Kotsina-Chpiwa Region, Alaska .: ' .5

Total Page:16

File Type:pdf, Size:1020Kb

Kotsina-Chpiwa Region, Alaska .: ' .5 ,A - ,., -,., &', ' - "' -".: ,,,.,,-I .,, DEPhRTMEHT OF THE INTERIOR I>= UNITED STA!I'ES GFDWOICAL SURVEY GEORGE OTIg WMiTE, D~DXOE i MINERAL RESOURCES KOTSINA-CHPIWA REGION, ALASKA .: ' .5. FRED Ii. MOF'FIT AND A. a. MADDREN -. , , ,I., - , . WASHlNaTON . QOVBBRMENT PFlIETIHB OFFIQI 19 0 0 .. .. m . , . ---- CONTENTS. Pmfaee, by $Vred B. Brnkfi-----,_,---,,,,,-.-.,,,----,--,--,-,-,--- ~n~n~tI~------------------------~----~-,~-------*--~------- wphgg~a hi&~m ---,,,------, ,- ---------,,_ ------------------------ PmItion-,---,----,,,-----,*-~~----,,---------------------~----- mfla d ran- ---,------,--,------,- --,---- Vdtimand cllmatlc condttlaarr--,,,-,--titititi-ti-----__,-- History ,---,------,d-----------,,,--,-----*d----------4----- heral mlogs----------------------------+--*--------------+--- lntrodnction---------------------------,----,-----,,----------- Undetermined rocks on Kotsina Rivet,,,,--,----,,,,-------------- Nikolai green&one-------+----,,-------~---,,,-,-,,,_-,,,-------- Dewription - -+-- -- - - -,.-- ---+ ,, .- ,, -,,- ,- - Occurrence and dlMrlbutIon,,--- --------. .,-- -- _,,---,,,----- Structure of the greenstni~r--------_,-------------*---,-+------- Age d the greens ton^------------^- ----,--.--,,,-,,,-------- Chitistone limealone (Trhi~ic)-----,---_-,,---,-, XXXXXXXXXXXXXXXX Dewrlptlon----,,----,-------,------------,---------- Orrcnrrenoe and dl~tribntinn-,,--------------------------,-+-- Thlcknesa of QtltI8tone limestone------,,--------------------- Age of the Chitimtone Ilm&one,,------,-----,,,-----,---,--,- Trlamde Timestones and sbalea-------------------------+---------- Dmpflm,-,-------------,-----,--------,----------+- Occnrreoce and dImtrfbnUon ----------------------------**-,+- Fmlla -I-,--------------,,,--- - -,,--- . -,,-, ,, , - ,-- --- Dtetnrb~nwfoll- depMtlon of Tela-lc ,-----,----------=---- Kenntcott fmadon--,-----------+-----------------------**~- Deacd~tition,-----------------,-------------~------------- Occertence and dlstrbntion---------------------,A*,---- dm of Kennfcott formation-----------------n--n---------n-, 1,,,, h8t-Kwnfmtt dlhrbance and emsfon-------------------*-------- -1-beaslng racks,--+---------------------------------,,-,,- TertIam volmnlc serIe~----------------------------------------- Ikwtlption and mnmnrp-----------,,----------,---,-- TlilcRneu8 of volcanic 8eri~~----------,----- 2 ---------------- Ajre of volcanic 8eries-----------------,-------,-,,----- rgumua rocks_--,-------,-------------------+---,,,-,,,,-- Prellmlnarg glatement _,- ------------------ Granular racks in the nnmetamorphoeed 8edlmwts ,-,,-,,,--,,, Porpbyrlea in the uumetAmorpbo& sedtmwt~,--,,,--,,------ Andtwite cutting the Triassic-------------_-I------------------ Intrarrlve rocks In Tertiary volmlc wries-------,,,,---------- Andesite