WP18–19 Executive Summary Unit 13, Remainder
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Crary-Henderson Collection, B1962.001
REFERENCE CODE: AkAMH REPOSITORY NAME: Anchorage Museum at Rasmuson Center Bob and Evangeline Atwood Alaska Resource Center 625 C Street Anchorage, AK99501 Phone: 907-929-9235 Fax: 907-929-9233 Email: [email protected] Guide prepared by: Mary Langdon, Volunteer, and Sara Piasecki, Archivist TITLE: Crary-Henderson Collection COLLECTION NUMBER: B1962.001, B1962.001A OVERVIEW OF THE COLLECTION Dates: circa 1885-1930 Extent: 19.25 linear feet Language and Scripts: The collection is in English. Name of creator(s): Will Crary; Nan Henderson; Phinney S. Hunt; Miles Bros.; Lyman; George C. Cantwell; Johnson; L. G. Robertson; Lillie N. Gordon; John E. Worden; W. A. Henderson; H. Schultz; Merl LaVoy; Guy F. Cameron; Eric A. Hegg Administrative/Biographical History: The Crary and Henderson Families lived and worked in the Valdez area during the boom times of the early 1900s. William Halbrook Crary was a prospector and newspaper man born in the 1870s (may be 1873 or 1876). William and his brother Carl N. Crary came to Valdez in 1898. Will was a member of the prospecting party of the Arctic Mining Company; Carl was the captain of the association. The Company staked the “California Placer Claim” on Slate Creek and worked outside of Valdez on the claim. Slate Creek is a tributary of the Chitina River, in the Chistochina District of the Copper River Basin. Will Crary was the first townsite trustee for Valdez. Carl later worked in the pharmaceutical field in Valdez and was also the postmaster. Will married schoolteacher Nan Fitch in Valdez in 1906. Carl died of cancer in 1927 in Portland, Oregon. -
Glenn Highway Tok Cutoff (GJ-125 to GJ-0) to Milepost a 160
Map GLENN HIGHWAY • TOK CUTOFF Glenn Highway To Chicken and Eagle © The MILEPOST To Delta Junction (see TAYLOR HIGHWAY section) Key to mileage boxes ver (see ALASKA HIGHWAY section) Tanana Ri miles/kilometres G miles/kilometres Tanacross 5 from: la A L c A Swb T-Tok V-Valdez ia S K 2 Tok Map Location G-Glennallen ted A ® GJ-Gakona Junction A re A-Anchorage a R 2 A 1 Tetlin Junction J-Junction N HJ-Haines Junction Mount Kimball G T-0 a To Haines DJ-Delta Junction in 10,300 ft./3,139m E ch r w GJ-125/201km Junction Chisto cie G la A-328/528km (see ALASKA Principal Route Logged Key to Advertiser er HIGHWAY Services T iv DJ-108/174km C -Camping ok R section) Paved Unpaved R HJ-296/476km D -Dump Station iv ok Other Roads Logged d -Diesel er T G -Gas (reg., unld.) Tetlin I -Ice Lake Other Roads Scenic Byway L -Lodging M -Meals T Refer to Log for Visitor Facilities P -Propane Tok Cutoff ok Cu L R -Car Repair (major) na i Scale Sla R Mineral Lakes t iv t r -Car Repair (minor) e l 0 10 Miles r e S -Store (grocery) 0 10 Kilometres T -Telephone (pay) . t Cr t Bartell off (GJ-125 r Mentasta Lake e r e t T r. o v iv C i R Mentasta Lake S t ation k R Mentasta Summit n T-65/105km 2,434 ft./742m M a . i r E N d J-0 t C T A n e S I . -
R. L. Smith, H. R. Shaw, R. G. Luedke, and S. L. Russell U. S. Geological
COMPREHENSIVE TABLES GIVING PHYSICAL DATA AND THERMAL ENERGY ESTIMATES FOR YOUNG IGNEOUS SYSTEMS OF THE UNITED STATES by R. L. Smith, H. R. Shaw, R. G. Luedke, and S. L. Russell U. S. Geological Survey OPEN-FILE REPORT 78-925 This report is preliminary and has not been edited or reviewed for conformity with Geological Survey Standards and nomenclature INTRODUCTION This report presents two tables. The first is a compre hensive table of 157 young igneous systems in the western United States, giving locations, physical data, and thermal en ergy estimates, where apropriate, for each system. The second table is a list of basaltic fields probably less than 10,000 years old in the western United States. These tables are up dated and reformatted from Smith and Shaw's article "Igneous- related geothermal systems" in Assessment of geothermal re sources of the United States 1975 (USGS Circular 