Chromite-Bearing Sands of the Southern Part of the Coast of Oregon

Total Page:16

File Type:pdf, Size:1020Kb

Chromite-Bearing Sands of the Southern Part of the Coast of Oregon UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. E. Wrather. Director Bulletin 945-E CHROMITE-BEARING SANDS OF THE SOUTHERN PART OF THE COAST OF OREGON BY ALLAN B. GRIGGS Strategic Minerals Investigations, 1944 (Pages 113-150) UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1945 For «ale by the Superintendent of Documents, U. S. Government Printing Office, Waehington 25, D. C. Price 55 cents CONTENTS Page Abstract ................................................... 113 Introduction ............................................... 113 Location ............................................... 113 Access and transportation .............................. 114 History ................................................ 115 Field work and acknowledgments ......................... 116 Geology .................................................... 116 General features ....................................... 116 Geology of terraces .................................... 117 Chromiferous sand deposits ................................. 118 General character ...................................... 118 Mineralogy ............................................. 119 Origin and distribution ................................ 122 Reserves ............................................... 125 Mining areas ............................................... 127 South Slough region .................................... 127 Explored deposit ................................... 128 N^SWi sec. 36, T. 26 S., R. 14 W. .............. 128 Other occurrences .................................. 128 NEiNE* sec. 13, T. 26 S., R. 14 W. ............. 128 SWiNEi sec. 36, T. 26 S., R. 14 W. ............. 128 Chickamin mine ................................. 128 sec. 25, T. 26 S., R. 14 W. ................. 129 sec. 36, T. 26 S., R. 14 W. ................ 129 sec. 36, T. 26 S., R. 14 W. .............. 129 sec. 1, T. 27 S., R. 14 W. ................. 129 Terrace area north of Coquille River ................... 129 Explored deposits on the Seven Devils terrace ...... 130 Section 33 deposit ............................. 130 Section 4 deposit .............................. 132 Seven Devils (Last Chance) mine ................ 132 Other occurrences on the Seven Devils terrace ...... 135 NEj sec. 5, T. 27 S., R. 14 W. ................. 135 sec. 3 and NE£ sec. 4, T. 27 S., R. 14 W.,... 135 sec. 4, NE£ sec. 9, NW£ sec. 10, T. 27 S., R. 14 W ...................................... 136 sec. 10 and NW£ sec. 15, T. 27 S., R. 14 Vt . 136 Near center sec. 15, T. 27 S., R. 14 H, ......... 137 Explored deposits on the Pioneer terrace ........... 137 Shepard mine ................................... 137 Rose mine ...................................... 138 Eagle and Pioneer mines ........................ 138 The Lagoons .................................... 140 Other occurrences on Pioneer terrace ............... 141 Kendall mine ................................... 141 Coquille (Norman) mine ......................... 141 SE$ sec. 27, T. 27 S., R. 14 W. ................. 141 Random exploration on the Pioneer terrace .......... 141 Occurrence on Whisky Run terrace ................... 141 Pivemile Point ................................. 141 Terrace area east and south of Bandon .................. 142 Explored depos it ................................... 142 Geiger (Little) mine ........................... 142 III TV CONTENTS Page Mining areas Continued Terrace area east and south of Bandon Continued Other occurrences .................................. 142 Iowa mine ...................................... 142 Prospect 2,000 feet south of the Iowa mine ..... 143 NW£ sec. 9, T. 29 S., R. 14 W. ................. 143 NiSEi sec. 32, T. 28 S., R. 14 W. .............. 143 Pits on Crooked Creek ......°.................... 143 Denmark area ........................................... 143 Explored deposit ................................... 144 Butler (Baker) mine ............................ 144 Other occurrences .................................. 144 NW£ sec. 34, and SWi sec. 27, T. 31 S., R. 15 W. ........................................ 144 Madden mine .................................... 145 Rogue River area ....................................... 145 TSk sec. 12, T. 36 S., R. 15 W. ..................... 