flo~&--,----------------~----------------------+-- S Wnlle --,-------4,,---,,,,,----------_--------------------~ Plelsto~weand Recent dmlts latrodnctlm-,,,,,,-----------~~---------------------------- Preaent fatures,,,,-----,---------------,--+------------ Pm-Plelntocene land m&c& ,,,,,--,--I----C&-C&C&C&C&C&--------C& Emaioa and depcaltlon dallng Pldstocene and Recent time---- Character of tbe v~lle~-plnlndemstte ,,,,,-------------------- hornic ~eoto~-----------,,_----------------------------------- Generat stntmeat--------..-------,,----+---------------------- Copper,,,-,,-,--,~~*~-",,-~----*~-*--,*~----~d-------------- The copper ml~etals---,---------~--,---,----------~-------,- PrPllmtnary Rtatement -- - -- -., _, - - - ,- .- - - - - .. ----- ----,_ Katlve copj~?r---,,,-------~----------- ,--,,,------,,---- Cuprite ,------------,,+,+,-----d--u--------------------- Tenorite ----,-=---------,,,--------------------------- Chalmite----------,------,---------,,-.---------------- Bornite ,-----,-d,, ----- .--,,-. +, +, ----------,,,,,,-,_,_ Chalcopyrite Melachite ----------------,--------------------------+-- dzuslte -,,,----,,,,-+,+,,-----------,-+-,+------------ Chal~anthite-----,----------~~~~~--~-~------+*---------- Occmrrence of the ore@ - -,+--,----+--+--,,-----+----- General ~temmt--,d,,,,---------~~~~--~~-~-~~-~~--h~ Copper sulphide deposlta In mnrttone r~ndllmwtone-,,- - - Native cogpcr amlated wttlr the mstonp,---,,-,,*---- Placer copper-,,,-,-+------------,,,------,, Rource and character of the copper depwlts-,-------,,,-+----- Dmriptlon of propertia,-----,-------------+-----------,--- Kobslns Hlwr basl~-------,------__,,-------~----*---- Kotsioa Bfver--,+,-------------------,,,,,----,, Amea Creek----------------------.-----------,--- Rock Creek- --,,---,,--------------------------*- Iionrlng Creet,---,------- t----t--tt----------- Peacock Cree-,-,----------+---------------- Roee cIaim-------------,,,----,,,------ White IMg and M3nt clafma------------,---------- BIoantain cIaim--------------------------------- 8hower Sorprie CmIr-,-----------,--------------------- bddle claim,--,,---------------------+---- Rheehan rlalm-----,-----------------------,__ Hubbard cldm--------------------------------- &lav~rmn Wk-----,,---------------,-------------- Oopp~rCreek---,,,,------------------------+--- General descrlptlo~----- ,---I,---I,---+ Coppet Rhg and MineraI Klng claims_ Clslm at the bend of Qnm Creek ---------------- Van Dyke claim Copper Qnew clalm---------,---,--------------- REver rwlon, Aln~ka,,,-,-,--,,----,-----,----4------- In pocket. II. Qeolodc mnnaloirnnce map and wtlons of the ChItLna copper belt, Ala~kn,,--,,,,,,,,,~~,~-,---,---- In pocket. m. A, Contact ni Nlkolnl maoneand Chitlame Hmestone west of Nlalna Itlv~r,nmr Nlkolal mine: B, UbmM mesnstone on gouth nlde of Kntmlna HIver helow Flnrprlrr~Creek------- IV. A, Thin-ledrlPd Trlna~lclirne~tone nud shale on WPMbrnnch of Rock