Volcano Type: Stratovolcano Composition: Andesite Most Recent Eruption: 6,700 Years Ago Threat Potential: High Glacier Peak

Total Page:16

File Type:pdf, Size:1020Kb

Volcano Type: Stratovolcano Composition: Andesite Most Recent Eruption: 6,700 Years Ago Threat Potential: High Glacier Peak High to Very High Threat Potential Low to Very Low Threat Potential WASHINGTON Mount Jefferson Mount Baker Belknap Glacier Peak Black Butte Crater Lava Field Mount Rainier Blue Lake Crater Mount St. Helens Cinnamon Butte Mount Adams Craters of the Moon Volcanic Field OREGON Davis Lake Volcanic Field Mount Hood Devils Garden Lava Field Three Sisters Diamond Craters Volcanic Field Newberry Volcano Four Craters Lava Field Crater Lake Hell's Half Acre Lava Field CALIFORNIA Indian Heaven Volcanic Field Medicine Lake Volcanno Jordan Craters Volcanic Field Mount Shasta Lava Mountain Lava Field Lassen Peak Sand Mountain Volcanic Field Moderate Threat Potential Wapi Lava Field Mount Bachelor West Crater Volcanic Field Mount Baker Location: Washington, Whatcom County Latitude: 48.777° N Longitude: 121.813° W Elevation: 3,286 (m) 10,781 (f) Volcano type: Stratovolcano Composition: Andesite Most recent eruption: 6,700 years ago Threat Potential: High Glacier Peak Location: Washington, Snohomish County Latitude: 48.112° N Longitude: 121.113° W Elevation: 3,213 (m) 10,541 (f) Volcano type: Stratovolcano Composition: Dacite Most recent eruption: 1,100 years ago Threat Potential: High * Mount Rainier Location: Washington, Pierce County Latitude: 46.853° N Longitude: 121.76° W Elevation: 4,392 (m) 14,410 (f) Volcano type: Stratovolcano Composition: Andesite to Dacite Most recent eruption: ∼1,000 years ago Nearby towns: Orting, Seattle, Tacoma, Yakima Threat Potential: High Mount St. Helens Location: Washington, Skamania County Latitude: 46.2° N Longitude: 122.18° W Elevation: 2,549 (m) 8,363 (f) Volcano type: Stratovolcano Composition: Basalt to Rhyodacite Most recent eruption: 1980, 2004-2008 Nearby towns: Castle Rock, WA; Olympia, WA; Vancouver, WA; Yakima, WA; Portland, OR Threat Potential: High Mount-Adams Location: Washington, Klickitat County Latitude: 46.206° N Longitude: 121.49° W Elevation: 3,742 (m) 12,277 (f) Volcano type: Stratovolcano Composition: Basalt to Andesite Most recent eruption: 3,800 years ago Threat Potential: High Mount Hood Location: Oregon, Clackamas/Hood River Counties Latitude: 45.374° N Longitude: 121.695° W Elevation: 3,426 (m) 11,240 (f) Volcano type: Stratovolcano Composition: Andesite to Dacite Most recent eruption: 1865 AD Threat Potential: High Three Sisters Location: Oregon, Lane County Latitude: 44.103° N Longitude: 121.768° W Elevation: 3,157 (m) 10,358 (f) Volcano type: Complex volcano Composition: Andesite to Rhyolite Most recent eruption: 2,000 years ago Threat Potential: High Newberry Location: Oregon; Deschutes, Klamath and Lake Counties Latitude: 43.722° N Longitude: 121.229° W Elevation: 2,434 (m) 7,986 (f) Volcano type: Shield-shaped Composition: Basalt to Rhyolite Most recent eruption: 1,300 years ago Nearby towns: Sunriver, Bend, LaPine, Redmond Threat Potential: High Crater Lake Location: Oregon, Klamath County Latitude: 42.93° N Longitude: 122.12° W Elevation: 2,487 (m) 8,159 (f) Volcano type: Caldera Composition: Basalt to Rhyolite Most recent eruption: 6,600 years ago Threat Potential: High Medicine Lake Location: California, Siskiyou & Modoc Counties Latitude: 41.611° N Longitude: 121.554° W Elevation: 2,412 (m) 7,913 (f) Volcano type: composite (red map area) Composition: basalt to rhyolite Most recent eruption: 950 years ago Nearby towns: