21. Geology Of Gold Deposits In The Southern Marginal Zone Of The Limpopo Belt And A geology of gold deposits in the Southern Marginal Zone of the Limpopo Belt and adjacent Sutherland greenstone belt, South Africa; Klein Letaba http://sajg.geoscienceworld.org/cgi/content/abstract/100/1/73

Quick Search: advanced search GSW Home GeoRef Home My GSW Alerts ... TABLE OF CONTENTS South African Journal of Geology ; March 1997; v. 100; no. 1; p. 73-83 This Article Alert me when this article is cited Alert me if a correction is posted Services Email this article to a friend Similar articles in this journal Alert me to new issues of the journal Download to citation manager ... Order Hardcopy of Full Text via AGI/GeoRef Citing Articles Citing Articles via Google Scholar Google Scholar Articles by Gan, S. Articles by van Reenen, D. D. Search for Related Content GeoRef GeoRef Citation Geology of gold deposits in the Southern Marginal Zone of the Limpopo Belt and adjacent Sutherland greenstone belt, South Africa; Klein Letaba S. Gan, and D. D. van Reenen Rand Afrikaans University, Department of Geology, Auckland Park, South Africa This record provided courtesy of AGI/GeoRef. JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ... TABLE OF CONTENTS

22. Leighton, Freeman Beach (1952-01-01) Geology Of The Vermiculite Deposits, Gold B Title, geology of the vermiculite deposits, gold Butte mining district, southern Virgin Mountains, Nevada. Ogives of the East Twin Glacier, Alaskatheir http://etd.caltech.edu/etd/available/etd-05042006-141511/

Caltech Library System About Browse Search Caltech Student Instructions Leighton, Freeman Beach (1952-01-01) Geology of the vermiculite deposits, Gold Butte mining district, southern Virgin Mountains, Nevada. Ogives of the East Twin Glacier, Alaskatheir nature and origin. Investigations in the Taku Glacier firn, Alaska. http://resolver.caltech.edu/CaltechETD:etd-05042006-141511 Type of Document Dissertation Author Leighton, Freeman Beach URN etd-05042006-141511 Persistent URL http://resolver.caltech.edu/CaltechETD:etd-05042006-141511 Title Geology of the vermiculite deposits, Gold Butte mining district, southern Virgin Mountains, Nevada. Ogives of the East Twin Glacier, Alaskatheir nature and origin. Investigations in the Taku Glacier firn, Alaska Degree PhD Option Geological and Planetary Sciences Advisory Committee Advisor Name Title Ian Campbell Committee Chair Keywords none Date of Defense Availability unrestricted Abstract Geology of the vermiculite deposits, Gold Butte mining district, southern Virgin Mountains, Nevada: Vermiculite deposits lie within a one mile square area in the Gold Butte mining district, Southern Virgin Mountains, Nevada. An integrated field and laboratory study of the deposits was undertaken in an attempt to determine their origin. Particular attention was devoted to the mineralogy of the vermiculite and associated minerals and the geochemistry of vermuculitization.

23. Gratacap Geology Of New York City Ball. Diamonds Coal and gold of India. Bastin. geology Pegmatites Maine. Beveridge. Baburnama. Bradford. The Nerrena Or Little Bendigo goldField. http://www.farlang.com/gemstones/gratacap-geology-new-york/page_001

24. IngentaConnect Geology Of Gold-bearing Skarn Deposits In The Middle And Lower Ya geology of goldbearing skarn deposits in the middle and lower Yangtze River Valley and adjacent regions. Authors Zhao Y.1; Zhang Y.; Bi C. http://www.ingentaconnect.com/content/els/01691368/1999/00000014/00000003/art000

var tcdacmd="dt"; Home About Ingenta Ingenta Labs Ingenta Blog ... Check our FAQs Or contact us to report problems with: Subscription access Article delivery Registration Library administrator tasks ... Other problems For Publishers Why go online? Why choose IngentaConnect? Beyond Print: enhancing your service Access and authentication ... Contact us For Researchers For Authors About IngentaConnect Search and browse Publications available ... Register For Librarians Resource Zone Why choose IngentaConnect? Why choose IngentaConnect Complete? Activating Subscriptions ... Register CM8ShowAd("HorizontalBanner"); Geology of gold-bearing skarn deposits in the middle and lower Yangtze River Valley and adjacent regions Authors: Zhao Y. ; Zhang Y.; Bi C. Source: Ore Geology Reviews , Volume 14, Number 3, September 1999 , pp. 227-249(23) Publisher: Elsevier view table of contents Key: - Free Content - New Content - Subscribed Content - Free Trial Content CM8ShowAd("Skyscraper"); Keywords: geology skarn Yangtze River Valley Language: English Document Type: Research article DOI: Affiliations: Institute of Mineral Deposits, Chinese Academy of Geological Sciences, Baiwanzhuang Road #26, Beijing, China

