Wildlife Report for the Newberry Volcano Enhanced Geothermal System (EGS) Demonstration Project
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Appendix a Conceptual Geologic Model
Newberry Geothermal Energy Establishment of the Frontier Observatory for Research in Geothermal Energy (FORGE) at Newberry Volcano, Oregon Appendix A Conceptual Geologic Model April 27, 2016 Contents A.1 Summary ........................................................................................................................................... A.1 A.2 Geological and Geophysical Context of the Western Flank of Newberry Volcano ......................... A.2 A.2.1 Data Sources ...................................................................................................................... A.2 A.2.2 Geography .......................................................................................................................... A.3 A.2.3 Regional Setting ................................................................................................................. A.4 A.2.4 Regional Stress Orientation .............................................................................................. A.10 A.2.5 Faulting Expressions ........................................................................................................ A.11 A.2.6 Geomorphology ............................................................................................................... A.12 A.2.7 Regional Hydrology ......................................................................................................... A.20 A.2.8 Natural Seismicity ........................................................................................................... -
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. -
Overview for Geologic Field-Trip Guides to Mount Mazama, Crater Lake Caldera, and Newberry Volcano, Oregon
Overview for Geologic Field-Trip Guides to Mount Mazama, Crater Lake Caldera, and Newberry Volcano, Oregon Scientific Investigations Report 2017–5022–J U.S. Department of the Interior U.S. Geological Survey Cover (top photo): View east-northeast from Garfield Peak on the south rim of Crater Lake caldera. Peak on skyline is 8,929 feet (2,722 meters) Mount Scott, an ~420 thousand years before present (ka) dacite stratovolcano considered to be part of Mount Mazama, the volcano that collapsed during the caldera-forming eruption ~7,700 years ago. The caldera walls in this view expose Mazama lava flows and fragmental deposits from as old as ~400 ka at Phantom Cone, adjacent to tiny Phantom Ship island, to as young as ~27 ka at Redcloud Cliff, the V-shaped face at the top of the wall left of center. The beheaded glacial valley of Kerr Notch, the low point on the caldera rim, is seen between Phantom Ship and Mount Scott. Photograph by Carly McLanahan. Cover (bottom photo): Newberry Volcano, Oregon, is the largest volcano in the Cascades volcanic arc. This north-facing view taken from the volcano’s peak, Paulina Peak (elevation 7,984 feet), encompasses much of the volcano’s 4-by-5-milewide central caldera, a volcanic depression formed in a powerful explosive eruption about 75,000 years ago. The caldera’s two lakes, Paulina Lake (left) and the slightly higher East Lake (right), are fed in part by active hot springs heated by molten rock (magma) deep beneath the caldera. The Central Pumice Cone sits between the lakes. -
Volcano Hazards at Newberry Volcano, Oregon
Volcano Hazards at Newberry Volcano, Oregon By David R. Sherrod1, Larry G. Mastin2, William E. Scott2, and Steven P. Schilling2 1 U.S. Geological Survey, Hawaii National Park, HI 96718 2 U.S. Geological Survey, Vancouver, WA 98661 OPEN-FILE REPORT 97-513 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1997 U.S. Department of the Interior U.S. Geological Survey CONTENTS Introduction 1 Hazardous volcanic phenomena 2 Newberry's volcanic history is a guide to future eruptions 2 Flank eruptions would most likely be basaltic 3 The caldera would be the site of most rhyolitic eruptions—and other types of dangerously explosive eruptions 3 The presence of lakes may add to the danger of eruptions in the caldera 5 The most damaging lahars and floods at Newberry volcano would be limited to the Paulina Creek area 5 Small to moderate-size earthquakes are commonly associated with volcanic activity 6 Volcano hazard zonation 7 Hazard zone for pyroclastic eruptions 7 Regional tephra hazards 8 Hazard zone for lahars or floods on Paulina Creek 8 Hazard zone for volcanic gases 10 Hazard zones for lava flows 10 Large-magnitude explosive eruptions of low probability 11 Monitoring and warnings 12 Suggestions for further reading 12 Endnotes 13 ILLUSTRATIONS Plate 1. Volcano hazards at Newberry volcano, Oregon in pocket Figure 1. Index map showing Newberry volcano and vicinity 1 Figure 2. -
DOGAMI Open-File Report O-83-03, Survey of Potential Geothermal
