Arcview Print

Total Page:16

File Type:pdf, Size:1020Kb

Arcview Print R03W R11W R10W R09W R08W R07W R06W R05W R04W o Ops Ops Ops Ops o Ogp # 92 00' # 43 30' R14W R13W R12W Dw Dw ### # Kw Dw # Kw # o # 43 30' # # # # Ops # ALLAMA# KEE Dc Ogp ### Ops # # # # Dc # # # # # # Dw # # # # # # r WINNESHIEK # # HOWARD e Om # # iv ## # Ops # # # # R # # a ## # # # w # # # Io # Dc r # Ops # e # # # # Ops T100N p # # Ogp # p # # U # Dc # # # # # Ops # # # Om # # # # # ## # Om # # # # # # # # Cjl Cw # # # # Om # # # # Cjl # 52 # # # /( # Ogp # # # # # # # # # # # # # 63 # ( Ogp r # # / # e # # # Ogp # iv # # Dw R Ops Dc Dc # # # # Dw # a ## # w # # o Ops Ops # # I # # # # # r # e # # p # # # # Om# p # Ops U # # # Ogp # # # Ops # Ogp # # # # # # # T99N # Cresco # # # # # # ## # DIGITAL GEOLOGIC MAP OF IOWA # # # # # # # # # # # Ogp # # Dw # # 9 !"9 # # !" # # # # M # # # # IS PHASE 2: NORTHEAST IOWA # # S # Ogp # IS # # # # S Ogp ### # IP # PI # # # R # # IV ## # # # # E # Dc # # # # # R # # # # Ogp # Prepared by # Ogp # # Decora# h Ogp Ops # # # # # # ## # # Dc # # Dw # # # # # # Brian J. Witzke # T # # # Ogp u # # # r Ogp # # k # Dc # # Greg A. Ludvigson # e # # y # # # # # # # # # # # # ## # # # R # # # # # # Dw # # # # i ## # # Robert M. McKay v # # # # # # # # # e # # # T98N # Ogp Kw # Dc r # # # # # # # C # Ogp # # # Ops Raymond R. Anderson # r # 9 ## # a # !" Kw Ogp n # ## # # e # # ## Bill J. Bunker # Waukon C # # # # # Cjl # # r # # # # # e # Om # # e Dc # # # James D. Giglierano # k # Dc # Ogp # # # # # # # John P. Pope # # # Cw # # 9 # Kw # " # # # ! Ogp # Adrian E. Goettemoeller Dc # # # # # # # Ogp # # # # # # # # # # Om Maureen K. Slaughter # # # # # Ogp # Dw Dw # # Dw # # # # # # # # # # # Cjl # # # # # # # T97N # # # # # L Energy and Geological Resources Division W Dc # I Dc Dw # Ogp # i # # t # # # # a t # le # p # # Geological Survey Bureau # # # # s CHICKASAW T Dw # # # # Cjl i # u # # p # r # # # # # i # # k # # # n e # # # # # # i # # y c # # # R Dw # o # # # # # i # August 1998 n # # # v # # # # # # # # Om e # # # R r # # # # # ## # i v # # # # e # ## # L Dc # # Ogp # r 63 # ( # # # i / # # t Dw # # # Produced under the STATEMAP program, in cooperation with the # t # # # l # e # # Ops # # Yel W # # low # # # R U.S. Geological Survey, Department of Interior, Supported by Dw # iv a # 52 # er # # # /( p # # # # 15# 0 # # # # s " # # Ogp ! # i # # assistance Award No. 1434-HQ-97-AG-01719 T96N p # # ### "24 # i Dc ! # # n ## Om # # # Ogp # c Dw # # Dw # o Sls # n # # R # # Cjl # Dc # Om i # # Ogp v Dc Sls # # # # e Om # Om r # Dw # # # # # # # # Sls # Sls # # # # New Hampton Dc # # # # # # # # # # # # # # # # Om ## ## # # # Ogp 18 # FAYETTE # # # ( # # # # # # # / # # # # # # # Ops # # CLAYTON # E Dw # # a # s # t Ogp # # # # B Sls # # # # # # # r Sls # # # # # # # W # # T95N # R # # Ogp # a o # # # p # b # # s e # # # r 18 # i # # ( p / # t i Shb s n # # C # o # i # Shb # # # # # # c # r # # # o e # Om # 43 00' # (18 e # n / # # # k Om o # R i Dw # v # 43 00' e Dc # # # # # # r Shb # # # # Shb # Dw # # # # # # Shb # # # West Union # Sls # # # # # Cjl # # # # # # # # Om ### # # # Shb # (18 # # # / # # # ## # Dc # # # # # # # Om # # Shb # # Om # T94N # # # # # Dw # # # # Iowa Department of Natural Resources # # Dc D#w # Om T # # # # u # Om # rk Sls e # # y # # # # Ri # # # Shb ve # Larry J. Wilson Shb r # Sls # # # # Dw # # # # # # Dw # Shb # # # # # Sls # # # # # # # # # # O# gp # # # ## # # # # ## # # # BREMER # Om Shb /(52 Dc # Om ACKNOWLEDGEMENTS # # # Om Om Shb # # # # Cjl # # # Om # # Om Elkader # Recognized for direct contributions to the map’s production: Donald L. Koch, Jackson L. Gilmore, T93N # Dw # 218 # /( Om # # # # # Lynette S. Seigley, and Orrin W. Plocher of the Iowa DNR Geological Survey Bureau # # # # # # ## ## # # # Shb # # # # # # # Shb Om # # # # # Dw Vo lg # # # a # # # R # # # iv # Om # er # ## # Om # # # # # # 150 Dw !" # # # # # Om # Ogp # # Dw # Om # # # Shb 63 Om # # ( / # # # L C # Dc "13 Shb i ! e Dw t t # # d l # # # e a # # # r # # # W T92N R a i # # v p e # s r # i # Shb Ops C p # ## Dw # r Dw i Om # # # n ## a # # # i Om o n c # # # # e Shb 91 00' o # n Om # C Om # # R r # e Shb Waverly# i # e v # ## k e # r # # Ogp # # # # # # # Om 3 # !"3 !" # # # # # # # # # Om # # Shb # # Ops # Ogp # # 3 # # Shb !" # # Om Dc # # # # # # # Om # # T91N # # # # # # # Om # # M # # IS # B # # SI # # SS # u # IPP # # # I R c Shb Om IVE Shb # Ogp R 218 k # # ( C Dw Dw # / # # # Shb r # # e # # # # # # Shb e # # # # # k # !"3 # # # # # # # # Dc Ss # # # # DUBUQUE # Ss # # # # # # # # Om # # # # # # Dw # # Om # # Dc DELAWARE # # # Shb # # # Shb # # BUCHANAN # # # # # Dw # # Ss # BLACK # # # # # # # # # Dc # Ss # Om # # # r # ## # # # e Om HAWK # # v # # # # i # # R (52 # # / T90N # # a # # t # ## # # # # e # ## # Ss # k O# ps # # # # # # # # o # Om # u # # q # # # # a # # Om # # (63 # # / # # M # # # # # # # # # # # Dc 150 # # # # k # # # " # ### # # ! r # # # Sls # # # o ## # # Om Om # # # # # Dw # F # # # # # # # # # M # # Ss # N Ogp # # Om # a Ss # # # # # # ## Ogp # q # # # # # # ### # u # Shb # # o # # # r # # k # # # e # e # # Shb # # # v # # # Dw # t i # # # a # # # # R # 61 # # ( # / R Ss # Dubuque # # # # ta # # ## # W i # # # # a v e # # o # # p k # # s Sls # e # o # # # i # r # 42 30' p # # Shb u Om # # i Ss # # # # # # n # q # # # # # # # i Manchester Sls # a # # # # c # # # o # # # n # M# # # # # # T89N # # R e # # # i Ss # # l # # # # Shb v # # t # # # e # t # # o # r # i # # # # # # # # I # C # # # # # # # 42 30' # ## # # # L # # # e # # # d # # # # # ## Ogp # # # # # ## # #a # ## ### # # # r # # # Cedar Falls R # # # # # Ss # i # # Dc # # # # # # # # # # # v # Ss # ## # # # # # # e # # Ss # # # # # r # # # # # 20 # # # /( # # # # # ## Waterloo Shb Independence # # # # # ## # # Ss Ss # # # # # Dl ## # # # Shb # # # # 20 # # # # ( # # / # # # # # # # # # # # 20 # # # # # # ( # # # # # # Shb / # # # Sls Ops # Sls # Sls Shb # # Sls # Om (20 # # # / # # # # 20 B # ( # Om # / # # # # # # ## # # # # u # # ## # # # # ## # # ## f ### # # # # f # # ## ## # # # # # # a # # # Sls # ### # # # # # l 13 Ss # # # # # o !" # # # Ogp # # # # # # # Ss # # # # Dl # ## C Ss # # # # # # # # # # # r # # # # # T88N # # # e # # e # # # # # # # # # # # Ops # # k # # # # # # # # # # ### ## # # Sls # # # # # # # # # Ss # # ##### # # # ##### # # # # # # # # # # # # # # # # # # # # # # # # # Ss # # # # # # # Dc # # ## # # # # # # # Dw # # # # # # # D# l 380 # # 218 . # # ## # - # # # , # ( # # / # # # ## # # # ## # # # Ss # # Ogp # # # # # Sls Om # # # # # # # # # # # Om Sls # # # # Dw ## # # 52 # # # # # Ss ( # # # / # # Ss # Dw # # # # Sls Sls # # # # # # 151 # # # ( # / # # # # # # 63 # # # Ss ( # # Om # # / # # # # # # # # # # # # # # # # # # # # # # # # # # ## Ss # # # # Ss # # # # # # # # # # # # # # 61 # # # ( # # # / # Dw Shb # # # # # Ss # # # # Ogp T87N # # # # # Dc # # # # # # ## # # Shb # # Ss # # # # Dc # # # # # # # # # # # # Dw # Ss Ss # Dl Ss # # # # # # # # # # # # # ## # # # # ## # # # # # S# s 150 # Shb # # # # # # # # # # # " # # # ! # # # # # Ss # # # # # # # # # # # # # # # # # # # # Shb # # # # Ss # # # # # # # # # # # # # # # # # Sls # # # # # # # # # # # # # # # # # # # # ## ## # # # JACKSON o # Ss # # # # # # # # # # # # 91 30' # # # # # # # # # R11W # # # # # R13W R12W # # # # R14W # # # # # # # # # # R09W LINN # # R10W JONES # # # # Dc # # # Ss Dw # # # # # # # # # # # # # # ## ## # # # Dw #### # # ### ## # # # # Ss # # # # Ss # # # # # # T86N # # # # # # # # Shb Dc # # # # Ss # # # # Ss # # Ss # # # # Ss # # # # # # # # Ss # # # # # # # # # # # Ss # # # # # # # Ss Dw # # # # # # # # # Ss # # # # # # # # Dw Sg # # # # # # # # # ## # ## # # # # # # # ### # # # Dw # # # # # # # # Ss # # # # Ss # # # # # # # Dw # Dc # # # # # LEGEND # # # # Ss Om Dc ## 151 # # # #( / # # # # Ss # # Ogp # # # # # # # # Ss # # # # Ss # # # # Shb # Sg Dw # # # # # # # # # Ss # # # # # # # # # # # # Dc Dc Sg # # # # Dw # Pcc Ss # # # # # # # # # # # # # # # # # # # # # Pcc # # # # Ss # # # # Description of Map Units # # # # # # # # Shb Ss Ss T85N # # 61 Ss # # # /( Ss # # # # Dw # Dw # # # # # # Dw # Ss C # # # # # Ss Ss # # Sg Dw # # Ss 52 e # # /( # Sg # # # d # # # # Sg # # # # Ogp 1# 3 # # # # # a !" # # S# s # Shb # # # r # # # # # # # R # # # # # # # # i # # # v # CRETACEOUS e Sg # # # # # # # # # r Dw # # M # # Ss # # # ## # # # aq # u Ss # Ss # # Ss Dw # # # o # # # # # ke # # # Ss# ta # # # # # R # Ss # # Ss i # # # # Shb # ve # # # WINDROW FM.; Iron Hill and Ostrander mbs.; mid Cretaceous (?upper Albian and/or Cenomanian). # Anamosa r # Dw # # # # # # # ult Zone Kw # # # er Fa # # Pcc Riv # # D Ogp Maximum thickness: 40 ft (12 m). Primary lithologies: sandstone, part pebbly to conglomeratic, part cemented by iron oxides. Secondary lithologies: mudstone; massive iron # Ss # Plum # # # # # # # U # # Ss # # # ore, silty to sandy. # # Shb # # # # # # ## ## # # # # # # # # # # # # # # # # # # # # # # # # Ss # # # ### # # # # # # Ss Sg # # # # Pcc # # Dc Dw # Pcc Om # Om # ## # # Sg # ## # Shb # # # 64 Ss # # # # Sg #### W " # # # # # # ! #.