145 NWfc sec. 13, T. 36 S., R. 15 W. .................... 145 Present beaches ............................................ 145 General character of beaches ........................... 145 Beach deposits ......................................... 146 Beach at mouth of Fivemile Creek ................... 146 Beach at mouth of Threemile Creek .................. 146 Beach at mouth of Twomile Creek .................... 147 Beach at mouth of Johnson Creek .................... 147 Black sand occurrences in the beach near the mouth of China Creek ................................... 147 Cape Blanco beach .................................. 147 Ophir beach ........................................ 147 Rogue River beach .................................. 147 Annotated bibliography ..................................... 148 ILLUSTRATIONS Page Plate 41. Map of southwestern Oregon, showing distribution of terrace deposits containing principal chro- mite concentrations and probable sources of the chromite in them..................... In pocket 42. Geologic map of parts of the Empire and Bandon quadrangles, showing distribution of terrace deposits and chromiferous sands.......... In pocket 43. Map of the southwest coast of Oregon between the 42°20» and 43* parallels, showing distribution of chromiferous sands and upper limit of lower coastal terraces......................... In pocket 44. Exploration map and section of Section 33 chro­ miferous sand deposit.................... In pocket 45. Map and sections of the Section 4 deposit.. In pocket 46. Map and sections of the Seven Devils mine.. In pocket 47. Map and sections of the Shepard mine....... In pocket 48. Plan and section of the Rose mine.......... In pocket 49. Map and sections of the Eagle and Pioneer mines.................................... In pocket 50. Map and sections of the Butler (Baker) mine. In pocket 51. Sketch maps showing deposits of chromiferous sand in the beaches between Coos Bay and Rogue River............................... In pocket ILLUSTRATIONS V Page Figure 11. Index map of Oregon, showing locations of chromiferous sand deposits ................... 114 12. Diagrammatic sketch of layering in sand in tunnel at the Shepard mine ................... 120 13. Diagrammatic sketch of the eastern edge of the black sand deposit at the Seven Devils mine .. 134 TABLES Table 7. Partial analyses of black sands from the ter­ race area north of Coquille River ............ 121 8. Minerals in black sand deposits in the terrace area north of Coquille River ................. 122 9. Proportions of minerals in black sands from several localities, determined by count of 200 grains from each sample .................. 123 10. Percentages of magnetite, ilmenite, chromite, and zircon in samples from the black sands ... 124 CHROMITE-BEARING SANDS OF THE SOUTHERN PART OF THE COAST OF OREGON By Allan B. Griggs ABSTRACT Chromiferous sands, commonly known as "black sands" because of their color, are found both in the present beaches and on raised marine terraces along the southern Oregon coast in Coos and Curry Counties. Most of the deposits are on the lower ter­ races between Cape Arago and the town of Port Orford, and in the South Slough region. The black sand occurs in layers and lenses that range in thickness from a few inches to 42 feet, in width from a few tens of feet to more than 1,000 feet, and in length from a few hundred feet to a mile or more. The deposits on the terraces are covered with 1 to 75 feet of sand, clay, and gravel. The deposits in the present beaches are transitory, varying from year to year, and were smaller than usual and remained relative­ ly unchanged in 1942 and 1943. Besides chromite, other minerals common in the black sands include quartz, olivine, pyroxene, zir­ con, ilmenite, rutile, garnet, magnetite and epidote. Zircon constitutes 1 to 2 percent of most of the deposits, and is of definite commercial interest. Gold and platinum are present in minute quantities. The known reserves of measurable and indicat­ ed ore, minus what was mined in 1943, are 1,913,000 long tons of sand in deposits averaging more than 5 percent chromic oxide (CrgOg), and 1,212,000 long tons of sand in deposits averaging between 3 and 5 percent chromic oxide. It is estimated that 100,000 long tons of sand in the present beaches contain 5 per­ cent or more CrgO-j. The reserves in many of the deposits can be substantially increased with more detailed exploration, and other favorable regions are as yet unexplored. In 1943, two plants (one owned by Humphreys Gold Corporation and the other by Krome Corporation) began making rough chromite concentrations which were treated in a third plant constructed by the Defense Plant Corporation to produce chromite concentrates containing about 40 percent CrgOj. INTRODUCTION Location Concentrations of chromiferous sands are found in the present beaches and on marine terraces along the southern coast of Oregon. These deposits are commonly called "black sands", because of their dark gray and brown to black colors, which are due in part to the predominance of the black minerals chromite ((Fe,Mg)0.