2006 Oil and Gas Assessment of North Aleutian Basin Planning Area

Total Page:16

File Type:pdf, Size:1020Kb

2006 Oil and Gas Assessment of North Aleutian Basin Planning Area North Aleutian Basin OCS Planning Area Assessment of Undiscovered Technically-Recoverable Oil and Gas As of 2006 U.S. Department of the Interior Minerals Management Service Alaska OCS Region Anchorage, Alaska Kirk W. Sherwood John Larson C. Drew Comer James D. Craig Cameron Reitmeier February 2006 This report is available online at http://www.mms.gov/alaska/re/reports/rereport.htm. A Compact Disk version of the report (in PDF format) may be obtained by contacting Rance Wall, Regional Supervisor for Resource Evaluation, Minerals Management Service, Centerpoint Financial Center, 3801 Centerpoint Drive, Suite 500, MS 8100, Anchorage, AK 99503-5823, or at Ph. 907-334-5320, or at e-mail [email protected] Table of Contents List of Text Topics Summary, page 1 Source Potential of Coal-Bearing Rocks, page 23 Location and General Geology of North Source Potential of “Amorphous” Aleutian Basin OCS Planning Area, Interval, 15,620-17,155 ft bkb, page 5 page 24 Source Potential of Tertiary Basin Exploration History of North Aleutian Fill and Assessment Model, page Basin, page 6 26 Past Exploration Onshore, page 6 Oil and Gas Occurrences and Leasing Onshore, page 6 Biomarker Correlations, page 26 Offshore/OCS Exploration, page 7 Petroleum System—Critical Events, Past OCS Leasing, page 7 page 31 Productive Analog Basin—Cook Inlet Petroleum System Elements and Oil and Basin, page 8 Gas Plays in North Aleutian Basin OCS Planning Area, page 37 Petroleum Geology of the North Aleutian Key Elements of Petroleum System, Basin, page 9 page 37 Regional Geology, page 9 Play Definition, page 37 Alaska Peninsula, page 9 Play Descriptions, North Aleutian Basin, Formation of North Aleutian Basin, Alaska, page 38 page 10 Play 1: Bear Lake-Stepovak Structures of Amak Basin, Black Hills (Oligocene-Miocene), page 38 Uplift, and North Aleutian Basin, Play 2: Tolstoi (Eocene-Oligocene), page 11 page 39 Nature of Basement Beneath North Play 3: Black Hills Uplift-Amak Aleutian Basin, page 13 Basin (Eocene-Miocene), page 41 Mesozoic Stratigraphy and Reservoir Play 4: Milky River Biogenic Gas Formations, page 15 (Plio-Pleistocene), page 43 Cenozoic Stratigraphy, Reservoir Play 5: Mesozoic Deformed Formations, and Play Sequences, page Sedimentary Rocks (Triassic- 16 Cretaceous), page 45 Petroleum Systems in North Aleutian Play 6: Mesozoic Buried Granitic Basin Plays, page 19 Hills (Jurassic-Cretaceous Thermal Maturity of North Aleutian Magmatic Rocks), page 47 Basin Fill, page 19 Source Rock Potential, page 21 Geologic Assessment Model, page 50 Mesozoic Source Rocks, page 21 Prospect Areas and Volumes, page 50 Tertiary Source Rocks, page 22 Prospect Numbers, page 51 i Pay Thickness Model, page 52 Play 4: Milky River Biogenic Gas (Plio- Construction of Probability Distributions Pleistocene), page 59 with Limited Data, page 53 Play 5: Mesozoic Deformed Computation of Oil and Gas Recovery Sedimentary Rocks (Triassic- Factors, page 54 Cretaceous), page 59 Oil Recovery Factor, page 54 Play 6: Mesozoic Buried Granitic Hills Gas Recovery Factor, page 54 (Jurassic-Cretaceous Magmatic Risk Assessment, page 56 Rocks), page 60 Overall Results for Oil and Gas Assessment Results for North Aleutian Endowments of North Aleutian Basin, Basin, page 57 page 61 Play 1: Bear Lake-Stepovak (Oligocene- Large Individual Gas Fields Are Miocene), page 57 Possible, page 61 Play 2: Tolstoi (Eocene-Oligocene), Economic Potential of North Aleutian page 58 Basin, page 62 Play 3: Black Hills Uplift-Amak Basin (Eocene-Miocene), page 59 References Cited, page 64 List of Tables 1. North Aleutian Basin and Alaska 7. Input Data for Play 5, Mesozoic Peninsula Exploration Wells, 1903- Deformed