Crppk; n, Crumpling In thtn-Wdal TrlamLc J!m&me on rld~rPIIR~ of U11nhlna RIrW ,,,,---,,,,,,,,--,------ V. Head of Nlknlnl Crwk -------,-,,-,------------------------ VI. A, Intraalon~of Rne-~rninodporph~lry In black ~hale(m Pnnng Crwk ; It, Ct~stleXIountatn ,------,,-,,----------------d VII, A, PMrrtmne gmrel btuR~along north bank d Chitina Rlver: R, Chlffstono Ilmmtone on the north Bide of Elliott Cree%--,- Tfff. Vlew of Ibnnnm mfn~fmm JFormhw trail+,----,,-----,,,, IX. A. View nb th~XfknluI v~lnnnd ~hnft;B. Vlew dmg the r~la of the Henry Prnther clnlrn,,---------,-,------+----,- X. A, Cdntact of the Chlti~tooetlmeatone and h'lkohl. grepnstonp formations on WR'~ ~tdeof Nlaba REV-; R, Vlew ncmm Nlzlnn Riper Into Dan Creek----,,--,,,,,,,,,,,,, Fram 1. Pmrnparatlve grad- of the four mpoeed mlImad routes from the eoacrt to th~Interlor Coppw Rlver heik,,------,--, 2 Rk~trhmap of part of Elllott Cmk,-,,,,,,,,,,----,-,-, .X Cmrm section of the Elliott Creek aatlcltae,,,,,,,-,,------- 4. Dlngmrn ~howlngthe rphtfon of the fnukted portloma of the Gnarlyear claim. Elliott Creek ----,,,----,,------,- 89 B. Sketch map or the kmama mlne-----,,,,,,,,------,------- Rl & Form of on? myexposed in the mafn OF north- tunnel at the Bonanza mlne-----L,,,-----------------d-------- a4 7. lbrm of ore body ex- in the mathern tunnel at the Bonanza rnIne,,------,,,,,,,,-----,-,-~---~,~~~-- 85 a Ore WJat the Jumbo claim ---,,,---,---,-,------------8-7 9. sketch map of a part of mtltu Creek ----~----88 Desrlptlon of pmpertiHantisti#l. IintPlna River h~aln--Continmil. Elliott Creek-Contlnunl. L-le II cERI~----,,,,,,, ,,------ ----*-,*-------= My~niend Henry Prrther clr!lma---- .-.----_-_ Ellm~hPtb claim----,,------,--------------------- MHT~PAntoinette clalnl,,-- ,---,----------- * - - - -- Alh~rtJohnm clnlm ,,,,--,--------------------.. Iinthrfe clnlm- ,,,,,,,,,,,.,--------------------- f~Fanttand Iamton claEma---- ..,------.---_,---_ clin clnI~--,-,,----,,--_------_---------,,-- mane clafm- Xn~knTnn~Mlvrr l~tasln--------------,,-,---------A+--: +--+- Gpotrrnl dnwrlptioll ------------------------------k-- 'Nnu~ettCt~c~k-------------------------------------,- (#mfnI uutllnt., ,-------+-,----+ .. --- ------------- 'lrnEdm clnlm ,,-----,-----+,,-------------------- One Olrl cl~lm-------------------------.----+--- RtreJnn Cd,,,-----------------------------, LakIna Kim,,-,,,,,,,-,,-+---------------..,--.-----,-- Kennlmtt RLva basln ,,,,,,,,---------------------------- Hldaw -k,,,,,,,-----,,,--,------------------.-- Blacler and Fourth of f ulg cswks-,--,--,,---- ..---- Nebmrrk~ ~Mrn,-,,,-,,,,-------f~~----~--------- Rckka ~ndBH elrlms ,,,,,,,,-,-,----+----. -.,,-- Rm~naaCreek,,,-,,,-,,,,,,,,,-,-------,---,----.,,- Jumbo Creek-,---,,,,.,,-,,--,-----,-----------,--,, LTrk rind Ind~deoaclnlms ------ ------------------ The NMU plam ,,--.,--,--,---,,---,--------.