Geology of Virginia Introduction and Geologic Background CD-ROM 1
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DECEMBER 2014201 VOLUME 23~ ISSUE 12 Lynchburg, VA, Inc
GEM & MINERAL JOURNAL Official Monthly Publication of the Gem & Mineral Society of DECEMBER 2014201 VOLUME 23~ ISSUE 12 Lynchburg, VA, Inc WWW.LYNCHBURGROCKCLUB.ORG Presidents Message: Hello To All, will supply the delicious fried chicken so we are counting What a great auction at the November GMSL meeting. on everyone else to bring in vegetables, pasta salads, We picked out a lot of different specimens in hopes of potato salads etc, and please don’t forget some sweet having something for everyone to bid on. It was a great desserts. We also have a Dirty Santa gift exchange. All success because of all the members and visitors that you need to do to participate is bring in a wrapped gift of came out and participated. A big thank you to all. I hope about $15.00 value that is hobby related. All gifts will be everyone got a nice specimen to add to their collection. It placed on a table and each person will draw a number, may be a long time, if ever, we are able to have such nice which will be the order for opening the gifts. Number one pieces as the Burmese Jade, beautiful Agates, and nice will choose a package and open it. Number two will then pieces of Turquoise just to name a few of the most open a gift and if the previously opened gift is more to popular specimens. We will keep our eyes open for their liking they can make a trade, and so on until all gifts collections for sale in the future. -
Hypersthene Syenite and Related Rocks of the Blue Ridge Region, Virginia1
BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA V o l. 27, pp. 193-234 June 1, 1916 HYPERSTHENE SYENITE AND RELATED ROCKS OF THE BLUE RIDGE REGION, VIRGINIA1 BY THOMAS L. WATSON AND JUSTUS H. CLINE (Presented before the Society December 29, 191k) CONTENTS Page Introduction.................................................................................................................. 194 Previous geologic work............................................................................................. 196 Quartz-bearing hypersthene-andesine syenite...................................................... 197 Distribution.......................................................................................................... 197 Megascopic character......................................................................................... 198 Microscopic character........................................................................................ 199 Chemical composition and classification...................................................... 202 Comparison with quartz monzonite.............................................................. 204 Origin and application of name............................................................. 204 Chemical composition................................................................................ 205 Comparison with akerite.................................................................................. 206 Comparison with syenite (andesine anorthosite) of Nelson County, Virginia............................................................................................................. -
Scenic Landforms of Virginia
Vol. 34 August 1988 No. 3 SCENIC LANDFORMS OF VIRGINIA Harry Webb . Virginia has a wide variety of scenic landforms, such State Highway, SR - State Road, GWNF.R(T) - George as mountains, waterfalls, gorges, islands, water and Washington National Forest Road (Trail), JNFR(T) - wind gaps, caves, valleys, hills, and cliffs. These land- Jefferson National Forest Road (Trail), BRPMP - Blue forms, some with interesting names such as Hanging Ridge Parkway mile post, and SNPMP - Shenandoah Rock, Devils Backbone, Striped Rock, and Lovers Leap, National Park mile post. range in elevation from Mt. Rogers at 5729 feet to As- This listing is primarily of those landforms named on sateague and Tangier islands near sea level. Two nat- topographic maps. It is hoped that the reader will advise ural lakes occur in Virginia, Mountain Lake in Giles the Division of other noteworthy landforms in the st& County and Lake Drummond in the City of Chesapeake. that are not mentioned. For those features on private Gaps through the mountains were important routes for land always obtain the owner's permission before vis- early settlers and positions for military movements dur- iting. Some particularly interesting features are de- ing the Civil War. Today, many gaps are still important scribed in more detail below. locations of roads and highways. For this report, landforms are listed alphabetically Dismal Swamp (see Chesapeake, City of) by county or city. Features along county lines are de- The Dismal Swamp, located in southeastern Virginia, scribed in only one county with references in other ap- is about 10 to 11 miles wide and 15 miles long, and propriate counties. -
