HGS Bulletin Volume 47 No.8
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B-50 Geology of the Coastal Plain of East Central Georgia
GEORGIA STATE DIVISION OF CONSERVATION DEPARTMENT OF MINES, MINING AND GEOLOGY GARLAND PEYTON, Director THE GEOLOGICAL SURVEY BULLETIN NUMBER 50- PART 1 GEOLOGY OF THE COASTAL PLAIN OF EAST-CENTRAL GEORGIA By PHILIP E. LA MOREAUX Geologist United States Geological Survey Published in cooperation with United States Department of Interior, Geological Survey, Washing.ton, D. C. ATLANTA 1946 I LETTER OF TRANSMITTAL DEPARTMENT OF MINES, MINING AND GEOLOGY ATLANTA, February 15, 1946. His Excellency, Ellis Arnall, Governor Commissioner Ex-Officio, State Division of Conservation Through The Honorable Nelson M. Shipp, Assistant Commissioner SIR: I have the honor to submit herewith Georgia Geological Survey Bulletin No. 50, Part I, "Geology of the Coastal Plain of East-Central Georgia." This is the first in a series of bulletins under this title. Others will be published from time to time until all of the Cretaceous area in the State has been mapped. The geology of east central Georgia, the area covered in this report, influences in three essential ways the economy of the State: The Tuscaloosa formation consists of thick beds of sand and gravel that are excellent aquifers. These water-bearing beds will furnish large additional quantities of water of good quality for industrial and municipal uses throughout a belt of 10 to 30 miles in width along the northern mar gin of the Coastal Plain of Georgia. Georgia produces approximately 80 per cent of the national output of kaolin. The major portion of this production is from deposits described in this report in Washington, Wilkinson a:nd Twiggs counties. Other com mercial minerals mined in this area include bauxite, fuller's earth, lime stone, and sand and gravel. -
Southeastern Part of the Texas Coastal Plain
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR WATER-SUPPLY PAPER 335 GEOLOGY AND UNDERGROUND WATERS OF THE SOUTHEASTERN PART OF THE TEXAS COASTAL PLAIN BY ALEXANDER DEUSSEN WASHINGTON GOVERNMENT PRINTING OFFICE 1914 CONTENTS. Page. Introduction.............................................................. 13 Physiography.............................................................. 14 General character..................................................... 14 Topographic features.................................................. 16 Relief............................................................ 16 Coast prairie.................................................. 16 Kisatchie Wold............................................... 16 Nacogdoches Wold............................................ 16 Corsicana Cuesta and White Rock Escarpment................... 18 Bottom lands................................................. 18 Mounds and pimple plains...................................... 19 Drainage.......................................................... 19 Timber............................................................... 21 General geologic features................................................... 21 Relation of geology to the occurrence of underground water............... 21 Principles of stratigraphy.............................................. 22 Erosion and sedimentation.......................................... 22 The geologic column.............................................. 22 Subdivision -
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Italic Page Numbers Indicate Major References]