Sedimentary Rocks (Triassic- 1985, page 71 Cretaceous), page 77 2. Selected Extract Data, Oil and Gas Show 8. Input Data for Play 6, Mesozoic Buried Interval, North Aleutian Shelf COST 1 Granitic Hills (Jurassic-Cretaceous well, page 72 Magmatic Rocks), page 78 3. Input Data for Play 1, Bear Lake- 9. Input Data for Oil and Gas Recovery Stepovak (Oligocene- Miocene), page Factor Calculation, Play 1, Bear Lake- 73 Stepovak (Oligocene- Miocene), page 79 4. Input Data for Play 2, Tolstoi (Eocene- Oligocene), page 74 10. Input Data for Oil and Gas Recovery Factor Calculation, Play 2, Tolstoi 5. Input Data for Play 3, Black Hills Uplift- (Eocene-Oligocene), page 80 Amak Basin (Eocene-Miocene), page 75 11. Input Data for Oil and Gas Recovery 6. Input Data for Play 4, Milky River Factor Calculation, Play 3, Black Hills Biogenic Gas (Plio-Pleistocene), page Uplift-Amak Basin (Eocene-Miocene), 76 page 81 ii 12. Input Data for Oil and Gas Recovery Pool Size Simulation Statistics for Play 3 Factor Calculation, Play 5, Mesozoic – Black Hills Uplift-Amak Basin Deformed Sedimentary Rocks (Triassic- (Eocene-Miocene), page 87 Cretaceous), page 82 20. Conditional (Un-risked) Recoverable 13. Input Data for Oil and Gas Recovery Sizes of Ranked Pools for Play 3 – Black Factor Calculation, Play 6, Mesozoic Hills Uplift-Amak Basin (Eocene- Buried Granitic Hills (Jurassic- Miocene), page 87 Cretaceous Magmatic Rocks), page 83 21. Conditional (Un-risked) Recoverable 14. 2006 Assessment Results for North Pool Size Simulation Statistics for Play 5 Aleutian Basin OCS Planning Area, page 84 – Mesozoic Deformed Sedimentary Rocks (Triassic-Cretaceous), page 88 15. Conditional (Un-risked) Recoverable Pool Size Simulation Statistics for Play 1 22. Conditional (Un-risked) Recoverable – Bear Lake-Stepovak (Oligocene- Sizes of Ranked Pools for Play 5 – Miocene), page 85 Mesozoic Deformed Sedimentary Rocks (Triassic-Cretaceous), page 88 16. Conditional (Un-risked) Recoverable Sizes of Ranked Pools for Play 1 – Bear 23. Conditional (Un-risked) Recoverable Lake-Stepovak (Oligocene-Miocene), Pool Size Simulation Statistics for Play 6 page 85 – Mesozoic Granitic Buried Hills (Jurassic-Cretaceous), page 89 17. Conditional (Un-risked) Recoverable Pool Size Simulation Statistics for Play 2 24. Conditional (Un-risked) Recoverable – Tolstoi (Eocene-Oligocene), page 86 Sizes of Ranked Pools for Play 6 – Mesozoic Granitic Buried Hills 18. Conditional (Un-risked) Recoverable (Jurassic-Cretaceous), page 89 Sizes of Ranked Pools for Play 2 - Tolstoi (Eocene-Oligocene), page 86 25. 2006 Economic Assessment Results for North Aleutian Basin OCS Planning 19. Conditional (Un-risked) Recoverable Area, page 90 List of Figures 1. Location map for North Aleutian basin with well control, Sale 92 (1988) leases, and other Tertiary-age basins of the and regional distribution of Tertiary-age Bering shelf, Pacific margin, and sedimentary rocks, page 92 southern Chukchi Sea, page 91 3. Seismic data coverage (CDP, Two- 2. Regional map for North Aleutian basin, Dimensional) for North Aleutian Basin iii OCS Planning Area, page 93 available as plate 3 4. Regional distribution of Mesozoic 11. Statistical summaries for sandstone bed sedimentary basin containing strata thicknesses for North Aleutian basin correlative to Middle Jurassic oil source play sequences, page 101 rocks that generated 1.4 billion barrels of oil reserves in the oil fields of northern 12. Core porosity versus depth in the North Cook Inlet basin, page 94 Aleutian Shelf COST 1 well, with linear regression function for porosity decline 5. Principal geologic structures of the with depth, page 102 North Aleutian basin and contiguous areas, including: 1) transtensional faults 13. Core porosity versus permeability for and basement uplifts in western parts of sandstones, North Aleutian Shelf COST the basin; 