Mineral Collecting Sites in North Carolina by W
.'.' .., Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie RUTILE GUMMITE IN GARNET RUBY CORUNDUM GOLD TORBERNITE GARNET IN MICA ANATASE RUTILE AJTUNITE AND TORBERNITE THULITE AND PYRITE MONAZITE EMERALD CUPRITE SMOKY QUARTZ ZIRCON TORBERNITE ~/ UBRAR'l USE ONLV ,~O NOT REMOVE. fROM LIBRARY N. C. GEOLOGICAL SUHVEY Information Circular 24 Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie Raleigh 1978 Second Printing 1980. Additional copies of this publication may be obtained from: North CarOlina Department of Natural Resources and Community Development Geological Survey Section P. O. Box 27687 ~ Raleigh. N. C. 27611 1823 --~- GEOLOGICAL SURVEY SECTION The Geological Survey Section shall, by law"...make such exami nation, survey, and mapping of the geology, mineralogy, and topo graphy of the state, including their industrial and economic utilization as it may consider necessary." In carrying out its duties under this law, the section promotes the wise conservation and use of mineral resources by industry, commerce, agriculture, and other governmental agencies for the general welfare of the citizens of North Carolina. The Section conducts a number of basic and applied research projects in environmental resource planning, mineral resource explora tion, mineral statistics, and systematic geologic mapping. Services constitute a major portion ofthe Sections's activities and include identi fying rock and mineral samples submitted by the citizens of the state and providing consulting services and specially prepared reports to other agencies that require geological information. The Geological Survey Section publishes results of research in a series of Bulletins, Economic Papers, Information Circulars, Educa tional Series, Geologic Maps, and Special Publications. -
Jun 2012 Rockhounder Starting Point
Page 1 THE JUNE 2 0 1 2 ROCKHOUNDER PURPOSE: The purpose of the Gem, Lapidary, and Mineral Society of Montgomery County MD., Inc. is “To increase knowledge and popular interest in earth sciences, geology, mineralogy, paleontology, lapidary arts, and related subjects.” REGULAR MEETING: Meetings are held the 2nd Monday of the month from September to June. The Society will meet on Monday June 11th in the dining room of the Rockville Senior Center, 1150 Carnation Drive, Rockville. A short business meeting will begin at 7:45 pm but the room is available to us at 7:30 pm so come early and chat with old friends. The speaker will Bob Farrar . The topic will be “The Cruzeiro Mine: World's Greatest Tourmaline Mine.” Bob Farrar has been collecting rocks, minerals, and fossils for over 40 years. He has traveled extensively in pursuit of rock collecting, including making several trips to Brazil. He has written a number of articles about his travels for Rock & Gem and other publications. Bob holds a Ph. D. in entomology, and works for the U. S. Dept. Of Agriculture in Beltsville, MD. A resident of Bowie, he is also a dealer of Minerals & Fossils. THE BOARD OF DIRECTORS will possibly meet Monday, June 18, at the Home of Andy Muir. The President will notify Board members if a meeting is necessary. All Board members are expected to at- tend if meeting is called. Any member is welcome to attend but kindly let Andy know if you plan to attend at: <[email protected]> or phone 301 990 1370. -
Catoctin Formation
Glimpses of the Past: THE GEOLOGY of VIRGINIA The Catoctin Formation — Virginia is for Lavas Alex Johnson and Chuck Bailey, Department of Geology, College of William & Mary Stony Man is a high peak in Virginia’s Blue Ridge Mountains that tops out at just over 1200 m (4,000’). Drive south from Thornton Gap along the Skyline Drive and you’ll see the impressive cliffs of Stony Man’s northwestern face. These are the cliffs that give the mountain its name, as the cliffs and slopes have a vague resemblance to a reclining man’s forehead, eye, nose, and beard. Climb to the top and you’ll see peculiar bluish-green rocks exposed on the summit that are ancient lava flows, part of a geologic unit known as the Catoctin Formation. From the presidential retreat at Camp David to Jefferson’s Monticello, from Harpers Ferry to Humpback Rocks, the Catoctin Formation underlies much of the Blue Ridge. This distinctive geologic unit tells us much about the long geologic history of the Blue Ridge and central Appalachians. Stony Man’s summit and northwestern slope, Shenandoah National Park, Virginia. Cliffs expose metabasaltic greenstone of the Neoproterozoic Catoctin Formation. (CMB photo). Geologic cross section of Stony Man summit area (modified from Badger, 1999). The Catoctin Formation was first named by Arthur Keith in 1894 and takes its name for exposures on Catoctin Mountain, a long ridge that stretches from Maryland into northern Virginia. The word Catoctin is rooted in the old Algonquin term Kittockton. The exact meaning of the term has become a point of contention; among historians the translation “speckled mountain” is preferred, however local tradition holds that that Catoctin means “place of many deer” (Kenny, 1984). -