Recommended publications
  • Rock Stratigraphy of the Silurian System in Northeastern and Northwestern Illinois
    2UJ?. *& "1 479 S 14.GS: CIR479 STATE OF ILLINOIS c. 1 DEPARTMENT OF REGISTRATION AND EDUCATION Rock Stratigraphy of the Silurian System in Northeastern and Northwestern Illinois H. B. Willman GEOLOGICAL ILLINOIS ""SURVEY * 10RM* APR 3H986 ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief Urbano, IL 61801 CIRCULAR 479 1973 CONTENTS Page Abstract 1 Introduction 1 Time-stratigraphic classification 3 Alexandrian Series 5 Niagaran Series 5 Cayugan Series 6 Regional correlations 6 Northeastern Illinois 6 Development of the classification 9 Wilhelmi Formation 12 Schweizer Member 13 Birds Member 13 Elwood Formation 14 Kankakee Formation 15 Drummond Member 17 Offerman Member 17 Troutman Member 18 Plaines Member 18 Joliet Formation 19 Brandon Bridge Member 20 Markgraf Member 21 Romeo Member 22 Sugar Run Formation . „ 22 Racine Formation 24 Northwestern Illinois 26 Development of the classification 29 Mosalem Formation 31 Tete des Morts Formation 33 Blanding Formation 35 Sweeney Formation 36 Marcus Formation 3 7 Racine Formation 39 References 40 GEOLOGIC SECTIONS Northeastern Illinois 45 Northwestern Illinois 52 FIGURES Figure 1 - Distribution of Silurian rocks in Illinois 2 2 - Classification of Silurian rocks in northeastern and northwestern Illinois 4 3 - Correlation of the Silurian formations in Illinois and adjacent states 7 - CM 4 Distribution of Silurian rocks in northeastern Illinois (modified from State Geologic Map) 8 - lis. 5 Silurian strata in northeastern Illinois 10 ^- 6 - Development of the classification of the Silurian System in |§ northeastern Illinois 11 7 - Distribution of Silurian rocks in northwestern Illinois (modified ;0 from State Geologic Map) 2 7 8 - Silurian strata in northwestern Illinois 28 o 9 - Development of the classification of the Silurian System in CO northwestern Illinois 30 10 - Index to stratigraphic units described in the geologic sections • • 46 ROCK STRATIGRAPHY OF THE SILURIAN SYSTEM IN NORTHEASTERN AND NORTHWESTERN ILLINOIS H.
    [Show full text]
  • As Pessoas Interessadas Em Receber Nossa Newsletter Via Mail, Podem Escrever Para [email protected] Pedindo Sua Adesão
    ***As pessoas interessadas em receber nossa newsletter via mail, podem escrever para [email protected] pedindo sua adesão. LIVROS http://eu.wiley.com/WileyCDA/Section/id-350717.html ÍNDICE DE NOTÍCIAS JORNAL DA CIÊNCIA Edição 4638 - Notícias de C&T - Serviço da SBPC 1. Para SBPC, Brasil precisa de Educação e CT&I para manter seu crescimento econômico 2. Senadora atende pleito da SBPC e ABC e adia votação do PL sobre revalidação de diplomas estrangeiros 3. Congresso tem até 13 de março para votar MP dos royalties 4. Sem bons professores não há futuro, artigo de Mozart Neves Ramos 5. Mercosul terá programa de mobilidade estudantil semelhante ao Ciência sem Fronteitas 6. Contra o conteudismo escolar e seus testes, artigo de Roberto Franklin de Leão 7. Pronatec atende mais de 2,5 milhões de jovens e será ampliado em 2013 8. Cristovam propõe sistema único de educação 9. A segurança alimentar e a desinformação do consumidor, artigo de Flávio Finardi Filho 10. Marco legal precisa amparar interação público-privada, defende ministro 11. Futuro tecnológico da geração elétrica nuclear, artigo de Leonam dos Santos Guimarães 12. Adeus a Oscar Niemeyer 13. Excesso de neurônio é tão ruim como falta, diz pesquisa da UFRJ 14. "Feijão verde": astrônomos descobrem novo tipo de galáxia 15. Homenagem a Renato Archer, com inauguração de Espaço Galeria, lançamento de Livro e selo comemorativo dos 30 anos do CTI Renato Archer 16. Ciência Hoje On-line: Terra partida 17. Campus Sorocaba da UFSCar realiza concurso para professores até 7 de dezembro 18. UFABC abre oportunidade de pós-doutorado em Microbiologia e Biologia Molecular 19.