(Cr,Al,Fe)2 03), magnetite (FeFegO^, and ilmenite (PeTiOs), and in part to 113 114 STRATEGIC MINERALS INVESTIGATIONS,
Recommended publications
  • Hawaiian Volcanoes US$1225
    The Geological Society of America’s Explore Hawaiian Volcanoes FIELD EXPERIENCE 27 July - 4 August 2014 Experience the wonders of active volcanism on the Earth’s most accessable and active volcano - Kilauea on the Big Island of Hawaii! This eight-day field trip on the Big Island of Hawaii will expand your knowl- edge in the field of plate tectonics, hot spot volcanism and the geologic features and hazards associated with living on an active volcano. We will discuss volcanic edifices, eruption styles, magma evolution and see various types of lava flows, lava lakes, tree molds and lava trees, fault scarps, rifts, craters and calderas. We will use our observations and new- found knowledge to discuss methods on how to effectively communicate geologic concepts. We will model inquiry in the field. US Prince does not include$1225 airfares to/from Hilo, HI. Trip ITINERARY* Sunday, July 27 - Participants arrive in Hilo, Hawaii for transfer via van to Kilauea Military Camp. No meals pro- vided. We will go to dinner as a group at Ken’s House of Pancakes (at your own expense) Monday, July 28 - Overview/logistics, Kilauea Visitor Center, Steaming Bluffs, Sulphur Banks, Kilauea Overlook, HVO, Jaggar Museum, SW Rift, Halema’uma’u Overlook (if open), Keanakako’I overlook, Devastation Trail, Pu’u Pua’i Overlook. ~ 4 miles of hiking on easy trails. BLD. Tuesday, July 29 - Chain of Craters Road including stops at Lua Manu Crater, Pauahi Crater and others, Mauna Ulu trail to Pu’u Huluhulu, Kealakomo Overlook, Alanui Kahiko, P’u Loa Petroglyphs, Holei Sea Arch, end of Chain of Craters Road.
    [Show full text]
  • Compilation of Reported Sapphire Occurrences in Montana
    Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area ....................................
    [Show full text]
  • COMPARATIVE STUDIES on the BLACK SAND CONCENTRATES of SOUTH INDIA by Dr
    COMPARATIVE STUDIES ON THE BLACK SAND CONCENTRATES OF SOUTH INDIA BY Dr. E. A. V. PRASAD [Department oJ Geology, Sri Venkateswara University, Tirupati (A.P.), Indic] Received June 24, 1971 (Communicated by Dr. K. Neelakantam, F.A.SC.) ABSTRACT Samples of the littoral and alluvial placer deposits of the black sand concentrates which contain radioactive resistate minerals were collected from various parts of South India and their characters with respect to colour, density and radioactivity were presented. With the aid of a hand magnet and a sensitive Frantz Isodynamic laboratory model Lj magnetic separator, each sample was subdivided into magnetic, paramagnetic and nonmagnetic components. The paramagnetic mineral assemblage was further subdivided into fractions of varying mass magnetic susceptibility. The amounts of these fractions constitute the frequency distribution of mass magnetic susceptibility, expressed in terms of current strength, of the sample whose character is ttien evaluated by means of certain standard statistical parameters. Variation in the characters with respect to grain size was also studied. Fm'ther, it is suggested that the amount of magnetite is an "Index of Maturity" for these residual deposits. THE voluminous black sand concentrates occurring along the East and West coasts of India, in a series of local concentrations, at favourable localities, constitute a thorium asset of world importance. These placer deposits contain the radioactive mineral, monazite, together with the other industrial minerals ilmenite, garnet, rutile, zircon, magnetite and leucoxene in varying proportions. Such placer deposits of radioactive resistate minerals have been reported from many parts of the world (Nininger,1954; United Nations, 1956; Heinrich, 1958).