25. Books - Geology Of Pluton-Related Gold Mineralization At Battle Mountain, Nevada Buy geology of PlutonRelated gold Mineralization at Battle Mountain, Nevada - Price Range $65.60 - $133.12 from 3 sellers. http://www.pricegrabber.com/search_getprod.php/isbn=9780966123302

Go back to home page Login Register Your Lists ... Valentine's Day Guide SHOP FOR IN All Products Appliances Auto Parts Books Cameras Clothing Computers Electronics Furniture Indoor Living Magazines Movies Music Musical Instruments Office Outdoor Living Software Sporting Goods Toys Video Games SEARCH Sell Yours Save Product to Your List(s) (Javascript required) Set Price Alert Geology of Pluton-Related Gold Mineralization at Battle Mountain, Nevada (English) (ISBN: 9780966123302) Price range: $65.60 (Refurb) - $133.12 from 3 Sellers Publisher: Univ of Arizona Pr Format: Paperback MSRP: $ 71.00 Synopsis: Not Available User Reviews Not Rated Write a Review Compare Prices Book Details New (1 Seller for $65.60) View All Conditions Enter Zip Code* Seller Price (USD) Tax* Shipping* BottomLinePrice* Availability Seller Rating Tower.com Merchant Info No Tax Free Your Best Price Not In Stock 30 Reviews Alibris Merchant Info No Tax In Stock 373 Reviews Enter Zip Code* * Enter your zip code above to get the best price for delivery in your area including shipping and tax. Shipping costs are based on an estimate of UPS ground or equivalent carrier within the contiguous US, excluding Alaska and Hawaii. Please see Seller's website for actual shipping costs.

26. Geology Of Epithermal Silver-gold Bulk-mining Targets, Bodie Your browser may not have a PDF reader available. Google recommends visiting our text version of this document. http://www.springerlink.com/index/752KVJ7662VM8686.pdf

27. JSTOR The Geology Of The Gold Fields Of British Guiana The geology of the gold Fields of British Guiana. By J. B. Harrison. With Historical, Geographical and other Chapters by Frank Fowler and C. Wilgress http://links.jstor.org/sici?sici=0190-5929(1909)41:8<514:TGOTGF>2.0.CO;2-B

28. GEOLOGY OF THE RAUL-CONDESTABLE IRON OXIDE-COPPER-GOLD DEPOSIT, CENTRAL COAST OF geology OF THE RAULCONDESTABLE IRON OXIDE-COPPER-gold DEPOSIT, CENTRAL COAST OF PERU. DE HALLER, Antoine, Mineralogy Department, University of Geneva, http://gsa.confex.com/gsa/2001AM/finalprogram/abstract_25106.htm

Paper No. 53-0 GEOLOGY OF THE RAUL-CONDESTABLE IRON OXIDE-COPPER-GOLD DEPOSIT, CENTRAL COAST OF PERU DE HALLER, Antoine , Mineralogy Department, University of Geneva, rue des Maraîchers 13, Genève 4, CH-1211, Switzerland, Antoine.dehaller@terre.unige.ch, ZUÑIGA ALVARADO, Julio, Geology department, Cía. Minera Condestable S.A, Calle Manuel Roaud y Paz Soldán 364, San Isidro, Lima, 27, Peru, and FONTBOTÉ, Lluís, Mineralogy Department, Univ of Geneva, Rue des Maraîchers 13, Genève 4, 1211, Switzerland Mineralization is predated by andesite-dacite porphyritic dikes and sills followed by a small granodiorite stock which is cut by dolerite dikes in originally subvertical fractures that grossly follow the NNW Andean trend. Most of the ore replaces porous (tuffs, volcanic breccias) or chemically reactive (limestone) beds and was generated by hydrothermal fluids flowing laterally from NE and NW trending veins. GSA Annual Meeting, November 5-8, 2001 General Information for this Meeting Session No. 53 Economic Geology I: Fe-oxide(-Cu-Au) Deposits, Fe-Sulfides in Black Shales, Taconite Ores, Geochronology