726, White and Williams, eds., 1975). This Open-File Report is a compan ion to Smith and Shaw's article "Igneous-related geothermal systems" in Assessment of geothermal resources in the United States 1978 (USGS Circular 790, Muffler, ed., 1979). The ar ticle in Circular 790 contains an abridged table showing only those igneous systems for which thermal estimates were made. The article also gives an extensive discussion of hydrothermal cooling effects and an explanation of the model upon which the thermal energy estimates are based. Thermal energy is calculated for those systems listed in table 1 that are thought to contribute significant thermal en ergy to the upper crust. As discussed by Smith and Shaw (1975), silicic volcanic systems are believed to be associated nearly always with high-level (<10 km) magma chambers. -
Table 4. Hawaiian Newspaper Sources
OCS Study BOEM 2017-022 A ‘Ikena I Kai (Seaward Viewsheds): Inventory of Terrestrial Properties for Assessment of Marine Viewsheds on the Main Eight Hawaiian Islands U.S. Department of the Interior Bureau of Ocean Energy Management Pacific OCS Region August 18, 2017 Cover image: Viewshed among the Hawaiian Islands. (Trisha Kehaulani Watson © 2014 All rights reserved) OCS Study BOEM 2017-022 Nā ‘Ikena I Kai (Seaward Viewsheds): Inventory of Terrestrial Properties for Assessment of Marine Viewsheds on the Eight Main Hawaiian Islands Authors T. Watson K. Ho‘omanawanui R. Thurman B. Thao K. Boyne Prepared under BOEM Interagency Agreement M13PG00018 By Honua Consulting 4348 Wai‘alae Avenue #254 Honolulu, Hawai‘i 96816 U.S. Department of the Interior Bureau of Ocean Energy Management Pacific OCS Region August 18, 2016 DISCLAIMER This study was funded, in part, by the US Department of the Interior, Bureau of Ocean Energy Management, Environmental Studies Program, Washington, DC, through Interagency Agreement Number M13PG00018 with the US Department of Commerce, National Oceanic and Atmospheric Administration, Office of National Marine Sanctuaries. This report has been technically reviewed by the ONMS and the Bureau of Ocean Energy Management (BOEM) and has been approved for publication. The views and conclusions contained in this document are those of the authors and should not be interpreted as representing the opinions or policies of the US Government, nor does mention of trade names or commercial products constitute endorsement or recommendation for use. REPORT AVAILABILITY To download a PDF file of this report, go to the US Department of the Interior, Bureau of Ocean Energy Management, Environmental Studies Program Information System website and search on OCS Study BOEM 2017-022. -
The Keltaeni
National Park Service U.S. Department of the Interior Park News + The Offcial Guide of Wrangell-St. Elias National Park and Preserve The K’ełt’aeni Volume 2019 OTHER PAGES YOU MIGHT LIKE: 3 Park Visitor 5 North District/ 8 South District/ Centers Nabesna Area Kennecott Area Activities & Itineraries 2 Bear Safety 4 The park has several visitor contact stations Picturesque scenery and mountain An adventure awaits the traveler who where you can get park information and viewing awaits the traveler who ventures ventures down the McCarthy Road to Nabesna Road Guide 6-7 down the Nabesna Road. Information historic McCarthy and the Kennecott Mill orientation from park rangers, as well as about the area and a road guide helps Town. Information about the area and a McCarthy Road Guide 10-11 view exhibits and the park flm. a traveler discover the mysteries of road guide helps a traveler discover the Nabesna. secrets of McCarthy-Kennecott. Information and Services 12 New Interpretive Exhibits at the Kennecott New Waysides at the Wrangell-St. Elias Mines National Historic Landmark Visitor Center in Copper Center The immersive exhibits include The interpretive waysides are personal stories of the workers located at the park entrance, and the families that lived in along the bluff trail and on Kennecott during the mining the Boreal Forest trail. The operation years from 1911 to outside panels describe the 1938. The displays include many scenic views of the Wrangell artifacts from the site that are on Mountains, the historic Valdez loan from local people or from Trail, an archeological site, the the park’s collection. -