    [Show full text]
  • Cambrian Cephalopods
    BULLETIN 40 Cambrian Cephalopods BY ROUSSEAU H. FLOWER 1954 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Eugene Callaghan, Director THE REGENTS MEMBERS Ex OFFICIO The Honorable Edwin L. Mechem ...................... Governor of New Mexico Tom Wiley ......................................... Superintendent of Public Instruction APPOINTED MEMBERS Robert W. Botts ...................................................................... Albuquerque Holm 0. Bursum, Jr. ....................................................................... Socorro Thomas M. Cramer ........................................................................ Carlsbad Frank C. DiLuzio ..................................................................... Los Alamos A. A. Kemnitz ................................................................................... Hobbs Contents Page ABSTRACT ...................................................................................................... 1 FOREWORD ................................................................................................... 2 ACKNOWLEDGMENTS ............................................................................. 3 PREVIOUS REPORTS OF CAMBRIAN CEPHALOPODS ................ 4 ADEQUATELY KNOWN CAMBRIAN CEPHALOPODS, with a revision of the Plectronoceratidae ..........................................................7
    [Show full text]
  • Deep Oil Possibilities of the Illinois Basin
    s Ccc 36? STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION DEEP OIL POSSIBILITIES OF THE ILLINOIS BASIN Alfred H. Bell Elwood Atherton T. C. Buschbach David H. Swann ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief URBANA CIRCULAR 368 1964 . DEEP OIL POSSIBILITIES OF THE ILLINOIS BASIN Alfred H. Bell, Elwood Atherton, T. C. Buschbach, and David H. Swann ABSTRACT The Middle Ordovician and younger rocks of the Illinois Basin, which have yielded 3 billion barrels of oil, are underlain by a larger volume of virtually untested Lower Ordovician and Cambrian rocks. Within the region that has supplied 99 percent of the oil, where the top of the Middle Ordovician (Trenton) is more than 1,000 feet be- low sea level, less than 8 inches of hole have been drilled per cubic mile of the older rocks. Even this drilling has been near the edges; and in the central area, which has yielded five- sixths of the oil, only one inch of test hole has been drilled per cubic mile of Lower Ordovician and Cambrian. Yet drilling depths are not excessive, ranging from 6,000 to 14,000 feet to the Precambrian. More production may be found in the Middle Ordovician Galena Limestone (Trenton), thus extending the present productive regions. In addition, new production may be found in narrow, dolomitized fracture zones in the tight limestone facies on the north flank of the basin . The underlying Platteville Limestone is finer grained and offers fewer possibilities. The Joachim Dolomite oil- shows occur in tight sandstone bodies that should have commercial porosity in some re- gions.