2) wrench-fault structures 1 well, with correlation, page 103 along the Black Hills uplift; and 3) fold/thrust belts along the southeast 14. Core permeability versus depth for margin of the basin, page 95 sandstones, North Aleutian Shelf COST 1 well, with function for permeability 6. Seismic profile through basement uplifts decline with depth, page 104 in western North Aleutian basin, showing Tertiary sedimentary sequences 15. Porosity histograms for Bear Lake- and basin structures, page 96. An Stepovak, Upper Tolstoi, and Lower undistorted Adobe Acrobat version of Tolstoi play sequences, page 105 figure 6 is available as plate 1 16. Permeability histograms for Bear Lake- 7. Magnetic intensity map with offshore Stepovak, Upper Tolstoi, and Lower speculative extrapolation of the Bruin Tolstoi play sequences, page 106 Bay fault, page 97 17. Vitrinite reflectance data for 94 samples 8. Mesozoic stratigraphy, Alaska Peninsula of cuttings, conventional cores, and and substrate beneath southwest part of percussion sidewall cores in the North North Aleutian basin, page 98 Aleutian Shelf COST 1 well, with statistical fits and forecasts for depths of 9. Wellbore stratigraphy, North Aleutian important isograds, page 107 Shelf COST 1 stratigraphic test well, page 99. An undistorted Adobe Acrobat 18. Depth to top of oil generation zone version of figure 9 is available as plate (0.6% vitrinite reflectance) with 2. probable areas of thermal maturity of Tertiary rocks sufficient for oil 10. Regional stratigraphic correlation, generation in and beneath the North Tertiary sequence in North Aleutian Aleutian basin, page 108 Shelf COST 1, Sandy River 1, Port Heiden 1, Ugashik 1, and Becharof Lake 19. Isopach map for thickness of Tertiary- 1 wells, North Aleutian basin and Alaska age rocks within oil generation zone Peninsula, page 100. An undistorted (0.6% to 1.35% vitrinite reflectance) Adobe Acrobat version of figure 10 is with probable areas of thermal maturity iv sufficient for oil generation within and 26. Histograms for Pristane/Phytane
Recommended publications
  • Geologic Maps of the Eastern Alaska Range, Alaska, (44 Quadrangles, 1:63360 Scale)
    Report of Investigations 2015-6 GEOLOGIC MAPS OF THE EASTERN ALASKA RANGE, ALASKA, (44 quadrangles, 1:63,360 scale) descriptions and interpretations of map units by Warren J. Nokleberg, John N. Aleinikoff, Gerard C. Bond, Oscar J. Ferrians, Jr., Paige L. Herzon, Ian M. Lange, Ronny T. Miyaoka, Donald H. Richter, Carl E. Schwab, Steven R. Silva, Thomas E. Smith, and Richard E. Zehner Southeastern Tanana Basin Southern Yukon–Tanana Upland and Terrane Delta River Granite Jarvis Mountain Aurora Peak Creek Terrane Hines Creek Fault Black Rapids Glacier Jarvis Creek Glacier Subterrane - Southern Yukon–Tanana Terrane Windy Terrane Denali Denali Fault Fault East Susitna Canwell Batholith Glacier Maclaren Glacier McCallum Creek- Metamorhic Belt Meteor Peak Slate Creek Thrust Broxson Gulch Fault Thrust Rainbow Mountain Slana River Subterrane, Wrangellia Terrane Phelan Delta Creek River Highway Slana River Subterrane, Wrangellia Terrane Published by STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS 2015 GEOLOGIC MAPS OF THE EASTERN ALASKA RANGE, ALASKA, (44 quadrangles, 1:63,360 scale) descriptions and interpretations of map units Warren J. Nokleberg, John N. Aleinikoff, Gerard C. Bond, Oscar J. Ferrians, Jr., Paige L. Herzon, Ian M. Lange, Ronny T. Miyaoka, Donald H. Richter, Carl E. Schwab, Steven R. Silva, Thomas E. Smith, and Richard E. Zehner COVER: View toward the north across the eastern Alaska Range and into the southern Yukon–Tanana Upland highlighting geologic, structural, and geomorphic features. View is across the central Mount Hayes Quadrangle and is centered on the Delta River, Richardson Highway, and Trans-Alaska Pipeline System (TAPS). Major geologic features, from south to north, are: (1) the Slana River Subterrane, Wrangellia Terrane; (2) the Maclaren Terrane containing the Maclaren Glacier Metamorphic Belt to the south and the East Susitna Batholith to the north; (3) the Windy Terrane; (4) the Aurora Peak Terrane; and (5) the Jarvis Creek Glacier Subterrane of the Yukon–Tanana Terrane.
