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IC-29 Geology and Ground Water Resources of Walker County, Georgia
IC 29 GEORGIA STATE DIVISION OF CONSERVATION DEPARTMENT OF MINES, MINING AND GEOLOGY GARLAND PEYTON, Director THE GEOLOGICAL SURVEY Information Circular 29 GEOLOGY AND GROUND-WATER RESOURCES OF WALKER COUNTY, GEORGIA By Charles W. Cressler U.S. Geological Survey Prepared in cooperation with the U.S. Geological Survey ATLANTA 1964 CONTENTS Page Abstract _______________________________________________ -··---------------------------- _____________________ ----------------·----- _____________ __________________________ __ 3 In trodu ction ------------------------------------------ ________________________________ --------------------------------------------------------------------------------- 3 Purpose and scope ------------------------------"--------------------------------------------------------------------------------------------------------- 3 Previous inv es tigati o ns ____ _____ ________ _______ __________ ------------------------------------------------------------------------------------------ 5 Geo Io gy _________________________________________________________________ --- ___________________ -- ___________ ------------- __________________ ---- _________________ ---- _______ 5 Ph ys i ogr a p hy ______________________________________________________ ---------------------------------------- __________________ -------------------------------- 5 Geo Io gi c his tory __________________________ _ __ ___ ___ _______ _____________________________________________ ------------------------------------------------- 5 Stratigraphy -·· __________________ -
Overview of the Strategic and Structural Evolution of the Talladega Slate Belt, Alabama Appalachians
fl d029-08 1st pgs page 1 The Geological Society of America Field Guide 29 2012 Overview of the stratigraphic and structural evolution of the Talladega slate belt, Alabama Appalachians James F. Tull* Department of Earth, Ocean, and Atmospheric Science, Florida State University Clinton I. Barineau* Department of Earth and Space Sciences, Columbus State University ABSTRACT The allochthonous Talladega belt of eastern-northeastern Alabama and north- western Georgia is a northeast striking, fault bounded block of lower greenschist facies metasedimentary and metaigneous rocks that formed along the margin of Lau- rentia at or outboard of the seaward edge of the Alabama promontory. Bounded by metamorphic rocks of the higher grade Neoproterozoic(?) to Carboniferous eastern Blue Ridge on the southeast and unmetamorphosed to anchimetamorphic Paleozoic rocks of the Appalachian foreland on the northwest, the Talladega belt includes shelf facies rocks of the latest Neoproterozoic/earliest Cambrian Kahatchee Mountain Group, Cambrian-Ordovician Sylacauga Marble Group, and the latest Silurian(?) to uppermost Devonian/earliest Mississippian Talladega Group. Along the southeast- ern fl ank of these metasedimentary sequences, a Middle Ordovician back-arc terrane (Hillabee Greenstone) was tectonically emplaced along a cryptic pre-metamorphic thrust fault (Hillabee thrust) and subsequently dismembered with units of the upper Talladega Group along the post-metamorphic Hollins Line fault system. Importantly, strata within the Talladega belt are critical for understanding the tectonic evolution of the southern Appalachian orogen when coupled with the geologic history of adjacent terranes. Rocks of the lower Talladega Group, the Lay Dam Formation, suggest latest Silurian-earliest Devonian tectonism that is only now being recognized in other areas of the southern Appalachians. -
Geologic Map of the Scottsboro 7.5-Minute Quadrangle, Jackson County, Alabama