Malin, Merrill, Tulelake, Klamath Falls (OR) Threat Potential: High Mount Shasta Location: California, Siskiyou County Latitude: 41.409° N Longitude: 122.193° W Elevation: 4,317 (m) 14,163 (f) Volcano type: Stratovolcano Composition: andesite, dacite Most recent eruption: 200- 300 years ago Nearby towns: Weed, Mount Shasta, Edgewood, Dunsmuir Threat Potential: High Lassen Volcanic Center Location: California, Shasta County Latitude: 40.492° N Longitude: 121.508° W Elevation: 3,187 (m) 10,456 (f) Volcano type: stratovolcano Composition: andesite, dacite Most recent eruption: 1917 Nearby towns: Mineral, Viola Threat Potential: High Mount Bachelor Location: Oregon, Deschutes County Latitude: 43.979° N Longitude: 121.688° W Elevation: 2,764 (m) 9,068 (f) Volcano type: Stratovolcano Composition: Basalt to Andesite Most recent eruption: About 9,500 years ago Threat Potential: Moderate Mount Jefferson Location: Oregon, Jefferson/Linn/Marion Counties Latitude: 44.674° N Longitude: 121.8° W Elevation: 3,199 (m) 10,495 (f) Volcano type: Stratovolcano Composition: Andesite to Dacite Most recent eruption: During last glaciation ~15,000 years ago Threat Potential: Low/Very Low Belknap Location: Oregon, Linn County Latitude: 44.285° N Longitude: 121.841° W Elevation: 2,095 (m) 6,873 (f) Volcano type: Shield volcano Composition: Basalt, Basaltic Andesite Most recent eruption: 1500 years ago Nearby towns: Sisters Threat Potential: Low/Very Low Black Butte Crater Lava Field Location: Idaho, Snake River Plain Latitude: 43.18° N Longitude: 114.35° W Elevation: 1,478 (m) 4,849 (f) Volcano type: Shield volcano Composition: Basalt Threat Potential: Low/Very Low Blue Lake Crater Location: Oregon, Jefferson County Latitude: 44.411° N Longitude: 121.774° W Elevation: 1,230 (m) 4,035 (f) Volcano type: Maar Composition: Basalt Most recent eruption: 1300 years ago Nearby towns: Sisters Threat Potential: Low/Very Low Cinnamon Butte Location: Oregon, Douglas County Latitude: 43.241° N Longitude: 122.108° W Elevation: 1,956 (m) 6,417 (f) Volcano type: Scoria cone Composition: Basalt Most recent eruption: between 7,780 and 15,000 years ago Threat Potential: Low/Very Low Craters of the Moon Volcanic Field Location: Idaho, Snake River Plain Latitude: 43.42° N Longitude: 113.5° W Elevation: 2,005 (m) 6,578 (f) Volcano type: Cinder cones Composition: Basalt Threat Potential: Low/Very Low Davis Lake Volcanic Field Location: Oregon, Deschutes County Latitude: 43.641° N Longitude: 121.818° W Elevation: 1,494 (m) 4,902 (f) Volcano type: Lava flows Composition: Andesite Most recent eruption: 5,300-5,600 years ago Nearby towns: Gilchrist, La Pine Threat Potential: Low/Very Low Devils Garden Lava Field Location: Oregon, Lake County Latitude: 43.512° N Longitude: 120.861° W Elevation: 1,698 (m) 5,571 (f) Volcano type: Volcanic field Composition: Basalt Most recent eruption: Holocene Nearby towns: La Pine, Gilchrist, Sunriver, Wagontire Threat Potential: Low/Very Low Diamond Craters Volcanic Field Location: Oregon, Harney County Latitude: 43.095° N Longitude: 118.785° W Elevation: 1,435 (m) 4,708 (f) Volcano type: Volcanic field Composition: Basalt Most recent eruption: 7,790 to 7,320 years ago Nearby towns: Diamond (8 mi), New Princeton (18 mi), Burns (50 mi) Threat Potential: Low/Very Low Four Craters Lava Field Location: Oregon, Lake County Latitude: 43.361° N Longitude: 120.669° W Elevation: 1,501 (m) 4,925 (f) Volcano type: Volcanic field Composition: Basalt Most recent eruption: 13,000 years ago Nearby towns: La Pine, Gilchrist, Sunriver, Wagontire Threat Potential: Low/Very Low Hell's Half Acre Lava