29. The Geology Of The Dolgellau Gold-belt The Dolgellau gold Belt and its geology. The Dolgellau goldbelt runs, arclike, southward from near Trawsfynydd, around the eastern and southern flanks http://www.geologywales.co.uk/dgb/

THE GEOLOGY OF THE DOLGELLAU GOLD-BELT BACK TO GEOLOGY PAGE Mesothermal gold-quartz lodes are common throughout the Gold-belt, but have only produced significant gold at certain localities. The total recorded output of the Gold-belt is ca. 4 tonnes of gold, mostly being produced by two mines, Clogau and Gwynfynydd, in the late 1800s and early 1900s. Intermittent exploration and production have continued to the present day, with the last large-scale mining activity being at Gwynfynydd mine in the 1983-1998 period. It is an area that has interested me since 1980, when I was taken to Clogau mine, then at work, and saw the stunning high-grade ore being mined at the time - chunks of quartz with visible gold sticking out all over the place, with here and there the glitter of tellurides. Since then much research has been done by several workers: the age and sequence of the mineralisation are both better understood as is the chemistry of the mineralising fluids. But there is still plenty to look at!

30. Buy.com - Geology Of Pluton-Related Gold Mineralization At Battle Mountain, Neva geology of PlutonRelated gold Mineralization at Battle Mountain, Nevada Ted G. Theodore ISBN 9780966123302 Book. http://www.buy.com/prod/geology-of-pluton-related-gold-mineralization-at-battle-

My Account Wishlist Help All Departments ... Warranties Books by Title by Author by ISBN by Publisher Buy.com New to Google Checkout? Try it and save $10. Books Best-sellers New ... Rewards UpdateProductViewHistoryCookie('Geology of Pluton-Related Gold Mineralization at Battle Mountain, Nevada','204033394'); Geology of Pluton-Related Gold Mineralization at Battle Mountain, Nevada (Paperback) Author: Ted G. Theodore Product Image Pricing Additional Info Currently Unavailable: This item is currently unavailable from the Manufacturer. Format: Paperback Format: Paperback ISBN: Publish Date: Publisher: University of Arizona, Center for Mineral Res Pages: Buy.com Sku: More about this product Item#: REKNQS View similar products Product Summary Reviews ISBN: Publisher: University of Arizona, Center for Mineral Res This new publication, which includes three major chapters by a number of authors from the mining industry, presents a comprehensive overview of gold mineralization in one of the classic mining districts in the Basin and Range country of the western United States. The publication is the latest in a protracted and wide-ranging collaborative investigation that documents the behavior of gold in pluton-related systems in the Battle Mountain Mining District. The monograph includes documentation of the three-dimensional relationship between distal-disseminated Ag-Au deposits and the skarn-related, porphyry Cu environment including revised grade-tonnage distributions for the former as well as documentation of a complex structural imbrication in the Devonian, Mississippian, Pennsylvanian, and Permian Havallah sequence in the upper plate of the Golconda thrust and its role in the genesis of the gold deposits. It also contains a comprehensive examination of petrochemical evolution of submarine volcanic rocks in the Havallah basin. As a result, regional exploration criteria are developed for distal-disseminated Ag-Au environments and their coeval relations with Carlin-type gold deposits.

31. Geology A description of the placer geology of the Fortymile River placer gold mining area. http://www.fortymilegold.ca/geology.htm

Fortymile Gold Placers Home Page - Fortymile Gold Placers Fortymile Gold Placers Company Profile Placer Gold Mining Property for Sale or Lease - Fortymile River Area History of Fortymile Placer Gold Mining District [ Geology of Fortymile Placer Gold Area ] Fortymile Placer Property Maps Investment Advantages of Placer Gold Mining in the Yukon Placer Gold Mining Consulting Services We are looking for placer property ... Contact Fortymile Placers Geology of Fortymile Placer Gold Area U.S. Geological Survey geologist Warren Yeend describes the bedrock of the Fortymile area as a metamorphic unit consisting mainly of gneiss, schist, amphibolite, and marble, and suggests that this rock is linked to the occurrence of lode gold in the area. (USGS Bulletin 2125, Gold Placers of the Historical Fortymile River Region , Alaska, 1996) High terrace gravels record a time from the late Tertiary to the late Pleistocene when the river had flood plains from 1 to 2 miles wide and had shallow gradients. The river subsequently incised into these auriferous flood plains and developed the youthful characteristics that it has today. The placer gold from these ancient benches reconcentrated in the present river valley. The Fortymile River drains an area of approximately 15,000 km