-*-_-------- LocaHon and blntory-,,,,,,-------------------,-------+,- GeoIoglcal dmtrnh ,---,,,,,,----------------,,----,,----,- ChItitu Cnepk,-,,,--------------------.------,--_----- PREFACE. Native copper from the district dawribed in this volume is the first mineral reported $rum Alaska. SteIIer, tho naturalist who nccompaaied Bering on his voyage of discovery in 1741, notad the use of copper Icnives among the natives of Kayak Island. This copper undoubtedly came from the Chitinn-Rotsina belt. Among the Alaskan natives the use of copper was widespread, for it was the only metal utilized by them, but appnmntly the century of occupation by the Russians pamd without. nny search on their part for the lditpfrom which the supply WBS derived. The only attempt made by the Russians to explore the Copper River (Serebmnikof, 1847 resulted in the massacre of the whale pfirty by the Indians. Tila fimt successful explomtions were made by Allen (1886) and by Schwatka
Recommended publications
  • A Data Set of Worldwide Glacier Length Fluctuations
    Portland State University PDXScholar Geology Faculty Publications and Presentations Geology 2014 A Data Set of Worldwide Glacier Length Fluctuations Paul W. Leclercq Utrecht University Johannes Oerlemans Utrecht University Hassan J. Basagic Portland State University, [email protected] Christina Bushueva Russian Academy of Sciences A. J. Cook Russian Academy of Sciences See next page for additional authors Follow this and additional works at: https://pdxscholar.library.pdx.edu/geology_fac Part of the Geology Commons, and the Glaciology Commons Let us know how access to this document benefits ou.y Citation Details Leclercq, P. W., Oerlemans, J., Basagic, H. J., Bushueva, I., Cook, A. J., and Le Bris, R.: A data set of worldwide glacier length fluctuations, The Cryosphere, 8, 659-672, doi:10.5194/tc-8-659-2014, 2014. This Article is brought to you for free and open access. It has been accepted for inclusion in Geology Faculty Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Authors Paul W. Leclercq, Johannes Oerlemans, Hassan J. Basagic, Christina Bushueva, A. J. Cook, and Raymond Le Bris This article is available at PDXScholar: https://pdxscholar.library.pdx.edu/geology_fac/50 The Cryosphere, 8, 659–672, 2014 Open Access www.the-cryosphere.net/8/659/2014/ doi:10.5194/tc-8-659-2014 The Cryosphere © Author(s) 2014. CC Attribution 3.0 License. A data set of worldwide glacier length fluctuations P. W. Leclercq1,*, J. Oerlemans1, H. J. Basagic2, I. Bushueva3, A. J. Cook4, and R. Le Bris5 1Institute for Marine and Atmospheric research Utrecht, Utrecht University, Princetonplein 5, Utrecht, the Netherlands 2Department of Geology, Portland State University, Portland, OR 97207, USA 3Institute of Geography Russian Academy of Sciences, Moscow, Russia 4Department of Geography, Swansea University, Swansea, SA2 8PP, UK 5Department of Geography, University of Zürich, Zurich, Switzerland *now at: Department of Geosciences, University of Oslo, P.O.
