Significant Metalliferous Lode Deposits and Placer Districts of Alaska
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Applicability of Siberian Placer Mining Technology to Alaska
MIRL Report No. 89 Applicability- - of Siberian Placer Mining Technology to Alaska Dr. Frank J. Skudrzyk, Project Manager E++W Engineering Consultants 461 1 Dartmouth Fairbanks, Alaska James C,Barker U.S. Bureau of Mines Alaska Field Operations Cenkr Fairbanks. Alaska Daniel E. Walsh School of Mineral Engineering University of Alaska Fairbanks Fairbanks, Alaska Rocky MacDonald American Arctic Company Fairbanks, Alaska Library of Congress Cataloging in Publication Data Library of Congress Catalog Card Number: 9 1-6 1923 ISBN 0-911043-12-8 May, 1991 Published bv Mined Industry Research Laboratory 212 ONeill Building University of Alaska Fairbanks Fairbanks, Alaska 99775-1 180 Alaska Science and Technology Foundation 550 West 7th Avenue Suite 360 Anchorage, Alaska 99501 ABSTRACT The result of Perestroyka and Glasnost has been an awakening of potential for cooperation between East and West. Nowhere has that been better demonstrated than between Alaska and Magadan Province, USSR. This report summarizes a one year effort financed by ASTF, with participation from several technical organizations, to establish contacts with the Siberian placer mining industry. The purpose of the project was to provide initial assessment of the Soviet technology for placer mining in permafrost. A ten day trip to Magadan province by an ASTF team and a similar length visit to Alaska by the Soviet mining group representing the All Union Scientific and Research Institute of Gold and Rare Metals, (VNII-I), Magadan are described. The report also reviews translated data on mining in permafrost and describes surface and underground placer mining technology developed by the Soviets. The report also lists relevant publications on Soviet mining research and state of the art Soviet mining technology and expertise. -
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. -
Exploration of Placer Gold Deposits by Geomagnetic Surveys
MTR-2 EXPLORATION OF PLACER GOLD DEPOSITS BY GEOMAGNETIC SURVEYS by Eric Anderson V. P. Exploration Placer Management Group, Ltd. EXPLORATION OF PLACER GOLD DEPOSITS BY GEOMAGNETIC SURVEYS by Eric Anderson V. P. Exploration Placer Management Group, Ltd. Exploration of Placer Gold Deposits by Geomagnetic Surveys Eric Anderson, V.P. Exploration Placer Management Group, Ltd. ABSTRACT Past attempts to explore for placer gold deposits by measuring the anomalous magnetic intensities of the magnetite normally found in the ”black sands” fraction of placer gravels were for the most part unsuccessful. Recent improvements in the sensitivity, reliability and portability of magnetometers have made it possible to cheaply and accurately delineate some types of placer gravels if they occur in a geological environment that is ”magnetically hospitable” and does not mask the signal of the overlaying gravels. The main benefit of this technique is that it can accurately delineate targets and thus dramatically reduce the overall cost of an exploration program in a given area. INTRODUCTION Whether or not this technique will work in a given area depends on three factors: 1. The amount of magnetite associated with the pay gravels. 2. The depth of the gravel deposit. 3. The nature of the underlying bedrock. In our work to date in Western Canada and United States, we have not encountered any pay gravels that did not have measurable concentrations of magnetite in the black sands. It is common to find gravel deposits with high concentrations of magnetite and no gold values whatsoever, but our experience and history have shown that gold values rarely occur without associated magnetic black sands; although the concentrates of magnetite do vary tremendously, In this regard it is important to keep two things in mind: 1. -