    [Show full text]
  • ICELAND 2006 Geodynamics Field Trip May 30 – June 8, 2006
    ICELAND 2006 Geodynamics Field Trip May 30 – June 8, 2006 Massachusetts Institute of Technology/ Woods Hole Oceanographic Institution Joint Program in Oceanography This field trip guide was compiled by Karen L. Bice using information from Bryndís Brandsdóttir, Richard S. Williams, Helgi Torfason, Helgi Bjornsson, Oddur Sigurðsson, the Iceland Tourist Board and World W. Web Maps from Thordarson and Hoskuldsson, 2002, Iceland (Classic Geology in Europe 3), Terra Publishing, UK. Logistical genius: Andrew T. Daly Field trip participants: Mark Behn, Karen Bice, Roger Buck, Andrew Daly, Henry Dick, Hans Schouten, Martha Buckley, James Elsenbeck, Pilar Estrada, Fern Gibbons, Trish Gregg, Sharon Hoffmann, Matt Jackson, Michael Krawczynski, Christopher Linder, Johan Lissenberg, Andrea Llenos, Rowena Lohman, Luc Mehl, Christian Miller, Ran Qin, Emily Roland, Casey Saenger, Rachel Stanley, Peter Sugimura, and Christopher Waters The Geodynamics Program is co-sponsored by Woods Hole Oceanographic Institution’s Academic Programs Office and Deep Ocean Exploration Institute. TUESDAY May 30 Estimated driving (km) Meet at Logan Airport, Icelandair ticket counter @ 7:00 PM (80 km ≈ 50 mi) Depart BOS 9:30 PM Icelandair flight Day 1 - WEDNESDAY May 31 Arrive Keflavík International Airport 6:30 AM (flight duration 5 hours) Pick up 2 vans, 2 trailers (Budget) Free day in Reykjavík Night @ Laugardalur campground, Reykjavík Dinner: on own in town Day 2 - THURSDAY June 1 270 Late start due to trailer problems (2 hrs @ AVIS) To Þingvellir N.P., then north to Hvalfjörður fjord, stop at Skorradalsvatn Night @ Sæberg Hostel (1 km. off Rte 1 in Hrútafjörður, west side of road) Tel. 354-4510015 Fax. 354-4510034 [email protected] Dinner: mexican-style chicken (Rachel, Trish, Chris) Day 3 - FRIDAY June 2 320 To Lake Myvatn Lunch stop in Akureyri, stop at Godafoss, stop at Skutustadir pseudocraters Night @ Ferdathjonustan Bjarg campsite, Reykjahlid, on shore of Lake Myvatn Tel.
    [Show full text]
  • Study of Black Sand Particles from Sand Dunes in Badr, Saudi Arabia Using Electron Microscopy
    Atmosphere 2015, 6, 1175-1194; doi:10.3390/atmos6081175 OPEN ACCESS atmosphere ISSN 2073-4433 www.mdpi.com/journal/atmosphere Article Study of Black Sand Particles from Sand Dunes in Badr, Saudi Arabia Using Electron Microscopy Haider Abbas Khwaja 1,2,*, Omar Siraj Aburizaiza 3,*, Daniel L. Hershey 4, Azhar Siddique 3,5, David A. Guerrieri P. E. 4, Jahan Zeb 3, Mohammad Abbass 6, Donald R. Blake 7, Mirza Mozammel Hussain 1,2, Abdullah Jameel Aburiziza 8, Malissa A. Kramer 4 and Isobel J. Simpson 7 1 Wadsworth Center, New York State Department of Health, Albany, New York, NY 12201, USA; E-Mail: [email protected] 2 Department of Environmental Health Sciences, School of Public Health, University at Albany, Albany, New York, NY 12201, USA 3 Unit for AinZubaida and Groundwater Research, King Abdulaziz University, Jeddah 21589, Saudi Arabia; E-Mails: [email protected] (A.S.); [email protected] (J.Z.) 4 New York State Department of Environmental Conservation, 625 Broadway, Albany, New York, NY 12233, USA; E-Mails: [email protected] (D.L.H.); [email protected] (D.A.G.P.E.); [email protected] (M.A.K.) 5 Chemistry Department, University of Karachi, Karachi 75270, Pakistan 6 Civil Engineering Department, King Abdulaziz University, Jeddah 21589, Saudi Arabia; E-Mail: [email protected] 7 Department of Chemistry, University of California-Irvine, Irvine, CA 92697, USA; E-Mails: [email protected] (D.R.B.); [email protected] (I.J.S.) 8 School of Medicine, Umm Ul Qura University, Mecca 21955, Saudi Arabia; E-Mail: [email protected] * Authors to whom correspondence should be addressed; E-Mails: [email protected] (H.A.K.); [email protected] (O.S.A.); Tel.: +1-518-474-0516 (H.A.K.); +966-12-695-2821 (O.S.A.); Fax: +1-518-473-2895 (H.A.K.); +966-12-695-2499 (O.S.A.).