    [Show full text]
  • 10Th Annual Northern Research Day
    Circumpolar Students’ Association 10th Annual Northern Research Day Monday, 19 April 2010 9:00 a.m. to 4:00 p.m. 3-36 Tory Building Featuring the Documentary Film Arctic Cliffhangers Show Time: 12:30 Followed by a Keynote with Filmakers: Steve Smith and Julia Szucs 1 NORTHERN RESEARCH DAY – SCHEDULE OF SPEAKERS TIME AUTHORS/SPEAKERS TITLE 9:00 Justin F. Beckers, Christian Changes in Satellite Radar Backscatter and the Haas, Benjamin A. Lange, Seasonal Evolution of Snow and Sea Ice Properties on Thomas Busche Miquelon Lake, a Small Saline Lake in Alberta 9:15 Benjamin A. Lange, Christian Sea ice Thickness Measurements Between Canada and Haas, Justin Becker and Stefan the North Pole: Overview and Results from Three Hendricks Campaigns in 2009 (CASIMBO-09, Polar-5 & CATs) 9:30 Hannah Milne, Martin Sharp Recording the Sight and Sound of Iceberg Calving Events on the Belcher Glacier, Devon Island, Nunavut 9:45 Gabrielle Gascon, Martin Sensitivity of Ice-atmosphere Interactions Since the Sharp and Andrew Bush Last Glacial Maximum 10:00 Brad Danielson and Martin Seasonal and Inter-Annual Variations in Ice Flow of a Sharp High Arctic Tidewater Glacier 10:15 Xianmin Hu, Paul G. Myers Numerical Simulation of the Arctic Ocean Freshwater and Qiang Wang Outflow 10:30 Coffee 10:45 Qiang Wang, Paul G. Myers, Numerical Simulation of the Circulation and Sea-Ice Xianmin Hu and Abdrew B.G. in the Canadian Arctic Archipelago Bush 11:00 Porter, L.L. and Rolf D. Impacts of Atmospheric Nitrogen and Phosphorous Vinebrooke. Deposition on the Alpine Ponds of Banff National Park: Effects on the Benthic Communities 11:15 Stephen Mayor The Changing Nature: Human Impacts on Boreal Biodiversity 11:30 Louise Chavarie, Kimberly Diversity of Lake Trout, Salvelinus namaycush, in Howland, and W.
    [Show full text]
  • Thurston Island
    RESEARCH ARTICLE Thurston Island (West Antarctica) Between Gondwana 10.1029/2018TC005150 Subduction and Continental Separation: A Multistage Key Points: • First apatite fission track and apatite Evolution Revealed by Apatite Thermochronology ‐ ‐ (U Th Sm)/He data of Thurston Maximilian Zundel1 , Cornelia Spiegel1, André Mehling1, Frank Lisker1 , Island constrain thermal evolution 2 3 3 since the Late Paleozoic Claus‐Dieter Hillenbrand , Patrick Monien , and Andreas Klügel • Basin development occurred on 1 2 Thurston Island during the Jurassic Department of Geosciences, Geodynamics of Polar Regions, University of Bremen, Bremen, Germany, British Antarctic and Early Cretaceous Survey, Cambridge, UK, 3Department of Geosciences, Petrology of the Ocean Crust, University of Bremen, Bremen, • ‐ Early to mid Cretaceous Germany convergence on Thurston Island was replaced at ~95 Ma by extension and continental breakup Abstract The first low‐temperature thermochronological data from Thurston Island, West Antarctica, ‐ fi Supporting Information: provide insights into the poorly constrained thermotectonic evolution of the paleo Paci c margin of • Supporting Information S1 Gondwana since the Late Paleozoic. Here we present the first apatite fission track and apatite (U‐Th‐Sm)/He data from Carboniferous to mid‐Cretaceous (meta‐) igneous rocks from the Thurston Island area. Thermal history modeling of apatite fission track dates of 145–92 Ma and apatite (U‐Th‐Sm)/He dates of 112–71 Correspondence to: Ma, in combination with kinematic indicators, geological
    [Show full text]
  • Glacier Fluctuations Globaltemperatureandsea-Levelchange
    GLACIER FLUCTUATIONS GLOBAL TEMPERATURE AND SEA-LEVEL CHANGE Paul Willem Leclercq Beoordelingscommissie: Prof. dr. M.R. van den Broeke Prof. dr. W. Haeberli Prof. dr. B.J.J.M. van den Hurk Prof. dr. C. Schneider ISBN: 978-90-393-5717-0 printing: Ipskamp Institute for Marine and Atmospheric research Utrecht (IMAU) Department of Physics and Astronomy Faculty of Science Universiteit Utrecht Financial support was provided by the Netherlands Organisation for Scientific Research NWO through research grant 816.01.016. Cover: false colour Landsat image of Sukkertoppen, West Greenland. Courtesy of USGS. GLACIER FLUCTUATIONS GLOBAL TEMPERATURE AND SEA-LEVEL CHANGE GLETSJER FLUCTUATIES, MONDIALE TEMPERATUUR EN ZEESPIEGEL VERANDERING (met een samenvatting in het Nederlands) PROEFSCHRIFT ter verkrijging van de graad van doctor aan de Universiteit Utrecht op gezag van de rector magnificus, prof. dr. G.J. van der Zwaan, ingevolge het besluit van het college voor promoties in het openbaar te verdedigen op woensdag 8 februari 2012 des middags te 12.45 uur door Paul Willem Leclercq geboren op 17 juli 1979 te Tilburg Promotor: Prof. dr. J. Oerlemans Contents Summary iii 1 Introduction and conclusions 1 1.1 Reconstructing climate of the past . .2 1.2 Glaciers . .4 1.3 Observed glacier length fluctuations . 16 1.4 Climate reconstructions from glacier length fluctuations . 19 1.5 Glacier contribution to sea-level rise . 23 1.6 Climate versus mass balance – the influence of adjustment of the glacier geometry . 26 1.7 Main conclusions . 28 1.8 Discussion and outlook . 28 2 A data set of world-wide glacier length fluctuations 31 2.1 Introduction .