Index [Italic page numbers indicate major references] Abbott Formation, 411 379 Bear River Formation, 163 Abo Formation, 281, 282, 286, 302 seismicity, 22 Bear Springs Formation, 315 Absaroka Mountains, 111 Appalachian Orogen, 5, 9, 13, 28 Bearpaw cyclothem, 80 Absaroka sequence, 37, 44, 50, 186, Appalachian Plateau, 9, 427 Bearpaw Mountains, 111 191,233,251, 275, 377, 378, Appalachian Province, 28 Beartooth Mountains, 201, 203 383, 409 Appalachian Ridge, 427 Beartooth shelf, 92, 94 Absaroka thrust fault, 158, 159 Appalachian Shelf, 32 Beartooth uplift, 92, 110, 114 Acadian orogen, 403, 452 Appalachian Trough, 460 Beaver Creek thrust fault, 157 Adaville Formation, 164 Appalachian Valley, 427 Beaver Island, 366 Adirondack Mountains, 6, 433 Araby Formation, 435 Beaverhead Group, 101, 104 Admire Group, 325 Arapahoe Formation, 189 Bedford Shale, 376 Agate Creek fault, 123, 182 Arapien Shale, 71, 73, 74 Beekmantown Group, 440, 445 Alabama, 36, 427,471 Arbuckle anticline, 327, 329, 331 Belden Shale, 57, 123, 127 Alacran Mountain Formation, 283 Arbuckle Group, 186, 269 Bell Canyon Formation, 287 Alamosa Formation, 169, 170 Arbuckle Mountains, 309, 310, 312, Bell Creek oil field, Montana, 81 Alaska Bench Limestone, 93 328 Bell Ranch Formation, 72, 73 Alberta shelf, 92, 94 Arbuckle Uplift, 11, 37, 318, 324 Bell Shale, 375 Albion-Scioio oil field, Michigan, Archean rocks, 5, 49, 225 Belle Fourche River, 207 373 Archeolithoporella, 283 Belt Island complex, 97, 98 Albuquerque Basin, 111, 165, 167, Ardmore Basin, 11, 37, 307, 308, Belt Supergroup, 28, 53 168, 169 309, 317, 318, 326, 347 Bend Arch, 262, 275, 277, 290, 346, Algonquin Arch, 361 Arikaree Formation, 165, 190 347 Alibates Bed, 326 Arizona, 19, 43, 44, S3, 67. -
Structural Framework of the Mississippi Embayment of Southern Illinois ^
<Olo£ 4.GV- Su&O&Ml STRUCTURAL FRAMEWORK OF THE MISSISSIPPI EMBAYMENT OF SOUTHERN ILLINOIS ^ Dennis R. Kolata, Janis D. Treworgy, and John M. Masters f^a>i^ < Illinois Institute of Natural Resources STATE GEOLOGICAL SURVEY DIVISION CIRCULAR 516 Jack A. Simon, Chief 1981 . COVER PHOTO: Exposure of Mississippian limestone along the Post Creek Cutoff in eastern Pulaski County, Illinois. The limestone is overlain (in ascending order) by the Little Bear Soil and the Gulfian (late Cretaceous) Tuscaloosa and McNairy Formations. Cover and illustrations by Sandra Stecyk. Kolata, Dennis R. Structural framework of the Mississippi Embayment of southern Illinois / by Dennis R. Kolata, Janis D. Treworgy, and John M. Masters. — Champaign, III. : State Geological Survey Division, 1981 — 38 p. ; 28 cm. (Circular / Illinois. State Geological Survey Division ; 516) 1. Geology — Mississippi Embayment. 2. Geology, Structural — Illinois, Southern. 3. Mississippi Embayment. I. Treworgy, Janis D. II. Masters, John M. III. Title. IV. Series. GEOLOGICAL SURVEY ILLINOIS STATE Printed by authority of State of Illinois (3,000/1981) 5018 3 3051 00003 STRUCTURAL FRAMEWORK OF THE MISSISSIPPI EMBAYMENT OF SOUTHERN ILLINOIS -*** t**- ILLINOIS STATE GEOLOGICAL SURVEY CIRCULAR 516 Natural Resources Building 1981 615 East Peabody Drive Champaign, IL 61820 Digitized by the Internet Archive in 2012 with funding from University of Illinois Urbana-Champaign http://archive.org/details/structuralframew516kola CONTENTS ABSTRACT 1 INTRODUCTION 1 METHOD OF STUDY 2 GEOLOGIC SETTING -
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. -
Possible Oil and Gas Fields in the Cretaceous Beds of Alabama
424 OIL AND GAS FIELDS IN THE CRETACEOUS BEDS OF ALABAMA Possible Oil and Gas Fields in the Cretaceous Beds of Alabama BY DORSEY HAGER, * TULf\A, OKI,A. (New York Meeting, February, 1918) Downloaded from http://onepetro.org/TRANS/article-pdf/59/01/424/2176944/spe-918424-g.pdf by guest on 01 October 2021 THE possibility of oil and gas production in Alabama has been little considered as yet. Gas and some oil have been found in northwestern Alabama, near Birmingham, in the Pennsylvanian beds, but the oil and gas possibilities in the Cretaceous beds are not generally appreciated. The recent activity of oil companies in that State has attracted much attention, and in this paper the main structural and the general strati graphic features are described. :Four favorable areas are outlined. These contain folds of major interest. 