    [Show full text]
  • General Plan for the County of Hawai'i
    COUNTY OF HAWAI‘I GENERAL PLAN February 2005 Pursuant Ord. No. 05-025 (Amended December 2006 by Ord. No. 06-153, May 2007 by Ord. No. 07-070, December 2009 by Ord. No. 09-150 and 09-161, and June 2012 by Ord. No. 12-089) Supp. 1 (Ord. No. 06-153) CONTENTS 1: INTRODUCTION 1.1. Purpose Of The General Plan . 1-1 1.2. History Of The Plan . 1-1 1.3. General Plan Program . 1-3 1.4. The Current General Plan Comprehensive Review Program. 1-4 1.5. County Profile. 1-7 1.6. Statement Of Assumptions. 1-11 1.7. Employment And Population Projections . 1-12 1.7.1. Series A . 1-13 1.7.2. Series B . 1-14 1.7.3. Series C . 1-15 1.8. Population Distribution . 1-17 2: ECONOMIC 2.1. Introduction And Analysis. 2-1 2.2. Goals . .. 2-12 2.3. Policies . .. 2-13 2.4. Districts. 2-15 2.4.1. Puna . 2-15 2.4.2. South Hilo . 2-17 2.4.3. North Hilo. 2-19 2.4.4. Hamakua . 2-20 2.4.5. North Kohala . 2-22 2.4.6. South Kohala . 2-23 2.4.7. North Kona . 2-25 2.4.8. South Kona. 2-28 2.4.9. Ka'u. 2-29 3: ENERGY 3.1. Introduction And Analysis. 3-1 3.2. Goals . 3-8 3.3. Policies . 3-9 3.4. Standards . 3-9 4: ENVIRONMENTAL QUALITY 4.1. Introduction And Analysis. 4-1 4.2. Goals .
    [Show full text]
  • Shifting Sands: Using Image Analysis and Laser Technology to Study Coastal Sand Dispersal
    NIWA WATER & ATMOSPHERE 9(1) 2001 COASTAL PROCESSES Shifting sands: using image analysis and laser technology to study coastal sand dispersal Andrew Swales Rapid and detailed analysis of sand particles using image Terry Hume analysis and laser technology is John Hawken providing new insights into our knowledge of sand dispersal Rick Liefting along the black sand beaches of Mark Cullingford the North Island's west coast. EVERY DAY, waves and currents shift thousands of tonnes of sand back and forth along the west coast of the North Island. This sand, either eroded from the land or swept from the seabed, has been sorted and transported during the past 6000 years or so since the sea reached its present level to form the coastal landforms that we see today. The size and shape of individual grains of sand provide important clues about the physical changes that transform these particles and the way they are dispersed along the coast. A current NIWA research project is using state-of-the-art technology to determine large-scale patterns of sand dispersal on the North A black-sand dune-beach system at Whatipu Beach at the north head of Manukau Harbour. View looking north Island's west coast. towards the pocket beaches of Karekare, Piha and Te Henga. Sands on the west coast titanomagnetite which is a magnetic iron ore. The 750-km of shoreline between Taranaki and Lighter-coloured sand comes from sources such Cape Reinga on the west coast of New Zealand's as the Waikato River. This sand derives from the North Island is well known for its black-sand rhyolitic (lava producing) Taupo volcanic centre beaches and rugged, varied coastal landforms.