32. McLaughlin Reserve geology. New Resources. Petrography, Mineralogy, and geochemistry of . In either case, it is agreed that much of the golddepositing water was http://nrs.ucdavis.edu/mclaughlin/naturalhis/geology.htm

UC Davis Natural Reserve System - McLaughlin Reserve Home UC Davis NRS Reserves McLaughlin Links Visitor Information Forms Contacts Submit Reserve Use Application ... Land Use Geology Travertine Geo Pictorial Plants Insects ... Data McLaughlin External Links: NRS Systemwide Homepage Systemwide UC Davis NRS Sites GEOLOGY New Resources Petrography, Mineralogy, and geochemistry of McLaughlin Reserve Travertines Travertine Petrography and Microbiology Mineralogy and Magnetics Homestake's McLaughlin Mine Geology The following pages are graphics-intensive, so it may require a few "geologic" seconds to fully load.) Geology of the McLaughlin Deposit McLaughlin Minerals San Quentin Sinter McLaughlin Gold Key to understanding all of the McLaughlin Reserve's natural features is its rich and complex geology. The reserve captures much of the geological diversity of the California Coast Ranges, which are internationally famous for spectacular exposures of rocks deposited or modified by plate tectonic processes over the past 140 million years. In this chapter we begin by describing the geologic history of the Coast Ranges in the vicinity of the reserve. We then describe some of the reserve's most important and easily seen physical features: the

33. Carbon Isotope Evidence For A Magmatic Origin For Archaean Gold-quartz Vein Ore Groves, D. I. et al. in gold 82 The geology, Geochemistry and Genesis of Hodgson, C. J. MacGeehan, P. J. in geology of Canadian gold Deposits (eds http://www.nature.com/nature/journal/v321/n6073/abs/321851a0.html

nature.com about npg news@nature.com naturejobs ... register SEARCH JOURNAL Journal Home Current Issue AOP Archive THIS ARTICLE Download PDF References Export citation Export references ... Table of Contents Nature , 851 - 854 (26 June 1986); doi:10.1038/321851a0 Carbon isotope evidence for a magmatic origin for Archaean gold-quartz vein ore deposits D. R. Burrows , P. C. Wood Department of Geology, University of Toronto, Toronto, Ontario M5S 1A1, Canada Archaean gold-quartz vein/shear zone systems constitute one of the most important types of gold ore deposit; however, their origin is controversial. Here we discuss newly obtained and for the largest such system in the world (Golden Mile, Western Australia ). All of the data are statistically identical to the C values, reported here, of proven magmatic carbonate recently found with Au- and W-enriched MoS mineralization in the Mink Lake sodic granodiorite stock, northwest Ontario. The , and granulite facies processes . We conclude that currently available carbon isotope data suggest that the H fluid which deposited this type of Archaean Au mineralization was magmatically derived.

34. Martha Mine Educational Resources For Schools: Geology The University of Otago Department of geology website features a wide range of material about geology and gold. www.otago.ac.nz/geology/ See gold from http://www.marthamine.co.nz/schools/geol_sch.html

intro geology gold silver ... Geothermal migration Regional geology: a recipe for gold: a brief description of the geological history of the Waihi region. Geysers, Mudpools and Gold 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. KEY Greywacke Andesite Ignimbrite Lava Quatrz Veins New Zealand is Born The oldest rocks, called basement rocks, in the Coromandel region of New Zealand's North Island are greywacke. These sedimentary rocks were deposited in deep sea trenches about 150 million years ago as the land mass known as Gondwanaland eroded.

35. Geology Of Gold Rush Mining The Valdez Creek Mining District s geology was affected primarily for four significant glacial episodes. The last one being in the Holocene period, http://www.goldrushmining.com/pages/geology.html

