Cave Development in Strata of Ordovician-And Silurian-Devonian- Age in Highland County, Virginia
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2Nd International Trilobite Conference (Brock University, St. Catharines, Ontario, August 22-24, 1997) ABSTRACTS
2nd International Trilobite Conference (Brock University, St. Catharines, Ontario, August 22-24, 1997) ABSTRACTS. Characters and Parsimony. Jonathan M. Adrain, Department of Palaeontology, The Natural History Museum, London SW7 5BD, United King- dom; Gregory D. Edgecombe, Centre for Evolutionary Research, Australian Museum, 6 College Street, Sydney South, New South Wales 2000, Australia Character analysis is the single most important element of any phylogenetic study. Characters are simply criteria for comparing homologous organismic parts between taxa. Homology of organismic parts in any phylogenetic study is an a priori assumption, founded upon topological similarity through some or all stages of ontogeny. Once homolo- gies have been suggested, characters are invented by specifying bases of comparison of organismic parts from taxon to taxon within the study group. Ideally, all variation in a single homology occurring within the study group should be accounted for. Comparisons are between attributes of homologous parts, (e.g., simple presence, size of some- thing, number of something), and these attributes are referred to as character states. Study taxa are assigned member- ship in one (or more, in the case of polymorphisms) character-state for each character in the analysis. A single char- acter now implies discrete groupings of taxa, but this in itself does not constitute a phylogeny. In order to suggest or convey phylogenetic information, the historical status of each character-state, and of the the group of taxa it sug- gests, must be evaluated. That is, in the case of any two states belonging to the same character, we need to discover whether one state is primitive (broadly speaking, ancestral) or derived (representative of an evolutionary innovation) relative to the other. -
Figure 3A. Major Geologic Formations in West Virginia. Allegheney And
82° 81° 80° 79° 78° EXPLANATION West Virginia county boundaries A West Virginia Geology by map unit Quaternary Modern Reservoirs Qal Alluvium Permian or Pennsylvanian Period LTP d Dunkard Group LTP c Conemaugh Group LTP m Monongahela Group 0 25 50 MILES LTP a Allegheny Formation PENNSYLVANIA LTP pv Pottsville Group 0 25 50 KILOMETERS LTP k Kanawha Formation 40° LTP nr New River Formation LTP p Pocahontas Formation Mississippian Period Mmc Mauch Chunk Group Mbp Bluestone and Princeton Formations Ce Obrr Omc Mh Hinton Formation Obps Dmn Bluefield Formation Dbh Otbr Mbf MARYLAND LTP pv Osp Mg Greenbrier Group Smc Axis of Obs Mmp Maccrady and Pocono, undivided Burning Springs LTP a Mmc St Ce Mmcc Maccrady Formation anticline LTP d Om Dh Cwy Mp Pocono Group Qal Dhs Ch Devonian Period Mp Dohl LTP c Dmu Middle and Upper Devonian, undivided Obps Cw Dhs Hampshire Formation LTP m Dmn OHIO Ct Dch Chemung Group Omc Obs Dch Dbh Dbh Brailler and Harrell, undivided Stw Cwy LTP pv Ca Db Brallier Formation Obrr Cc 39° CPCc Dh Harrell Shale St Dmb Millboro Shale Mmc Dhs Dmt Mahantango Formation Do LTP d Ojo Dm Marcellus Formation Dmn Onondaga Group Om Lower Devonian, undivided LTP k Dhl Dohl Do Oriskany Sandstone Dmt Ot Dhl Helderberg Group LTP m VIRGINIA Qal Obr Silurian Period Dch Smc Om Stw Tonoloway, Wills Creek, and Williamsport Formations LTP c Dmb Sct Lower Silurian, undivided LTP a Smc McKenzie Formation and Clinton Group Dhl Stw Ojo Mbf Db St Tuscarora Sandstone Ordovician Period Ojo Juniata and Oswego Formations Dohl Mg Om Martinsburg Formation LTP nr Otbr Ordovician--Trenton and Black River, undivided 38° Mmcc Ot Trenton Group LTP k WEST VIRGINIA Obr Black River Group Omc Ordovician, middle calcareous units Mp Db Osp St. -