Booker T. Washington National Monument
National Park Service U.S. Department of the Interior Natural Resource Program Center Booker T. Washington National Monument Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2010/234 THIS PAGE: A spring box, used as an early refrig- erator. Holes at each end of the box allow fresh, cool water to flow through, keeping perishables cool and fresh for several days at a time. ON THE COVER: The kitchen cabin (right) and smoke- house, historic buildings on the Burroughs Plantation where Booker T. Washington lived as a boy. National Park Service photographs courtesy Timbo Sims (Booker T. Wash- ington National Monument) Booker T. Washington National Monument Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2010/234 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 August 2010 U.S. Department of the Interior National Park Service Natural Resource Program Center Fort Collins, Colorado The National Park Service, Natural Resource Program Center publishes a range of reports that address natural resource topics of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. -
Geology and Mineral Deposits of the Roseland District of Central Virginia
Geology and Mineral Deposits of the Roseland District of Central Virginia U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1371 Geology and Mineral Deposits of the Roseland District of Central Virginia By NORMAN HERZ and ERIC R. FORCE U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1371 Relations among anorthosite, ferrodioritic rocks, and titanium-mineral deposits in Nelson and Amherst Counties in the Blue Ridge of Virginia UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1987 DEPARTMENT OF THE INTERIOR DONALD PAUL HODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Herz, Norman, 1923- Geology and mineral deposits of the Roseland district of central Virginia. (U.S. Geological Survey professional paper; 1371) Bibliography: p. Supt. of Docs, no.: I 19.16:1371 1. Geology-Virginia-Roseland Region. 2. Mines and mineral resources- Virginia-Roseland Region. I. Force, Eric R. II. Title. III. Series: Geological Survey professional paper ; 1371. QE174.R67H47 1987 557.55'49 85-600280 For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 CONTENTS Page Abstract_____________________________ 1 Post-Grenville rocks-Continued Introduction_________________. 1 Surficial deposits ___ 33 General geologic and economic setting _. I Deposits of present valley systems _____________ 33 Previous geological work ____________ 3 Inactive boulder fans ______________________ 33 Mapping and stratigraphy _____. 3 Ridgetop gravel deposits ______________________ 33 Economic geology _________. 4 Radiometric age determinations ____________________ 33 Proposed lithologic units _______. 4 Previous determinations in the region ______________ 33 Field work _______________________ 5 New age data __________________ 34 Acknowledgments _________________ 5 Petrogenesis of the igneous rocks _____________________ 35 Pre-Grenville and Grenville rocks _________ 6 Origin of anorthosite and ferrodiorites ______________ 35 Banded granulites and associated rocks. -
GEMSTONES by Donald W
GEMSTONES By Donald W. Olson Domestic survey data and tables were prepared by Christine K. Pisut, statistical assistant, and the world production table was prepared by Glenn J. Wallace, international data coordinator. Gemstones have fascinated humans since prehistoric times. sustaining economically viable deposits (U.S. International They have been valued as treasured objects throughout history Trade Commission, 1997, p. 23). by all societies in all parts of the world. The first stones known The total value of natural gemstones produced in the United to have been used for making jewelry include amber, amethyst, States during 2001 was estimated to be at least $15.1 million coral, diamond, emerald, garnet, jade, jasper, lapis lazuli, pearl, (table 3). The production value was 12% less than the rock crystal, ruby, serpentine, and turquoise. These stones preceding year. The production decrease was mostly because served as status symbols for the wealthy. Today, gems are not the 2001 shell harvest was 13% less than in 2000. worn to demonstrate wealth as much as they are for pleasure or The estimate of 2001 U.S. gemstone production was based on in appreciation of their beauty (Schumann, 1998, p. 8). In this a survey of more than 200 domestic gemstone producers report, the terms “gem” and “gemstone” mean any mineral or conducted by the USGS. The survey provided a foundation for organic material (such as amber, pearl, and petrified wood) projecting the scope and level of domestic gemstone production used for personal adornment, display, or object of art because it during the year. However, the USGS survey did not represent possesses beauty, durability, and rarity. -
Gneiss Times
