Mineral Resources Southeastern Alaska M.I.R.L
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Alaska Tideland Surveys
Alaska Tideland Surveys “Who, What, When, Where, How, Why” A Paper Presented at the th 37 Annual Alaska Surveying and Mapping Conference By Gerald Jennings, P.L.S., and Joe Kemmerer, P.L.S. February, 2002 State of Alaska Department of Natural Resources Division of Mining, Land and Water, Technical and Data Management 550 West 7th Ave, Suite 650 Anchorage, Alaska 99501-3576 (907) 269-8523 Fax (907) 269-8914 ii ABSTRACT Alaska Tideland Surveys – the 5 w’s. Surveys of tideland parcels are unique in several ways. Typically all corners are monumented with witness corners. DNR is usually the fee owner of the parcel, and the landward boundary is usually the mean high water line. Frequently, the line is fixed and limiting, because of avulsion, or placement of fill. This paper will briefly discuss how an applicant applies for a tideland lease or conveyance and how to conduct the survey and obtain state approval. Presenter: Gerald Jennings The Department of Natural Resources, Division of Mining, Land and Water, Technical and Data Management staff dealing with Alaska Tideland Surveys: Gerald Jennings, P.L.S., Statewide Platting Supervisor Joe Kemmerer, P.L.S., Coastal Boundary. William (Bill) Brown, P.L.S., Riparian Specialist iii Alaska Tideland Surveys Introduction – who what why? Title to most of the tide and submerged lands surrounding Alaska was vested in the State of Alaska under the Submerged Lands Act of May 22, 1953. Most of those lands remain in state ownership and in most cases, the state will lease, but retain fee title. As a surveyor, you will be contacted about Alaska Tideland Surveys (ATS) by a public or private party who desires to lease or acquire tidelands for various reasons such as construction of docks, bridges, harbors, log transfer facilities, etc. -
Formation of Chrysocolla and Secondary Copper Phosphates in the Highly Weathered Supergene Zones of Some Australian Deposits
Records of the Australian Museum (2001) Vol. 53: 49–56. ISSN 0067-1975 Formation of Chrysocolla and Secondary Copper Phosphates in the Highly Weathered Supergene Zones of Some Australian Deposits MARTIN J. CRANE, JAMES L. SHARPE AND PETER A. WILLIAMS School of Science, University of Western Sydney, Locked Bag 1797, Penrith South DC NSW 1797, Australia [email protected] (corresponding author) ABSTRACT. Intense weathering of copper orebodies in New South Wales and Queensland, Australia has produced an unusual suite of secondary copper minerals comprising chrysocolla, azurite, malachite and the phosphates libethenite and pseudomalachite. The phosphates persist in outcrop and show a marked zoning with libethenite confined to near-surface areas. Abundant chrysocolla is also found in these environments, but never replaces the two secondary phosphates or azurite. This leads to unusual assemblages of secondary copper minerals, that can, however, be explained by equilibrium models. Data from the literature are used to develop a comprehensive geochemical model that describes for the first time the origin and geochemical setting of this style of economically important mineralization. CRANE, MARTIN J., JAMES L. SHARPE & PETER A. WILLIAMS, 2001. Formation of chrysocolla and secondary copper phosphates in the highly weathered supergene zones of some Australian deposits. Records of the Australian Museum 53(1): 49–56. Recent exploitation of oxide copper resources in Australia these deposits are characterized by an abundance of the has enabled us to examine supergene mineral distributions secondary copper phosphates libethenite and pseudo- in several orebodies that have been subjected to intense malachite associated with smaller amounts of cornetite and weathering. -
Gossans and Leached Cappings