    [Show full text]
  • NSF 03-021, Arctic Research in the United States
    This document has been archived. Home is Where the Habitat is An Ecosystem Foundation for Wildlife Distribution and Behavior This article was prepared The lands and near-shore waters of Alaska remaining from recent geomorphic activities such by Page Spencer, stretch from 48° to 68° north latitude and from 130° as glaciers, floods, and volcanic eruptions.* National Park Service, west to 175° east longitude. The immense size of Ecosystems in Alaska are spread out along Anchorage, Alaska; Alaska is frequently portrayed through its super- three major bioclimatic gradients, represented by Gregory Nowacki, USDA Forest Service; Michael imposition on the continental U.S., stretching from the factors of climate (temperature and precipita- Fleming, U.S. Geological Georgia to California and from Minnesota to tion), vegetation (forested to non-forested), and Survey; Terry Brock, Texas. Within Alaska’s broad geographic extent disturbance regime. When the 32 ecoregions are USDA Forest Service there are widely diverse ecosystems, including arrayed along these gradients, eight large group- (retired); and Torre Arctic deserts, rainforests, boreal forests, alpine ings, or ecological divisions, emerge. In this paper Jorgenson, ABR, Inc. tundra, and impenetrable shrub thickets. This land we describe the eight ecological divisions, with is shaped by storms and waves driven across 8000 details from their component ecoregions and rep- miles of the Pacific Ocean, by huge river systems, resentative photos. by wildfire and permafrost, by volcanoes in the Ecosystem structures and environmental Ring of Fire where the Pacific plate dives beneath processes largely dictate the distribution and the North American plate, by frequent earth- behavior of wildlife species.
    [Show full text]
  • Alaska Range
    Alaska Range Introduction The heavily glacierized Alaska Range consists of a number of adjacent and discrete mountain ranges that extend in an arc more than 750 km long (figs. 1, 381). From east to west, named ranges include the Nutzotin, Mentas- ta, Amphitheater, Clearwater, Tokosha, Kichatna, Teocalli, Tordrillo, Terra Cotta, and Revelation Mountains. This arcuate mountain massif spans the area from the White River, just east of the Canadian Border, to Merrill Pass on the western side of Cook Inlet southwest of Anchorage. Many of the indi- Figure 381.—Index map of vidual ranges support glaciers. The total glacier area of the Alaska Range is the Alaska Range showing 2 approximately 13,900 km (Post and Meier, 1980, p. 45). Its several thousand the glacierized areas. Index glaciers range in size from tiny unnamed cirque glaciers with areas of less map modified from Field than 1 km2 to very large valley glaciers with lengths up to 76 km (Denton (1975a). Figure 382.—Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the Alaska Range in summer 1995. National Oceanic and Atmospheric Administration image mosaic from Mike Fleming, Alaska Science Center, U.S. Geological Survey, Anchorage, Alaska. The numbers 1–5 indicate the seg- ments of the Alaska Range discussed in the text. K406 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD and Field, 1975a, p. 575) and areas of greater than 500 km2. Alaska Range glaciers extend in elevation from above 6,000 m, near the summit of Mount McKinley, to slightly more than 100 m above sea level at Capps and Triumvi- rate Glaciers in the southwestern part of the range.
