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Gold Geology Of: more books (100)

Geology of the Oatman gold district, Arizona: A preliminary report (United States Geological Survey bulletin) by Frederick Leslie Ransome, 1923
Gold placer deposits of the Pioneer district, Montana (Contributions to economic geology) by J. T Pardee, 1951
Geology of Gold Deposits Perspective in 1988 (monograph series #6) by Keays Reids R, 1989-06
Geology of the Carlin gold deposit, Nevada : a detailed study of the largest disseminated-replacement gold deposit in North America (SuDoc I 19.16:1267) by Arthur S. Radtke, 1985
Geology and ore deposits of the Gold brick district, Colorado, (Colorado Geological Survey. Bulletin) by R. D Crawford, 1916
Califonia Division of Mines & Geology Gold Districts of Califonia by William B. Clark, 1992
Geology of the tungsten, antimony and gold deposits near Stibnite, Idaho (Contributions to economic geology) by John Roberts Cooper, 1951
Geology and gold resources of Boise basin, Boise county, Idaho, (Idaho Bureau of Mines and Geology. Bulletin) by Samuel Milroy Ballard, 1924
Gold investigations in precambrian clastic and pelitic rocks, southwestern Colorado and northern New Mexico (Contributions to economic geology) by Fred Barker, 1969
The geology of the lower Gwanda gold belt, by A. E Phaup, 1933
Geology of the Robertson, Humdinger, and Robert E. Gold mines, southwestern Oregon, (Contributions to economic geology) by Philip John Shenon, 1933
Reconnaissance of the gold fields of southern Alaska: With some notes on general geology by George Ferdinand Becker, 1898
Geologic guidebook along Highway 49, Sierran Gold Belt: The Mother Lode country (California. Division of Mines and Geology. Bulletin) by Olaf Pitt Jenkins, 1948
Monthly Journal of California Geology: Elemental Analysis of Mica Resources in California and Gold Miners from South America by California Geology., 1988-01-01

lists with details

Geology And Gold In The Rattlesnake Hills And Barlow Gap Areas
geology gold in the Rattlesnake Hills Barlow Gap Areas. The RattlesnakeHills lie along the northern margin of the Barlow Gap
http://www.wsgs.uwyo.edu/metals/Barlow_gap.asp

Extractions: Whats New Wyoming Geology Data Services Pubs and Sales ... UW Home Email: wsgs-info@uwyo.edu The Rattlesnake Hills lie along the northern margin of the Barlow Gap 1:24,000 scale quadrangle in central Wyoming. The Barlow Gap quadrangle was mapped by Wayne Sutherland and assisted by W. Dan Hausel in 1999. The Rattlesnake Hills district was mapped by W. Dan Hausel of the Metals and Precious Stones Section of the Wyoming State Geological Survey (WSGS) in 1995 ( Geological Map of the Rattlesnake Hills ). The results of the Rattlesnake Hills appeared in WSGS Report of Investigations 52. These mapping projects are part of an ongoing Precambrian geology and economic geology research project by the WSGS. Mapping of the Barlow Gap Quadrangle was partially funded by the US Geological Survey STATEMAP program. The Rattlesnake Hills project was funded entirely by the WSGS budget. This region of the northern Granite Mountains contains one of the best gold prospects in the State for open-pitable gold mineralization. Barlow Gap lies within the ancient Archean craton known as the Wyoming Province, and includes geologic units ranging in age from
Gold Brochure
The North Carolina Geological Survey sells publications on gold in North Carolina. TheUS Geological Survey distributes several pamphlets on gold prospecting.
http://www.geology.enr.state.nc.us/Gold brochure/Gold Brochure 12222000.htm