Geologic Map of Alaska
Geologic Map of Alaska Compiled by Frederic H. Wilson, Chad P. Hults, Charles G. Mull, and Susan M. Karl Pamphlet to accompany Scientific Investigations Map 3340 2015 U.S. Department of the Interior U.S. Geological Survey Front cover. Color shaded relief map of Alaska and surroundings. Sources: 100-meter-resolution natural image of Alaska, http://nationalmap.gov/small_scale/mld/nate100.html; rivers and lakes dataset, http://www.asgdc.state.ak.us/; bathymetry and topography of Russia and Canada, https://www.ngdc.noaa.gov/mgg/global/global.html. Back cover. Previous geologic maps of Alaska: 1906—Brooks, A.H., Abbe, Cleveland, Jr., and Goode, R.U., 1906, The geography and geology of Alaska; a summary of existing knowledge, with a section on climate, and a topographic map and description thereof: U.S. Geological Survey Professional Paper 45, 327 p., 1 sheet. 1939—Smith, P.S., 1939, Areal geology of Alaska: U.S. Geological Survey Professional Paper 192, 100 p., 18 plates. 1957—Dutro, J.T., Jr., and Payne, T.G., 1957, Geologic map of Alaska: U.S. Geological Survey, scale 1:2,500,000. 1980—Beikman, H.M., 1980, Geologic map of Alaska: U.S. Geological Survey Special Map, scale 1:2,500,000, 2 sheets. Geologic Map of Alaska Compiled by Frederic H. Wilson, Chad P. Hults, Charles G. Mull, and Susan M. Karl Pamphlet to accompany Scientific Investigations Map 3340 2015 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Director U.S. -
Gold, Platinum and Diamond Placer Deposits in Alluvial Gravels, Whitecourt, Alberta Special Report 89
Special Report 89 Gold, Platinum and Diamond Placer Deposits in Alluvial Gravels, Whitecourt, Alberta Special Report 89 Gold, Platinum and Diamond Placer Deposits in Alluvial Gravels, Whitecourt, Alberta G.G. Mudaliar1, J.P. Richards1 and D.R Eccles2 1 Department of Earth & Atmospheric Sciences, University of Alberta 2 Alberta Geological Survey May 2007 ©Her Majesty the Queen in Right of Alberta, 2007 ISBN 0-7785-3851-6 The Alberta Geological Survey and its employees and contractors make no warranty, guarantee or representation, express or implied, or assume any legal liability regarding the correctness, accuracy, completeness, or reliability of this publication. Any digital data and software supplied with this publication are subject to the licence conditions (specified in 'Licence Agreement for Digital Products'"). The data are supplied on the understanding that they are for the sole use of the licensee, and will not be redistributed in any form, in whole or in part, to third parties. Any references to proprietary software in the documentation, and/or any use of proprietary data formats in this release does not constitute endorsement by the Alberta Geological Survey of any manufacturer's product. This product is an EUB/AGS Special Report; the information is provided as received from the author and has had minimal editing for conformity to EUB/AGS standards. When using information from this publication in other publications or presentations, due acknowledgment should be given to the Alberta Geological Survey/Alberta Energy and Utilities Board. The following reference format is recommended: Mudaliar, G.G., Richards, J.P. and Eccles, D.R. (2007): Gold, platinum and diamond placer deposits in alluvial gravels, Whitecourt, Alberta; Alberta Energy and Utilities Board, EUB/AGS, SPE 089, 24 p. -
Colloform High-Purity Platinum from the Placer Deposit