Field Location: Idaho, Bonneville/Bingham Counties Latitude: 43.5° N Longitude: 112.45° W Elevation: 1,631 (m) 5,351 (f) Volcano type: Shield volcano Composition: Basalt Most recent eruption: 5,200 years ago Threat Potential: Low/Very Low Indian Heaven Volcanic Field Location: Washington, Skamania County Latitude: 45.93° N Longitude: 121.82° W Elevation: 1,806 (m) 5,925 (f) Volcano type: Shield volcanoes Composition: Basalt to Andesite Most recent eruption: 9,000 years ago Threat Potential: Low/Very Low Jordan Craters Volcanic Field Location: Oregon, Malheur County Latitude: 43.147° N Longitude: 117.46° W Elevation: 1,473 (m) 4,833 (f) Volcano type: Volcanic field Composition: Basalt Most recent eruption: 3,200 years ago Nearby towns: Jordan Valley Threat Potential: Low/Very Low Lava Mountain Lava Field Location: Oregon Latitude: 43.472° N Longitude: 120.754° W Elevation: 1,711 (m) 5,614 (f) Volcano type: Volcanic field Composition: Basalt Most recent eruption: 13,000 years ago Nearby towns: La Pine, Gilchrist, Sunriver, Wagontire Threat Potential: Low/Very Low Sand Mountain Volcanic Field Location: Oregon Latitude: 44.38° N Longitude: 121.93° W Elevation: 1,664 (m) 5,459 (f) Volcano type: Cinder cones Composition: Basalt, Basaltic Andesite Most recent eruption: About 2,000 years ago Threat Potential: Low/Very Low Wapi Lava Field Location: Idaho, Snake River Plain Latitude: 42.88° N Longitude: 113.22° W Elevation: 1,604 (m) 5,262 (f) Volcano type: Shield volcano Composition: Basalt Most recent eruption: 2,270 years ago Threat Potential: Low/Very Low West Crater Volcanic Field Location: Washington, Skamania County Latitude: 45.88° N Longitude: 122.08° W Elevation: 1,329 (m) 4,360 (f) Volcano type: Volcanic field Composition: Basalt to Andesite Threat Potential: Low/Very Low .
Recommended publications
  • The Geological Newsletter
    JAN 90 THE GEOLOGICAL NEWSLETTER ·• GEOLOGICAL SOCIETY OF THE OREGON COUNTRY GEOLOGICAL SOCIETY Non-Profit Org. U.S. POSTAGE OF THE OREGON COUNTRY PAID P.O. BOX ?a 7- Portland, Oregon PORTLAND, OR 97207- -:· ·--~··, Permit No. 999 - -- '~ Dr. Frank Boersma 120 W. 33~d Street Vancouver, WA 98660 GEOLOGICAL SOCIETY OF THE OREGOt\ COllNTRY 1989-1990 ADMINISTRATION BOARD OF DIRECTORS President Directors Rosemary Kenney 221-0757 Peter E. Baer (3 years) 661-7995 4211 S\-1 Condor Charlene Holzwarth (2 years) 284-3444 Portland, OR 97201 Esther Kennedy (1 year) 287-3091 Vice President Margaret L. Steere 246-1670 Immediate Past Presidents Joline Robustelli 223-2852 6929 SW 34 Ave. ~ Portland, OR 97219 R.E. (Andy) Corcoran 244-5605 Secretary Alta B. Fosback 641-6323 THE GEOLOGICAL NEWSLETTER 8942 SW Fairview Place Tigard, OR 97223 Editor: Sandra Anderson 775-5538 Treasurer Calendar: Margaret Steere 246-1670 Braden Pillow 659-6318 Business Manager: Carol Cole 220-0078 19562 SE Cottonwood St. Assist: Cecelia Crater 235-5158 Milwaukie, OR 97267 ACTIVITIES CHAIRS Calligrapher Properties and PA System Wallace R.· McClung 637-3834 (Luncheon) Donald Botteron 245-6251 Field Trips (Evening) Walter A. Sunderland 625-6840 Charlene Holzwarth 284-3444 Publications Alta B. Fosback 641-6323 Geneva E. Reddekopp 654-9818 Geology Seminars Publicity Donald D. Barr 246-2785 Roberta L. Walter 235-3579 Historian Refreshments Phyllis G. Bonebrake 289-8597 (Friday Evening) Hospitality David and Marvel Gillespie 246-2368 254-0135 (Luncheon) Margaret Fink 289-0188 Harold and Patricia Gay Moore (Evening) Maxine Harrington 297-ll86 (Geology Seminars) Catherine Evenson 654-2636 Library: Esther Kennedy 287-3091 ' ' Betty Turner 246-3192 Telephone n Past Presidents Panel Jean L.
