjacent Western Cascades of Oregon. In Toolstone Geography of the Pacific Northwest, edited by Terry L. Ozbun and Ron L. Adams, pp. 218-233. Archaeology Press, Simon Fraser University, Burnaby, British Columbia. 1 U. S. OBSIDIAN SOURCE CATALOG # WWW.SOURCECATALOG.COM Bennett, Roy B. and J. M. D'Auria 1974 The Application of Energy Dispersive Spectroscopy to Determining the Provenience of Obsidian. International Journal of Applied Radiation and Isotopes 25:361-371. -
The Little Belknap Crater Cave System
Craig Skinner i j \ KIND OF LOST AND FOOND: The Little Belknap Crater Cave System "No visitor to this region should fail to climb to the top of Little Belknap, and see for himself the stalac tites, the stalagmites, the splatter cones, the conduits through which the lava poured, and other details of this marvelous crater." Edwin Hodge, 1925, in Mount Multnomah The Little Belknap Crater Cave System is a rather unique and certainly unusual two-level lava tube and conduit located nearly at the summit of Little Belknap Crater, the focus of some of the most recent and spec tacular volcanic action in. Oregon. I'd wanted to find and look at this little-known (so I thought) cave on top of Little Belknap ever since I read an account of it in a newly ac quired publication (3:29) a couple of years ago. The mention of the cave as a "lead" and a pit in the July, 1979, Speleograph finally spurred me and an old friend, Scott Murdock, into action. And so, on a sunny and late August morning, we found ourselves on the I Oregon Skyline Trail near the Dee Wright Observatory at the McKenzie r' Pass. Heading up the well-worn trail, we quickly ran into the barren and spectacular Little Belknap lava flows. Some eager young burnout specialists (tends to be anyone in better condition than I am) that we passed on our way out of the trees to the lava fields called sagely to us, "It's a long one." TWo or three miles later at the top of the long uphill climb (done strategically in the heat of the day in August), wondering if we hadn't grossly underestimated our water supply, we were forced to agree. -
Our Vanishing Glaciers”
Jim E. O’CONNOR “Our Vanishing Glaciers” One Hundred Years of Glacier Retreat in Three Sisters Area, Oregon Cascade Range GLACIERS OF THE PACIFIC NoRTHWEST — bright white flow- ing masses of ice that mantle the region’s high mountain slopes — have attracted climbers, photographers, and scientists since their first recorded discovery here in the mid 18s. They are beautiful, of course, covering and balancing the dark craggy volcanic peaks; but they also are scientifically significant. Glaciers shape landscapes — sometimes at continental scales, as during global ice ages. Glaciers are also extremely sensitive to climate, their size and deposits indicating past and ongoing changes in temperature and precipitation. These geologic and climatologic aspects of glaciers had just been discovered and were hotly debated during the mid 18s, meaning such conversations often occurred in conjunction with exploration of the Pacific Northwest. Since that time, explorers and scientists have continued to monitor shrinking glaciers in the Pacific Northwest with photography and measurements. Regional glacier shrinkage was perhaps most clearly first described in “Our vanishing glaciers,” a 1938 Mazamas Mountaineering Club publication describing glaciers in the Cascade Range of Oregon.1 The Three Sisters region of the central Oregon Cascade Range, where glaciers are numerous and accessible and scenery has attracted photographers and outdoor recreation since the early 19s, has been a central place for that monitoring. Photographs and measurements reproduced here show that glaciers continue to shrink and disappear. Glaciers exist by the grace of climate. Only where snowfall is deep enough and the summer melting season short enough can persistent snowfields thicken and expand so that they transform into glacial ice masses that slowly flow down slopes. -
Geologic Map of Three Sisters Volcanic Cluster, Cascade Range, Oregon by Wes Hildreth, Judy Fierstein, and Andrew T
Geologic Map of Three Sisters Volcanic Cluster, Cascade Range, Oregon By Wes Hildreth, Judy Fierstein, and Andrew T. Calvert Pamphlet to accompany Scientific Investigations Map 3186 Aerial view northward along glaciated summits of South Sister, Middle Sister, and North Sister volcanoes. Snow and ice- filled South Sister crater (rim at 10,358 ft) was created between 30 and 22 ka, during most recent of several explosive summit eruptions; thin oxidized agglutinate that mantles current crater rim protects 150-m-thick pyroclastic sequence that helped fill much larger crater. Middle Sister (10,047 ft) is capped by thick stack of radially dipping, dark-gray, thin mafic lava flows; asymmetrically glaciated, its nearly intact west flank contrasts sharply with its steep east face. Blue lake (near far right edge) is impounded by sharp-crested Neoglacial moraine. North Sister (10,085 ft) is glacially ravaged stratocone that consists of hundreds of thin rubbly lava flows and intercalated falls that dip radially and steeply; remnants of two thick lava flows cap summit. Broad mafic shield beyond North Sister is Black Crater; distant peak on horizon is Mount Jefferson; and Mount Hood is in dim distance. Photograph by John Scurlock, 2007. 2012 U.S. Department of the Interior U.S. Geological Survey This page intentionally left blank Contents Introduction.....................................................................................................................................................1 Physiography and Access ...................................................................................................................1 -