Gossans and Leached Cappings Roger Taylor Gossans and Leached Cappings Field Assessment Roger Taylor Townsville Queensland 4810 Australia [email protected] ISBN 978-3-642-22050-0 e-ISBN 978-3-642-22051-7 DOI 10.1007/978-3-642-22051-7 Springer Heidelberg Dordrecht London New York Library of Congress Control Number: 2011934477 © Springer-Verlag Berlin Heidelberg 2011 This work is subject to copyright. All rights are reserved, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilm or in any other way, and storage in data banks. Duplication of this publication or parts thereof is permitted only under the provisions of the German Copyright Law of September 9, 1965, in its current version, and permission for use must always be obtained from Springer. Violations are liable to prosecution under the German Copyright Law. The use of general descriptive names, registered names, trademarks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. Typesetting & Prepress: Elisabeth Sillmann, Landau, www.blaetterwaldDesign.de Cover design: deblik, Berlin Printed on acid-free paper Springer is part of Springer Science+Business Media (www.springer.com) Acknowledgements iven a 30–40 years germination period, it is not surprising that the list of con- tributors is considerable, and it is not feasible to list the input of every student, G colleague, and professional geologist. Th ank you everybody. -
Deposits of Manganese Ore in Arizona
DEPOSITS OF MANGANESE ORE IN ARIZONA. By E. L. JONES, Jr., and F. L. RANSOME. INTRODUCTION. By E. L. JONES, Jr. FIELD WORK. Deposits of manganese ore have long been known in some of the old mining districts of Arizona, notably in the Bisbee, Tombstone, Globe, and Patagonia districts, but prior to 1915 the ore had not been mined except as it formed the gangue of silver ores and was needed as a flux for use in local smelters. Manganese ore as such was first shipped from the Tombstone district in 1915, and from the Globe and Bisbee districts in 1916. The high prices that were offered, for manganese ore in 1916, 1917, and 1918, and the fact that the opening of the new deposits would render the Government patriotic service greatly stimulated the production of the ore and the search' for new deposits. As a result of this search discoveries in many parts of the State have been reported to Government bureaus from time to time. In order to obtain information concerning these newly discovered deposits, their character and grade of ore, ore reserves, and pro ductive capacity, two geologists of the United States Geological Survey examined manganese deposits in Arizona, E. L. Jones, jr., visiting many scattered deposits throughout the State, > and F. L. Ransome those of the Bisbee and Tombstone districts. The work of Mr. Jones was done in August and September, 1917, and in April, May, and June, 1918. It was geologic reconnaissance work, and generally not more than a few hours could be devoted to the examination of each deposit. -
THE GOSSAN LEAD, CARROLL COUNTY, VIRGINIA R. J. Wright, and N. D. Raman U. S. Geological Survey
THE GOSSAN LEAD, CARROLL COUNTY, VIRGINIA R. J. Wright, and N. D. Raman U. S. Geological Survey /?*! Co JO V . CONTENTS Manuscript Page Abstract .............................. 1 Introduction ............................ 1 History ............................ 2 Geology .... .......................... 3 Structure .............................. 4 Mineralogy ............................. 5 Secondary Copper Enrichment ................... 6 Description of Individual segments ................ 8 Betty Baker segment ....... .............. 9 Little Vine segment ..............."...... 9 Little Reed Island segment. ................. 10 Cranberry segment ...................... 11 Wild Cat segment ....................... 12 Sarah Ellen segment ..................... 13 Copperas Hill segment .................... 14 Chestnut Creek segment ................... 14 Dalton Hill area ........................ 16 The Great Outburst ..................... 16 Minor deposits in Carroll and Grayson Counties ......... 17 Ore reserves ............................ 18 Secondary copper ore ..................... 18 Gossan iron ore ........................ 19 Primary sulfide ore ..................... 19 ii. LIST OF ILLUSTRATIONS Figure 1. Index map of Gossan Lead, Carroll County, Virginia. 2. Goasan Lead, Carroll County, Virginia. 3. Northeast end of the Betty Baker segment, Gossan Lead. 4. Sections of diamond drill holes, northeast end Betty Baker segment, Gossan Lead. 5. Structure countour map northeast end of the Betty Baker segment, Gossan Lead. 6. Northeast end of the -