Stratigraphy, Structure, and Tectonics: an East-To-West Transect of the Blue Ridge and Valley and Ridge Provinces of Northern Virginia and West Virginia
FLD016-05 2nd pgs page 103 The Geological Society of America Field Guide 16 2010 Stratigraphy, structure, and tectonics: An east-to-west transect of the Blue Ridge and Valley and Ridge provinces of northern Virginia and West Virginia Lynn S. Fichter Steven J. Whitmeyer Department of Geology and Environmental Science, James Madison University, 800 S. Main Street, Harrisonburg, Virginia 22807, USA Christopher M. Bailey Department of Geology, College of William & Mary, Williamsburg, Virginia, USA William Burton U.S. Geological Survey, Reston, Virginia 22092, USA ABSTRACT This fi eld guide covers a two-day east-to-west transect of the Blue Ridge and Valley and Ridge provinces of northwestern Virginia and eastern West Virginia, in the context of an integrated approach to teaching stratigraphy, structural analysis, and regional tectonics. Holistic, systems-based approaches to these topics incorpo- rate both deductive (stratigraphic, structural, and tectonic theoretical models) and inductive (fi eld observations and data collection) perspectives. Discussions of these pedagogic approaches are integral to this fi eld trip. Day 1 of the fi eld trip focuses on Mesoproterozoic granitoid basement (associated with the Grenville orogeny) and overlying Neoproterozoic to Early Cambrian cover rocks (Iapetan rifting) of the greater Blue Ridge province. These units collectively form a basement-cored anticlinorium that was thrust over Paleozoic strata of the Val- ley and Ridge province during Alleghanian contractional tectonics. Day 2 traverses a foreland thrust belt that consists of Cambrian to Ordovician carbonates (Iapetan divergent continental margin), Middle to Upper Ordovician immature clastics (asso- ciated with the Taconic orogeny), Silurian to Lower Devonian quartz arenites and car- bonates (inter-orogenic tectonic calm), and Upper Devonian to Lower Mississippian clastic rocks (associated with the Acadian orogeny). -
Organism-Sediment Relationships in Silurian Marine Environments
ORGANISM-SEDIMENT RELATIONSHIPS IN SILURIAN MARINE ENVIRONMENTS by C. E. BRETT ABSTRACT.Organisms pIayed major roles as producers and modifiers of sediments in many Silurian marine env~ronments.Pelrnarozoan skeietal debris famed extensive shoals and banks in many high-enerw, tropical environments : algae. bvozoans. tabulate corals. and strematoporoids were the major skeieral contributors to reeial buridups common in mid and late SiIunan subtropical shelves. ArtlcuIare brachiopods and Lesser numben oiosrracodes, trilobites, and molluscs formed extensive. although reIatively !Em (5-15 mi. shell beds in shaIloiv shelf fac~es:pefagc. cephalopod limestones characrerized the circum-Gondwana region. Skeletd hard substrates and hardgrounds supported relarively complex eprfaunal suspenaan-feeding communities. The apparent scarclry of encollthic sponges and bivalves indicates thac rates of hard subsrrare bioerosron were far below those of post-Palaeozolc times. Substra~eselection. spatial compeotion. anc porarlry of c:Tpnc versus exposed subcommun~tiesare clearly evidenr. for the first rzme. in Ordovician to latesr Siiurian hard substrate cornrnuniries. Unconsoi~datedsediments displayed a wide variety of characrerisrtc trace and body fossd assoclatlons that were. to some degree. subsrrare conrrolled. Sand and silt subsrrates mpporred a low die'ersltv oi shelly organisms bur preserved abundant rraccs, nngmg from fkoiirhas ana .