Guide to Newberry National Volcanic Monument
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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. -
Field Guides
Downloaded from fieldguides.gsapubs.org on June 1, 2012 Field Guides The post-Mazama northwest rift zone eruption at Newberry Volcano, Oregon Daniele Mckay, Julie M. Donnelly-Nolan, Robert A. Jensen and Duane E. Champion Field Guides 2009;15;91-110 doi: 10.1130/2009.fld015(05) Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Field Guides Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. Notes © 2009 Geological Society of America Downloaded from fieldguides.gsapubs.org on June 1, 2012 The Geological Society of America Field Guide 15 2009 The post-Mazama northwest rift zone eruption at Newberry Volcano, Oregon Daniele Mckay* Department of Geological Sciences, 1272 University of Oregon, Eugene, Oregon 97403-1272, USA Julie M. -
Newberry National Volcanic Monument U.S
Deschutes National Forest Newberry National Volcanic Monument U.S. Forest Service U.S. Department of Agriculture Summer/Fall 2015 Volcanic Vistas Visitor Guide “Frost at Paulina Lake” Photo: A. Jewell EBRATIN EL G Volcanic Wonders… C Yours to Discover! Visiting Newberry National Volcanic Monument allows you to explore Newberry Volcano, YEARS the largest volcano in the Cascade Range. There are extraordinary Volcanic Wonders within the Monument, making it a great place to learn about Central Oregon’s fiery past. Newberry’s erup- tive history began 400,000 years ago and has created massive lava flows covering 1,200 square Newberry’s visitors of yesteryear: stopping by Paulina miles, producing lava tubes, and over 400 cinder cones and volcanic vents during it’s active Peak along old Forest Road 21. periods. The last eruption—just 1,300 years ago—formed the youngest lava flow in Oregon. Welcome! Newberry’s rich cultural history offers many ways for you to connect with those who came before. From the native communities who first crossed this land to the early European and June marks the beginning of a year- American explorers, from the grass-roots led Monument creators to casual visitors today, long celebration of the designation people have marveled at this rugged landscape for thousands of years. of Newberry National Volcanic Monument. Join us to celebrate this The Volcanic Wonders of Newberry National Volcanic Monument offer boundless opportunities remarkable volcanic landscape, its for exploration and recreation… yours to discover! diversity of outstanding recreation opportunities, and its rich cultural Lava Butte rises 500 feet above its history. -
Newberry National Volcanic Monument U.S
Deschutes National Forest Newberry National Volcanic Monument U.S. Forest Service U.S. Department of Agriculture Summer/Fall 2015 Volcanic VistasVisitor2016 Guide Look Inside! EBRATIN EL G 2… Camping, Lodging, Food Volcanic Wonders… C 3… Activities 4… Hiking Trails Yours to Discover! 5… Monument Map Visiting Newberry National Volcanic Monument allows you to explore Newberry Volcano, YEARS 6… Could It Erupt Again? the largest volcano in the Cascade Range. There are extraordinary Volcanic Wonders within the 7… Caves, Bats, & Bears! Monument, making it a great place to learn about Central Oregon’s fiery past. Newberry’s erup- 8… Support Your Monument! tive history began 400,000 years ago and has created massive lava flows covering 1,200 square miles, producing lava tubes, and over 400 cinder cones and volcanic vents during it’s active periods. The last eruption—just 1,300 years ago—formed the youngest lava flow in Oregon. Newberry’s rich cultural history offers many ways for you to connect with those who came before. From the native communities who first crossed this land to the early European and American explorers, from the grassroots led Monument creators to casual visitors today, peo- ple have marveled at this rugged landscape for thousands of years. The Volcanic Wonders of Newberry National Volcanic Monument offer boundless opportunities for exploration and recreation… yours to discover! Lava Butte rises 500 feet above its Forest Service leadership unveils Newberry’s new sign 9 square-mile lava flow. It erupted 7,000 at the Monument dedication in 1991. years ago and is one of Newberry’s Welcome! many cinder cones. -
Land and Resource Management Plan