VOLUME 49, Issue 4 APRIL 2017 GNEISS TIMES Wickenburg Gem & Mineral Society, Inc. P.O. Box 20375, Wickenburg, Arizona, 85358 E-Mail — [email protected] www.wickenburggms.org The purpose of this organization shall be to educate and to provide fellowship for people interested in rocks and minerals; to foster love and appreciation of minerals, rocks, gems, and the Earth. The name ‘epidote’ was derived from the Greek EPIDOTE “epidosis”, for “increase”, in allusion to crystals By Susan Celestian having one side longer at the base. Epidote is a fairly abundant rock-forming mineral. Of secondary origin, either during metamorphosis Epidote is a group classified within the Clinozoisite or hydrothermal alteration, epidote is commonly Group, along with the Allanite Group, the found among the igneous and metamorphic rocks Ȁskagenite Group, and the Dollaseite Group. The of Arizona. Crystals are commonly encountered in Epidote minerals are Epidote-(Pb) or Hancockite, Arizona; however, the more common massive and Epidote-(Sr). And it forms a series with pistachio-green rocks make an interesting lapidary Clinozoisite, with the latter being more iron-rich. material. It is in the Monoclinic System, which has three axes o 3+ of different lengths, and no 90 angles. When you Formula: Ca2Fe Al2(Si2O7)(SiO4)O(OH) (Copper Iron Aluminum Silicate Oxide Hydroxide) find simple prismatic crystals, you may at first think Crystal System: Monoclinic you are looking at a 4-sided column, with a square Crystal Forms: Prismatic (long slender; cross-section. But look closely! None of the o sometimes striated), fibrous, wheat-sheaf groups, edges will meet at 90 . -
Commercial Granites and Other Crystalline Rocks of Virginia
T>WArA,J- l/a-tt you have no 'further Pl€ase return this publieation to the Virginia Geo-loEical Survey when use for it' Postage will be refunded' ilTgLOGI TIBflAHY COMMONWEALTH OF VIRGINIA SPR 2 iVo t VIRGINIA CONSERVATION COMMISSION VIRGINIA GEOLOGICAL SURVEY A'RTHUR BEVAN' State Geologict Commercial Granites and Other Crystalline Rocks of Virginia By EDWARD STEIDTMAI{N it13 J ,/' UNIVERSITY, VIRGINIA 1945 ,brl ..)/) COMMONWEALTII OF VIRGINIA VIRGINIA CONSERVATION COMMISSION VIRGINIA GEOLOGICAL SURVEY .A,RTHUR BEVAN, State Geologitt Bulletin 64 Commercial Granites and Other Crystalline Rocks of Virginia By EDWARD STEIDTMANN UNIVERSITY, VIRGINIA 1945 Coacuorwrartn or VrncrNtr Division of Purchase and Printing Richmond 1945 VIRGINIA COI\SERVATION COMMISSION Wrr,r,rarr A. Wnrcnr, Chai,rman, Richmond L. E. Lrcnrono, V,i,ce-Chai,rnmn, Lynchburg Jeues AsHnv, Stafford C. S. CenrBn, Bristol Eowenn W. Laucx, Lutay Geonce Pnruce Annor-r. Assistant C orw ttis si,oner, Richmond Rrcnanp A. Grnrem, E r e c ut i,zt e S e c r e t ar y an d T r e as urar, Richmond lr1 FOREWORD The field work upon which this report is based was conducted mainly during the summers of 1941 and 1942, and the manuscript and illustrations were submitted to the printer on June 5, 1945, dur- ing the administration of Dr. Arthur Bevan as State Geologist, for publication. Because of unprecedented difficulties and delays, beyond the control of the Virginia Geological Survey, this Bulletin was not printed and delivered to us until the date stamped below. The Commonwealth of Virginia and the Virginia Geological Sur- vey suffered a great loss in the untimely death, on May 25, 1948, ol Colonel Edward Steidtmann, the author of this Bulletin. -
COMMONWEALTH of VIRGINIA DEPARTMENT of CONSERVATION and ECONOMIC DEVELOPMENT DIVISION of MINERAL RESOURCES Robert C
VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 27 CONTRIBUTIONS TO VIRGINIA GEOLOGY- IV COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHAR LOTTESVI LLE, VI RGIN IA 1980 VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 27 CONTRIBUTIONS TO VIRGINIA GEOLOGY- IV COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHAR LOTTESVILLE, VIRGINIA 1980 FRONT CoVER: Isoclinal folds (FJ in kyanite quartzite of the Arvonia Forma- tion at woods Mountain, Buckingham county, Virginia. (pocket knife just below center of photo serves as scale.) VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 27 CONTRIBUTIONS TO VIRGINIA GEOLOGY-IV COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHAR LOTTESVI LLE, VI RGI N IA 1980 COMMONWEALTH OF VIRGINIA DEPARTMENT OF PURCHASES AND SUPPLY RICHMOND 1980 DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond, Virginia FRED W. WALKER, Director JERALD F; MOORE, Deputy Director BOARD J. H. JOHNSON, West Point, Chairman ARTHUR P. FLIPPO, Doswell, Vice Chairman FRANK ARMSTRONG, III, Winchester MYRON P. ERKILETIAN, Alexandria HENRY T. N. GRAVES, Luray ADOLF U. HONKALA, Midlothian MILDRED LAYNE, Williamsburg FREDERIC S. REED, Manakin-Sabot GEORGE P. SHAFRAN, Arlington SHELTON H. SHORT,III, Chase City NICHOLAS D. STREET, Grundy E. FLOYD YATES. Powhatan CONTRIBUTIONS TO VIRGINIA GEOTOGY-TV CONTENTS Page Evidence for the correlation of the kyanite quartzites of Willis and Woods mountains with the Arvonia Formation, by James F.