    [Show full text]
  • USGS Professional Paper 1739-A
    Studies by the U.S. Geological Survey in Alaska, 2006 U.S. Geological Survey Professional Paper 1739–A Blue Mountain and The Gas Rocks: Rear-Arc Dome Clusters on the Alaska Peninsula By Wes Hildreth, Judy Fierstein, and Andrew T. Calvert Abstract pal nearby town) and 15 to 20 km behind (northwest of) the volcanic-front chain, which is locally defined by Kejulik and Behind the single-file chain of stratovolcanoes on the Peulik stratovolcanoes (fig. 1). The Gas Rocks form a knobby Alaska Peninsula, independent rear-arc vents for mafic mag- peninsula at the south shore of Becharof Lake, and Blue mas are uncommon, and for silicic magmas rarer still. We Mountain is a group of rounded hills a few kilometers west of report here the characteristics, compositions, and ages of two Upper Ugashik Lake (fig. 2). Both dome clusters rise abruptly andesite-dacite dome clusters and of several nearby basaltic above a nearly flat (virtually treeless and roadless) plain of units, all near Becharof Lake and 15 to 20 km behind the late Pleistocene glacial deposits (Detterman and others, 1987a, volcanic front. Blue Mountain consists of 13 domes (58–68 b), consisting largely of till and outwash, supplemented by the bog and lacustrine deposits of hundreds of ponds and by weight percent SiO2) and The Gas Rocks of three domes (62–64.5 weight percent SiO ) and a mafic cone (52 weight beach and terrace deposits along the lakeshores. The enor- 2 mous moraine-dammed lakes (fig. 2) are generally shallower percent SiO2). All 16 domes are amphibole-biotite-plagio- clase felsite, and nearly all are phenocryst rich and quartz than 5 m, and their surfaces are barely 10 m above sea level.
    [Show full text]
  • Terrestrial Mollusks of Attu, Aleutian Islands, Alaska BARRY ROTH’ and DAVID R
    ARCTK: VOL. 34, NO. 1 (MARCH 1981), P. 43-47 Terrestrial Mollusks of Attu, Aleutian Islands, Alaska BARRY ROTH’ and DAVID R. LINDBERG’ ABSTRACT. Seven species of land mollusk (2 slugs, 5 snails) were collected on Attu in July 1979. Three are circumboreal species, two are amphi-arctic (Palearctic and Nearctic but not circumboreal), and two are Nearctic. Barring chance survival of mollusks in local refugia, the fauna was assembled overwater since deglaciation, perhaps within the last 10 OOO years. Mollusk faunas from Kamchatka to southeastern Alaska all have a Holarctic component. A Palearctic component present on Kamchatka and the Commander Islands is absent from the Aleutians, which have a Nearctic component that diminishes westward. This pattern is similar to that of other soil-dwelling invertebrate groups. RESUM& Sept espbces de mollusques terrestres (2 limaces et 5 escargots) furent prklevkes sur I’ile d’Attu en juillet 1979. Trois sont des espbces circomborkales, deux amphi-arctiques (Palkarctiques et Nkarctiques mais non circomborkales), et deux Nkarctiques. Si I’on excepte la survivance de mollusques due auhasard dans des refuges locaux, cette faune s’est retrouvke de part et d’autre des eauxdepuis la dkglaciation, peut-&re depuis les derniers 10 OOO ans. Les faunes de mollusques de la pkninsule de Kamchatkajusqu’au sud-est de 1’Alaska on toutes une composante Holarctique. Une composante Palkarctique prksente sur leKamchatka et les iles Commandeur ne se retrouve pas aux Alkoutiennes, oil la composante Nkarctique diminue vers I’ouest. Ce patron est similaire il celui de d’autres groupes d’invertkbrks terrestres . Traduit par Jean-Guy Brossard, Laboratoire d’ArchCologie de I’Universitk du Qukbec il Montrkal.