, Department of Agriculture Land and Resource Forest Service Pacific Management Plan Northwest Region Deschutes National Forest [Deschutes National Forest Deschutes National Forest Land and Resource Management Plan This National Forest Land and Resource Management Plan (Forest Plan or Pian) was developed to guide all natural resource management activities and establish standards/guidelines for the Deschutes National Forest. The purpose of the Plan is to provide for the use and protectionof Forest resources, fulfill legislative requirements, and address local, regional, and national issues and concems. To accomplish this, the Forest Plan: Establishes the management direction and associated long-range goals and objectives for the Forest for the next 10 to 15 years; Sets the allowable sale quantity for timber and identlfies land sultable for timber management; Specifies standards/guldelines for Forest-wide application; Creates management areas with goals, themes and objectives and additional standards/guideiines: Calls for a monitoring and evaluation program to ensure that the direction is carried out. It includes measures which must be taken if outputs and environmental effects are other than those which were predicted. This Forest Plan has been prepared according to Secretary of Agriculture regulations (36 CFR 219) which are based on the Forest and Rangeland Renewable Resources Planning Act (RPA) as amended by the National Forest Management Act of 1976 (NFMA). The plan has aim been developed in accordance with regulations (40 CFR 1500) for implementing the National Environmental Policy Act (NEPA). Because this plan is considered a major Federal action significantly affecting the qualrty of the human environment, a detailed environmental impact statement has been prepared as required by the NEPA. -
Newberry National Volcanic Monument U.S
Deschutes National Forest U.S. Forest Service Newberry National Volcanic Monument U.S. Department of Agriculture Volcanic Vistas 2019 photo: “Kayaks waiting out the storm on East Lake” by Heidi Walker Look Inside! Volcanic Wonders… Yours to Discover 2… Activities 3… Lodging, Food, & Shuttle Visiting Newberry National Volcanic Monument allows you to explore Newberry Volcano, the largest volcano in 4… Hiking & Camping the Cascade Range. There are extraordinary Volcanic Wonders within the Monument, making it a great place to learn 5… Area Maps about Central Oregon’s fi ery past. Newberry’s eruptive history began 500,000 years ago and created massive lava 6… Caves, Bats, & Wildlife fl ows covering 1,200 square miles, producing lava tubes, and over 400 cinder cones and volcanic vents during it’s 7… Your Monument active periods. The last eruption—just 1,300 years ago—formed the youngest lava fl ow in Oregon. 8… Overview Map Newberry’s rich cultural history offers many ways for you to connect with those who came before. From the na- tive communities who fi rst crossed this land to the early European and American explorers, from the grassroots led Monument creators to casual visitors today, people have marveled at this rugged landscape for thousands of years. Discovery Awaits You Lava Butte rises 500 feet above its 9 square-mile lava fl ow. It erupted 7,000 years ago and is one of Newberry’s many cinder cones. Lava Cast Forest formed when Lava Butte photo: Heidi Walker Welcome! a lava fl ow overtook an old-growth forest and cooled to form casts of the Newberry National Volcanic Monument trees that once stood there. -
1 Decision Notice & Finding of No Significant Impact Lava Cast Project
Decision Notice & Finding of No Significant Impact Lava Cast Project USDA Forest Service Bend-Ft. Rock Ranger District, Deschutes National Forest Deschutes County, Oregon T. 20 S., R. 11and 12 E. and T. 21 S., R. 11and 12 E BACKGROUND The Lava Cast Project Environmental Assessment (hereinafter referred to as the EA) has been prepared to describe the effects of implementing each of the three alternatives, including one No Action alternative and two action alternatives, that address vegetation and fuels conditions in the project area. Activities would occur on approximately 9,500 acres on the Bend-Fort Rock Ranger District. The project would move vegetative resource conditions closer to the goals and desired future conditions identified in the Deschutes National Forest Land and Resource Management Plan and the Newberry National Volcanic Monument Plan. The analysis describes the effects of using various means to move forest stands towards historic conditions to improve stand health and reduce the likelihood of a stand