'there are other favorable areas which have not been mapped,l Commercial pools discovered in this area would have the advantage of being near tidewater. Mobile, Ala., on the Gulf of Mexico, would be the logical site for refineries and shipping facilities. A pipe line could readily be laid to that city from the Hatchitigbee and the Jackson areas. The logical outlet for the Geneva and the Gordon areas would be Panama City, ma., on the Gulf of Mexico. TOPOGRAPHY The whole of the area under consideration lies in the Gulf coastal· plain and slopes gently to the southwest and west. The elevations vary from 200 to 400 ft. (60 to 121 m.) above sea level. The streams have . sunk their channels into this gently sloping plain, the main drainage flowing south or southwest into tho Gulf of Mexico. -
Bedrock Geology of Paducah Nequadrangle
BEDROCK GEOLOGY OF PADUCAH NE QUADRANGLE Illinois Department of Natural Resources Illinois Geologic Quadrangle Map ILLINOIS STATE GEOLOGICAL SURVEY MASSAC AND POPE COUNTIES, ILLINOIS IGQ Paducah NE-BG William W. Shilts, Chief F. Brett Denny and W. John Nelson 2005 A Km Mts Msb Qc Km Mgd Mgd Mgd Mm BARNES CREEK QTm Qc FAULT ZONE Mpo 15 Mgd 67.5 6 QTm Km 15 Qc 78 4 Msb Mts EXPLANATION Qc E Msb N Mts Mps O QTm Z Mh T Qc Km Mts L Cahokia Formation U Mwb A Qm F Holocene Y 5 Qc T 32 I Cahokia overlying 594 Mpo C 10 Qc/e Msb Equality Formation Qc Y 4 12 Mm A B Qc Mgd Qc Quaternary Unconformity Gravel Pit Mwb 3 Henry Formation Km Qh(d) Dolton Member Mm Msb Mts QTm Unconformity Pleistocene Mh QTm 770 Mpo Mpo Mh QTm Qm Metropolis Formation 10 Mgd Mps Unconformity 15 Mh Mcy Qm 4 QTm Mounds Gravel Qc Mm Tertiary Pliocene Mpo Km Unconformity Msb 70 7 Upper 335 Mts Km McNairy Formation QTm Cretaceous Cretaceous Mm E N 70 Unconformity 180 O 128 Z Mm Qc Mg QTm T Msb L U A Mps Palestine Sandstone F Qc Mg E 7 Km IN Unconformity 104 M Mg QTm QTm N Mm Menard Limestone 207 O T 9 61 P M Qc O C Mwv Waltersburg Formation Mcy and Vienna Limestone Mwv Km Qc 78 Km AЈ Mts Tar Springs Sandstone Km 240 36 Km QTm 397 Mgd Glen Dean Limestone Km MALLARDMALLARD CREEKCREEK Gravel Pit FAULTFAULT AREAAREA Mcy Qm (fig.(fig. -
GEOLOGY of OLMSTED QUADRANGLE Institute of Natural Resource Sustainability William W
GEOLOGY OF OLMSTED QUADRANGLE Institute of Natural Resource Sustainability William W. Shilts, Executive Director PULASKI COUNTY, ILLINOIS Illinois Geologic Quadrangle Map ILLINOIS STATE GEOLOGICAL SURVEY IGQ Olmsted-G E. Donald McKay III, Interim Director W. John Nelson, F. Brett Denny, John H. McBride, and Laura Williams 2009 CYPRESS 8 MI. R. 1 E. R. 2 E. 2.6 MI. TO ILL. 169 S J 140 N K 250 " 350 k 350 N Kom e" Kom J 37 br T QTm Kom 350 400 T. 15 S. 400 350 Qe 360 Qe J N Qe 33 QTm 32 QTm N J 31 400 32 33 34 Kom 400 35 400 400 400 J N 36 48 T k" N J 400 C 24 Kom Kom 0 k" 210 40 66 350 e" "k Kom br T. 14 S. N J Kom 38 Kom QTm K 0 T. 15 S. 350 T N J N J 380 T. 15 S. Price C 56 N " J R k A o 350 400 a Kom N J d Kom Kom C 60 350 QTm 400 k" C 66 400 N J T Tw k" N J Kom 5 S N J K 400 185 J Kom N 430 e" N 450 J br 350 4 6 350 N 400 J N J 400 N J 350 4 360 5 N J 3 C 24 " 400 J k C 54 2 N Kom N J k" Kom T 1 350 N J 85 N J k" 400 Kom QTm N J 450 T 450 Qe 450 N J 380 C 72 J 400 N k" N J QTm QTm K N 400 J N J 280 Qm k" S N J br 400 k" 81 66 N J k" QTm GEOLOGIC UNITS 400 Kom Qe K 350 J 350 N N Qe J 400 N J 450 380 N J 9 N J N J T 300 sm Bethlehem Road 8 Surface mine (clay) K J N N 450 J k"79 N J K T N Kom J 450 260 N J 450 N k" J 350 Holocene 450 br Qc N J Kom 400 350 450 J N N N J J 310 C Qc Cahokia Formation k" 205 400 k" 310 T k" N Kom J 65 Kom N J 400 N J Tpc br 285 C 40 Tpc k" QTm k" 470 Kom e" br 8 N 150 J 150 K 9 Tpc e" K Ck" 60 Kom Tpc N J Quaternary N J Tpc 10 250 J N Qm 11k"Kpc Clark Road Wisconsinan N J 250 N N J " J e Qe QTm 12 br Equality Formation N 52 7 J k" T N 450 450 J 400 Kom Unconformity J 350 N Tpc 370 J K QTm N N J 450 450 N J N 37 J Illinoian 450 Metropolis Formation 450 Qm 3885 C 84 T and older J N N 47 J 450 k" N J 440 ª k" QTm St. -