    [Show full text]
  • Bedrock Geology of Dodge County, Wisconsin (Wisconsin Geological
    MAP 508 • 2021 Bedrock geology of Dodge County, Wisconsin DODGE COUNTY Esther K. Stewart 88°30' 88°45' 88°37'30" 88°52'30" 6 EXPLANATION OF MAP UNITS Tunnel City Group, undivided (Furongian; 0–155 ft) FOND DU LAC CO 630 40 89°0' 6 ! 6 20 ! 10 !! ! ! A W ! ! 1100 W ! GREEN LAKE CO ! ! ! WW ! ! ! ! DG-92 ! ! ! 1100 B W! Includes Lone Rock and Mazomanie Formations. These formations are both DG-53 W ! «49 ! CORRELATION OF MAP UNITS !! ! 7 ! !W ! ! 43°37'30" R16E _tc EL709 DG-1205 R15E W R14E R15E DG-24 W! ! 1 Quaternary ! 980 ! W W 1 ! ! ! 6 DG-34 6 _ ! 1 R17E Os Lake 1 R16E 6 interbedded and laterally discontinuous and therefore cannot be mapped 1 6 W ! ! 1100 !! 175 940 Waupun DG-51 ! 980 « Oa ! R13E 6 Emily R14E W ! 43°37'30" ! ! ! 41 ¤151 B «49 ! ! ! ! Opc ! Drew «68 ! W ! East ! ! ! individually at this scale in Dodge County. Overlies Elk Mound Group across KW313 940 ! ! ! ! ! ! 940 ! W B ! ! - ! ! W ! ! ! ! ! ! !! Waupun ! W ! Undifferentiated sediment ! ! W! B 000m Cr W! ! º Libby Cr ! 3 INTRUSIVE SUPRACRUSTAL 3 1020 ! ! Waupun ! DG-37 W ! ! º 1020 a sharp contact. W ! 50 50 N ! ! KS450 ! ! ! IG300 ! B B Airport ! RO703 ! ! Brownsville ! ! ! ! ! ! 1060 ! ROCKS W ! ! ROCKS Unconsolidated sediments deposited by modern and glacial processes. 940 ° ! Qu ! W Br Rock SQ463 B ! Pink, gray, white, and green; coarse- to fine-grained; moderately to poorly 980 B River B B ! ! KT383 ! ! Generally 20–60 feet (ft) thick; ranges from absent where bedrock crops ! !! ! ! ! ! ! Su Lower Silurian ° ! ! ! ! ! 940 860 ! ! ! ! ! ! ! ! ! ! sorted; glauconitic sandstone, siltstone, and mudstone with variable W ! B B B ! ! ! 980 ! ! ! 780 ! Kummel !! out to more than 200 ft thick in preglacial bedrock valleys.
    [Show full text]
  • Dynamics of Appearance, Flourishing, and Extinction in the Devonian of Radiolarians with Two Porous Spheres and One Main Spine
    Dynamics of appearance, flourishing, and extinction in the Devonian of radiolarians with two porous spheres and one main spine Marina S. AFANASIEVA1 and Edward O. AMON2 1 A.A. Borissiak Paleontological Institute, Russian Academy of Sciences, Laboratory of Protistology, Profsoyuznaya 123, 117997 Moscow, Russia; [email protected] 2 Zavaritsky Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences, Pochtovyi per. 7, Yekaterinburg 620151, Russia; [email protected] The origin, basic evolutionary patterns, and great biotic crises in Phanerozoic radiolarian develop- ment were intimately connected with the geological history of the Earth. Glaciations and cold climate played a special role in radiolarian evolution. Radiolarians, which were typical for warm interglacial periods (greenhouse) disappeared during interglacial to glacial transition intervals (icehouse), and vice versa. Some possible regularities that resulted in increase radiolarian interglacial biodiversity, could be circumstanced by stabilization of climate and enhanced oceanic production. Biological mechanism, explaining these events, may be caused by phenomenon of solitary population waves (Kovalev, 2007). New species constantly appear under both favourable and severe conditions. Therefore, it is in- correct to propose that changes in global climatic conditions necessarily result in general deterioration of conditions in the habitats of all species. A crisis for some taxa is a chance for others (Kovalev et al., 2007; Chernykh et al., 2007). New morphological formations occurred usually under general stress. They probably invaded into global radiolarian fauna like a pandemic virus and instantaneously mi- grated to populations of remote water areas. Processes of expansion of species with morphological and/or physiological innovations into new ecological systems and adaptation to new niches are re- garded as different phases of existence of populations.