    [Show full text]
  • Volcanic Vistas Discover National Forests in Central Oregon Summer 2009 Celebrating the Re-Opening of Lava Lands Visitor Center Inside
    Volcanic Vistas Discover National Forests in Central Oregon Summer 2009 Celebrating the re-opening of Lava Lands Visitor Center Inside.... Be Safe! 2 LAWRENCE A. CHITWOOD Go To Special Places 3 EXHIBIT HALL Lava Lands Visitor Center 4-5 DEDICATED MAY 30, 2009 Experience Today 6 For a Better Tomorrow 7 The Exhibit Hall at Lava Lands Visitor Center is dedicated in memory of Explore Newberry Volcano 8-9 Larry Chitwood with deep gratitude for his significant contributions enlightening many students of the landscape now and in the future. Forest Restoration 10 Discover the Natural World 11-13 Lawrence A. Chitwood Discovery in the Kids Corner 14 (August 4, 1942 - January 4, 2008) Take the Road Less Traveled 15 Larry was a geologist for the Deschutes National Forest from 1972 until his Get High on Nature 16 retirement in June 2007. Larry was deeply involved in the creation of Newberry National Volcanic Monument and with the exhibits dedicated in 2009 at Lava Lands What's Your Interest? Visitor Center. He was well known throughout the The Deschutes and Ochoco National Forests are a recre- geologic and scientific communities for his enthusiastic support for those wishing ation haven. There are 2.5 million acres of forest including to learn more about Central Oregon. seven wilderness areas comprising 200,000 acres, six rivers, Larry was a gifted storyteller and an ever- 157 lakes and reservoirs, approximately 1,600 miles of trails, flowing source of knowledge. Lava Lands Visitor Center and the unique landscape of Newberry National Volcanic Monument. Explore snow- capped mountains or splash through whitewater rapids; there is something for everyone.
    [Show full text]
  • Pacific Crest National Scenic Trail FY 2017 Appropriations Request
    Photo ©2016 Alasdair Fowler Pacific Crest National Scenic Trail FY 2017 Appropriations Request Prepared by: Pacific Crest Trail Association www.pcta.org Graphic design donated by Cover Photos by Alasdair Fowler, Shonda Feather and Carolyn Tepolt Pacific Crest National Scenic Trail FY2017 Appropriations Request The Pacific Crest Trail Association (PCTA) respectfully asks Congress to support the following FY2017 appropriations to protect, preserve and promote the Pacific Crest National Scenic Trail (PCT): I. Land PCT Corridor Acquisition Projects & Water U.S. Forest Service (USFS) Budget Request Conservation $7.0 million Fund California—Landers Meadow, trail and resource (LWCF) protection within the Sequoia National Forest; Trinity Divide, trail and resource protection within the Shasta- Trinity National Forest, Donomore Meadows, trail and resource protection within the Rogue River-Siskiyou National Forest. Washington—Columbia Gorge, trail and resource protection in and adjacent to the Columbia River Gorge National Scenic Area; Stevens Pass, purchase portion of the trail that currently has no easement. $250,000—LWCF line item for program administration Bureau of Land Management (BLM) Budget Request $515,000 California—California Desert Southwest, purchase parcels within the San Gorgonio Wilderness to create an uninterrupted wilderness experience. Oregon—Cascade-Siskiyou Area, trail and resource $7.8 million protection in southern Oregon near the Klamath Basin. U.S. Forest Service (USFS) Budget Request II. Capital $2.1 million—allocation
    [Show full text]
  • GEOLOGIC MAP of the MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE of SOUTHERN WASHINGTON by Wes Hildreth and Judy Fierstein