Bedrock Geology of the Thebes Quadrangle Alexander County, Illinois, and Cape Girardeau and Scott Counties, Missouri
STATEMAP Thebes-BG Bedrock Geology of the Thebes Quadrangle Alexander County, Illinois, and Cape Girardeau and Scott Counties, Missouri Joseph A. Devera, Jeremy R. Breeden, and Franck Delpomdor 2017 Prairie Research Institute ILLINOIS STATE GEOLOGICAL SURVEY 615 East Peabody Drive Champaign, Illinois 61820-6918 (217) 244-2414 http://www.isgs.illinois.edu © 2017 University of Illinois Board of Trustees. All rights reserved. For permission information, contact the Illinois State Geological Survey. Introduction Mesozoic Era sediments. The Mississippi River changed its course from flowing west at Grays Point to the south by The Thebes Quadrangle is located in extreme southwestern cutting through indurated Paleozoic bedrock at Thebes Gap Illinois and southeastern Missouri. This report covers only during the Late Pleistocene 10,000 yrs. BP (Blum et al., the Illinois portion of the Thebes Quadrangle. The Thebes 2000). The Gulf Coastal Plain sediments also blanket the Quadrangle contains rocks and sediments that were depos- southern portion of the quadrangle from east to west. Paleo- ited during the Paleozoic, Mesozoic and Cenozoic Eras. gene sediments are confined to structural grabens, whereas The oldest formation in the study area is the Kimmswick Neogene sediments cap the ridges, and terrace the valleys. Limestone (Ordovician) the youngest deposit is Holocene The bedrock hills are highly dissected, in some cases along alluvium. The Thebes Quadrangle occurs south of the Il- structurally or vertical joint controlled valleys. The bed- linoisan glacial boundary and most Quaternary deposits rock valleys are choked with Pleistocene to Holocene chert were not drawn on the map. The loess deposits that blanket gravels derived from the local thick, cherty limestones and the upland surfaces, were not depicted in order to better silicified beds of Bailey and Grassy Knob Chert. -
General Geology of the Mississippi Embayment by E
General Geology of the Mississippi Embayment By E. M. GUSHING, E. H. BOSWELL, and R. L. HOSMAN WATER RESOURCES OF THE MISSISSIPPI EMBAYMENT GEOLOGICAL SURVEY PROFESSIONAL PAPER 448-B UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1964 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director First printing 1964 Second printing 1968 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Stratigraphy Continued Page Abstract Bl Tertiary System Continued Introduction.. __ 1 Paleocene Series Continued Method of study 3 Midway Group Continued Acknowledgments-__ ____. 4 Porters Creek Clay____ B14 Geology- 4 Wills Point Formation.. 15 Stratigraphy, _______ 5 Naheola Formation 15 Paleozoic rocks _ 5 Eocene Series._. .. 16 Cretaceous System 5 Wilcox Group. 16 Lower Cretaceous Series 5 NanafaUa Formation __ 16 Trinity Group _._ ____ 9 Tuscahoma Sand.. 16 Upper Cretaceous Series __ 9 Hatchetigbee Formation__ ___ 16 Tuscaloosa Group _ 10 Berger and Saline Formations and Massive sand 10 Detonti Sand_.__. ... 17 Coker Formation.___._ _____ 10 Naborton Formation ___ 17 Gordo Formation.... _.__ 10 Dolet Hills Formation 17 Woodbine Formation 11 Claiborne Group 17 Eagle Ford Shale. ______________ 11 Tallahatta Formation_________ 17 McShan Formation._______ __._ 11 Carrizo Sand. 18 Eutaw Formation______________ 11 Mount Selman Formation ___________ 18 Tokio Formation._.____________ 11 Cane River Formation._____________ 18 Blossom Sand and Bonham Marl..__.__ 11 Winona Sand_____ _ 19 Selma Group _____ _______ 11 Zilpha Clay..._._ ___ _ 19 Mooreville Chalk_____________ 11 Sparta Sand 19 Coffee Sand_______________ 12 Cook Mountain Formation___ _ 20 Demopolis Chalk___________.___._ 12 Cockfield Formation._______ 21 Ripley Formation _ ..... -