Wrangell-St. Elias Alaska
Wrangell - St. Elias National Park Service National Park and National Preserve U.S. Department of the Interior Wrangell-St. Elias Alaska The wildness of Wrangell-St. Elias National Park The Alaska National Interest Lands Conservation vest harbor seals, which feed on fish and In late summer, black and brown bears, drawn and Preserve is uncompromising, its geography Act (ANILCA) of 1980 allows the subsistence marine invertebrates. These species and many by ripening soapberries, frequent the forests awe-inspiring. Mount Wrangell, namesake of harvest of wildlife within the park, and preserve more are key foods in the subsistence diet of and gravel bars. Human history here is ancient one of the park's four mountain ranges, is an and sport hunting only in the preserve. Hunters the Ahtna and Upper Tanana Athabaskans, and relatively sparse, and has left a light imprint active volcano. Hundreds of glaciers and ice find Dall's sheep, the park's most numerous Eyak, and Tlingit peoples. Local, non-Native on the immense landscape. Even where people fields form in the high peaks, then melt into riv large mammal, on mountain slopes where they people also share in the bounty. continue to hunt, fish, and trap, most animal, ers and streams that drain to the Gulf of Alaska browse sedges, grasses, and forbs. Sockeye, Chi fish, and plant populations are healthy and self and the Bering Sea. Ice is a bridge that connects nook, and Coho salmon spawn in area lakes and Long, dark winters and brief, lush summers lend regulati ng. For the species who call Wrangell the park's geographically isolated areas. -
GULF of ALASKA N NUN K JO a Permission Before Entering Roads And/Or Trails So You H a a NUNATAKR GLACIER K Malaspina H D the One Million Acres of Do Not Trespass
N District Ranger Station ab Slana 4 iver es Noyes Mtn M T E T L I N L O W L A N D S Fish Lake To Delta Junction R na E jek 8147 ft N 2 on and Fairbanks y Roa TA D a Chistochina d S TETLIN NATIONAL hw er NATIONAL TA ig pp G H Co u r PRESERVE lk e n M WILDLIFE REFUGE 1 n a v Jack i e 1 r O n l r U a R G e DAWSON e Lake N Ewan ff v i v a i T R to A R n R Lake i u I v N o C a Tanada R e sn S k k e i Crosswind r b Wellesley v a o Lake Copper a T Capital Mountain e N r Lake G r Mountain r 7731 ft e Lake e Beaver Creek N v p 4960 ft Wellesley Nabesna U i p R Lake o Caution. Private T R k iv C Z RANGE Gulkana Gakona rd er e property interspersed O a fo re n San Tanada Peak C with public lands. T a I is 9358 ft a N h Drive Mt Sanford sin C k Y 16237 ft Jac Cooper Pass Mt Allen 9480 ft U R K E M I B O O Nabesna Rd C U au r N l A e Tolsona Lake Glennallen A N to N v I i L f i S 1 T L s R Mt Drum f R i G a a v A T L A C lin r e NATIONAL PRESERVE I I z ve w r r To a Ri 12010 ft N E N T a e l Mt Gordon S R S G K R t Anchorage E K 9040 ft i R E Mt Zanetti P G A h R A N P Chisana Braye I 13009 ft T Mt Jarvis O CIER W A Lakes O Tazlina C 13421 ft L Caution. -
Mount Wrangell District, Alaska
A, Economic Qeol y, 25 Rofeasional Paper No. 15 Series{ B, Dwmiptins Q&, 80 DEPARTMENT OF THE INTERIOR UNlTED S'l'hTES GEOLOGICAL SURVEY CHARLES U. \flALCOTT, I)IRECTOR THE MINERAL RESOURCES OF THE MOUNT WRANGELL DISTRICT, ALASKA BY WALTER C, MENDENHALL AND FRANK C, SCHRADER WASHINGTON GOVERNMENT PRINTING OFFICE 1903 .I MOUNT WRANGELL. VIFW t-keri frnm thi, Giivr,~nment im1 above To~is~iaBr~iloe 41 mles from tire sumtnit of tits maunin,~ I; NkDlNA RIVER BARS, Mnunt Drum in backgniuncl. Page . Introduction ................................................................................ 9 Copper ................................................................................... 