GEOLOGICAL SURVEY OF ALABAMA QUADRANGLE SERIES 63 PLATE (PRINCETON) o 5 o 86 07'30" 581000m E 82 583 5 5 (MUD CREEK) 5 5 5 440,000 FEET 5 5 5 86 00' (WANNVILLE) A 5' 84 85 86 87 R 5 E R 6 E 2'30" 88 89 90 91 34o45' eD D e 34o45' CORRELATION OF MAP UNITS D Mm Mb Mb D Mb D Qal Qal Quaternary Mm CENOZOIC D unconformity 3845000m N D e !pv D 3845 Pennsylvanian D D D Mp !pv D Mb Mb Mh Qal Mississippian D Qal D Mp Mp Mm Qal Qal 3844 D Mtfpm D Qal 38 Mb 44 unconformity Dc Devonian PALEOZOIC Mp Qal 1,540,000 MhD D Qal FEET D e unconformity Mb Mb T 3 S Srm D T 3 S Silurian T 4 S D T 4 S D unconformity D D Mm 3843 D Osli Qal D e D 38 D !pv 43 Mp Qal !pv Onvsr Ordovician unconformity O\k Cambrian D D Qal 3842 Qal e 38 42 MhD MhD DESCRIPTION OF MAP UNITS D Qal Alluvium (Quaternary)—Unconsolidated sand, silt, clay, and chert gravel derived from local bedrock. Mb D D Mb !pv Pottsville Formation (Pennsylvanian)—Light-gray, medium- to coarse-grained, quartzose D D sandstone locally containing scattered to abundant, well-rounded, white quartz pebbles; quartz D D !pv pebble and ferruginous claystone conglomerate is locally present at the base. Interbeds and 38 D 41 Qal 3841 intervals of dark-gray shale and mudstone and wavy-bedded sandstone are locally common. -
Chapter 02 Figure 2.5-209
Bellefonte Nuclear Plant, Units 3 & 4 COL Application Part 2, FSAR Explanation Geologic contact Fault; arrows show relative directional movement Thrust or reverse fault; sawteeth on upper plate, ? ?? Nature of contact uncertain (may posibly be a dashed where inferred, dotted where concealed fault or a stratigraphic contact) U C C' D Normal fault; U on upthrown side, D on Line of cross section downthrown side, dashed where inferred Fault for which sense of movement is unknown; dashed where inferred Qalt Alluvial and low terrace deposits HOLOCENE QUATERNARY Qt High terrace deposits PLEISTOCENE INTERIOR LOW APPALACHIAN VALLEY AND RIDGE PROVINCE PLATEAUS PROVINCE PLATEAUS PROVINCE (western part) (easternpart) Ppv Pottsville Formation Ppv1u Pottsville Formation Ppv2u Pottsville Formation (upper part) (upper part) Ppv2l Pottsville Formation Ppv1l Pottsville Formation (lower part) (lower part) PENNSYLVANIAN PMpw Parkwood Formation Pmpwp Parkwood and Pmpwp Parkwood and Pennington Formations Pennington Formations Pzu Parkwood Formation (undifferentiated) (undifferentiated) Mp Pennington Formation and Floyd Shale (undifferentiated) Mbm Bangor and Monteagle Limestones (undiff.) Pzu Paleozoic Shale Pzu Paleozoic Shale (undifferentiated) (undifferentiated) Mf Floyd Shale Mf Floyd Shale Mh Hartselle Sandstone Mh Hartselle Sandstone Mm Monteagle Limestone Mm MISSISSIPPIAN Monteagle Limestone Mpm Pride Mountain Formation Mpm Pride Mountain Formation Mt Tuscumbria Limestone Mtfp Tuscumbria Limestone Mtfp Tuscumbria Limestone and Fort Payne Chert and Fort -
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. ______________________________ -
Eastern Section American Association of Petroleum Geologists 46Th Annual Meeting Morgantown, West Virginia September 24-27, 2017
Eastern Section American Association of Petroleum Geologists 46th Annual Meeting Morgantown, West Virginia September 24-27, 2017 Program with Abstracts Hosted by: Appalachian Geological Society West Virginia University Department of Geology and Geography With support from the West Virginia Geological and Economic Survey Meeting Sponsors We appreciate your support! Marcellus Level Meeting Sponsors Utica Level Rogersville Level We appreciate your support! Eastern Section American Association of Petroleum Geologists 46th Annual Meeting Morgantown, West Virginia September 24-27, 2017 Program with Abstracts Hosted by: Appalachian Geological Society West Virginia University Department of Geology and Geography With support from the West Virginia Geological and Economic Survey Cover photo used with permission from Jacob Everhart, Canary, LLC Contents Welcome………………………………………………………………………………………………………………………………………1 2017 Meeting Organizing Committee……………………………………………………………………………….1 Eastern Section AAPG Officers………………………………………………………………………………………….2 Appalachian Geological Society Officers……………………………………………………………………………2 General Information…………………………………………………………………………………………………………………….3 Registration Hours……………………………………………………………………………………………………………3 Parking………………………………………………………………………………………………………………………….