Colloform high-purity platinum from the placer deposit of Koura River (Gornaya Shoriya, Russia) Nesterenko G.V.1, Zhmodik S.M.1,2, Airiyants E.V.1, Belyanin D.K.1,2, Kolpakov V.V.1, Bogush A.A.1,3,* 1V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, Novosibirsk 630090, Russia 2Novosibirsk State University, Novosibirsk 630090, Russia 3Department of Civil, Environmental & Geomatic Engineering, University College London, London WC1E 6BT, UK *Corresponding author: A.A. Bogush, E-mail: [email protected] Abstract A microinclusion of colloform high-purity platinum in a grain of platinum-group minerals (PGM) from the alluvial gold-bearing placer deposit in the south of Western Siberia (Russia) was detected and characterized for the first time. It is different in composition, texture, and conditions of formation from high-purity platinum of other regions described in the literature. The main characteristics of investigated high-purity platinum are colloform-layered texture, admixture of Fe (0.37-0.78 wt.%), and paragenesis of Cu-rich isoferroplatinum, hongshiite, and rhodarsenide. The PGM grain with high-purity platinum is multiphase and heterogeneous in texture. It is a product of intensive metasomatic transformation of Cu-rich isoferroplatinum (Pt3(Fe0.6Cu0.4)). The transformation was carried out in two stages: 1 - copper stage including three substages (Cu-rich isoferroplatinum, copper platinum and hongshiite); and 2 - arsenic (rhodarsenide). The formation of high-purity platinum was separated in time from the formation of isoferroplatinum and was carried out by precipitation from postmagmatic solutions. Keywords: platinum-group elements (PGE), platinum-group minerals (PGM), high-purity platinum, Cu-rich isoferroplatinum, hongshiite, alluvial placer, Gornaya Shoriya Introduction High-purity platinum was discovered in the gold-bearing placer deposit of Koura River situated in Gornaya Shoriya (south-western Siberia, Russia, Fig. -
Accomplish Me Cover Photograph South Sawyer Glacier in Southeastern Alaska
m Accomplish me Cover photograph South Sawyer Glacier in southeastern Alaska. View southeast from head of Tracy Arm. The United States Geological Survey in Alaska: Accomplishments during 1977 Kathleen AA. Johnson, Editor GEOLOGICAL SURVEY CIRCULAR 772-B 1978 United States Department of the Interior CECIL D. ANDRUS, Secretary Geological Survey H. William Menard, Director Free on application to Branch of Distribution, U.S. Geological Survey, 1200 South Eads Street, Arlington, VA 22202 CONTENTS Page Abstract. ___________________________ Bl Northern Alaska Continued Summary of important results _______________! Organic geochemistry of rocks from three Introduction. _______________________! NPRA wells, by Leslie B. Magoon and Statewide projects ____________________! George E. Claypool _____________B25 Mineral resources of Alaska, by Edward H. Release of NPRA (NPR-4) data, by Robert D. Cobb _________________1 Carter ______________________26 Landsat color mosaic of Alaska, by Nairn R. D. Fossil reconnaissance study, eastern NPRA, Albert, Wm. Clinton Steele, and James R. by Charles A. Repenning____________ 27 LeCompte ____________________! Reconnaissance snow survey of NPRA, April Landsat data interpretation of various AM- 1977, by Charles E. Sloan, Dennis Trabant, RAP quadrangles, Alaska by Nairn R. D. Al and William Glude _ ___ ____ ____ 28 bert, Wm. Clinton Steele and James R. Hydrologic reconnaissance of lakes in NPRA, LeCompte ____________________4 1977, by Charles E. Sloan and Richard F. Geochemical exploration studies in Alaska, by Snyder ______________________28 G. C. Curtin, T. D. Hessin, R. M. O'Leary, E. Streamflow in NPRA, 1977, by S. H. Jones _ _ 29 F. Cooley, G. W. Day, and R. B. Tripp _ _ _ 5 Development and operation of gas fields in the Streamflow and channel erosion investigations South Barrow area, by Robert D. -
Mineralogy of Platinum-Group Elements and Gold in the Ophiolite-Related Placer of the River Bolshoy Khailyk, Western Sayans, Russia