13 Southern area ......................................................................... 13 Location ................................................................ ., ....... 13 Routes and trails ................................................................. 13 Geologic sketch .................................................................. 14 Nikolai greenstone ............................................................. 14 Chitistone limestone .......................................................... 14 Triassic shales and limestones ............................ .. .......... 15 Kennicott formation .......................................................... 15 Intrusive rocks ............................................................... 15 Copper occurrences ............................................................... 16 General statement ........................................................... -
Geospatial Distribution of Tephra Fall in Alaska: a Geodatabase Compilation of Published Tephra Fall Occurrences from the Pleistocene to the Present
GEOSPATIAL DISTRIBUTION OF TEPHRA FALL IN ALASKA: A GEODATABASE COMPILATION OF PUBLISHED TEPHRA FALL OCCURRENCES FROM THE PLEISTOCENE TO THE PRESENT Katherine M. Mulliken, Janet R. Schaefer, Cheryl E. Cameron Miscellaneous Publication 164 $5.00 This publication is PRELIMINARY in nature and meant to allow rapid release of field observations or initial interpretations of geology or analytical data. It has undergone limited peer review, but does not necessarily conform to DGGS editorial standards. Interpretations or conclusions contained in this publication are subject to change. March 2018 State of Alaska Department of Natural Resources Division of Geological & Geophysical Surveys STATE OF ALASKA Bill Walker, Governor DEPARTMENT OF NATURAL RESOURCES Andrew T. Mack, Commissioner DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS Steve Masterman, State Geologist & Director Publications produced by the Division of Geological & Geophysical Surveys are available for free download from the DGGS website (dggs.alaska.gov). Publications on hard-copy or digital media can be examined or purchased in the Fairbanks office: Alaska Division of Geological & Geophysical Surveys (DGGS) 3354 College Road | Fairbanks, Alaska 99709-3707 Phone: 907.451.5010 | Fax 907.451.5050 [email protected] | dggs.alaska.gov DGGS publications are also available at: Alaska State Library, Historical Collections & Talking Book Center 395 Whittier Street Juneau, Alaska 99801 Alaska Resource Library and Information Services (ARLIS) 3150 C Street, Suite 100 Anchorage, Alaska 99503 Suggested citation: Mulliken, K.M., Schaefer, J.R., and Cameron, C.E., 2018, Geospatial distribution of tephra fall in Alaska: a geodatabase compilation of published tephra fall occurrences from the Pleistocene to the present: Alaska Division of Geological & Geophysical Surveys Miscellaneous Publication 164, 46 p. -
Ahtna Place Names Lists 0
Ahtna Place Names Lists 0. Extraterritorial and Regional 1 Dghelaay, Dghelaay Tah the Alaska Range, the 'mountains', or ( archaically) Wrangell Mts., in the 'plural objects that are mountains suspended' [1] Tarkhonov 1797; Moffit 1904 "telo country" 1.1 Dghelaay Ce'e, Deghilaay Mount McKinley, Denali 'big mountain' Ce'e, Ggalaay Ce'e 62.5, -149.7 [1] Wrangell 1839 "Tenada" from Western Alaska Athabascan 3 'Atna' Nene' Copper River Valley 'Ω river land' 61.9517, -145.7966 [1] 4 'Atna' (L, C), K'etna' (U) Copper River 'Ω river' 61.827, -145.0794 [1] Analysis of 'At-, K'et- is uncertain. Wrangell 1839 map "Atna"; Dall 1875 "Atna"; deLaguna 1970:1, Geohagen 1903; also used in ethnonym 'Atnahwt'aene 'Ahtna people' 4.1 ['Atna' Bene'] Glacial A> Lake Ahtna 'Ω river lake' [0] 5 Ts'itu' Copper River 'major river'; 'straight water' 61.273, -144.8426 [1] deLaguna 1970:1 6 Xentna' lower copper river below 'bend river' Tonsina 61.3389, -144.7698 [2-JMc] deLaguna 1970:2 7 I'na' Daa'a, C'ena' Daa'a lower Copper River area 'the stream downriver' [1] Possible source for Kanata Ck, (see entry 61) formerly for the north fork of the Teikel River, Rohn 1899 8 Bes Nezdlaayi bluff on E bank of CR 'river bank that extends in a line (rope-like)' 62.282, -145.2417 [2-FJ] Refers to east bank of Copper River curving around Mt. Drum. 9 Hwtsaay Nene' Upper Gulkana R & Upper 'small timber land' Susitna R plateau 62.8785, -146.5058 [1] deLaguna 1970:37 10 Datggadi Nene' K'et westerly Ahtna uplands 'upper country' [1] 11 Tatl'ah Nene' upper Copper River above 'headwaters land' Slana 62.7054, -143.8512 [1] Also refers to Slana River area. -