….3 Maps………………………………………………………………………………………………………………………………..3 Exhibits……………………………………………………………………………………………………………………….……3 Presenters and Judges Room……………………………………………………………………………………..….…3 Presenters, Judges and Session Chairs Breakfast and Information……………………………………3 -
Plate 1A Geology Explanation
GEOLOGICAL SURVEY OF ALABAMA PLATE 1A LEGEND FOR THE HYDROGEOLOGIC CROSS SECTIONS LINES AND WELL LOCATIONS, ALABAMA Qalt, Alluvial, coastal, and low terrace Olp, Leipers Limestone kwx, Waxahatchee Slate Qt, High terrace deposits Oscmg, Sequatchie Formation, Colvin Mt. Sandstone, Greensport Formation undifferentiated hf, Higgins Ferry Group Trs, Residuum Oi, Inman Formation hfgr, Higgins Ferry Group graphitic unit QTci, Citronelle Formation Onv, Nashville Group hfgt, Higgins Ferry Group garnet quartzite unit Tm, Miocene Series undifferentiated Ou, Ordovician System undifferentiated pbm, Poe Bridge Mountain Group To, Oligocene Series undifferentiated Oc, Chickamauga Limestone pbmgr, Poe Bridge Mountain Group graphitic unit Tj, Jackson Group undifferentiated Ocm, Colvin Mountain Sandstone pbmgt, Poe Bridge Mountain Group garnet quartzite unit Tgl, Gosport Sand and Lisbon Formation undifferentiated in part Og, Greensport Formation hcp, Pinchoulee Gneiss Tl, Lisbon Formation Onvsr, Nashville and Stones River Groups undifferentiated hch, Hanover Schist Tt, Tallahatta Formation Oca, Attalla Chert Conglomerate Member of the Chickamauga Limestone mi, Mad Indian Group Th, Hatchetigbee Formation Oa, Athens Shale migr, Mad Indian Group graphitic unit Ttu, Tuscahoma Sand Osr, Stones River Group we, Wedowee Group undifferentiated Tnf, Nanafalia Formation Oal, Athens Shale and Lenoir Limestone undifferentiated weh, Hackneyville Schist Tsm, Salt Mountain Limestone Olol, Little Oak and Lenoir Limestones undifferentiated wec, Cornhouse Schist Tn, Naheola -
Description of the Bessemer and Vandiver
DESCRIPTION OF THE BESSEMER AND VANDIVER INTRODUCTION the west of the Appalachian Plateaus are the Interior Low mentary, including limestone, dolomite, conglomerate, sand LOCATION AND EXTENT OF THE AREA Plateaus, which are included in the Interior Plains by the stone, and shale, which have been greatly disturbed by folding United States Geological Survey but which in the opinion of and faulting, as hereinafter described. The Bessemer and Vandiver quadrangles, which are called some, including the writer, should be included in the Appala in this folio the Bessemer-Vandiver area, are in Jefferson and chian Highlands. SUBDIVISIONS IN ALABAMA Shelby counties in the north-central part of Alabama. (See The boundary between the Piedmont and Blue Ridge Gahaba Ridges. Although the province is in general a fig. 1.) The area is bounded by parallels 33° 15' and 33° provinces is the east foot of the Blue Ridge and the foot of valley, there are within it many high ridges that extend the high but irregular eastern scarp of the mountains of west parallel to its general direction, of which Red Mountain is a ern North Carolina and northern Georgia which form the good example. These ridges are generally grouped along the southern extension of the Blue Ridge. The boundary between west side of the valley from New York to Alabama. In Ala the Blue Ridge and Appalachian Valley provinces is the west bama the ridge section includes all the valley west of the east foot of the Blue Ridge of Virginia and of the high mountains margin of the Coosa coal field and of a line in continuation of of eastern Tennessee. -