    [Show full text]
  • This Document Consists of 4§ Pages, Plus 1 Figure
    Geology aad Mineralogy <* This document consists of 4§ pages, plus 1 figure. Series A UTIITE1J" STATES-DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY SELECTED ANNOTATED BIBLIOGRAPHY AND INDEX MAP OF THORIUM AND RARE-EARTH DEPOSITS IN THE UNITED STATES AND ALASKA* By Katharine L. Buck July 1955 TraeeBEiementst Investigations Report 531 This preliminary report is distributed \ without editorial and technical review for conformity with official standards and nomenclature. It is not for public inspection or quotation. *ThisTeport concerns work done on belialf of the Division of Raw Materials of the U. S. Atomic Energy Commission. USGS - TEI -531 GEOLOGY AND MINERALOGY No, of copies Atomic Energy Commission, Washington «, 2 Division of Raw Materials, Albuquerque. 0 1 • Division of Raw Materials, Austin ...... 1 - Division of Raw Materials,, Butte „ . „ . 1 Division of Raw Materials, Casper ...... 1 Division of Raw Materialsc Denver „ 1 Division of Raw Materials, Hot Springs . 1 Division of Raw Materials. Ishpeming . 1 Division of Raw Materials, Phoenix „ . 1 Division of Raw Materials, St0 George . 1 Division of Raw Materials, Salt Lake City .... 1 Division of Raw Materials, Washington „„.«,. 3 . Exploration Division, Grand Junction Operations Office 1 Grand Junction Operations Office,, «„.<,.. 1 Tecfeiical Information Sdtvice, Oak Ridge . 6 TJ8 S0 Geological Survey : Alaskan Geology Branch, Menlo Park „ 2 Fuels Branch, Washington„ „ 0 e 1 Geochemistry and Petrology Branch, Washington » 1 Geophysics Branch, Washington „ 1 Mineral Deposits Branch, Washington ..... 2 P8 C8 Bafemari, Menlo Park ........ 1 A0 L. Brokaw 0 Grand Junction . 1 N0 M8 Denson, Denver 0 . 0 «».«.. 1 C. Ea Dutton, Madison ......... 1 V0 L0 Freeman, College . „ „ . D . 1 R.
    [Show full text]
  • U.S. Industrial Garnet Industrial U.S
    U.S. Industrial Garnet Chapter L of Contributions to Industrial-Minerals Research Evans and Moyle—U.S. Industrial Garnet—U.S. Geological Survey Bulletin 2209–L Bulletin 2209–L U.S. Department of the Interior Printed on recycled paper U.S. Geological Survey U.S. Industrial Garnet By James G. Evans and Phillip R. Moyle Chapter L of Contributions to Industrial-Minerals Research James D. Bliss, Phillip R. Moyle, and Keith R. Long, Editors Bulletin 2209–L U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior P. Lynn Scarlett, Acting Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia: 2006 This report and any updates to it are available online at: http://pubs.usgs.gov/bul/b2209-l/ For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1–888–ASK–USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1–888–ASK–USGS Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Cataloging-in-Publication data are on file with the Library of Congress (URL http://www.loc.gov/). Produced in the Western Region, Menlo Park, California Manuscript approved for publication, March 29, 2006 Text edited by George A.
    [Show full text]
  • Magnetic Survey of the Natashquan Iron-Sands, North Shore of the Saint-Lawrence Magnetic Survey Pu Vi C 1
    GM 24160 MAGNETIC SURVEY OF THE NATASHQUAN IRON-SANDS, NORTH SHORE OF THE SAINT-LAWRENCE MAGNETIC SURVEY PU VI C 1 Ministère des Richesses Naturelles, Ruébec OF SERVICE DES GÎTES Tv1INÉRAUX No GM- :2...1//60 THE NAT ASHQUAN IRON—SANDS NORTH SHORE OF THE SAINT-LAWRENCE TABLE OF CONTENTS F.ge INTRODUCTION 1 General Statement 1 Location of the area 2 Means of access 3 Previous exploration work 4 Acknowledgments 6 DESCRIPTION OF THE AREA 7 Topography 7 Drainage 8 Natural resources and climate 8 Settlements 10 GEOLOGY 11 Consolidated rocks 11 Unconsolidated deposits 12 OUTLINE OF THE.1951 FIELDWORK 13 Airborne survey 13 Ground magnetometer survey 15 SAMPLING 21 TONNAGE ESTIMATION 25 PHYSICAL PROPERTIES AND COMPOSITION OF THE IRON-SANDS 27 Granularity ......,, 27 Chemical composition 28 Mineralogical composition 28 Concentration of the magnetite 29 Concentration of the ilmenite ...,,......p•.••.• 29 Radioactivity and concentration of the monazite 30 Conclusion .. • . , . ,F 30 -II- Page ORIGIN OF THE IRON-SANDS 30 OTHER ECONOMIC POSSIBILITIES 32 Peat 32 Clay 33 Ochre 33 Cement sand _ 3+ CONCLUSION 31f BIBLIOGRAPHY _ 36 MAPS AND ILLUSTRATIONS Map A.' Airborne Magnetoneter,Survey,Area, from,Natashquan To Kégashka Bay ... (in pocket) ►' t wAAUL eit.iirov. Map B.'- Map of the Drilling done by Mackenzie-Parsons in 1912-1912 ... (in, pocket) t.".-4- ‘Qa4).6 Map C.- Ground Magnetometer Magnetic Profiles.... (in,pocket) Map D: - Ground Magnetomeer Magnetic Contours of part_of the Deposits ... (in pocket) 1"1=k000' Map E. Ground Magnetometer Magnetic Profiles ... (n p ocket € avloia Map F." - Airborne Magnetometer Pr•lesofi over lain Deposits ..