Nesting Ecology of Marbled Murrelets at a Remote Mainland Fjord in Southeast Alaska
Nesting ecology of Marbled Murrelets at a remote mainland fjord in southeast Alaska Barbaree, B. A., Nelson, S. K., Dugger, B. D., Roby, D. D., Carter, H. R., Whitworth, D. L., & Newman, S. H. (2014). Nesting ecology of Marbled Murrelets at a remote mainland fjord in southeast Alaska. The Condor, 116(2), 173-184. doi:10.1650/CONDOR-13-116.1 10.1650/CONDOR-13-116.1 Cooper Ornithological Society Version of Record http://cdss.library.oregonstate.edu/sa-termsofuse Volume 116, 2014, pp. 173–184 DOI: 10.1650/CONDOR-13-116.1 RESEARCH ARTICLE Nesting ecology of Marbled Murrelets at a remote mainland fjord in southeast Alaska Blake A. Barbaree,1,a* S. Kim Nelson,2 Bruce D. Dugger,1 Daniel D. Roby,2 Harry R. Carter,3 Darrell L. Whitworth,4 and Scott H. Newman 5 1 Department of Fisheries and Wildlife, Oregon State University, Corvallis, Oregon, USA 2 U.S. Geological Survey Oregon Cooperative Fish and Wildlife Research Unit, Department of Fisheries and Wildlife, Oregon State University, Corvallis, Oregon, USA 3 Carter Biological Consulting, Victoria, British Columbia, Canada 4 California Institute of Environmental Studies, Davis, California, USA 5 EMPRES Wildlife Unit, Emergency Centre for Transboundary Animal Diseases, Animal Health Division, FAO of the United Nations, Rome, Italy a Current address: Point Blue Conservation Science, Petaluma, California, USA * Corresponding author: [email protected] Received December 11, 2013; Accepted December 12, 2013; Published February 19, 2014 ABSTRACT Studying the ecology of endangered species in portions of their range where the population remains abundant can provide fundamental information for conservation planners. -
Stephens Passage
254 ¢ U.S. Coast Pilot 8, Chapter 9 19 SEP 2021 134°W Chart Coverage in Coast Pilot 8—Chapter 9 NOAA’s Online Interactive Chart Catalog has complete chart coverage 17300 http://www.charts.noaa.gov/InteractiveCatalog/nrnc.shtml 135°W L 17316 Y N N C A N A L UNITED STCANADA ATES 17315 T Juneau E L N DOUGLAS I ISLAND U K A T I C Y S T R A I T 17313 A 17314 D 58°N M I S R T 17360 E A P H L 17300 E T N S C Y 17311 H P A A S T S H 17363 A I A 17362 WINDHAM BAY G M S E L S T GAMBIER BAY A R A HOBART BAY N I T D PYB PORT HOUGHTON US B AY 17363 17365 I C K S O F R E D E R U N D 19 SEP 2021 U.S. Coast Pilot 8, Chapter 9 ¢ 255 Stephens Passage (1) This chapter describes Stephens Passage, Holkham during the winter, reaching its maximum in January. Bay, Endicott Arm, Tracy Arm, Taku Harbor, Gastineau The least fog occurs during April to July, inclusive, the Channel, Auke Bay, Tee Harbor and the city of Juneau, minimum being in May. including the communities of Douglas and Auke Bay. (10) (2) Ice ENC - US2AK30M (11) Ice is discharged from glaciers in Tracy and Endicott Chart - 16016 Arms, is always found in Holkham Bay and is prevalent in Stephens Passage off the entrance to that bay. -
Metavolcanic Host Rocks, Mineralization, and Gossans of The