Extractions: This page provides information about gold in North Carolina. This page was designed to answer many of the frequently asked questions about gold in North Carolina. Contact the North Carolina Geological Survey for further information about gold in North Carolina. Click here to link to the Reed Gold Mine State Historic Site. INFORMATION AVAILABLE The North Carolina Geological Survey sells publications on gold in North Carolina. For information on publications and prices, please contact us at the address below. Many of the North Carolina publications written about gold in the late 1800s and early 1900s contain valuable information, but are now out-of-print. Bulletin 3, Gold Deposits of North Carolina Bulletin 10, Gold Mining in North Carolina and Adjacent South Appalachian Regions ; and Bulletin 38, Gold Deposits in North Carolina , are especially useful. These publications are on file in the Raleigh office of the North Carolina Geological Survey, and are also available in many university libraries. Public libraries can obtain the publications through inter-library loan. A complete
DoIR - Geological Survey Of Western Australia - Discover Geology - Life Of A Gol
DoIR Home Geological Survey of Western Australia Discover geology Life of a gold Mine, Life of a gold Mine Follow the life
http://www.doir.wa.gov.au/GSWA/8663FFF81E094F4A8965910A7D297DDD.asp

Extractions: Contact Us Search DoIR Home Geological Survey of Western Australia ... Discover Geology Life of a Gold Mine Life of a Gold Mine Follow the life of a gold mine from exploration to rehabilitation in this series of slides and notes. View or download individual sections or the Complete Presentation Exploration to Discovery Exploration is commonly the longest and riskiest stage on the road to establishing a gold mine, and can take up to several years for each project. Mining Several mines in the Kalgoorlie region have been used to exemplify the different styles of mining. Processing An overview of the processing techniques used in some operations. Uses of Gold Some of the ways we use gold in science, industry, and culture. Rehabilitation Environmental management in the exploration and mining industry. LIFE OF A GOLD MINE LINKS Complete Presentation Part 1 Exploration to Discovery Part 2 Mining Part 3 Processing ... Part 5 Rehabilitation GEOLOGICAL SURVEY
The Geology Of Coarse Gold Formation
The geology of Coarse gold Formation. By Chris Ralph. The goal ofmetal detecting for gold is finding coarse nuggets. In order to
http://www.nuggetshooter.com/articles/CRGeologyofcoarsegoldformation.html

Extractions: The Geology of Coarse Gold Formation By Chris Ralph The prospector using a metal detector is primarily interested in coarser gold as larger nuggets are easier to detect, and of course, more valuable! It turns out that coarse gold most commonly forms in small veins (for the sake of argument, lets say for our discussion that coarse gold is stuff a Penney weight or larger). Big veins, with a width and length large enough to be mined commercially underground, almost always produce small gold - wires, small pieces, etc - even though they may be fairly rich. Of course, there are a number of exceptions to this rule, but generally speaking, it is true. So why, in general,does big gold form in small veins, while mostly only small gold forms in big veins? Often, the source of the heat is some sort of cooling magma (lava, still molten or solidified but still hot). This kind of heat source throws off so much heat energy that the rock may well be warm to within 100 feet of the surface, even if the source is over 2000 feet down. The temperature does not drop off suddenly once the solution gets a short distance from the source. The drop in temperature as you move away from the heat source is gradual, and usually fairly linear, at least within a few hundred feet of the surface. So the temperature of the rock (and the water solutions as well) becomes directly related to how far they are from the heat source. The rate of cooling then becomes a simple function of how fast the fluids move upward.
Turning Red Lead Into Gold
to other places, cleansed by the aforenamed vapors, where the earth is subtle,pure, and moist, fills the pores of it, and so gold is made. 4. BRIEF geology.
http://www.crocoite.com/redleadintogold/ch4.htm