    U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-2460 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE OF SOUTHERN WASHINGTON By Wes Hildreth and Judy Fierstein When I climbed Mount Adams {17-18 August 1945] about 1950 m (6400') most of the landscape is mantled I think I found the answer to the question of why men by dense forests and huckleberry thickets. Ten radial stake everything to reach these peaks, yet obtain no glaciers and the summit icecap today cover only about visible reward for their exhaustion... Man's greatest 2.5 percent (16 km2) of the cone, but in latest Pleis­ experience-the one that brings supreme exultation­ tocene time (25-11 ka) as much as 80 percent of Mount is spiritual, not physical. It is the catching of some Adams was under ice. The volcano is drained radially vision of the universe and translating it into a poem by numerous tributaries of the Klickitat, White Salmon, or work of art ... Lewis, and Cis pus Rivers (figs. 1, 2), all of which ulti­ William 0. Douglas mately flow into the Columbia. Most of Mount Adams and a vast area west of it are Of Men and Mountains administered by the U.S. Forest Service, which has long had the dual charge of protecting the Wilderness Area and of providing a network of logging roads almost INTRODUCTION everywhere else. The northeast quadrant of the moun­ One of the dominating peaks of the Pacific North­ tain, however, lies within a part of the Yakima Indian west, Mount Adams, stands astride the Cascade crest, Reservation that is open solely to enrolled members of towering 3 km above the surrounding valleys.
    [Show full text]
  • Diamond Craters Oregon's Geologic
    Text by Ellen M. Benedict, 1985 Features at stops correspond to points on a clock ago, a huge mass of hot gases, volcanic ashes, bits face. Imagine that you are standing in the middle of a of pumice and other pyroclastics (fire-broken rock) Travel And Hiking Hints clock face. Twelve o’clock is the road in front of you violently erupted. The blast – greater than the May and 6 o’clock the road behind. If you always align the 18, 1980, eruption of Mt. St. Helens – deposited a Diamond Craters is located in the high desert country clock face with the road, you should be able to locate layer of pyroclastics 30 to 130 feet thick over an area about 55 miles southeast of Burns, Oregon. It’s an the features. almost 7,000 square miles! isolated place and some precautions should be taken . when traveling in the area. Start Tour. Mileage begins halfway Pyroclastics are between milepost 40 and 41 on State normal behavior Diamond Craters has no tourist facilities. The nearest Highway 205 at the junction to Diamond. for magmas place where gasoline is sold is at Frenchglen. Turn left. (subsurface That’s the opinion held by scores of molten rocks) Keep your scientists and educators who have visited Diamond, Oregon, a small ranching community, was of rhyolitic (a vehicle on named in 1874 for Mace McCoy’s Diamond brand. volcanic material and studied the area. It has the “best and hard-packed The nearby craters soon became known as Diamond related to granite) most diverse basaltic volcanic features in the road surfaces Craters.
    [Show full text]
  • Diamond Pond, Harney County, Oregon: Vegetation History and Water Table in the Eastern Oregon Desert
    Great Basin Naturalist Volume 47 Number 3 Article 7 7-31-1987 Diamond Pond, Harney County, Oregon: vegetation history and water table in the eastern Oregon desert Peter Ernest Wigand Washington State University, Pullman, Washington Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Wigand, Peter Ernest (1987) "Diamond Pond, Harney County, Oregon: vegetation history and water table in the eastern Oregon desert," Great Basin Naturalist: Vol. 47 : No. 3 , Article 7. Available at: https://scholarsarchive.byu.edu/gbn/vol47/iss3/7 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. DIAMOND POND, HARNEY COUNTY, OREGON VEGETATION HISTORY AND WATER TABLE IN THE EASTERN OREGON DESERT Peter Ernest Wigand' Abstract —Cores obtained in 1978 from Diamond Pond, Diamond Craters, Harney County, Oregon, as part of the Steens Mountain Prehistory Project, provide a record of vegetation change on the sagebrush/shadscale ecotone and of local and perhaps regional water tables. Pollen, macrofossils, sediments, and charcoal from these radiocarbon-dated cores were analyzed. Varying abundance ofjuniper, grass, sagebrush, and greasewood pollen, and of aquatic to littoral plant macrofossils reflects changing regional effective moisture and local water table since 6000 B. P. Eleven dates spanning 5200 radiocarbon years and four regionally correlated volcanic ashes establish the dating of seven periods of diflferent moisture regimes; 1. Greasewood and saltbush pollen dominance before 5400 B.P.