International Geology Review ISSN: 0020-6814 (Print) 1938-2839 (Online) Journal homepage: http://www.tandfonline.com/loi/tigr20 Metavolcanic host rocks, mineralization, and gossans of the Shaib al Tair and Rabathan volcanogenic massive sulphide deposits of the Wadi Bidah Mineral District, Saudi Arabia John C. Volesky, Matthew I. Leybourne, Robert J. Stern, Jan M. Peter, Daniel Layton-Matthews, Sarah Rice & Peter R. Johnson To cite this article: John C. Volesky, Matthew I. Leybourne, Robert J. Stern, Jan M. Peter, Daniel Layton-Matthews, Sarah Rice & Peter R. Johnson (2017) Metavolcanic host rocks, mineralization, and gossans of the Shaib al Tair and Rabathan volcanogenic massive sulphide deposits of the Wadi Bidah Mineral District, Saudi Arabia, International Geology Review, 59:16, 1975-2002, DOI: 10.1080/00206814.2017.1307789 To link to this article: http://dx.doi.org/10.1080/00206814.2017.1307789 View supplementary material Published online: 04 Apr 2017. Submit your article to this journal Article views: 58 View related articles View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=tigr20 Download by: [The University of Texas at Dallas] Date: 03 October 2017, At: 06:07 INTERNATIONAL GEOLOGY REVIEW, 2017 VOL. 59, NO. 16, 1975–2002 https://doi.org/10.1080/00206814.2017.1307789 Metavolcanic host rocks, mineralization, and gossans of the Shaib al Tair and Rabathan volcanogenic massive sulphide deposits of the Wadi Bidah Mineral District, Saudi Arabia John C. Voleskya, Matthew I. Leybourneb, Robert J. Sterna, Jan M. Peterc, Daniel Layton-Matthewsd, Sarah Ricee and Peter R. -
Technical Report for the Greens Creek Mine, Juneau, Alaska, Usa
TECHNICAL REPORT FOR THE GREENS CREEK MINE, JUNEAU, ALASKA, USA NI 43-101 Report Qualified Persons: Paul Jensen, M.Sc., C.P.G. Dean McDonald, Ph.D., P. Geo. Kyle Mehalek, M.Sc., P.E. Keith Blair, M.Sc., C.P.G. Bill Hancock, R.M., S.M.E., QP MMSA. M. Dale Butikofer, P.E. Paul Glader, M.Sc., M.B.A., P.E. Effective Date: December 31, 2018 Filed: April 1, 2019 CAUTIONARY STATEMENT ON FORWARD-LOOKING INFORMATION This Technical Report contains forward-looking statements within the meaning of the U.S. Securities Act of 1933 and the U.S. Securities Exchange Act of 1934 (and the equivalent under Canadian securities laws), that are intended to be covered by the safe harbor created by such sections. Such forward-looking statements include, without limitation, statements regarding the Company’s expectation of the Greens Creek Mine and its expansions, including estimated capital requirements, expected production, cash costs and rates of return; mineral reserve and mineral resource estimates; estimates of silver, lead and zinc grades; and other statements that are not historical facts. We have tried to identify these forward-looking statements by using words such as “may,” “might”, “will,” “expect,” “anticipate,” “believe,” “could,” “intend,” “plan,” “estimate” and similar expressions. Forward-looking statements address activities, events or developments that Hecla Mining Company expects or anticipates will or may occur in the future and are based on information currently available. All forward-looking statements in this Technical Report are necessarily based on opinions and estimates made as of the date such statements are made and are subject to important risk factors and uncertainties, many of which cannot be controlled or predicted. -
Investigations of Gossans of Hot Springs Dome, Near Manley Hot Springs, Alaska
INVESTIGATIONS OF GOSSANS OF HOT SPRINGS DOME, NEAR MANLEY HOT SPRINGS, ALASKA by Raymond P. Maloney * * * * * * * * * * * * * * * * * * * * * * open-file report UNITED STATES DEPARTMENT OF THE INTERIOR Dr. Rogers C. B. Morton, Secretary BUREAU-OF MINES Dr. Elburt F. Osborn, Director 2 CONTENTS Abstract Introduction Acknowledgments. 4 Location and accessibility..6 6 6 History and ownership. .. 76. Physical features and climate. .. Description of the deposit . General geology 9 The deposits. Work performed by the 9 Bureau of Mines.. Mechanical operations .12 .. 12 Exploratory operations. Appendix 13 14 A-~~~~~~~~~~~~~~~~~~~~~~~~~ 3 ILLUSTRATIONS Fig Follows Page 1. Index Map of Alaska. .6 . 2. Location map, Hot Springs Dome, Alaska . 6 3. Geologic map of the Manley Hot Springs and Rampart District, Central Alaska . 4. Geologic and topographic map of Hot Springs Dome, Alaska . .. 5. Geologic section of drill hole 1 7 . 13 6. Geologic section of drill hole 2 ...... 13 7. Geologic section of drill hole 3 . 13 8. Geologic section of drill hole 4 . 13 9. Geologic section of drill hole 5 .. 