-~rthropir~cus-aomina~ed nensshore sed~mentsro offshore diverse ichnolicles. Some Silur~annearshore sediments display b~orurbat~on up to Im deep and contaln very Fen epifaunal organisms. susgesting destabiiizat~onof substrares. However. b1ogentc disturbance of offsfshore, soft substrates rematned relat~velyresrricted In the Sllur~anwnh tnfauna extenarng onlv abour 1C-15 cm tnro the sediment. Silunan epthunai organlrrns dispIayea varled morpnolo_eical ad~ptationsrs soft substrates. -
Illustration.Pdf
exio GENERALIZED SECTION OF THE ROCKS IN THE HOLLIDAYSBURG AND HUNTINGDON QUADRANGLES SCALE: 1 INCH = 1000 FEET SYSTEM SERIES GROUP THICKNESS FORMATION. SYMBOL SECTION IN FEET MINOR DIVISIONS CHARACTER OF MEMBERS GENERAL CHARACTER OF FORMATIONS PENNSYL- Brookville coal member. Probably 41 to 5 feet thick. Impure; inferior quality. Shale and sandstone with workable coal beds. VANIAN Allegheny formation. Ca ^-^^50 Homewood sandstone member Coarse thick -bedded sandstone. Mercer shale member Clay, coal, and shale 130 300 Mainly coarse sandstone with shale, coal, and clay in middle. Pottsville formation Cpv ^JcrorgTqoijuuuuiMranacxx Connoquenessing sandstone member. Coarse thick-bedded sandstone. _ -~ '~^^~^~=^ In Hollidaysburg quadrangle coarse, lumpy, red and green shale, mostly red; 80 feet of sandstone at bottom. CARBONIFEROUS Mauch Chunk formation. Cmc 180-1000 In Huntingdon quadrangle a little yellowish-green sandstone in midst of red shale and at top; at bottom, V-'i' -V-' r'-'i'.v: 'i ' '!' ' Trough Creek limestone member, red and gray, coarsely crystalline. ~~~~^-- _ ^&>;&^:^&;& Siliceous cross-bedded limestone. (Cb) (300-500) Burgoon sandstone member Rather coarse micaceous, arkosic yellowish or greenish-gray thick-bedded MISSISSIPPI sandstone. Patton shale member. _- - - -- - Red shale on Allegheny Front and westward. Pocono formation. Cpo 990 Lower 700 feet in Hollidaysburg quadrangle, shale and sandstone, considerable red shale. Lower 900 feet in Huntingdon quadrangle, shale, sandstone, and conglomerate, very little red shale. Shale mostly stiff, imperfectly fissile, greenish. ^-j-i-^-'. ' "*" '.. '' _» =y^=-^-- "ZZT??*?1^^ - .-T^ ' ' - ' ' ' ^ About 80 percent bright red shale, alternating with layers of reddish or brown sandstone, which is generally 8000- thick-bedded and medium-grained. Some laminated layers. The red .shale is in places mottled with Hampshire formation. -
A Billion Years of Deformation in the Central Appalachians: Orogenic Processes and Products
Downloaded from fieldguides.gsapubs.org on October 15, 2015 The Geological Society of America Field Guide 40 2015 A billion years of deformation in the central Appalachians: Orogenic processes and products Steven J. Whitmeyer Department of Geology and Environmental Science, James Madison University, Harrisonburg, Virginia 22807, USA Christopher M. Bailey Department of Geology, College of William & Mary, Williamsburg, Virginia 23187, USA David B. Spears Virginia Department of Mines, Minerals, and Energy, Division of Geology and Mineral Resources, Charlottesville, Virginia 22903, USA ABSTRACT The central Appalachians form a classic orogen whose structural architecture developed during episodes of contractional, extensional, and transpressional defor- mation from the Proterozoic to