Extractions: A. E. Waite 4. BRIEF GEOLOGY The ore bodies of the Zeehan and Dundas areas are quite similar. Why then, does crocoite occur in so much abundance at Dundas and not nearby Zeehan? To find the answer, we must first of all travel back in time more than 500 million years, to the period known as the Cambrian. This period of time, named for the Roman name for Wales (Cambria), was, at the time, the oldest system of rocks in which fossils could be used for dating and correlation. The period commenced around 600 million years ago with a duration of about 100 million years. During the Cambrian period in Tasmania, sedimentary rocks, derived from the erosion of earlier formed Pre-Cambrian rocks, were deposited over a long period of time. Many of these rocks were formed in marine environments, a fact indicated by the traces of marine fossils such as trilobites, brachiopods, sponges, and other organisms. Igneous rocks (that is, rocks that have melted, and then solidified by cooling) also formed during the Cambrian. Some of these rocks, such as serpentines, and the Mount Read volcanics, are important hosts for economic minerals. The serpentines are also known as ultrabasic rocks (rocks that are comprised predominantly of ferromagnesian minerals), and may contain chromite, nickel sulphides, or "osmiridium" and other platinum group minerals. These serpentines outcrop in a number of areas in Tasmania, including Dundas, Heazlewood, Adamsfield, Ulverstone, and Beaconsfield. Only in the first two areas however, does the chromium in the serpentine combine with the other necessary ingredient, lead, that has allowed that spectacular mineral crocoite to form.
Basic Dolgellau Gold-belt Geology
Cambrian goldfields Ltd working towards a sustainable Welsh goldIndustry. BASIC DOLGELLAU gold-BELT geology, BACK TO HISTORY PAGE.
http://www.cambriangoldfields.co.uk/geology.htm

Extractions: BASIC DOLGELLAU GOLD-BELT GEOLOGY BACK TO HISTORY PAGE FOR A DETAILED ACCOUNT CLICK HERE Any geological queries? Email John Mason HERE This tale takes us back into the Lower Palaeozoic era, when North Wales was under the sea, on the margin of the ancient ocean that geologists call Iapetus (fig. 1). Scotland and Northern Ireland sat on the ocean's opposite shore. The shales that make up the Gold-belt were originally silts and muds, deposited on the old sea-bed. Fig. 1: Sketched reconstruction of Iapetus Ocean at the time of the formation of the Dolgellau Gold-belt, with present-day landmasses shown in grey. Most of these, apart from E Scandanavia and NW Canada, were in fact submerged beneath shallow seas at the time - the marginal seas of Iapetus. When the ocean closed, the ensuing continenatal collision joined together the two halves of Britain and added E New England, Nova Scotia and E Newfoundland to the American continent. The Atlantic started to open hundreds of millions of years later.
Mining And Geology
gold and Civilisation *** (8) Tells the story of gold in Australia in an internationalcontext. Coal geology and Resource Data Online *** (9) From the Illinois
http://www.geologyshop.co.uk/mining.htm

Extractions: A A portfolio of some of the best Mining and Quarrying websites worldwide. From GeologyShop 50 of the best worldwide links for hydropower, dams and tunnels (select useful links) Dam inspection service, UK and overseas One of the main sites for geological information worldwide . This is one of over 50 link pages plus there are many original articles. Try our site specific SEARCH ENGINE to find the information you want or go to our MAIN INDEX page. Or try our site specific ORIGINAL articles, FREE geological stuff, or use our HOMEWORK AND TUTORIAL GUIDE POPULAR PAGES: Chalk facts Channel Tunnel facts Channel Tunnel geology Dinosaurs, top 20 sites Dictionaries Dinosaurs, early finds Dinosaur pictures Dinosaurs, facts Earthquakes, top 20 sites Education Fossils, top 20 sites Fossils by group Free stuff Gems Geology jobs Geology of Kent Geotechnical engineering Hominids (early man) Ice ages Igneous rocks Landslips of Kent Mesozoic Metamorphic rocks Museums Mineralogy Mining Natural disasters Palaeogeography Palaeozoic Petroleum Planetary geology Plate tectonics Precambrian Sedimentary rocks Stratigraphy
GEOLOGY OF THE RIDGEWAY GOLD DEPOSITS
geology OF THE RIDGEWAY gold DEPOSITS. RIDGEWAY, SOUTH CAROLINA. Returnto the Central Page. INTRODUCTION. Kennecott Minerals Company
http://www.kennecottminerals.com/krmc/KRMC/geopaper.html
GEOLOGY AND STRUCTURE OF THE SUROZH GOLD DEPOSIT
Regional geology, Soroki greenstone belt of the Priazovian granulitegreenstone terrain. Oremineralogy, Native gold, pyrite, pyrrhotite, chalcopyrite, sphalerite.
http://www.geofuel.lviv.net/PETGF/MGOLD/suroz.htm