minerals Article Mineralogy of Platinum-Group Elements and Gold in the Ophiolite-Related Placer of the River Bolshoy Khailyk, Western Sayans, Russia Andrei Y. Barkov 1,*, Gennadiy I. Shvedov 2, Sergey A. Silyanov 2 and Robert F. Martin 3 1 Research Laboratory of Industrial and Ore Mineralogy, Cherepovets State University, 5 Lunacharsky Avenue, 162600 Cherepovets, Russia 2 Institute of Mining, Geology and Geotechnology, Siberian Federal University, 95 Avenue Prospekt im. gazety “Krasnoyarskiy Rabochiy”, 660025 Krasnoyarsk, Russia; [email protected] (G.I.S.); [email protected] (S.A.S.) 3 Department of Earth and Planetary Sciences, McGill University, 3450 University Street, Montreal, QC H3A 0E8, Canada; [email protected] * Correspondence: [email protected]; Tel.: +7-8202-51-78-27 Received: 21 May 2018; Accepted: 5 June 2018; Published: 12 June 2018 Abstract: We describe assemblages of platinum-group minerals (PGM) and associated PGE–Au phases found in alluvium along the River Bolshoy Khailyk, in the western Sayans, Russia. The river drains the Aktovrakskiy ophiolitic complex, part of the Kurtushibinskiy belt, as does the Zolotaya River ~15 km away, the site of other placer deposits. Three groups of alloy minerals are described: (1) Os–Ir–Ru compositions, which predominate, (2) Pt–Fe compositions of a Pt3Fe stoichiometry, and (3) Pt–Au–Cu alloys, which likely crystallized in the sequence from Au–(Cu)-bearing platinum, Pt(Au,Cu), Pt(Cu,Au), and PtAuCu2, to PtAu4Cu5. The general trends of crystallization of PGM appear to be: [Os–Ir–Ru alloys] ! Pt3Fe-type alloy (with inclusions of Ru-dominant alloy formed by exsolution or via replacement of the host Pt–Fe phase) ! Pt–Au–Cu alloys. -
North America Summary, 1968
240 CLIMBS A~D REGIONAL ?\OTES North America Summary, 1968. Climbing activity in both Alaska and Canada subsided mar kedly from the peak in 1967 when both regions were celebrating their centen nials. The lessened activity seems also to have spread to other sections too for new routes and first ascents were considerably fewer. In Alaska probably the outstanding climb from the standpoint of difficulty was the fourth ascent of Mount Foraker, where a four-man party (Warren Bleser, Alex Birtulis, Hans Baer, Peter Williams) opened a new route up the central rib of the South face. Late in June this party flew in from Talkeetna to the Lacuna glacier. By 11 July they had established their Base Camp at the foot of the South face and started up the rib. This involved 10,000 ft of ice and rotten rock at an angle of 65°. In the next two weeks three camps were estab lished, the highest at 13,000 ft. Here, it was decided to make an all-out push for the summit. On 24 July two of the climbers started ahead to prepare a route. In twenty-eight hours of steady going they finally reached a suitable spot for a bivouac. The other two men who started long after them reached the same place in ten hours of steady going utilising the steps, fixed ropes and pitons left by the first party. After a night in the bivouac, the two groups then contin ued together and reached the summit, 17,300 ft, on 25 July. They were forced to bivouac another night on the return before reaching their high camp. -
The Placer Gold Mining Game
The Placer Gold Mining Game Game designed by Rob Chapman, School of Earth and Environment, University of Leeds. Software designed by Matt Bindoff, Bindoff Media Top: Preparing to mine gold-bearing gravel in Sulphur Creek, Klondike District Yukon Canada. Below: a portable sluice retains the gold in the riffles Overview Welcome to this interactive computer game in which you get to make the decisions made by real placer miners. When you play the game there are instructions which provide you with various options and tell you what you can and cannot do. To give yourself the best chance at the game you have to understand something about placer