DOE/BP/272 STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1005 State Office Building Portland, Oregon 97201 OPEN-FILE REPORT 0-83-3 SURVEY OF POTENTIAL GEOTHERMAL EXPLORATION SITES AT NEWBERRY VOLCANO, DESCHUTES COUNTY, OREGON 1983 edited by George R. Priest, Beverly F. Vogt, and Gerald L. Black, Oregon Department of Geology and Mineral Industries This work was supported by the Bonneville Power Administration under Cooperative Agreement No. DE-AC79-82BP36734. Governi Board State Geologist Allen P. St·inchfield, Chairman, North Bend Donald A. Hull Donald A. Haagensen, Portland Sidney R. Johnson, Baker Deputy State Geologist John D. Beaulieu NOTICE The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. Reference herein to any specific commercial product, process, or service by trade name, mark, manufacturer, or otherwise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. NOTICE The Oregon Department of Geology and Mineral Industries is publishing this paper because the subject matter is consistent with the mission of the Department. To facilitate timely distribution of information, this paper ~as not been edited to our usual standards. ii CONTENTS CHAPTER 1. EXECUTIVE SUMMARY, by George R. Priest 1 Introduction 1 Objectives 1 Methodology 1 Assumptions 2 Conclusions 2 Acknowledgments 4 CHAPTER 2. GEOLOGY OF THE NEWBERRY VOLCANO AREA, DESCHUTES COUNTY, OREGON, by George R. Priest 5 Introduction . 5 Genera 1 Geo 1 ogy . 5 Results of USGS Drilling Program 10 Geophysical Evidence for a Shallow Intrusive 12 Distribution of Volcanic Centers: Implications for the Lateral Extent of a Silicic Intrusive Body 13 Caldera Geometry: Implications for Depths to Former Magma Chambers . -
Volcano Hazards at Newberry Volcano, Oregon by David R
This map shows areas that could be affected in the future by various kinds of eruptions and related events. Although we show sharp boundaries between DESCHUTES CO CROOK CO hazard zones, the degree of hazard does not change abruptly at these boundaries but decreases gradually as distance from the volcano increases. Areas immediately beyond hazard zones should not be regarded as hazard free, because the boundaries can only be approximately located. See accompanying pamphlet for methodology used to define hazard zones and to locate boundaries. Hazard zone for explosive pyroclastic eruptions of small to moderate volume in or near caldera −− Subject to tephra falls, pyroclastic flows and surges, and ballistic projectiles from eruptions of caldera or near − caldera vents. Can also be affected by lava flows and domes. Probability of tephra−fall hazard resulting from explosive eruptions at Newberry and other volcanoes in region is depicted in pamphlet (fig. 4) Hazard zone for lahars or floods on Paulina Creek −− Subject to lahars and flooding in event of volcanically induced surges of water from Paulina Lake. Shown only as far north as confluence of Little Deschutes and Deschutes Rivers; farther north, zone is thought to coincide with 100 − year floodplain of Deschutes River Area of upper west flank where Paulina Creek canyon might not contain peak flows during an exceptionally large flood event (see pamphlet) Hazard zone for volcanic gases −− During volcanic unrest and periods of increased gas emission, hazard lies chiefly in small topographic depressions, caves, and artificially created enclosures such as manholes, excavations, tents, or snowcaves where atmospheric circulation is inadequate to disperse gas Hazard zones for lava flows from flank eruptions −− Also includes areas subject to near − vent deposits of cinder cones and fissure vents. -
Cladouhos.Pdf
PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 31 - February 2, 2011 SGP-TR-191 THE ROLE OF STRESS MODELING IN STIMULATION PLANNING AT THE NEWBERRY VOLCANO EGS DEMONSTRATION PROJECT Trenton T. Cladouhos1, Susan Petty1, Owen Callahan1, Will Osborn1, Stephen Hickman2 and Nicholas Davatzes3 1AltaRock Energy, 7900 E. Green Lake Drive N, Seattle, WA, 98115, USA e-mail: [email protected] 2U.S. Geological Survey, Menlo Park, CA 3Temple University, Philadelphia, PA ABSTRACT NEWBERRY EGS DEMONSTRATION Field work and planning has begun on the Enhanced A DOE-funded EGS demonstration project is now Geothermal Systems (EGS) Demonstration Project at underway at Newberry Volcano in central Oregon. Newberry Volcano in central Oregon. The tectonic Preliminary investigations suggest that this is one of and volcanic setting of the site suggests that the stress the most promising EGS sites in the United States, state and fracture patterns may be complex. Because with a large conductive thermal anomaly yielding the stress state is a primary control on the growth of high-temperature wells, but with permeability orders an EGS reservoir, the technical team has begun of magnitude less than conventional hydrothermal building a preliminary 3-D stress model for wells. Northwest Geothermal (NWG) 55-29, drilled Newberry by collecting new field and laboratory in 2008 to a total measured depth of 10,060, is very data, including borehole imaging using an ultrasonic hot but with very low permeability, making it an borehole televiewer, micro-seismic monitoring ideal EGS target. through a local network, mineralogical characterization and mechanical testing of existing The project has brought together a multi-disciplinary core, and regional fault and fracture mapping using team led by AltaRock Energy (ARE) with LiDAR. -