    [Show full text]
  • IC-62, Heat Flow Studies in the Steamboat Mountain-Lemei Rock
    ,. \\ :\ .J ~\ .... 7 \; t,6 i u2 W~~fnffl:RY u.no C ';I, .... DEPARTMENT OF NATURAL RESOURCES i n BERT L. COLE, Commissioner of Public Lands ; RALPH A. BESWICK Supervisor I: s DIVISION OF GEOLOGY AND EARTH RESOURCES VAUGHN E. LIVINGSTON, JR., State Geologist INFORMATION CIRCULAR 62 HEAT FLOW STUDIES IN THE STEAMBOAT MOUNTAIN-LEMEI ROCK AREA, SKAMANIA COUNTY, WASHINGTON BY J. ERIC SCHUSTER, DAVID D. BLACKWELL, PAUL E. HAMMOND, and MARSHALL T. HUNTTING Final report to the NATIONAL SCIENCE FOUNDATION on sponsored proiect AER75 ... 02747 1978 STATE OF WASHINGTON DEPARTMENT OF NATURAL RESOURCES BERT L COLE, Commissioner of Public Lands RALPH A. BESWICK Supervisor DIVISION OF GEOLOGY AND EARTH RESOURCES VAUGHN E. LIVINGSTON, JR., State Geologist INFORMATION CIRCULAR WA He<1.t iluw 33.J. -7 stu.diei::,; ln the .M6 t> i Stean, l:on. t --- bJ. ~uu,i ta i u-.Lem~ i 1970 Jiuck d.rea, Skaina11ia Cuunt),, W a i'ii1 i u ~ton HEAT FLOW STUDIES IN THE STEAMBOAT MOUNTAIN-LEMEI ROCK AREA, SKAMANIA COUNTY, WASHINGTON BY J. ERIC SCHUSTER, DAVID D. BLACKWELL, PAUL E. HAMMOND, and MARSHALL T. HUNTTING Final report to the NATIONAL SC !ENCE FOUNDATION on sponsored project AER75-02747 1978 CONTENTS Abstract ................. , . .. .. .. .. .. .. .. .. .. 1 Introduction ..................................................................... , • . 2 Acknowledgments • • • • • • . • • . • . • • . • . • . • . • . • . • • • • • • . • • • • . • . 3 Geo logy • . • • • • • • . • • • • • • . • • . • • . • . • . • • . • . 4 Genera I features ............................
    [Show full text]
  • A Tale of Three Sisters: Reconstructing the Holocene Glacial History and Paleoclimate Record at Three Sisters Volcanoes, Oregon, United States
    Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 2005 A Tale of Three Sisters: Reconstructing the Holocene glacial history and paleoclimate record at Three Sisters Volcanoes, Oregon, United States Shaun Andrew Marcott Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geology Commons, and the Glaciology Commons Let us know how access to this document benefits ou.y Recommended Citation Marcott, Shaun Andrew, "A Tale of Three Sisters: Reconstructing the Holocene glacial history and paleoclimate record at Three Sisters Volcanoes, Oregon, United States" (2005). Dissertations and Theses. Paper 3386. https://doi.org/10.15760/etd.5275 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 Shaun Andrew Marcott for the Master of Science in Geology were presented August II, 2005, and accepted by the thesis committee and the department. COMMITTEE APPROVALS: (Z}) Representative of the Office of Graduate Studies DEPARTMENT APPROVAL: MIchael L. Cummings, Chair Department of Geology ( ABSTRACT An abstract of the thesis of Shaun Andrew Marcott for the Master of Science in Geology presented August II, 2005. Title: A Tale of Three Sisters: Reconstructing the Holocene glacial history and paleoclimate record at Three Sisters Volcanoes, Oregon, United States. At least four glacial stands occurred since 6.5 ka B.P. based on moraines located on the eastern flanks of the Three Sisters Volcanoes and the northern flanks of Broken Top Mountain in the Central Oregon Cascades.