USGS Geologic Investigations Series I 2585, Pamphlet
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I–2585 U.S. GEOLOGICAL SURVEY DIGITAL SHADED-RELIEF IMAGE OF ALASKA By J.R. Riehle1, M.D. Fleming2, B.F. Molnia3, J.H. Dover1, J.S. Kelley1, M.L. Miller1, W.J. Nokleberg4, George Plafker4, and A.B. Till1 INTRODUCTION drawn by Harrison (1970; 1:7,500,000) for The National Atlas of the United States. Recently, the State of Alaska digi- One of the most spectacular physiographic images tally produced a shaded-relief image of Alaska at 1:2,500,000 of the conterminous United States, and the first to have scale (Alaska Department of Natural Resources, 1994), us- been produced digitally, is that by Thelin and Pike (1991). ing the 1,000-m digital elevation data set referred to below. The image is remarkable for its crispness of detail and for An important difference between our image and the natural appearance of the artificial land surface. Our these previous ones is the method of reproduction: like the goal has been to produce a shaded-relief image of Alaska Thelin and Pike (1991) image, our image is a composite that has the same look and feel as the Thelin and Pike im- of halftone images that yields sharp resolution and pre- age. The Alaskan image could have been produced at the serves contrast. Indeed, the first impression of many view- same scale as its lower 48 counterpart (1:3,500,000). But ers is that the Alaskan image and the Thelin and Pike im- by insetting the Aleutian Islands into the Gulf of Alaska, age are composites of satellite-generated photographs we were able to print the Alaska map at a larger scale rather than an artificial rendering of a digital elevation (1:2,500,000) and about the same physical size as the model. -
GLACIERS of ALASKA by BRUCE F
Glaciers of North America— GLACIERS OF ALASKA By BRUCE F. MOLNIA With sections on COLUMBIA AND HUBBARD TIDEWATER GLACIERS By ROBERT M. KRIMMEL THE 1986 AND 2002 TEMPORARY CLOSURES OF RUSSELL FIORD BY THE HUBBARD GLACIER By BRUCE F. MOLNIA, DENNIS C. TRABANT, ROD S. MARCH, and ROBERT M. KRIMMEL GEOSPATIAL INVENTORY AND ANALYSIS OF GLACIERS: A CASE STUDY FOR THE EASTERN ALASKA RANGE By WILLIAM F. MANLEY SATELLITE IMAGE ATLAS OF THE GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–K About 5 percent (about 75,000 km2) of Alaska is presently glacierized, including 11 mountain ranges, 1 large island, an island chain, and 1 archipelago. The total number of glaciers in Alaska is estimated at >100,000, including many active and former tidewater glaciers. Glaciers in every mountain range and island group are experiencing significant retreat, thinning, and (or) stagnation, especially those at lower elevations, a process that began by the middle of the 19th century. In southeastern Alaska and western Canada, 205 glaciers have a history of surging; in the same region, at least 53 present and 7 former large ice-dammed lakes have produced jökulhlaups (glacier-outburst floods). Ice-capped Alaska volcanoes also have the potential for jökulhlaups caused by subglacier volcanic and geothermal activity. Satellite remote sensing provides the only practical means of monitoring regional changes in glaciers in response to short- and long-term changes in the maritime and continental climates of Alaska. Geospatial analysis is used to define selected glaciological parameters in the eastern part of the Alaska Range.