    [Show full text]
  • A Revised Geochronology of Thurston Island, West Antarctica and Correlations Along the Proto
    1 A revised geochronology of Thurston Island, West Antarctica and correlations along the proto- 2 Pacific margin of Gondwana 3 4 5 6 T.R. Riley1, M.J. Flowerdew1,2, R.J. Pankhurst3, P.T. Leat1,4, I.L. Millar3, C.M. Fanning5 & M.J. 7 Whitehouse6 8 9 1British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK 10 2CASP, 181A Huntingdon Road, Cambridge, CB3 0DH, UK 11 3British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK 12 4Department of Geology, University of Leicester, Leicester, LE1 7RH, UK 13 5Research School of Earth Sciences, The Australian National University, Canberra ACT 0200, Australia 14 6Swedish Museum of Natural History, Box 50007, SE-104 05 Stockholm, Sweden 15 16 17 18 19 20 21 22 23 24 *Author for correspondence 25 e-mail: [email protected] 26 Tel. 44 (0) 1223 221423 1 27 Abstract 28 The continental margin of Gondwana preserves a record of long-lived magmatism from the Andean 29 Cordillera to Australia. The crustal blocks of West Antarctica form part of this margin, with 30 Palaeozoic – Mesozoic magmatism particularly well preserved in the Antarctic Peninsula and Marie 31 Byrd Land. Magmatic events on the intervening Thurston Island crustal block are poorly defined, 32 which has hindered accurate correlations along the margin. Six samples are dated here using U-Pb 33 geochronology and cover the geological history on Thurston Island. The basement gneisses from 34 Morgan Inlet have a protolith age of 349 ± 2 Ma and correlate closely with the Devonian – 35 Carboniferous magmatism of Marie Byrd Land and New Zealand.
    [Show full text]
  • Debris-Covered Glaciers and Rock Glaciers in the Nanga Parbat Himalaya, Pakistan
    DEBRIS-COVERED GLACIERS AND ROCK GLACIERS IN THE NANGA PARBAT HIMALAYA, PAKISTAN BY JOHNF. SHRODER',MICHAEL P. BISHOP',LUKE COPLAND2 AND VALERIEF. SLOAN3 1Departmentof Geography and Geology, University of Nebraska at Omaha, USA 2Departmentof Geology, University of Alberta, Edmonton, Canada 3 INSTAAR, University of Colorado, Boulder, USA Shroder,John F., Bishop,Michael P., Copland,Luke and Sloan, surface from steep surrounding slopes. Kick ValerieF., 2000:Debris-covered glaciers and rock glaciers in the (1962) noted thatAdolf Schlagintweit first used the NangaParbat Himalaya, Pakistan. Geogr. Ann., 82 A (1): 17-31. termfirnkessel glaciers in 1856 for the types of gla- ABSTRACT.The origin and mobilization of theextensive debris ciers in High Asia that are fed predominantly by av- coverassociated with the glaciersof the NangaParbat Himalaya alanches from the high cliffs, as opposed to the is In this a complex. paperwe propose mechanismby whichgla- firnmulden types in the Alps that are nourished by ciers can form rock glaciersthrough inefficiency of sediment transferfrom glacier ice to meltwater.Inefficient transfer is slow ice flow from a firn field. Because of the ir- causedby variousprocesses that promote plentiful sediment sup- regular or punctuated delivery of ice avalanches, ply anddecrease sediment transfer potential. Most debris-covered the mass balance of the Himalayan glaciers is on Parbatwith velocitiesof glaciers Nanga higher movementand/ thought to be much more irregularthan elsewhere, or efficientdebris transfer mechanisms do notform rock glaciers, perhapsbecause debris is mobilizedquickly and removedfrom with the result that considerable variation from one suchglacier systems. Those whose ice movementactivity is lower glacier to another can occur in advance, retreat, ice andthose where inefficient sediment transfer mechanisms allow buildup, or downwasting (Mercer 1963, 1975a, b; plentifuldebris to accumulate,can formclassic rock glaciers.