    [Show full text]
  • The Plumbing Systems and Parental Magma Compositions Of
    THE PLUMBING SYSTEMS AND PARENTAL MAGMA COMPOSITIONS OF SHIELD VOLCANOES IN THE CENTRAL OREGON HIGH CASCADES AS INFERRED FROM MELT INCLUSION DATA by STANLEY PAUL MORDENSKY II A THESIS Presented to the Department of Geological Sciences and the Graduate School of the University of Oregon in partial fulfillment of the requirements for the degree of Master of Science September 2012 THESIS APPROVAL PAGE Student: Stanley Paul Mordensky II Title: The Plumbing Systems and Parental Magma Compositions of Shield Volcanoes in the Central Oregon High Cascades as Inferred from Melt Inclusion Data This thesis has been accepted and approved in partial fulfillment of the requirements for the Master of Science degree in the Department of Geological Sciences by: Dr. Paul Wallace Chair Dr. Ilya Bindeman Member Dr. Katharine Cashman Member Dr. Dana Johnston Member and Kimberly Andrews Espy Vice President for Research & Innovation/Dean of the Graduate School Original approval signatures are on file with the University of Oregon Graduate School. Degree awarded September 2012 ii © 2012 Stanley Paul Mordensky II iii THESIS ABSTRACT Stanley Paul Mordensky II Master of Science Department of Geological Sciences September 2012 Title: The Plumbing Systems and Parental Magma Compositions of Shield Volcanoes in the Central Oregon High Cascades as Inferred from Melt Inclusion Data Long-lived and short-lived volcanic vents often form in close proximity to one another. However, the processes that distinguish between these volcano types remain unknown. Here, I investigate the differences of long-lived (shield volcano) and short- lived (cinder cone) magmatic systems using two approaches. In the first, I use melt inclusion volatile contents for shield volcanoes and compare them to published data for cinder cones to investigate how shallow magma storage conditions differ between the two vent types in the Oregon Cascades.
    [Show full text]
  • DOGAMI Open-File Report O-92-09, Preliminary Geologic Map of the Jordan Craters South Quadrangle, Malheur County, Oregon
    OPEN-FILE REPORT 0-92-09 PRELIMINARY GEOLOGIC MAP OF THE JORDAN CRATERS SOUTH QUADRANGLE MALHEUR COUNTY, OREGON By M. L. Ferns, and N. S. MacLeod Oregon Department of Geology and Mineral Industries This unpublished Open-File Report has not been reviewed and may not meet all Oregon Department of Geology and Mineral Industries' standards. Field work conducted in 1990/1991 Map Scale: 1:24,000 Funding Statement: Funded jointly by the Oregon Department of Geology and Mineral Industries, the Oregon State Lottery, and the U. S. Geological Survey COGEOMAP Program as part of a cooperative effort to map the west half of the lo by 2O Boise sheet, eastern Oregon. Jordan Craters South A distinctive, densely-welded, high-silica rhyolite ashflow tuff (Ttlg?) comprises the oldest unit exposed in the Jordan Craters South quadrangle. The ashflow is characterized by high silica and low alumina abundance5 and is correlative with tuffs mapped by Plumley (1984) as Leslie Gulch Tuff in The Hole in the Ground quadrangle to the northwest. If his correlation is correct, Ttlg? is part of the outflow sheet erupted during formation of the Mahogany Mountain caldera tn the northeast. The ashflow is overlain by tuffaceous siltstones (Tsts) and aphyric platy andesite flows (Tmv). Tilted fault blocks comprised of all three units from steptoes around which younger basalts (Tbdb, Tbtm, QTb, Qbcb, Qbrb, and Qbjc) have flowed. The youngest of these (Qbjc) erupted at about 3,000 years ago from a small vent north of the quadrangle at Jordan Crater. The surface of the Qbjc flow is free of wind- blown silt and soil and contains many fragile surface features that are characteristic of very young basalt flows.