Extractions: This presentation includes results reported to the International Symposium GOLD'99 "Precambrian gold in the Fennoscandian and Ukrainian Shields and related areas" held on May 4th to 6th, 1999 in Trondheim, Norway under sponsorship of the Norway Geological Survey. Some blocks are published in the Abstract volume while pictures mainly represent unpublished versions that have been partially shown during oral reports at the Symposium. ECONOMIC GOLD MINERALIZATION OF THE SOROKI GREENSTONE BELT A.B.Bobrov , A.A.Sivoronov , T.B.Yaskevitch , K.M.Pozdeev , B.I.Malyuk Department of Geology, Lviv State University, Ukraine IGGMF UNAS, Lviv, Ukraine Soroki greenstone belt has been encountered in Priazovian granulite-greenstone terrane of the Ukrainian Shield (Figure). Stratigraphy of the belt is mainly defined by age-different metamorphosed volcano-plutonic associations (VPA) of the komatiite-tholeiite formation (from the base): lower tholeiite-gabbro-diabase (KT-1), lower komatiite-dunite-harzburgite (KT-2), upper tholeiite-gabbro-diabase (KT-3) and upper komatiite-dunite-harzburgite (KT-4). As well, ore-hosting litho-facial complex also includes schist-BIF-tholeiite formation which is spatially linked to the above VPA of komatiite-tholeiite formation replacing them laterally. The section is capped by rhyodacite-plagiogranite VPA which is extremely important in the Ukrainian Shield greenstone belts structure and their ore-forming processes development. It is suggested the gold mineralization is genetically linked to the fluid systems of this VPA which have been separated from the parent VPA within 3.15-3.3 Ga.
Cal-Gold Books: Geology And Technical
Calgold Books. geology AND TECHNICAL. G119 GEMS, GRANITES, AND GRAVELSDietrich Skinner. Basic geology of the formation of mineral
http://www.calgold.net/Book14.htm

Extractions: Cal-Gold Books GEOLOGY AND TECHNICAL G137 PRACTICAL GEOLOGISTDixon-A complete course in one book. $15.00. G159 A FIELD MANUAL FOR THE AMATEUR GEOLOGISTCvancara. Geology, Mineralogy, Collecting. $1 G90 GEOLOGY IN THE FIELDCompton. Field geology methods. Newest edition of Manual of Field Geology. $49.95 G148 FIELD GEOLOGY ILLUSTRATED-Maley. Exellent aid to learn physical geology. Photos of geologic interest with explanatory sketches and diagrams. Sections on hard rock and placer deposits. $16.95. G9 DICTIONARY OF GEOLOGICAL TERMSAGI. Nearly 8500 commonly used terms in geology and related sciences. $16.95 G130 CONCISE OXFORD DICTIONARY OF EARTH SCIENCES. $14.95 G170 DICTIONARY OF EARTH SCIENCEMcMilan. $17.95 G172 HOW TO SMELT YOUR GOLD AND SILVERChapman. Complete Guide. Color Pictures. $ G145 MINERAL DEPOSIT EVALUATIONAnnels. A practical approach. Symposium proceedings. $120.95 G76 MINERAL EXPLORATIONLacy. Comprehensive handbook on technical aspects of mining. Symposium proceedings. $55.00 G77 MINING GEOLOGYLacy. Technical manual for the serious miner. Symposium proceedings. $59.95 G126 GEOLOGY OF ORE DEPOSITSGuillon and Park-Text. $59.95.
Meridian Gold - Operations - Rossi - Joint Venture, Exploration, Geology
STORM resource is a highgrade, structurally controlled refractory gold deposit occurringat The local geology consists of chert, siltstone and mudstone of the
http://www.meridiangold.com/operations_rossi_details.cfm