13 10. Geologic section of drill hole 6....... ... .. 13 11. Geologic section of drill hole 7 . 13 12. Geologic section of drill hole 8 . 13 TABLES Page 1. Summary of surface sampling data . 25 2. Summary of diamond core drill sampling data. 26 4 INVESTIGATIONS OF GOSSANS ON HOT SPRINGS DOME, NEAR MANLEY HOT SPRINGS, ALASKA by Raymond P. Maloneyl/ ABSTRACT Prominent gossans on the summit of Hot Springs Dome were investigated during 1953-54 to determine whether commercially valuable metal sulfides were below the zone of oxidation. The gossan-capped zones are 100 to 500 feet long and 20 to 50 feet wide in metamorphosed sedimentary rocks near their contact with a large body of granitic intrusives. -
Iberian Pyrite Belt): from Subaerial to Underground Conditions
Ore Geology Reviews 80 (2017) 377–405 Contents lists available at ScienceDirect Ore Geology Reviews journal homepage: www.elsevier.com/locate/oregeorev Mineralogical evolution of the Las Cruces gossan cap (Iberian Pyrite Belt): From subaerial to underground conditions Lola Yesares a,⁎, Reinaldo Sáez a, Gabriel Ruiz De Almodóvar a,JoséMiguelNietoa, Carmelo Gómez b, Gobain Ovejero c a Department of Earth Sciences, University of Huelva, Avenida de las Fuerzas Armadas, S/N, 21071 Huelva, Spain b Geological Area, Mining Drepartment of Cobre Las Cruces S.A., Ctra. SE-3410, Km 41,100, 41860 Gerena, Seville, Spain c Cobre Las Cruces S.A., Ctra. SE-3410, Km 41,100, 41860 Gerena, Seville, Spain article info abstract Article history: The Las Cruces VMS deposit is located at the eastern corner of the Iberian Pyrite Belt (SW Spain) and is overlain by Received 13 November 2015 the Neogene–Quaternary sediments of the Guadalquivir foreland Basin. The deposit is currently exploited from Received in revised form 16 May 2016 an open pit by Cobre Las Cruces S.A., being the supergene Cu-enriched zone the present mined resource. The Accepted 20 May 2016 Las Cruces orebody is composed of a polymetallic massive sulfide orebody, a Cu-rich stockwork and an overlying Available online 1 June 2016 supergene profile that includes a Cu-rich secondary ore (initial reserves of 17.6 Mt @ 6.2% Cu) and a gossan cap (initial reserves of 3.6 Mt @ 3.3% Pb, 2.5 g/t Au, and 56.3 g/t Ag). Keywords: fi Massive sulfide deposit The mineralogy of the Las Cruces weathering pro le has been studied in this work. -
Inventory and Cataloging of the Sport Fish Waters in Southeast Alaska
Volume 14 Study No. G-I Job No. G-I-A STATE OF ALASKA WilliamA. Egan, Governor Annual Progress Report for Inventory and Cataloying of the Sport Fish and Sport Fish Waters in Southeast Alaska by Artwin Schmidt, Stuart Robards, and Michael McHugh ALASKA DEPARTMENT OF FISH AND GAME James W. Brooks, Commissioner DIVISION OF SPORT FISH Rupert E. Andrews, Director Howard E. Metsker, Coordinator IN MEMORIAM l\1ike McHugh was born in Port Angeles, Washington, on September 24, 1935. He graduated from Columbia High School in Richland, Washington, in 1953. In Aug ust of 1953, he entered the U. S. Air Force where he served until 1957 , when he re ceived an honorable discharge. From 1957 to 1962, Mike attended Riverside College, and Humboldt State College in California, receiving his Bachelor of Arts in zoology from the latter. He was employed by the If. S. Fish & Wildlife Service, as a Fish ery Biologist at LUdington, Michigan, from 1962 to 1964, where he was engaged in the lamprey control program . Mike joined the Alaska Department of Fish and Game in June, 1964, as a Fishery Biologist, with the Commer cial Fisheries Division. Mike first served as Assistant Area Management Biologist, then transferred to pink salmon research. In September, 1969, he transferred to the Sport Fish Division, where he was appointed Upper Southeast Area Management Biologist. He served in this position until his death on July 29, 1973. Mike was a member of the American Institute of Fishery Research Biologists, the American Fisheries Society, and member and founder of the Juneau Rifle and Pistol Club.