replacing wildfire. Methods to accomplish this include commercial and pre-commercial thinning, mechanical shrub treatment (mowing), hand and grapple piling slash and fuels, and prescribed fire. LOCATION The Lava Cast planning area is approximately 36,000 acres, including a portion of the Newberry National Volcanic Monument (Transition Zone, 5,935 acres). Approximately 2,369 acres lie within the wildland- urban interface zone (WUI), which as defined within the Upper Deschutes River Natural Resources Coalition Community Wildfire Protection Plan. The planning area is located approximately 10 miles south of the urban growth boundary of Bend and one mile east of Sunriver. -
Ore Bin / Oregon Geology Magazine / Journal
OCTOBER 1977 VOLUME 39, No. 10 SUBSCRIPTION RENEWAL ISSUE SUBSCRIPTION EXPIRATION DATE ON BACK COVER STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES The Ore Bin Published Monthly By STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES Head Office: 1069 State Office Bldg., Partland, Oregon 9n01 Telephone: [503] 229-5580 FIELD OFFICES 2033 First Street 521 N.E. "E" Street Baker 97814 Grants Pass 97526 Subscription Rates 1 year, $3.00; 3 years, $8.00 Available back issues, $.25 at caunter, $.35 mailed Second class postage paid at Portland, Oregon GOVERNING BOARD Leeanne MacCo", Portland Robert W. Daly, Ta lent John l. Schwabe, Portland ACTING STATE GEOLOGIST Ralph S. Mason GEOLOGISTS IN CHARGE OF FIELD OFFICES Haward C. Brooks, Ba ker Len Ramp, Grants Pass EDITOR Beverly F. Vogt Permission is granted to reprint information contained herein. Credit given the State of Oregon Department of Geology and Mineral Industries for compiling this information will be appreciated. State of Or egon The ORE BIN Depa rtme nt of Geology and Mineral Industries Volume 39, No. 10 1069 State Officf' Bl dg_ Port land. Oregon 97201 October 1977 THE AGE OF LAVA BUTTE Lawrence A. Chitwood*, Robert A. Jensen**, and Edward A. Groh*** La va Butte and its jagged black fields of lava, located 10 mi (16 km) south of Bend along U.S. Highway 97 . have been major scenic and geologic attractions since at least 1900 (Figure 1). Public interest in the natural history of Lava Butte and the vast volcan ic and glacial panorama seen from its summit led the U.S. -
STATE of OREGON DEPARTMENT of GEOLOGY and MINERAL INDUSTRIES the Ore Bin
aLoi .11 SLI.EV untversity • Vol. 31, No.4 April 1969 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES The Ore Bin Published Monthly By STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES • Head Office: 1069 State Office Bldg., Portland, Oregon - 97201 Telephone: 226 - 2161, Ext. 488 FIELD OFFICES 2033 First Street 521 N. E. "E" Street Baker 97814 Grants Pass 97526 X X X XX X X XX X X XX X X XX X X X Subscription rate $1.00 per year. Available back issues 10 cents each. Second class postage paid at Portland, Oregon 5Z 5Z 5Z 5z 5Z 9' 9' 9. 9. >7'tir x x '9‘ 5? • GOVERNING BOARD Fayette I. Bristol, Rogue River, Chairman Harold Banta, Baker STATE GEOLOGIST R. E. Corcoran GEOLOGISTS IN CHARGE OF FIELD OFFICES Norman S. Wagner, Baker Len Ramp, Grants Pass Permission is granted to reprint information contained herein. Credit given the State of Oregon Department of Geology and Mineral Industries for compiling this information will be appreciated. State of Oregon The ORE BIN Department of Geology and Mineral Industries Volume 31, No. 4 1069 State Office Bldg. Apri I 1969 Portland, Ore. 97201 THE AGES OF SOME HOLOCENE VOLCANIC ERUPTIONS • IN THE NEWBERRY VOLCANO AREA, OREGON By N. V. Peterson* and E. A. Groh** Several episodes of volcanism of Holocene age (since the last 11,000 years) are well recorded within Newberry Crater and on the flanks of Newberry Volcano in central Oregon. Newberry Volcano is a huge shield volcano which rises from the basalt plateau south of Bend and east of the Cascade Range. -
Mckay Et Al., 2009, Newberry Volcano