Description of the Birmingham Quadrangle
DESCRIPTION OF THE BIRMINGHAM QUADRANGLE. By Charles Butts. INTRODUCTION. that flow across it toward the Atlantic. The Appalachian Tennessee, in Sequatchie Valley, and along Big Wills Creek Mountains occupy a broad belt extending from southwestern are parts of the same peneplain. Below the Coosa peneplain LOCATION, EXTENT, AND GENERAL RELATIONS. Virginia through western North Carolina and eastern Ten the streams of the southern part of the Appalachian province As shown by the key map (fig. 1), the Birmingham quad nessee to northeastern Georgia. This belt is a region of strong have eroded their present channels. rangle lies in the north-central part of Alabama. It is bounded relief, characterized by points and ridges 3000 to 6000 feet or Drainage. The northern part of the Appalachian province by parallels 33° 30' and 34° and meridians 86° 30' and 87° over in height, separated by narrow V-shaped valleys. The is drained through St. Lawrence, Hudson, Delaware, Susque- and contains, therefore, one-quarter of a square degree. Its general level of the Appalachian Valley is much lower than hanna, Potomac, and James rivers into the Atlantic and length from north to south is 34.46 miles, its width from east that of the Appalachian Mountains on the east and of the through Ohio River into the Gulf of Mexico; the southern Appalachian Plateau on the west. Its surface is character part is drained by New, Cumberland, Tennessee, Coosa, and 87 ized by a few main valleys, such as the Cumberland Valley in Black Warrior rivers into the Gulf. In the northern part £35 Pennsylvania, the Shenandoah Valley in Virginia, the East many of the rivers rise on the west side of the Great Appa Tennessee Valley in Tennessee, and -the Coosa Valley in lachian Valley and flow eastward or southeastward to the Alabama, and by many subordinate narrow longitudinal val Atlantic; in the southern part the direction of drainage is leys separated by long, narrow ridges rising in places 1000 to reversed, the rivers rising in the Blue Ridge and flowing west 1500 feet above the general valley level. -
Birmingham Valley and Warrior Coal Field Shades
.GTIO GENERALIZED SECTION OF THE SEDIMENTARY ROCKS OF THE BESSEMER AND VANDIVER QUADRANGLES SCALE: 1 INCH = 1,000 FEET BIRMINGHAM VALLEY AND SHADES VALLEY AND CAHABA VALLEY AND WARRIOR COAL FIELD CAHABA COAL FIELD i COOSA COAL FIELD Character of Rocks and Topography Straven conglomerate member. Thompson coal. Smithshop coal. Quarry coal. Gholson ? coal (Little Pittsburgh) coal. Moyle coal. Youngblood (Black shale, Coke) coal Buck (Atkins) coal Rocky Ridge sandstone member. Pump (Alice and Jones) coal. Coke Oven (Big Bone) coal. "Wadsworth coal. Shale, sandstone, conglomerate, and coal beds. Sandstone siliceous and feldspathic (arkosic). thick-bedded and flaggy. The Shades, Pine, Chestnut, and Boyles sandstone members, which are siliceous, hard ridge makers, compose the "Millstone grit" of Alabama. The shale is generally of clayey composition and of dark color, but some is siliceous. This formation contains all the coal of Alabama. Straight Ridge coal. Straight Ridge sandstone member Nunnally coal group. Wolf Ridge coal. Wolf Ridge sandstone member. Chestnut sandstone member Howard coal. Nivens coal. Clow coal. Pine sandstone member. Gwin coal. Razburg sandstone member Shades sandstone member Cobb coal group. Camp Branch sandstone member. XPratt coal group Cunningham coal Sandstone of Bee Ridge. Pottsville formation. Parkwood formation Shale and saiiuouuuc,mdstone, predominantly^icuu gray, much like the Pottsville, but without coal. Carries a sparse Mississippian fauna in Sandstone of Bluff Ridge. lower part; and a sparse faunaf; of Pennsylvanian aspect in upper part. Generally unfossiliferous. Mainly dark to black clay shale including thin layers of argillaceous limestone and a considerable proportion of fine-grained greenish sandstone, apparently as a general rule in lenticular layers of no great extent. -