    [Show full text]
  • Glaciers of the Canadian Rockies
    Glaciers of North America— GLACIERS OF CANADA GLACIERS OF THE CANADIAN ROCKIES By C. SIMON L. OMMANNEY SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–1 The Rocky Mountains of Canada include four distinct ranges from the U.S. border to northern British Columbia: Border, Continental, Hart, and Muskwa Ranges. They cover about 170,000 km2, are about 150 km wide, and have an estimated glacierized area of 38,613 km2. Mount Robson, at 3,954 m, is the highest peak. Glaciers range in size from ice fields, with major outlet glaciers, to glacierets. Small mountain-type glaciers in cirques, niches, and ice aprons are scattered throughout the ranges. Ice-cored moraines and rock glaciers are also common CONTENTS Page Abstract ---------------------------------------------------------------------------- J199 Introduction----------------------------------------------------------------------- 199 FIGURE 1. Mountain ranges of the southern Rocky Mountains------------ 201 2. Mountain ranges of the northern Rocky Mountains ------------ 202 3. Oblique aerial photograph of Mount Assiniboine, Banff National Park, Rocky Mountains----------------------------- 203 4. Sketch map showing glaciers of the Canadian Rocky Mountains -------------------------------------------- 204 5. Photograph of the Victoria Glacier, Rocky Mountains, Alberta, in August 1973 -------------------------------------- 209 TABLE 1. Named glaciers of the Rocky Mountains cited in the chapter
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Glacier Length Records (E.G
    Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | The Cryosphere Discuss., 7, 4775–4811, 2013 Open Access www.the-cryosphere-discuss.net/7/4775/2013/ The Cryosphere TCD doi:10.5194/tcd-7-4775-2013 Discussions © Author(s) 2013. CC Attribution 3.0 License. 7, 4775–4811, 2013 This discussion paper is/has been under review for the journal The Cryosphere (TC). A data set of Please refer to the corresponding final paper in TC if available. world-wide glacier length fluctuations A data set of world-wide glacier length P. W. Leclercq et al. fluctuations Title Page P. W. Leclercq1, J. Oerlemans1, H. J. Basagic2, I. Bushueva3, A. J. Cook4, and 5 R. Le Bris Abstract Introduction 1 Institute for Marine and Atmospheric research Utrecht, Utrecht University, Princetonplein 5, Conclusions References Utrecht, the Netherlands 2 Department of Geology, Portland State University, Portland, OR 97207, USA Tables Figures 3Institute of Geography Russian Academy of Sciences, Moscow, Russia 4 Department of Geography, Swansea University, Swansea, SA2 8PP, UK J I 5Department of Geography, University of Zürich, Zürich, Switzerland J I Received: 11 September 2013 – Accepted: 12 September 2013 – Published: 28 September 2013 Back Close Correspondence to: P. W. Leclercq ([email protected]) Full Screen / Esc Published by Copernicus Publications on behalf of the European Geosciences Union. Printer-friendly Version Interactive Discussion 4775 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract TCD Glacier fluctuations contribute to variations in sea level and historical glacier length fluctuations are natural indicators of climate change. To study these subjects, long- 7, 4775–4811, 2013 term information of glacier change is needed.