gold: how it occurs, how you find out if there is any there at all and how you can recover it. The object of the game, (of course) is to make as much profit as you can. You gain cash by selling the gold that you recover, but everything that you do to find, mine and separate the gold from the gravel cost you either time, money, or both. As far as possible we have made the game faithful to the real activity, so that you can make the same decisions and be faced with the same challenges that real placer miners encounter. However any real placer miners who have a go will quickly realize that we have had to make some simplifications to make the game workable in an educational context, (such as large claim sizes and a very understanding bank manager!) The key elements of the game can be summarized as follows: 1. -
Subject Index
Subject Index NOTE: This index lists Abrams, Pete 21:3 Lands Conservation Act Aleutian Islands 1:4, 3:2, 21:2, 22:2, 23:2 Barnette, E.T. 22:1 most of the subjects Active, John 6:3 (ANILCA) 8:4, 18:3, 3:4, 5:4, 7:2, 7:3, 9:1, Arctic 3:2, 5:4, 6:2, 7:2, Barren Islands 19:3 Adak Island 7:3, 22:2, 19:3, 20:2, 20:3 10:3, 13:2, 18:2, 18:4, 9:4, 12:1,12:4, 13:2, Barrow 1:1, 5:4, 16:2, and people The Alaska 22:4 Alaska Native Arts and 19:2, 21:1, 21:3, 21:4, 20:3 19:2, 21:3, 25:4 Geographic Society has Admiralty Island 1:3, 5:2, Crafts 6:1, 6:3, 7:3, 8:3, 22:2, 22:4, 24:4, 25:4 Arctic Circle 7:1, 7:2, Barter Island 16:2, 20:3 covered in its first 100 7:2, 8:4, 18:3, 20:2, 9:2, 11:3, 12:3, 16:2, Aleutian Islands National 10:4 Bats 8:2, 19:3 issues. The numbers 20:4 17:3, 17:4, 20:2, 21:2, Wildlife Refuge 22:2 Arctic National Wildlife Bears 1:3, 3:4, 4:3, 8:2, (for example, 21:3) Adney, Edwin Tappan 21:4, 22:2, 23:2 Aleutian Range 9:1 Refuge 4:2, 16:2, 19:2, 9:2, 12:4, 15:3, 15:4, 19:1 Alaska Native Claims Alexandrovski 17:1 20:3, 20:4, 23:3 16:1, 17:3, 18:3, 19:2, refer to the Volume and Afognak (community) Settlement Act Alsek River 2:4, 25:2 Arctic Ocean 5:4, 16:2 19:3, 20:2, 20:3, 20:4, Number of the issue 4:3, 19:3 (ANCSA) 3:2, 4:4, 6:3, Alutiiq 12:3, 21:2, 23:2 Arctic Village 7:1, 20:3 21:1, 21:2, 21 :4, 23:4 containing that subject. -
DEPARTMENT of the INTERIOR in the SERIES of U.S. GEOLOGICAL SURVEY CIRC(Ilbgs
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY BIBLIOGW.PEY AlUl INDEX OF ARTICLES IN THE SERIES OF U.S. GEOLOGICAL SURVEY CIRC(ILBgS DEVOTED TO CZOLOGIC RESKBBCE AND ACCOMPLISBWE~S LN BLASu 1975-1986 Compiled by Katherine M. Reed 1 and Jane K. Marks 2 OPEN-FILE REPORT 87-420 This report is preliminary and has not been reviewed for conformity with Geological Survey editorial standards and stratigraphic nomenclature. 1 Washington Dept, of Natural Resources, Olympia, WA 98504 Anchorage, AK 99508 Page Introduction .......................................................1 Articles arranged alphabetically by author ......................... 7 Articles arranged regionally. then by subject matter Statewide .................................................... 37 Northern Alaska ..............................................41 West-central Alaska .......................................... 53 East-central Alaska .......................................... 59 Southwestern Alaska ..........................................65 Southern Alaska .............................................. 69 Southeastern Alaska ..........................................85 Offshore Alaska ..............................................95 Author index ..................................................... 101 1 . Map showing regions of Alaska used as the basis for geographic grouping of articles............................... 3 1 . U.S. Geological Survey circulars on Alaskan research 1975-1986 ..................................................... 2 2 . Regional