the Mesozoic. These episodes include components of the Grenville orogenic cycle, the eastern breakup of Rodinia, Appalachian orogenic cycles, the breakup of Pangea, and the opening of the Atlantic Ocean basin. This fi eld trip examines an array of rocks deformed via both ductile and brittle processes from the deep crust to the near-surface environment, and from the Mesoproterozoic to the present day. The trip commences in suspect terranes of the eastern Piedmont in central Vir- ginia, and traverses northwestward across the Appalachian orogen through the thick- skinned Blue Ridge basement terrane, and into the thin-skinned fold-and-thrust belt of the Valley and Ridge geologic province. The traverse covers a range of deformation styles that developed over a vast span of geologic time: from high-grade metamorphic rocks deformed deep within the orogenic hinterland, to sedimentary rocks of the fore- land that were folded, faulted, and cleaved in the late Paleozoic, to brittle extensional structures that overprint many of these rocks. -
Key, M. M., Jr. and N. Potter, Jr. 1992
Guidebook for the llth Annual Field Trip of the Harrisburg Area Geological Society May 9, 1992 Paleozoic Geology of the Paw Paw-Hancock Area of Maryland and West Virginia by Marcus M. Key, Jr. and Noel Potter, Jr. Dickinson College TABLE OF CONTENTS . .. List of F1gures . .............................................. 111 Introduction . ....................................... · ......... 1 Road Log • ..•... • ..... · .... • •.....•....•...•......• e ••• '0 ••••••••• 3 Stop 1. Roundtop Hill . ............ o •••••••••• o •••••••••••••••••• 5 stop 2. Sideling Hill Road Cut ..•.••............••.••••......... 8 Stop 3. Sideling Hill Diamictite Exposure ....•.•....•.•....•... 11 Stop 4. Cacapon Mountain Overlook .••.......•......•.•••••...... 15 Stop 5. Fluted Rocks Overlook .•..•••.••....•.•.•••.•........... 16 Stop 6. Fluted Rocks ................. .,. .......... ., o ••••• ., •••••• • 19 Stop 7. Berkeley Springs state Park •...•.....................•. 20 Acknowled·gments . ........................... :- ... e ••••••••••••••• 21 References .....••.•..•.•••.•..•.•..•.••......................•. 2 2 Topogrpphic maps covering field trip stops: USGS 7 1/2 minute quadrangles Bellegrove (MD-PA-WV), Great Cacapon (WV-MD), Hancock (WV-MD-PA) Cover Photo: Anticline in Silurian Bloomsburg Formation. From Stose and swartz (1912). The anticline is visible from the towpath of the c & 0 Canal at Roundtop Hill (Stop# 1). Guidebook copies may be obtained by writing: Harrisburg Area Geological Society cjo Pennsylvania Geological Survey P.O. Box 2357 Harrisburg, -
Rocks of Augusta, Rockingham Highland, and Bath Counties, Virginia
COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES FIELD TRIP TO THE IGNEOUS ROCKS OF AUGUSTA, ROCKINGHAM HIGHLAND, AND BATH COUNTIES, VIRGINIA ROBERT W. JOHNSON, JR. CHARLES MILTON, AND JOHN M. DENNISON INFORMATION CIRCUI.AR I 6 VIRGINIA DIVISION OF MINERAL RESOURCES Jomes L. Colver Commissioner of Minerol Resources ond Stote Geologist CHARLOTTESVILLE, VIRGINIA 't971 COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES FIELD TRIP TO THE IGNEOUS ROCKS OF AUGUSTA, ROCKINGHAM, HIGHLAND, AND BATH COUNTIES, VIRGINIA ROBERT W. JOHNSON, JR. CHARLES MILTON, AND JOHN M. DENNISON INFORMATION CIRCULA,R I 6 VIRGINIA DIVISION OF MINERAL RESOURCES Jomes L. Colver Commissioner of Minerol Resources ond Stoie Geologisl CHARLOTTESVILLE, VI RGINIA 1971 CoMMoNWEALTH or VIncrr.rr.l DnrAnt1vrsNr or Puncnesss AND Suppl,y RTCHMoND !97L Portions of this publication may be quoted