6 IA 6 – Volcano
6 IA 6 – Volcano THIS PAGE LEFT BLANK INTENTIONALLY Table of Contents 1 Purpose ..................................................................... IA 6-1 2 Policies ...................................................................... IA 6-1 3 Situation and Assumptions ..................................... IA 6-2 4 Concept of Operations ............................................. IA 6-9 5 Roles and Responsibilities ...................................... IA 6-9 5.1 Primary Agency: Oregon Emergency Management ................. IA 6-9 5.2 Supporting Agencies .............................................................. IA 6-10 5.3 Adjunct Agencies ................................................................... IA 6-10 6 Hazard Specific Information – Volcano ................. IA 6-10 6.1 Definition ................................................................................ IA 6-10 6.2 Frequency .............................................................................. IA 6-11 6.3 Territory at Risk ...................................................................... IA 6-12 6.4 Effects .................................................................................... IA 6-12 6.5 Predictability ........................................................................... IA 6-13 7 Supporting Documents .......................................... IA 6-13 8 Appendices ............................................................. IA 6-13 IA 6-iii State of Oregon EOP Incident Annexes IA 6. Volcano THIS PAGE LEFT BLANK INTENTIONALLY -
LA PINE the Newberry National Monument Is Located in the Town Of
LA PINE The Newberry National Monument is located in the town of La Pine. It is just 5 miles north of the Chamber office on Hwy 97. Turn Left (east) and travel up into the crater to enjoy the world’s largest obsidian flow, Paulina Lake and resort and the wonderful little East Lake resort. Both Lakes feature camping, a store, restaurant, boats, fishing, and camping or cab- ins to rent. Paulina is open for the winter, too and you can go into the resort to stay on a snowmobile! This is the one thing in La Pine you do not want to miss! For information about any of the Lava Lands destinations call the Newberry National Monument Hotline number at 541-383-5700. Inside the Caldera: Paulina Creek Water slides. Go on Paulina Lake road to McKay Campground (McKay Crossing Campground) then take the 1-1/2 mile trail to the waterslides. To get to the Hot Springs go to the far end of Little Crater Campground on Paulina Lake and hike on the lakeshore trail approximately 1 mile. You will see the little hot spring pools that people have made through the years. Rosland Campground is located ¼ mile past the Little Deschutes River on Burgess Road (Wickiup turn off from Hwy 97) The little park is a Park District owned park that features a day use area with access to the river, camping and they are remodeling the park to include a new pavilion that is a covered area for your picnics, gatherings and meetings. WEST Places to go within 45 minutes of the Chamber of Commerce in La Pine: 541-536-9771 South Twin Lake/North Twin Lake- Take Huntington Road through town, north to Burgess. -
Volcano Hazards in the Three Sisters Region, Oregon
Volcano Hazards in the Three Sisters Region, Oregon Open-File Report 99-437 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior U.S. Geological Survey Volcano Hazards in the Three Sisters Region, Oregon By W.E. Scott, R.M. Iverson, S.P. Schilling, and B.J. Fisher U.S. Geological Survey Cascades Volcano Observatory 5400 MacArthur Boulevard Vancouver, WA 98661 Open-File Report 99-437 U.S. Department of the Interior Bruce Babbitt, Secretary U.S. Geological Survey Charles G. Groat, Director This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. To purchase USGS publications contact: U.S. Geological Survey Information Services P.O. Box 25286 Denver, CO 80225 (303) 202-4210 This report is also available in digital form on the World Wide Web. URL: http://vulcan.wr.usgs.gov/Volcanoes/Sisters/Hazards Contents Summary .................................................................................................................................. 1 Introduction .............................................................................................................................. 1 Past hazardous events .............................................................................................................. 2 Two types of volcanoes ...................................................................................................... -
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.