Downloaded from fieldguides.gsapubs.org on May 6, 2011 The Geological Society of America Field Guide 15 2009 The post-Mazama northwest rift zone eruption at Newberry Volcano, Oregon Daniele Mckay* Department of Geological Sciences, 1272 University of Oregon, Eugene, Oregon 97403-1272, USA Julie M. Donnelly-Nolan* U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025, USA Robert A. Jensen* U.S. Forest Service (retired), Bend, Oregon 97701, USA Duane E. Champion* U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025, USA ABSTRACT The northwest rift zone (NWRZ) eruption took place at Newberry Volcano ~7000 years ago after the volcano was mantled by tephra from the catastrophic erup- tion that destroyed Mount Mazama and produced the Crater Lake caldera. The NWRZ eruption produced multiple lava fl ows from a variety of vents including cinder cones, spatter vents, and fi ssures, possibly in more than one episode. Eruptive behav- iors ranged from energetic Strombolian, which produced signifi cant tephra plumes, to low-energy Hawaiian-style. This paper summarizes and in part reinterprets what is known about the eruption and presents information from new and ongoing studies. Total distance spanned by the eruption is 32 km north-south. The northernmost fl ow of the NWRZ blocked the Deschutes River upstream from the city of Bend, Oregon, and changed the course of the river. Renewed mafi c activity in the region, particu- larly eruptions such as the NWRZ with tephra plumes and multiple lava fl ows from many vents, would have signifi cant impacts for the residents of Bend and other cen- tral Oregon communities. -
Jensen Et Al., 2009, Field Guide to Newberry Volcano
Downloaded from fieldguides.gsapubs.org on May 6, 2011 The Geological Society of America Field Guide 15 2009 A fi eld guide to Newberry Volcano, Oregon Robert A. Jensen* U.S. Forest Service (retired), Bend, Oregon 97701, USA Julie M. Donnelly-Nolan* U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025, USA Daniele Mckay* Department of Geological Sciences, 1272 University of Oregon, Eugene, Oregon 97403-1272, USA ABSTRACT Newberry Volcano is located in central Oregon at the intersection of the Cas- cade Range and the High Lava Plains. Its lavas range in age from ca. 0.5 Ma to late Holocene. Erupted products range in composition from basalt through rhyolite and cover ~3000 km2. The most recent caldera-forming eruption occurred ~80,000 years ago. This trip will highlight a revised understanding of the volcano’s history based on new detailed geologic work. Stops will also focus on evidence for ice and fl ooding on the volcano, as well as new studies of Holocene mafi c eruptions. Newberry is one of the most accessible U.S. volcanoes, and this trip will visit a range of lava types and compositions including tholeiitic and calc-alkaline basalt fl ows, cinder cones, and rhyolitic domes and tuffs. Stops will include early distal basalts as well as the youngest intracaldera obsidian fl ow. OVERVIEW Total volume of erupted lavas probably exceeds 500 km3. Total area is ~3000 km2, including basaltic lavas that extend well Newberry Volcano is a large shield-shaped volcano (Fig. 1), beyond the main edifi ce. The edifi ce itself covers ~1300 km2. -
Replacing Lodgepole Pine (Pinus Contorta) Stand in Central Oregon
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 2-16-2006 Regeneration Patterns and Facilitation Following Blowdown in a Self- Replacing Lodgepole Pine (Pinus contorta) Stand in Central Oregon Jennifer Michelle Karps Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Physical and Environmental Geography Commons Let us know how access to this document benefits ou.y Recommended Citation Karps, Jennifer Michelle, "Regeneration Patterns and Facilitation Following Blowdown in a Self- Replacing Lodgepole Pine (Pinus contorta) Stand in Central Oregon" (2006). Dissertations and Theses. Paper 1482. https://doi.org/10.15760/etd.1482 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 Jennifer Michelle Karps for the Master of Science in Geography were presented February 16, 2006, and accepted by the thesis committee and the department. COMMITTEE APPROVALS: _______________________________________ Keith S. Hadley, Chair _______________________________________ Heejun Chang _______________________________________ Martin D. Lafrenz _______________________________________ Jeffrey Gerwing Representative of the Office of Graduate Studies DEPARTMENT APPROVAL: _______________________________________ Martha A. Works, Chair Department of Geography 2 ABSTRACT An abstract of the thesis of Jennifer Michelle Karps for the Master of Science in Geography presented February 16, 2006. Title: Regeneration Patterns and Facilitation Following Blowdown in a Self- Replacing Lodgepole Pine (Pinus contorta) Stand in Central Oregon Nurse plant and object facilitation is an important factor mitigating abiotic stress, improving seedling recruitment, and shaping the fine-scale spatial patterns of many plant communities.