    [Show full text]
  • Stratigraphy and Structure of the Subsurface Cambrian and Ordovician Carbonates of New York
    DOCUMENT RESUME ED 093 640 SE 017 316 AUTHOR Rickard, Lawrence V. TITLE Stratigraphy and Structure of the Subsurface Cambrian and Ordovician Carbonates of New York. INSTITUTION New York State Education Dept., Albany. PUB DATE 73 NOTE 30p. EDRS PRICE EF-$0.75 HC-$1.85 PLUS POSTAGE DESCRIPTORS Bibliographies; Earth Science; *Geology; Instruction; *Instructional Materials; *Maps; *Paleontology; Science Education IDENTIFIERS New York State Museum and Science Service ABSTRACT This publication presents a description pf 137 wells in New York State and adjacent parts of Pennsylvania. Correlations with surface exposures are established. Maps and cross sections display the thickness, structure, and stratigraphic relationships of the carbonates described. ,A paleogeologic map of New York State at the end of the Early Ordovician is presented. Two distinct series of rocks which comprise the Cambrian and Ordovician carbonates of New York'are described and studied in detail. The monograpil includes an extensive bibliography, several schematic figures and diagrams, and two appendices which give data relevant to the identification of control wells and subsurface data from control wells. (Author/EB) U S. DEPARTMENT OF HEALTH. EDUCATION B WELFARE NATIONAL INSTITUTE OF EDUCATION THIS DOCUMENT HAS BEEN REPRO OUCEO EXACTLY AS RECEIVED FRO': THE PERSON OR ORGANIZATION ORIGIN ATING IT POINTS OF VIEW OR OPINIONS STATED DO NOT NECESSARILY REPRE SENT OFFICIAL NATIONAL INSTITUTE DI EDUCATION POSITION OR POLICY Stratigraphy and Structure of .the', Subsurface Cambrian OrdoVician arbonates of New York LAWRENCE V. RICKARD NEW YORK STATE MUSEUM AND SCIENCE SERVICE MAP AND CHART SERIES NUMBER 18 The Ulu:Trill) of the Slate of New .York The Stale Education Department Albany, 1973 THE UNIVERSITY OF THE STATE OF NEW YORK Regents of the University (with years when terms expire) 1984 JOSEPH W.
    [Show full text]
  • Late Cambrian Hard Substrate Communities from Montana/ Wyoming: the Oldest Known Hardground Encrusters
    Late Cambrian hard substrate communities from Montana/ Wyoming: the oldest known hardground encrusters CARLTON E. BREIT, W. DAVID LIDDELL AND KRAIG L. DERSTLER Brett. Carlton E., Liddell, W. David & Derstler, Kraig L. 1983 10 IS: Late Cambrian hard substrate I JETHAIA communities from MontandWyoming: the oldest known hardground encrustcrs. Lethaia, Vol. 16, pp. 281-289. Oslo. ISSN 0024-1164. Hardground surfaces from the Late Cambrian Snowy Range Formation in MontanalWyoming are the oldest known non-reefal hard substrates exhibiting encrusting fossils. These surfaces range in age from Early Franconian to early Trempealeauan. Hardgrounds were developed on slightly hummocky to planar, truncated surfaces of glauconite-rich, carbonate, flat pebble conglomerates, which were deposited during episodes of storm scouring in shallow subtidal environments of the Montana/Wyoming shelf. Snowy Range hardgrounds are encrusted by a low diversity assemblage of fossils dominated by simple discoidal holdfasts of pelmatozoans, probably crinoids, and including small conical spongiomorph algae? and probable stromatolites. Macroborings (e.g. Trypanites) are notably absent from all hardground surfaces, although sharp-walled, vertical, cylindrical holes (borings?) occur in micrite clasts imbedded in certain flat pebble conglomerates. No evidence of faunal succession or microecologic partitioning of irregular surfaces was observed on these Cambrian hardgrounds. 0 Hardgrounds, epibionts, macrobor- ings, pelmatozoan echinoderms, paleoecology, Cambrian, MontanaiWyoming. Cariton E. Brett, Department of Geological Sciences, The University of Rochesrer, Rochester. New York 14627; W. David Liddell, Department of Geology, Utah Stare University, Logan, Utah 84322; Kraig L. Derstler, Department of Geology, University of New Orleans, New Orleans, Louisiana 70122; 9th September, 1982. Hardgrounds afford a unique opportunity for pa- morph algae? and pelmatozoan echinoderm leoecological studies.