Main Contents Partners Geology History Location Placer Evaluation Method Gold Rush Mining Geology The Geology Of Valdez Creek The Valdez Creek Mining District's geology was affected primarily for four significant glacial episodes. The last one being in the Holocene period, a relatively young period which occurred 9,5000 years ago. According to USGS geologist, Fred Moffit, the glacial deposits in the lower valley of White Creek indicate flow directions had changed probably due to the fact of the changes in ice production and accumulation. As a result, these movement contain irregularities net usually found in the White Creek drainage. Two types of gold nuggets were found, one pale colored, smooth and round, the other bright and rough with attached pieces of quartz. Moffit concluded that the ice had brought them into White Creek from the valley of Valdez Creek on the north end of Lucky and Gold hills. Placer gold is the end product of a long process. Transportation of gold happens mainly by erosion and glaciers. Agents of erosion includes: running water, waves, currents in bodies of standing water and wind. Glacier movement scours and transports minerals, bedrock, gold, and other precious metals. When the glacier melts, it typically deposits the metals directly form the melting ice. Upon further melting of the glacier, streams form and rework the placer deposits, occasionally under the ice. Most pieces of gold in the Valdez Creek Mining District, especially at the mouth of the valley, have characteristics proving glacial abrasion. These characteristics included a roundish shape with flat and smooth surfaces. Even though gold is the most malleable the ductile of metals, it still requires a thousand meters or more of ice transportation to take on these characteristics. Nuggets recovered form the tributary system such as Timberline Creek, White Creek, and Lucky Gulch are still shinny, course and rough. These nuggets indicate that they have not traveled a great distance, Therefore, they are probably close to the source.

36. Geology Of The Cripple Creek Mining District geology of the Cripple Creek and Victor area gold mining. http://www.ccvgoldmining.com/Geology/geology.html

A Joint Venture Manager Golden Cycle Gold Corporation Geology By D.M.Vardiman, T.R. Brown, E. Roy, M. Ward, I.P. Hutchinson The Cripple Creek Mining District is located within a Tertiary age alkaline volcanic/diatreme complex dated at approximately 33.4 Ma (Jensen, 2003). Surrounding country rocks are Precambrian granites and metamorphic units. Figure 3 is a physiographic map of the Western United States showing the location of the Cripple Creek district relative to the Walker Lane – Trans Pecos structural boundary and the subsequently developed Rio Grande Rift. The extensional Rio Grande system is most obvious in the Cripple Creek area along northwest striking horst and graben structures, such as the Four Mile and Oil Creek faults (Wobus, 1976). Subtle northeast regional trends also exist and may be related to a preexisting fabric that was developed during the Proterozoic. Work completed by Klipfel (1992) documents evidence for a possible Precambrian rift environment in northern Colorado along a general northeast trend. This rift environment may have extended south into the Cripple Creek area and may have been the mechanism for creating the subtle northeast fabric. DISTRICT GEOLOGY The principal Precambrian basement lithologies in the Cripple Creek area as described by Hutchinson and Hedge (1968) are: Biotite gneiss (postulated to be a metamorphic volcanogenic rock 1.7±? Ga); granodiorite (1.7 ±? Ga); Cripple Creek quartz monzonite (Silver Plume age, 1.5 ±? Ga); Pikes Peak granite (1.0 ±? Ga). The biotite gneiss and granodiorite were intruded by the Pikes Peak batholith, a large regional subalkaline intrusive complex. The intersection of these four units formed an area of structural weakness, which facilitated the emplacement of the Tertiary volcanic complex.

37. Geology Of Moore Creek, Alaska gold is concentrated at the base of the gravel and the upper 1.5 ft (0.46 m) 1988 A summary of the geology and mineral resources along a 32 km (20 mi) http://www.moorecreek.com/geology.htm

Moore Creek Mining LLC Home History Geology General ... Photo Album Bedrock underlying upper Moore Creek is Upper Cretaceous undifferentiated sedimentary rocks consisting of interbedded sandstone and shale. The placer deposit occurs in multiple ages of ancestral terrace gravels and in modern stream gravels. The older terrace deposits are inferred to be Late Tertiary to early Pleistocene, based on similarities with other dated deposits in Interior Alaska (Hopkins and others, 1971). Pleistocene fossils (mammoth and horse bones) in the overburden were dated at 36,000 BP with radiocarbon methods (Jeff Kline written communication, 1986). In the modern stream gravel is about 10 ft (3.0 m) thick. On the bench placers the gravel is only about 3 ft (1 m) thick and covered by 2 ft (0.61 m) of clay and vegetation (Mertie and Harrington, 1924). The principal heavy minerals identified in concentrates include native gold, cinnabar, scheelite, native silver, tetrahedrite, chromite, magnetite, and zircon (Mertie, 1936; Bundtzen and others, 1987, 1988; McGimsey and others, 1988). Concentrates from mining contain up to 35.00 percent chromite, i.e., a low grade chrome resource. A mineral separate of screened, minus-28-mesh material from a 100-kilogram, bulk sample of gravel contained 2,300 parts per million (ppm) chromium, 5,200 ppm titanium, 70 parts per billion (ppb) palladium, 200 ppm nickel, and 8.25 percent iron (Bundtzen, Laird, and Lockwood, 1988). Although the nuggets contain abundant quartz rock, the tailing piles are remarkably lacking in quartz. However, abundant large agates occur, derived from the volcanic rocks in the area. A piece of cinnabar was found with agate attached (S. Herschbach).