    [Show full text]
  • GEOLOGICAL SURVEY of DENMARK and GREENLAND BULLETIN 21 · 2010 Exploration History and Place Names of Northern East Greenland
    GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 21 · 2010 Exploration history and place names of northern East Greenland Anthony K. Higgins GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF CLIMATE AND ENERGY Geological Survey of Denmark and Greenland Bulletin 21 Keywords Exploration history, northern East Greenland, place names, Lauge Koch’s geological expeditions, Caledonides. Cover illustration Ättestupan, the 1300 m high cliff on the north side of Kejser Franz Joseph Fjord discovered and so named by A.G. Nathorst in 1899. Frontispiece: facing page Map of Greenland by Egede (1818), illustrating the incorrect assumption that the Norse settlements of Greenland were located in South-West and South-East Greenland. Many of the localities named in the Icelandic Sagas are placed on this map at imaginary sites on the unknown east coast of Greenland. The map is from the second English edition of Hans Egede’s ‘Description of Greenland’, a slightly modified version of the first English edition published in 1741. Chief editor of this series: Adam A. Garde Editorial board of this series: John A. Korstgård, Department of Earth Sciences, University of Aarhus; Minik Rosing, Geological Museum, University of Copenhagen; Finn Surlyk, Department of Geography and Geology, University of Copenhagen Scientific editor of this volume: Adam A. Garde Editorial secretaries: Jane Holst and Esben W. Glendal Referees: Ian Stone (UK) and Christopher Jacob Ries (DK) Illustrations: Eva Melskens Maps: Margareta Christoffersen Digital photographic work: Benny M. Schark Layout and graphic production: Annabeth Andersen Geodetic advice: Willy Lehmann Weng Printers: Rosendahls · Schultz Grafisk a/s, Albertslund, Denmark Manuscript received: 22 April 2010 Final version approved: 1 July 2010 Printed: 21 December 2010.
    [Show full text]
  • A Cool Way to Spend Summer Skater's Edge
    University of Alaska Southeast W h a le s o n g Editorial & Opinion 2 News & Features 4 I nside: Cantus & Community 6 Arts 4 Entertainment 10 A cool way to spend summer By Melissa Adams, Whalesong Staff A UAS student gazes down into a deep Glacier research opportunities abound blue chasm of ice. The radiant white planes at UAS. Dr. Roman Motyka UAS Faculty of the glacier’s surface stretch for miles affiliate researcher regularly engages students around. Equipped with his trusty rope and in projects across the state, at sites including harness he begins his descent into a crevasse, the Mendenhall Glacier, Le Conte Glacier, a deep icy split stretching 150 feet into the Hubbard Glacier near Yakutat, and in Glacier glacier. Bay, This spring semester Dr. Eran Hood All in a day’s work for a student UAS ENVS Program and UAF researcher researcher in the week long UAS Environ- Adam Bucki will team up to offer Geology mental Science (ENVS) Program Glacier 315, a glacier surveying field experience. Field Surveying class on the Mendenhall Icefield research sheds light on the total Glacier or in the longer eight week Juneau “health of the glacier,” according to Cathy Icefield Research Program (JIRP). The JIRP Connor, UAS geology associate professor is based at the University of Idaho in Mos- who has worked both with Motyka on the cow and directed by Dr. Maynard Miller. Leconte and Mendenhall glaciers and on the Taku Glacier with Miller as a JIRP summer While many undergraduates spend the JIRP students conduct a GPS survey to determine the movement of the Photo credit: Scott McGee majority of their time learning in the class- faculty mentor since 1994.
    [Show full text]