    [Show full text]
  • Evaluation of Glass-Grade Silica Sand Resources, Nellore District, Andhra Pradesh, India Using GIS
    IOSR Journal of Applied Geology and Geophysics (IOSR-JAGG) e-ISSN: 2321–0990, p-ISSN: 2321–0982.Volume 2, Issue 4 (Jul-Aug. 2014), PP 18-25 www.iosrjournals.org Evaluation of glass-grade silica sand resources, Nellore District, Andhra Pradesh, India using GIS. P. Rameshchandra Phani Cyient Limited, Plot No.11, Software Units Layout 2, Infocity, Madhapur, Hyderabad 500 081, India. Abstract: In India silica sands are produced from loosely consolidated sands and weakly cemented sandstones ranging from Recent to Pre-Cambrian in age. In this paper an attempt has been made to estimate the silica sand resources, belonging to Holocene age, located at about 20km east of Gudur town, Nellore District, Andhra Pradesh. Silica sand occurs in this region as dunes of marine origin covering an area of 110 Sq.Km. Ayyavaraiah et al (2013) reported that production and reserves estimated and declared by State Mines & Geology and Indian Bureau of Mines do not match and a difference exists. Hence an attempt has been made to estimate the actual reserves of silica sand deposits of this area using Google Earth imagery, GIS and field auger hole data. The total area that was mined already is about 9.538 Sq.Km. amounting to 117 Million Tons of silica sand that was produced in past 10-15 years with 59 Million Tons still to be excavated in the currently active mines. By surface area mapping using GIS, the prospective areas for further exploration and exploitation are suggested, giving rise to total prospective reserves of silica sand of 849 Million Tons.
    [Show full text]
  • Mines Branch, Feb., 1950, Ottawa, Canada
    *4 4V MM SCIENCE Li 3RpRY UMI. r " Y ! a .fie! :- . ' O.F l©plRrr o s . 1817 A R T E S SCIENT'i A V R I TAS TITANIUM A Suwiry of the Literature Presented as a Thesis in Economic Geology by Charles D. Campbell )*15 Qm---- i9 3 4- TABLE OF CONTENTS Introduction ... O.........................O.."....1. Purpose of the Paper Chemical Properties of Titanium Nine ral1ogy and Petrography ......... ............. 3. Origin O..........O..OS........ 5. ~........oo. 4. Distribution Domestic .................................. 5. Foreign NothAmerica ........... 0ee~.. .. 5..13 Central America *..."o."..."."""""""."14. South America ... "...000........""""... 15. Asia *..O..O.................:.......15. Af'rica .........................SSSO 17. Oceania """"""""""""".""""""S""""""..".S18. Europe """""..""".""."""19. mining and Concentration ".""""""""""""""."""""" .20. Uses of Titaniam S....................OOOO.....22. Bibliograpy.......SS@ ... ..................... 25. Introduction There has been, of late years, a growing demand for titanium in various forms for use in the paint industry, in metal making, in dyeing, pottery manufacture, and as an incandescent medium. For this reason, the problems of its occurrence in nature, its mining, and its preparation for use, have received some attention in the form of numerous articles and monographs. In this paper, I wish to give a summary of the more prominent of these writings, with spe- cial emphasis on the geologic phases of them. Titanium is generally classed with the rare elem- ents, although it is the ninth element in abundance on the lithosphere. In analyses of 800 igneous rocks, carried out in the laboratories of the United States Geological Survey, all but sixteen contained titanium. Because it was found in the dust of the Mt.
    [Show full text]