38. Ouachita National Forest - Minerals And Geology, Inventory Alabama NFsAL; Caribbean NF-PR - geology, Topography, Soil Catagories, Landslides; La Coca Falls, La Mina Waterfall; Chattahoochee-Oconee NFs-GA - gold http://www.fs.fed.us/r8/ouachita/natural-resources/minerals/inventory.shtml

@import url(../../global-websites/styles/screen.css); [Jump to the main content of this page] Forest Service National Links Forest Service Home Employment Fire and Aviation International Forestry Just for Kids Maps and Brochures Passes and Permits Photo and Video Gallery Publications Recreational Activities Research and Development State and Private Forestry Southern Region Page Ouachita Home Page About Us Contact Us ... Volunteering Minerals and Geology USDA-FOREST SERVICE Minerals and Geology Inventory for National Forest Lands Compiled By: John C. Nichols, Forest Geologist, Ouachita National Forest Minerals and Geology related programs and features on National Forests are extensive, educational, and important to National interests. This is a listing of some of the Forest Service Minerals and Geology related features and information found on many of the National Forests across the United States. Most of this information was collected from Forest Service web pages from 2001 to the present. Changes in Forest Service web pages over the years have resulted in some of this material no longer being available on the web, or temporarily made unavailable. Regardless, the information listed here is provided as a starting point for persons interested in obtaining more minerals and geology related information pertaining to National Forests they are interested in. The National Forest Service website will link you to the webpage listings and links for each National Forest, cross-referenced by Forest name and State in which it is located. Take time to visit the webpages of the Forests you are interested in to find a variety of information regarding the National Forests.

39. Geology Of The Sierra Nevada, Revised Edition gold The California Story, by Mary Hill A Land in Motion California s San Andreas Fault, by Michael Collier geology of the San Francisco Bay Region, http://www.ucpress.edu/books/pages/1260001.html

Subjects: Anthropology Art Film Classical Studies Global Issues History Literature/Poetry Music Natural Sciences Religion Sociology DISTRIBUTED TITLES: British Film Institute Sierra Club Huntington Library Ecology, Evolution, Environment Natural History Geology MORE INFO AND CHOICES Email: Mary Hill Geology of the Sierra Nevada Revised Edition California Natural History Guides, 80 $50.00, £29.95 hardcover In stockships in 2-3 days $19.95, £11.95 paperback In stockships in 2-3 days 468 pages, 4-1/2 x 7-1/4 inches, 117 color illustrations, 16 b/w photographs, 39 line illustrations, 12 maps Published May 2006 Available worldwide Categories: Ecology, Evolution, Environment Natural History Geology Earth ... Explore full text using Google Book Search "With her enchanting prose, Hill explains the Sierra's many natural wonders. Her work is spiked with entertaining historical anecdotes. . . . She not only points out the many attractions (and the best places to see them) but puts them in perspective. What makes Yosemite so beautiful? She'll tell you." Sacramento Bee "It's an armchair traveler's delight and remains an authoritative guide that will well serve a new generation of hikers, campers, and explorers."

40. Los Angeles Area Geology During the mid to late 1800 s, there was gold fever here. The following sections will give more detailed descriptions of each areas geology. http://www.scvresources.com/geology/

Los Angeles Area Geology Welcome to the Los Angeles Geology Page. This site will cover some of the more unique aspects of the geology around Los Angeles. I hope to cover each valley and mountain range. Watch for updates in the coming weeks! Mountains San Gabriel Mountains San Bernardino Mountains Santa Monica Mountains Puente Hills Santa Susana Mountains Valleys the main Los Angeles basin San Fernando Valley San Gabriel Valley Chino and Corona area San Bernardino Valley Simi Valley Thousand Oaks area Santa Clarita Valley Geological Drives Information on the San Andreas Fault Current Earthquake Report from CalTech Los Angeles Area earthquake map from USGS Geology outside of the Los Angeles Area - Special Reports Death Valley Geology - Photos and Information Geologic Time Scale Glossary of Geologic Terms used List of resources used Links to other Geology sites About Me, Michael Ballard. Comments, Suggestions, Questions? E-mail me at webmaster @ scvresources.com (remove spaces) Return to Main Page This was updated on : January 24, 2008

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