MS Surface Geologic Unit Desc
Surface Geologic Unit Descriptions for Mississippi (after Geologic Map of Mississippi, Bicker, 1969) Qa - Alluvium (Quaternary, Holocene) Loam, sand, gravel, and clay; mapped on in Mississippi River Alluvial Plain. Qc - Coastal Deposits (Quaternary, Holocene) Loam, sand, gravel, and clay UNCONFORMITY Ql - Loess and brown loam (Quaternary, Pleistocene) Grayish to yellowish-brown massive silt; the pattern indicates the area within which the loess is generally thicker than ten feet; remnants of the mantle are present many miles farther east. UNCONFORMITY Pc - Citronelle formation (Quaternary, Pleistocene) Red sand and gravel and white clay; may be of Pliocene age; the formation mapped is equivalent to the Willis sand and does not include the terrace deposits, colluvium, and residuum commonly considered “Citronelle”. UNCONFORMITY Mph - Pascagoula and Hattiesburg formation (Tertiary, Miocene) Green and bluish-green clay, sandy clay, and sand; gray siltstone and sand; locally fossiliferous. Mc - Catahoula formation (Tertiary, Miocene) Irregularly bedded gray sand and sandstone; mottled red and gray, green, and chocolate- colored clay; some quartzite; and some gravel; the Paynes Hammock sand, sandy limestone cross-bedded fine green sand, and thin-bedded sand and clay, is mapped with the underlying Chickasawhay limestone in eastern Mississippi. UNCONFORMITY Ov - Vicksburg group and Chickasawhay limestone (Tertiary, Oligocene) Chickasawhay limestone, sandy limestone and sand, present only in eastern Mississippi (mapped with it is the overlying Paynes Hammock sand of Miocene age); Vicksburg group, predominantly limestone and marl, but contains some bentonite and near the top chocolate-colored clay and some sand. UNCONFORMITY Of - Forest Hill formation and Red Bluff clay (Tertiary, Oligocene) Forest Hill sand, cross-bedded fine gray sand, laminated fine sand and clay, and a little lignite; in Wayne and Clarke counties lower part merges eastward into Red Bluff clay, blue-green glauconitic, gypsiferous, fossiliferous clay and thin limestone beds. -
Regional Character of the Lower Tuscaloosa Formation Depositional Systems and Trends in Reservoir Quality
Copyright by Kurtus Steven Woolf 2012 The Dissertation Committee for Kurtus Steven Woolf Certifies that this is the approved version of the following dissertation: REGIONAL CHARACTER OF THE LOWER TUSCALOOSA FORMATION DEPOSITIONAL SYSTEMS AND TRENDS IN RESERVOIR QUALITY Committee: Lesli J. Wood, Supervisor William Fisher Ronald Steel Kitty Milliken Kyle Spikes REGIONAL CHARACTER OF THE LOWER TUSCALOOSA FORMATION DEPOSITIONAL SYSTEMS AND TRENDS IN RESERVOIR QUALITY by Kurtus Steven Woolf, B.S., M.S. Dissertation Presented to the Faculty of the Graduate School of The University of Texas at Austin in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy The University of Texas at Austin December 2012 Dedication To Julie, Trevor, and Lily Acknowledgments I would like to thank Dr. Lesli Wood for providing guidance and support throughout my time at the University of Texas. I appreciate the additional advice and support given by the other members of my committee: Dr. William Fisher, Dr. Ronald Steel, Dr. Kitty Milliken, and Dr. Kyle Spikes. I would like to thank Dr. Peter Flaig for assistance in taking core photographs and for reviewing portions of this dissertation. I appreciate the collaboration and data provided by Dr. Susan Hovorka, Ramon Trevino, and David Carr from the Gulf Coast Carbon Center at the Bureau of Economic Geology. This dissertation was made possible by the financial support of The Jackson School of Geosciences, and the Bureau of Economic Geology. I appreciate the support of the members of the Quantitative Clastics Laboratory Industrial Associates consortium including Anadarko, BHP Billiton, Cairn, ExxonMobil, Marathon, Saudi Aramco, Statoil, and Woodside.