Extractions: History N.L. Baroid Corporation began gold exploration on the Rossi property in 1982 and by 1985 had identified several areas of shallow low- grade gold mineralization . In 1986, Meridian Gold (then FMC Gold) entered into a 50/50 joint-venture agreement with N.L. Baroid to conduct further gold exploration on the property. Shallow exploration continued through 1989. High- grade gold mineralization was discovered in 1990 as the result of a deep exploration program. Two of 12 deep holes encountered gold grades greater than 6.8 g/t: 6.1 meters of 10.5 g/t at 479 meters; and 9.1 meters of 9.7 g/t at 404 meters. By the end of 1992, 14 of 30 deep holes drilled contained intercepts of greater than 6.8 g/t. In 1993, Meridian Gold purchased all the precious metals rights to the property, without royalties, and expanded the deep exploration program. As of December 2002, the STORM resource is defined by 141 drill holes, 113 surface and 28 underground. In 60 of these holes, there are 91 intercepts of more than 1.5 meters, each of which grades better than 6.8 g/t. These 91 intercepts have an average thickness of 6.5 meters and a weighted average grade of 15.7 g/t Au. The STORM resource contains an inferred resource of 2.5 million tonnes at an average grade of 11.8 g/t Au, at a gold cutoff of 6.8 g/t, for 960,000
Arthur Lakes Library
geology and resources of gold in the United States. series US Geological SurveyBulletin 1857A - J. In-depth survey of gold geology, genesis, locations.
http://www.mines.edu/library/reference/gold.html

Extractions: Help: Using Gold literature General research tips: Check with your librarian to find out about new resources and electronic databases. If you are not on campus, try the online Ask A Librarian form Look for library guides in related disciplines. Know your librarys classification system. The CSM Library uses Library of Congress (LC). Use it to browse for information. In our Library, most engineering materials are located in the Ts.Become familiar with core works in your field. Use these as a base to start your search. Keyword choices are important. Add keywords to your search from publications you've already identified and from thesauri and indexes. Evaluate your sourcesespecially Internet sources. Check for updating, type and date of coverage, publisher and/or author. To Table of Contents Books about Gold Catalyst - to find CSM materials Prospector - to find materials at Colorado libraries. WorldCat - to find materials elsewhere.
FindingWeb Directory - /Science/Earth_Sciences/Geology/Rocks_and_Minerals/Metall
Recreational gold Panning. See also Top/Science/Technology/Mining/Prospecting. Links. GuidedJeep tours into the Superstition Mountain Foothills to pan for gold.
http://dir.findingweb.com/Top/Science/Earth_Sciences/Geology/Rocks_and_Minerals/
Ohio History Central - Nature - Geology - Minerals - Gold
October, 1995. US Geological Survey on gold. gold in Ohio by the OhioDivision of Geological Survey. gold at mineral.galleries.com. Pough
http://www.ohiohistorycentral.org/ohc/nature/geology/minerals/gold.shtml

Extractions: -Nicholas Vachel Lindsay [1879-1931] The English word gold comes from a series of ancient words that refer to the color yellow. Its rarity, beauty and ability to be shaped by man have made it a highly desired precious metal throughout the history of mankind. "Gold fever" has been a frequently recurring affliction for humans. Today, artists and artisans use gold extensively in making jewelry and other objects of beauty. Also, because of its distinctive characteristics as a metal, gold has important uses in dentistry, photography, industry and electronics.
Cover: Alaska, Gold-bearing Rocks. / Geological Survey (U.S.) ; Emmons, S.F. / 1
Title (Covers to) Map of Alaska Showing Known goldBearing Rocks With DescriptiveText Containing Sketches of the Geography, geology, and gold Deposits and
http://www.davidrumsey.com/maps500.html