if credit is given to the Virginia Division of Mineral Resources. It is recomrnended that reference to this repor."t be made in the following form: Johnson, R, W., Jr., Milton, Charles, and Dennison, J. M., 1971, Field trip to the igneous rocks of Augusta, Rockingham, I{ighland, and Bath counties, Virginia: Virginia Division of Mineral Resources Information Circ. 16, 68 p. DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond, Virginia MARVIN M. SumnnLAND, Director Culnlps A. CnnrsropHERsEN, DeputA Director A. S. RlcnAL, JR., E*ecutiae Assi,stant BOARD Wrllrlu H. KrNc, Burkeville, Chuirman Wrr,r,rAu H. Sraxn,q.cEN, Alexandria, Vi,ce Chairman D. HnNny ALMoND, Richmond Ml.ron T. BENToN, Suffolk Josnps C. Canrnn, Jn., Richmond Aoor,r' U. -
Geology of the Elkton Area Virginia
Geology of the Elkton area Virginia GEOLOGICAL SURVEY PROFESSIONAL PAPER 230 Geology of the Elkton area Virginia By PHILIP B. KING GEOLOGICAL SURVEY PROFESSIONAL PAPER 230 A detailed report on an area containing interesting problems of stratigraphy', structure, geomorphology, and economic geology UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1950 UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1.75 (paper cover) CONTENTS Page Page Abstract-- _ ________________________________________ 1 Stratigraphy—Continued Introduction. ______________________________________ 1 Cambrian system—Continued Previous work. _ ____________________________________ 2 Elbrook dolomite.________-_____._--_-__-__. 32 Present work. ______________________________________ 3 Name._ _____________-_-_-____---_____- 32 Acknowledgments. _________________________________ 3 Outcrop.____-___-------_--___----.-___ 32 Geography.. _ ______________________________________ 4 Character, _____________________________ 32 Stratigraphy _______________________________________ 6 Age_.____-_..-__-_---_--___------_-_._ 32 Pre-Cambrian rocks__ . __________________________ 7 Residuum of Elbrook dolomite ___________ 33 Injection complex. __________________________ 8 Stratigraphic relations-__________________ 33 Name. _ ----_-______----________-_-_-__ 8 Conococheague limestone.___________________ 33 Outcrop. ______________________________ -
Geologic Names of North America Introduced in 19364955
Geologic Names of North America Introduced in 19364955 ^GEOLOGICAL SURVEY BULLETIN 1056-A Names of North America Introduced in 1936-1955 By DRUID WILSON, WILLIAM J. SANDO? and RUDOLPH W. KOPF Prepared with the assistance of BARBARA BEDETTE, JEAN L. EGGLETON, GRACE C. KEROHER, CAROLYN MANN, WILLIAM G. MELTON, JR., KATHERINE DENNISON PALMER, and JACK E. SMEDLEY GEOLOGIC NAMES OF NORTH AMERICA -G E O L O G I C AL SURVEY BULLETIN 1056-A A compilation of new geologic names of North America, including Greenland, the finest Indies, the Pacific Island pos sessions of the United States, and the Trust Territory of the Pacific Islands UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1957 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director ' For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1. (paper cover) FOEEWOBD The "Lexicon of geologic names of the United States" by M. Grace Wilmarth, published in 1938 and reprinted in 1951 and 1957, met a long standing need and continuing demand for a compilation of geologic names. Plans made for future compilations as new names and revisions appeared were interrupted during the years of World War II. In 1952 a sustained effort was begun toward review of geo logic publications necessary to furnish a background for preparation of a new edition. After the review was brought up to date in 1956, the present compilation was prepared in order to furnish to the geo logic profession, as quickly as possible, some of the essential data concerning the new names that have appeared since 1935. -