Stratigraphic Lexicon for Michigan
Stratigraphic Lexicon for Michigan AUTHORS Paul A. Catacosinos David B. Westjohn [Professor Emeritus, United States Geological Survey Delta College [Associate Professor (Adjunct), University Center, MI 48710] Michigan State University] 1001 Martingale Lane SE 6520 Mercantile Way #6 Albuquerque, NM 87123-4305 Lansing, MI 48911 William B. Harrison, III Mark S. Wollensak, CPG Professor, Department of Geosciences EarthFax Engineering, Inc. Western Michigan University 15266 Ann Drive Kalamazoo, MI 49008 Bath, MI 48808 Robert F. Reynolds Reynolds Geological, L.L.C. 504 Hall Blvd. Mason, MI, 48854 Bulletin 8 Lansing, Michigan, 2001 Geological Survey Division and the Michigan Basin Geological Society State of Michigan John Engler, Govenor Michigan Department of Environmental Quality Russell J. Harding, Director MDEQ Geological Survey Division, P O Box 30256, Lansing, MI 48909-7756 On the Internet @ HTTP://W WW .DEQ.STATE.MI.US/GSD Printed by Authority of Act 451, PA 1994 as amended The Michigan Department of Environmental Quality (MDEQ) will not discriminate Total number of copies printed ........... 1,000 against any individual or group on the basis of race, sex, religion, age, national origin, Total cost: .................................... $2,500.00 color, marital status, disability or political beliefs. Directed questions or concerns to the Cost per copy: ..................................... $2.50 MDEQ Office of Personnel Services, P.O. Box 30473, and Lansing, MI 48909 Page 2 - - Stratigraphic Lexicon for Michigan DEDICATION The authors gratefully dedicate this volume to the memories of Helen M. Martin and Muriel Tara Straight. This volume would not have been possible without their monumental reference work Bulletin 50, An Index of Helen Melville Martin Michigan Geology published by the Michigan Geological Survey in 1956. -
Lower Carboniferous Bangor Limestone in Alabama: a Multicycle Clear Water Epeiric Sea Sequence
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1974 Lower Carboniferous Bangor Limestone in Alabama: a Multicycle Clear Water Epeiric Sea Sequence. Robert Francis Dinnean Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Dinnean, Robert Francis, "Lower Carboniferous Bangor Limestone in Alabama: a Multicycle Clear Water Epeiric Sea Sequence." (1974). LSU Historical Dissertations and Theses. 2720. https://digitalcommons.lsu.edu/gradschool_disstheses/2720 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. 75- 14,243 DINNEAN, Robert Francis, 1932- LOWER CARBONIFEROUS BANGOR LIMESTONE IN ALABAMA: A MULTICYCLE CLEAR WATER EPEIRIC SEA SEQUENCE. The Louisiana State University and Agricultural and Mechanical College, Ph.D., 1974 Geology Xerox University Microfilmst Ann Arbor, Michigan 48106 LOWER CARBONIFEROUS BANGOR LIMESTONE IN ALABAMA A MULTICYCLE CLEAR-WATER EPEIRIC SEA SEQUENCE A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Geology by Robert Francis Dinnean B.S., University of Alabama, 1954 M.S., Louisiana State University, 1958 December, 1974 ACKNOWLEDGEMENTS The writer wishes to acknowledge the guidance and support provided by Dr. C. H. Moore, Jr., who served as Comnittee Chairman and supervised manuscript preparation. Acknowledgement is also due Doctors R.