Extractions: Full Title: (Covers to) Map of Alaska Showing Known Gold-Bearing Rocks With Descriptive Text Containing Sketches of the Geography, Geology, and Gold Deposits and Routes to the Gold Fields. 55th Congress, 2d Session, Senate Doc. 195. Prepared in accordance with Public Resolution No. 3 of the Fifty-fifth Congress Second Session, Approved January 20, 1898. Printed in the Engraving and Printing Division of the United States Geological Survey, Washington, D.C. 1898.
The Gold And Coal Fields Of Alaska. / Geological Survey (U.S.) ; Emmons, S.F. /
Date 1898 Pub Title Map of Alaska Showing Known goldBearing Rocks With DescriptiveText Containing Sketches of the Geography, geology, and gold Deposits and
http://www.davidrumsey.com/maps5795.html

Extractions: Note: Important Alaska Gold Rush Map. Map is taken from the Coast Survey map, with much information added. Emmons' booklet, 24x15, is 44 pages, useful description of the country, trails, etc. The first edition of the Coast Survey map was 1890 (in the 1890 annual report), with subsequent updated editions in 1895 (in the 1896 annual) and 1898 (in the 1897 annual). This map is based on the 1898 Coast Survey map.
Geology
Discoverer of the South Atlantic Submarine gold Placers _ 40 Millions Tons Estimate_Founder of The TRUE geology mailto mining_pioneer@hotmail.nospam.com
http://members.austarmetro.com.au/~hubbca/geology.htm

Extractions: Geology Home CONSPIRACY Health NESARA ... LINKS Jean Paul Turcaud and the true geology For some time now I have been searching for independent confirmation of the existence of Jean-Paul Turcaud and his claims. The following URL appears to be a through treatment of the issues' involved. The Golden Riddle: Finder's Keepers? Produced by Bronwyn Adcock Sunday 6/06/99 http://www.abc.net.au/rn/talks/bbing/stories/s28534.htm 4. Quote: Bronwyn Adcock: Jean-Paul Turcaud is not a formally trained geologist. Nevertheless, he developed his own geological theories about the origins of mineral deposits. These theories are different to conventional THE GREATEST AUSTRALIAN MINING COVERED UP SWINDLE OF THE 20TH CENTURY Disclosure of Australian Mining Crimes and Political Corruptness http://membres.lycos.fr/jpturcaud/
A Recipe For Gold
Regional geology a recipe for gold a brief description of the geologicalhistory of the Waihi region. Volcanic Violence Around
http://www.marthamine.co.nz/recipe_for_gold.html

Extractions: Around 20 million years ago volcanoes burst through the landscape around what we now know as Waihi. Tall, steep sided andesite volcanoes formed as the hot lava was thrown out to coat the sides of the volcanoes and the surrounding land. These volcanoes were similar in size and shape to Ruapehu and Ngauruhoe in the central North Island. Volcanic eruptions continued throughout the Coromandel for more than 15 million years. The Mountains Wear Down Any rock raised above the ground is subjected to a range of forces that gradually wear it away. Over time the forces of weathering and erosion can reduce mountains to hills. 20 million years of weathering and erosion has taken its toll on the local landscape. It is hard to make out the shape of those ancient volcanoes. Hundreds of metres of rock have been gradually eroded away from the original mountains.
Martha Mine Educational Resources For Schools: Geology
clicking here. The University of Otago Department of geology websitefeatures a wide range of material about geology and gold. www.otago
http://www.marthamine.co.nz/schools/geol_sch.html

Extractions: The Waihi landscape was very different seven million years ago. The land was higher, probably by several hundred metres. Geysers threw boiling, mineral rich water high into the air, mudpools bubbled and hot springs dotted the countryside, very much like Rotorua today. Hot rock far below the ground provided heat energy for those spectacular features and also provided the ingredients for the gold deposit to be formed at Martha Hill. Over time the volcanic activity dwindled as the volcanic 'hot spot' gradually migrated southeast, passing through Tauranga and Te Puke to be centred around the Central Plateau today. Below is an impression of how the land has changed over the last 20 million years, showing how the forces of nature comine to produce a recipe for gold.
Eldorado Gold Corp. - Kisladag Project - Geology And Mineralization - Wed May 26
geology and Mineralization The Kisladag project is located in one of several mid Goldmineralization at the Kisladag project is hosted by a number of latitic
http://www.eldoradogold.com/s/KisladagProject.asp?ReportID=37135

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