Silurian Times 2007
SILURIAN TIMES No. 15 Year 2007 (July 2008) CONTENTS OF SILURIAN TIMES No. 15: ISSS 2 List of voting and corresponding members of the ISSS 3 Chairman’s Corner & Editor's Notes 4 Web Site for the Silurian Subcommission 4 Annual Report of the Sub-Commission on Silurian Stratigraphy on 2007 5 – 9 Message from the President of the IUGS to the secretary of the IUGS 9 Report of the Subcommission on Silurian Stratigraphy Restudying the Global Stratotype for the base of the Wenlock: report by David Loydell 10-12 Future Meetings of the ISSS 13-22 Silurian Research 2007 23-32 Silurian Publications 2007 33-40 New Names, Address Changes 40 41 E-Mail Addresses readers of Silurian Times 42-46 SILURIAN TIMES A NEWSLETTER OF THE INTERNATIONAL SUBCOMMISSION ON SILURIAN STRATIGRAPHY (ISSS) INTERNATIONAL COMMISSION ON STRATIGRAPHY INTERNATIONAL UNION OF GEOLOGICAL SCIENCES President: Prof. Zhang Hongren (China) Secretary General: Dr. Peter T. Bobrowsky (Canada) http://www.iugs.org/ I NTERNATIONAL COMMISSION ON STRATIGRAPHY Chairman: Dr. Felix Gradstein (Norway) Vice-Chairman: Prof. Stanley Finney (USA) Secretary-General: Prof. James G. Ogg (USA) http://www.stratigraphy.org/ INTERNATIONAL SUBCOMMISSION ON SILURIAN STRATIGRAPHY (ISSS) Subcommission officers Outgoing Chairman: Rong Jiayu, Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39# East Beijing Road, Nanjing, 210008, P R China, e-mail: [email protected] Chairman (sept. 2008-2012): Michael J. Melchin, Professor, Department of Earth Sciences, St. Francis Xavier University, P.O. Box 5000, Antigonish, Nova Scotia B2G 2W5, Canada, e-mail: [email protected]. -
Fracture Analysis and Dye Trace Report Fracture Analysis and Dye Trace Report
ATLANTIC COAST PIPELINE, LLC ATLANTIC COAST PIPELINE and DOMINION ENERGY TRANSMISSION, INC. SUPPLY HEADER PROJECT Implementation Plan EC26 Attachment 1 Fracture Analysis and Dye Trace Report Fracture Analysis and Dye Trace Report Dominion ACP Augusta, Bath and Highland Counties, Virginia & Pocahontas and Randolph Counties, West Virginia August 30, 2017 19955 Highland Vista Drive, Suite 170 Ashburn, Virginia 20147 703-726-8030 19955 Highland Vista Dr., Suite 170 Ashburn, Virginia 20147 (703) 726-8030 www.geoconcepts-eng.com August 30, 2017 Colin Olness, PE Contractor Atlantic Coast Pipeline - Construction 99 Edmiston Way Buckhannon, WV 26201 Subject: Fracture Analysis and Dye Trace Report Dominion ACP, Augusta, Bath and Highland Counties, Virginia & Pocahontas and Randolph Counties, West Virginia (GeoConcepts Project No. 11002.04) Dear Mr. Olness: GeoConcepts Engineering, Inc. (GeoConcepts) is pleased to present this fracture analysis and existing dye trace report for the proposed Atlantic Coast Pipeline. Sincerely, GEOCONCEPTS ENGINEERING, INC. Joshua D. Valentino, PhD Robert K. Denton Jr., CPG, LPSS Senior Staff Geologist Senior Geologist [email protected] [email protected] Table of Contents Executive Summary ............................................................................................................................. 1 Introduction........................................................................................................................................ 1 Scope of Services ...............................................................................................................................