    [Show full text]
  • United States Department of the Interior Geological
    UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY AGE AND TECTONIC SIGNIFICANCE OF VOLCANIC ROCKS ON ST. MATTHEW ISLAND, BERING SEA, ALASKA BY William W. Patton, Jr., Marvin A. Lanphere, Thomas P. Miller, and Richard A. Scott Menlo Park, Calif., Anchorage, Alaska, Denver, Colo. Open-file report 75-150 1975 This report is preliminary and has not been edited or reviewed for conformity with Geological Survey standards AGE AND TECTONIC SIGNIFICANCE OF VOLCANIC ROCKS ON ST. MATTHEW ISLAND, BERING SEA, ALASKA By WILLIAM W. PATTON, JR., MARVIN A. LANPHERE, THOMAS P. MILLER, and RICHARD A. SCOTT Menlo Park, Calif., Anchorage, Alaska, Denver, Colo. Abstract.-- 'Reconnaissance investigations of the heretofore little known volcanic assemblage on St. Matthew Island provide significant information on the tectonic history of the Bering Sea shelf. St. Matfhew Island is made up of approximately 500 m of subaerial calc-alkaline volcanic rocks ranging in composition from high-alumina basalt to rhyolite. Four K-Ar analyses of samples from this volcanic sequence give Late Cretaceous ages of 65-77 m.y., and intercalated carbonaceous tuff layers yield Cretaceous pollen assemblages. Along the northeast coast of St. Matthew Island the volcanic rocks are intruded by granodiorite that gives an early Tertiary K-Ar age of 61 m.y. Correlations with on-land geology in northeast Siberia and marine geophysical data from the western Bering Sea strongly suggest that St. Matthew Island represents a southeastward extension of the Okhotsk- Chukotsk belt, a Late Cretaceous and early Tertiary volcanic arc that borders the Pacific margin of Siberia for 3,000 km.
    [Show full text]
  • Alaska Peninsula Becharof National Wildlife Refuges
    Fishery Management Plan ALASKA PENINSULA BECHAROF NATIONAL WILDLIFE REFUGES July 1994 Region 7 U.S. Fish and Wildlife Service • Department of the Interior FISHERY MANAGEMENT PLAN ALASKA PENINSULA AND BECHAROF NATIONAL WILDLIFE REFUGES Fiscal Years 1994 - 1998 Prepared By: King Salmon Fishery Resource Office U.S. Fish and Wildlife Service P.O. Box 277 King Salmon, Alaska 99613 May 1994 SUMMARY STATEMENT The Alaska Peninsula and Becharof National Wildlife Refuges Fishery Management Plan (Plan) provides the management direction necessary to ensure conservation of fishery resources and habitat. In addition, the Plan provides for continued use of fishery resources by subsistence, commercial, and recreational users consistent with the purposes for which the Alaska Peninsula and Becharof refuges (Complex) were established and are managed. The Complex's biological and physical environment is described and fishery resources, human use, management history, and major issues and concerns are discussed. This information was obtained from the Refuge Comprehensive Conservation Plans, a literature search, and discussions with Alaska Department of Fish and Game personnel. Objectives and tasks are developed to address the issues and concerns. Federal tasks are assigned priorities and costs for each year of continuation. The Plan encompasses a five year period, at which time it will be revised. Major issues and concerns identified include the following: competition between user groups; incomplete salmon escapement data bases to refine management of the Complex fish populations; and inadequate fishery law enforcement. In some cases, concerns were identified because of the perception that they would develop into serious problems if current levels of use or consumption were allowed to continue or expand.