2006 Administration Board of Directors
~~;~:·;·,.-·:;::·,~(·:·:-.;-~;-~(.·.:~:._?:IS:::·.~~~~-/ _t~~ Non-Proft Org. GEOLOGICAL SOCIETY OF , ·, U.S. POSTAGE PAID THE oR£&j~'c6u~~y.:·.)::·,-~:. Portla1d, ()regal ' '\7-:'•<' > I' !<•-.:'~~~;\;\~~.~~~~?;.\ ·:; ',. \;' P. 0. BOX907.:.> .... :..... ·.... ·. ·. Permit No. 999 ~~, ·~.·:,";/ ·.. •• ,... .; •.;J\ ·~""' r ~ ,... : ... ~, .-· .... ~ :~<- ~.rl~... ·.; ."'· •• , ~ ~~ \ , \ ... PORTLAND; OR 97207:··,' '; ~ :;~:::.i:·. :·.:x~.:>.;·L~-~;;~~~-::~:~-:::r/ ?>' .~J-~-:~:~] .'·;~~;;~~v.:~;~;L :.~:~·~;~:;t~~~ :; ·:'-'::1 ,:,'-: .' ; 00 .::;;:;·~~.:' ::;., .. _, .. r-~->;J,.. .·:.- ~·,/ -~~~~ ... · · ..:·:~-::: . • -,;... ~.,:.. r { 0 .~. '0,'•, .. ·:': ,,.·J .; '·, .' )- l;·_ ... 1J.J 0 .) ... ·, .,., ··;·. :;;.,, ..... ,.r ··;,;,, 1 ' .. ~ . ' (i>,:·:~·':' .:. ,· ·. :·:: -:;"\: .. ··.·.·. ' . -. '* . ·,- ·>":: ·.. GOI'I .... v .. -::J··· . ·:::. ·.. \~~i:0.·.i:·E:::;·.~ )·'<.··. __ .:·SINCE 1935 .·.:·.:;:·~;~:.A ... :~,::·;: .. : · ·._:_;:-_>:~· :/J\·~·-_p_:.. :.· _.,_ ·:··l .: :···. :.. ·.:•·• ..· .·., ,:·G.;:; ·.~B~l~id THE GEOLOGICAL NEWSI=, ·-· IER GEOLOGICAL SOCIETY OF THE OREGON COUNTRY N 2005-2006 ADMINISTRATION BOARD OF DIRECTORS President: Directors: Charles Carter- 503/469-8353 Janet Kaye-Rasmussen (3 years)- 503/244-3194 Vice-President: John Teskey (2 years)- 503/641-7746 Bonnie Prange - 360/693-8396 Richard Meyer (1 year) - 503/236-7795 Secretary Beverly Vogt - 503/292-6939 Past Presidents: Treasurer Clay Kelleher- 5031775-6263 Marvel Gillespie - 503/246-2368 Rosemary Kenney- 503/892-6514 .MI:'M'M'~.:I.~.JJJI':'~~~~,.,.,., -
Memorial to Edwin Thomas Hodge 1887-1970
Memorial to Edwin Thomas Hodge 1887-1970 JOHN ELIOT ALLEN Department of Earth Sciences, Portland State University, Portland, Oregon Edwin Thomas Hodge, born in Atlanta, Illinois, on July 12, 1887, died at his home in Portland, Oregon, on November 7, 1970. lie was the only son of an itinerant minister, who had abandoned his family when Edwin was 4 years old. His early years were full of hardship that spurred him on in his later ambitions and successes. He attended school in Minneapolis and completed high school in three years. One of his early talents was his ability to memorize; he tells in a memoir how he read and committed to memory whole sections of Darwin’s Origin o f Species and Hudson’s Laws of Physical Phenomena while he was still in grade school. He early developed a high degree of competence in gymnastics, and during high school and college taught night “settlement” classes in gymnastics and boxing to contribute to the family finances. He worked his way through the North American Normal School for Gymnastics in Milwaukee and, after receiving a degree in 1907, took his first academic job as director of high school physical education at Ashland, Wisconsin. In one year he was able to save enough money to go to the University of Minnesota, receiving a B.A. in 1913 and, with the assistance of a fellowship, a M.A. in Biology (pre-Med.) in 1914. While at the University of Minnesota, he met Lydia I.. Herrick whom he married in 1912. She was an accomplished artist and a gracious woman who enriched Edwin’s life. -
DOGAMI MP-10, Articles on Recent Volcanism in Oregon
STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1088 STATE OFFICE BUILDING PORTLAND OREGON 97201 Miscellaneous Paper No. 10 ARTICLES ON RECENT VULCANISM IN OREGON Reprinted from The ORE BIN 1965 STATE GOVE RNING BOARD Frank L .\1cColloch. Clza1rman Portland Harold Hanta BakP• Fa}t>tlf' I. Bri:-:.tul G1ant� Pa:. Holli M. Dole STATE GEOLOGIST The ORE BIN Volume 25, No. 3 March, 1963 RECENT VOLCANIC LANDFORMS IN CENTRAL OREGON* By Norman V. Peterson and Edward A. Groh** Introduction As the race to be the first mortals on the moon continues, the questions of how the lunar surface features originated and what rock types they contain are st iII not answered • Many of the lunar configurations that are telescopically visible cer tainly resemble volcanoes and features associated with them . Even if only a part of the moon's surface has been formed by valcan ic processes, some of the smaller volcanic forms; such as hummocky lava flow surfaces, spatter cones, and lava tubes could be present. If these features exist, they could provide ready-made shelters to protect men and vehicles from the hostile environment of radiation, high temperatures, and mef:eorite and dust bom bardment. A reconnaissance of the Bend-Fort Rock area in central Oregon shows that it has a wealth and variety of fresh volcanic landforms that should be of interest to the planners of our lunar programs as well as to the students of volcanology or to those curious about the rocks of Oregon . Recent Volcanic Activity in Oregon Before discussing central Oregon specifically, it may be well to look at the pattern of Recent volcanic activity in all of Oregon.