    [Show full text]
  • PDF Linkchapter
    Index [Italic page numbers indicate major references] Abajo Mountains, 382, 388 Amargosa River, 285, 309, 311, 322, Arkansas River, 443, 456, 461, 515, Abort Lake, 283 337, 341, 342 516, 521, 540, 541, 550, 556, Abies, 21, 25 Amarillo, Texas, 482 559, 560, 561 Abra, 587 Amarillo-Wichita uplift, 504, 507, Arkansas River valley, 512, 531, 540 Absaroka Range, 409 508 Arlington volcanic field, 358 Acer, 21, 23, 24 Amasas Back, 387 Aromas dune field, 181 Acoma-Zuni scction, 374, 379, 391 Ambrose tenace, 522, 523 Aromas Red Sand, 180 stream evolution patterns, 391 Ambrosia, 21, 24 Arroyo Colorado, 395 Aden Crater, 368 American Falls Lava Beds, 275, 276 Arroyo Seco unit, 176 Afton Canyon, 334, 341 American Falls Reservoir, 275, 276 Artemisia, 21, 24 Afton interglacial age, 29 American River, 36, 165, 173 Ascension Parish, Louisana, 567 aggradation, 167, 176, 182, 226, 237, amino acid ash, 81, 118, 134, 244, 430 323, 336, 355, 357, 390, 413, geochronology, 65, 68 basaltic, 85 443, 451, 552, 613 ratios, 65 beds, 127,129 glaciofluvial, 423 aminostratigraphy, 66 clays, 451 Piedmont, 345 Amity area, 162 clouds, 95 aggregate, 181 Anadara, 587 flows, 75, 121 discharge, 277 Anastasia Formation, 602, 642, 647 layer, 10, 117 Agua Fria Peak area, 489 Anastasia Island, 602 rhyolitic, 170 Agua Fria River, 357 Anchor Silt, 188, 198, 199 volcanic, 54, 85, 98, 117, 129, Airport bench, 421, 423 Anderson coal, 448 243, 276, 295, 396, 409, 412, Alabama coastal plain, 594 Anderson Pond, 617, 618 509, 520 Alamosa Basin, 366 andesite, 75, 80, 489 Ash Flat, 364 Alamosa
    [Show full text]
  • MINERAL RESOURCES of the JORDAN CRATERS WILDERNESS STUDY AREA, MALHEUR COUNTY, OREGON By
    DEPARTMENT OF THE INTERIOR UNTIED STATES GEOLOGICAL SURVEY MINERAL RESOURCES OF THE JORDAN CRATERS WILDERNESS STUDY AREA, MALHEUR COUNTY, OREGON By J.P. Calzia1, Susan Hubbard-Sharpless2, R.L. Turner3, Andrew Griscorn1, and D.L. Sawatzky3 U.S. Geological Survey and J.M. Linne3 U.S. Bureau of Mines U.S. Geological Survey Open-File Report 88-572 Prepared by the U.S. Geological Survey and the U.S. Bureau of Mines for the U.S. Bureau of Land Management This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey. 1 - Menlo Park, CA 94025 2Blacksburg, VA 24060 3Spokane, WA 99202 1988 STUDIES RELATED TO WILDERNESS Bureau of Land Management Wilderness Study Area The Federal Land Policy and Management Act (Public Law 94-579, October 21,1976) requires the U.S. Geological Survey and the U.S. Bureau of Mines to conduct mineral surveys on certain areas to determine the mineral values, if any, that may be present Results must be made available to the public and be submitted to the President and the Congress. This report presents the results of a mineral survey of the Jordan Craters Wilderness Study Area (OR-003-128), Malheur County, Oregon. CONTENTS Summary 1 Abstract 1 Character and setting 1 Identified mineral resources and mineral resource potential 1 Introduction 1 Location and physiography 1 Previous studies 3 Present investigations 3 Appraisal of identified resources 3 Assessment of mineral resource potential 3 Geology 3 Geochemistry 4 Geophysics 4 Mineral resource potential 5 References cited 6 Appendixes 8 Definition of levels of mineral resource potential and certainty of assessment 9 Resource/reserve classification 10 Geologic time chart 11 FIGURE 1.
    [Show full text]