    [Show full text]
  • U.S. Geological Survey Circular 1249
    ��� � Geothermal Energy—Clean Power From the Earth’s Heat Circular 1249 U.S. Department of the Interior U.S. Geological Survey Geothermal Energy—Clean Power From the Earth’s Heat By Wendell A. Duffield and John H. Sass C1249 U.S. Department of the Interior U.S. Geological Survey ii iii U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director U.S. Geological Survey, Reston, Virginia: 2003 Available from U.S. Geological Survey Information Services� Box 25286, Denver Federal Center� Denver, CO 80225� This report and any updates to it are available at� http://geopubs.wr.usgs.gov/circular/c1249/� Additional USGS publications can be found at� http://geology.usgs.gov/products.html� For more information about the USGS and its products;� Telephone: 1-888-ASK-USGS� World Wide Web: http://www.usgs.gov/� Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply� endorsement of the U.S. Government.� Although this report is in the public domain, it contains copyrighted materials that are noted in the text. Permission� to reproduce those items must be secured from the individual copyright owners.� Published in the Western Region, Menlo Park, California� Manuscript approved for publication March 20, 2003� Text and illustrations edited by James W. Hendley II and Carolyn Donlin� Cataloging-in-publication data are on file with the Library of Congress (http://www.loc.gov/). Cover—Coso geothermal plant, Navy One, at Naval Air Weapons Station China Lake in southern California (U.S.
    [Show full text]
  • Geology of Pavlof Volcano and Vicinity Alaska
    Geology of Pavlof Volcano and Vicinity Alaska By GEORGE C. KENNEDY and HOWARD H. R7ALDRON INVESTIGATIONS OF ALASKAN VOLCANOES GEOLOGICAL SURVEY BULLETIN 1028-A Prepared in cooperation with the Ofice, Chief of Enpiseers, U,S. Army - UNITED STATES GOVERNMENT PRLNTING OFFICE, WASHINGTON : 1955 UNITED STATE$ DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY W. E. Wmther, -for PREFACE fn October 1345 the War Department (now Department of the Army) requested the Geological Survey to undertake a program of volcano investigations in the Aleutian I~lan&Alaska Peninaula araa, The fist field studies, under general direction of Q. D. Robbn, were begun as soon as weather permitted in the spring of 1948. The results of the first year's field, laboratory, and library work were ambled hastily as two administrative reporta Part of the data was published in 1950 in Gmlogid Survey BulIetin 97443, Volcanic activity in the Aleutian arc, by Rabert B. Coats. The remainder of Badata have been revised for publication in Bulletin 10B. The geologic and geophysical investigations covered ky this mprt were reconnaissance, The factual information presented is believed to be accurate, but many of the tentative interpretations afld conclu- &ion8will bB modified as the investigations continue and knowledge growa. The investigations of 1946 were support~dalmost entirely by the Military Intelligence Division of the Office, Chief of Engineers, U. S. &my. The Geological Survey is indebtad to the Office, Chief of Engin- for its early recognition of tho value of geologic studies
    [Show full text]
  • 2019 Complete Southwest Sport Fish Regulation Booklet
    BRISTOL BAY SALT AND FRESH WATER 12 Major Drainages of Bristol Bay k See the Northern ar Cl Alaska Sport Fish e Regulation Summary Lak Port Alsworth es ag in ra Iliamna D Wood River er age Togiak River iv rain Ungalikthluk Drainage R r D Drainage a ive River Drainage tn R Lake Iliamna a k h a lc h u ic M v / K k a g a Riv Dillingham gnak er Drain h Ala ag s e See the Southcentral u Alaska Sport Fish N Regulation Summary Cape Newenham King Salmon Naknek Rive r Dra B inag ris e to l Ege Ba gik y Ri S ver alt D wa ra te in rs a ge Cape Menshikof U ga sh ik R i Dr ve ain r ag Alaska Peninsula & e Kodiak Island Aleutian Islands See pages 24 - 28 Miles See pages 22 - 23 0 25 50 ARCTIC CHAR AND DOLLY VARDEN LINGCOD General Regulations - Bristol Bay • Season: June 8–October 31 . • No limit . • 3 per day, 3 in possession . Inclusive waters: All fresh waters draining into Bristol ROCKFISH Bay between Cape Menshikof and Cape Newenham, and • Season: November 1–June 7 . • No limit . all salt waters east of a line from Cape Newenham to • 10 per day, 10 in possession. KING CRAB Cape Menshikof . RAINBOW TROUT • Season: June 1–January 31 . The fishing season for all species is open year-round • Season: June 8–October 31 . • Males only: unless otherwise noted below. • 2 per day, 2 in possession, only 1 of which may • 6½ inches or more: 6 per day, 6 in possession.
    [Show full text]
  • Egegik, Becharof
    Chapter 3 - Region 12: Egegik, Becharof Region 12: Egegik, Becharof Summary of Resources and Uses in the Region Region Boundary Region 12 includes the uplands and tidelands on a portion of the Alaska Peninsula, generally south of the Bristol Bay Borough, which contains most of the Egegik-Becharof Lake drainage and borders on the western shore of the Ugashik Lake system (Map 3-11). The Region is bounded on the northeast by the Katmai National Park and Preserve, the Lake and Peninsula Borough boundary, and the western shore of Ugashik Lake. The southern boundary is generally north of Pilot Point. The principal community is Egegik (pop. 127). State Lands: Ownership and Acreage State-owned land dominates the western one third of the Region while much of the eastern two- thirds is Federally-owned. Native ownership of land is concentrated around the community of Egegik and west of Becharof Lake. The eastern portion of the Region is within the Becharof and Alaska Peninsula National Wildlife Refuges. The Egegik Critical Habitat Area is contained within Region 12. The plan applies to 884,300 acres of state-owned and state-selected uplands and 127,229 acres of state-owned tidelands in this region. The plan also applies to state-owned shorelands (acreages of shorelands have not been calculated). Physical Geography The western portion of Region 12 is within the Bristol Bay Lowlands ecological province; the eastern portion of the Region is in the Alaska Peninsula ecological province. Drainage is predominantly westward towards Bristol Bay. The principal drainages are the King Salmon River, which flows westward from Katmai National Park and Preserve, and the Egegik River, which flows from Becharof Lake; also included is the upper section of the Ugashik River and the Kejulik River.
    [Show full text]
  • Cook Inlet Areawide Oil and Gas Lease Sale
    November 2, 2018 COOK INLET AREAWIDE OIL AND GAS LEASE SALE Final Finding of the Director Recommended citation: DNR (Alaska Department of Natural Resources). 2018. Cook Inlet areawide oil and gas lease sale: Written Finding of the Director. November 2, 2018. Questions or comments about this final finding should be directed to: Alaska Department of Natural Resources Division of Oil and Gas 550 W. 7th Ave., Suite 1100 Anchorage, AK 99501-3560 907-269-8800 The Alaska Department of Natural Resources (DNR) administers all programs and activities free from discrimination based on race, color, national origin, age, sex, religion, marital status, pregnancy, parenthood, or disability. The department administers all programs and activities in compliance with Title VI of the Civil Rights Act of 1964, Section 504 of the Rehabilitation Act of 1973, Title II of the Americans with Disabilities Act (ADA) of 1990, the Age Discrimination Act of 1975, and Title IX of the Education Amendments of 1972. If you believe you have been discriminated against in any program, activity, or facility, please write to: Alaska Department of Natural Resources ADA Coordinator P.O. Box 111000 Juneau, AK 99811-1000 The department’s ADA Coordinator can be reached via phone at the following numbers: (VOICE) 907-465-2400 (Statewide Telecommunication Device for the Deaf) 1-800-770-8973, or (FAX) 907-465-3886 For information on alternative formats and questions on this publication, please contact: Alaska Department of Natural Resources, Division of Oil and Gas 550 W. 7th Ave., Suite 1100 Anchorage, AK 99501-3560 Phone 907-269-8800 Division of Oil and Gas Contributors: Kirk Morgan Lynn Noel Bryan Taylor Michael Redlinger Jonathan Schick Kyle Smith COOK INLET AREAWIDE OIL AND GAS LEASE SALE FINAL FINDING OF THE DIRECTOR Prepared by: Alaska Department of Natural Resources Division of Oil and Gas November 2, 2018 Executive Summary Contents Page A.
    [Show full text]