    [Show full text]
  • IGS 2015B-Maquoketa Group
    ,QGLDQD*HRORJLFDO6XUYH\ $ERXW8V_,*66WDII_6LWH0DS_6LJQ,Q ,*6:HEVLWHIGS Website Search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
    [Show full text]
  • Presented to the Uníversity of Manítoba Ín Partial Fulfillment of the Requírements for the Degree of Master of Science
    UPPERMOST ORDOVICIAN AND LOI^IERMOST SILURIAN STRATIGRAPHY AND SOLITARY RUGOSE CORALS OF THE EAST-CENTRAL UNITED STATES Robert J. McAuleY A thesis presented to the Uníversity of Manítoba ín Partial fulfillment of the requírements for the degree of Master of Science I^linnipeg, Manítoba 1985 UPPERMOST ORDOVICIAN AND LOWERMOST SILURIAN STRATIGRAPHY AND SOLITARY RUGOSE CORALS OF THE EAST-CENTRAL UNITED STATES BY ROBERT J. MCAULEY A tlresis st¡bmitted to the Faculty of Graduate Studies of the University of Ma¡litoba in partial fulfìll¡ne¡rt of the requiretttettts of the degree of MASTER OF SCIENCE o 1985 Permission has been grartted to the LIBRARY OF THE UNIVER- SITY OF MANITOBA to lend or sell copies of this thesis. to the NATIONAL LIBRARY OF CANADA to microfilnr this thesis and to lend or sell copies of the film, and UNIVERSITY MICROFILMS to publish an abstract of this thesis. The author reserves other publicatiolt rights, altd neitlter tlte thesis nor extensive ext¡acts from it may be printed or other- wise reproduced without the author's written perntissiott. l_ CONTENTS 1 Abs trac t Introduc tíon 4 Abbrevíations and RePositories 8 9 Acknowledgments Stratígraphic Sections and Collectíons 10 Eastern I.^Jísconsin 11 l1 Northeastern Illinoís . Eastern lowa 13 i3 Nor thr¿estern I11inoís T4 Northeastern Missourí . Southeastern Míssouri 15 16 Eastern Oklahoma I6 South-central Oklahoma StratígraPhY and SolitarY Rugose Corals 18 South-central Oklahoma 18 1B Lí thos tra tigraPhY Biota 23 24 Age of units Depositional envíronments 25 26 Northeastern Oklahoma LithostratígraPhY .. 26 26 Bio ta 26 Age of uníts 29 Depo sitional environments Southern Illínois and Southeastern 1l- Missouri 30 30 Lí thos tra tigraPhY 30 Bío ta Age of uníts 36 Depositíonal envíronments' 3l Northeastern Míssourí and 38 üles t-central Illinois 3B Li tho s tra tigraPhY Biota ..
    [Show full text]
  • Petrology and Diagenesis of the Cyclic Maquoketa Formation (Upper Ordovician) Pike County, Missouri
    Scholars' Mine Masters Theses Student Theses and Dissertations 1970 Petrology and diagenesis of the cyclic Maquoketa Formation (Upper Ordovician) Pike County, Missouri Edwin Carl Kettenbrink Jr. Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Geology Commons Department: Recommended Citation Kettenbrink, Edwin Carl Jr., "Petrology and diagenesis of the cyclic Maquoketa Formation (Upper Ordovician) Pike County, Missouri" (1970). Masters Theses. 5514. https://scholarsmine.mst.edu/masters_theses/5514 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. .,!) l PETROLOGY AND DIAGENESIS OF THE CYCLIC MAQUOKETA FORMATION (UPPER ORDOVICIAN) PIKE COUNTY, MISSOURI BY EDWIN CARL KETTENBRINK, JR., 1944- A THESIS submitted to the faculty of UNIVERSITY OF MISSOURI - ROLLA in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE IN GEOLOGY Rolla, Missouri 1970 T2532 231 pages c. I Approved by ~ (advisor) ~lo/ ii ABSTRACT The Maquoketa Formation (Upper Ordovician-Cincinnatian Series) has been extensively studied for over one hundred years, but a petrographic study of its cyclic lithologies has been neglected. The following six distinct Maquoketa lithologies have been recognized in this study in Pike County, Missouri& 1) phosphatic biosparite, 2) phos­ phorite, 3) micrite-microsparite, 4) dolomitic shale, 5) dolomitic marlstone, and 6) dolomitic quartz siltstone. Three cycle types are present in the Maquoketa. They are expressed as thin beds (1-20 inches) of alternating micrite-shale, micrite-marlstone, and shale-siltstone.
    [Show full text]
  • Upper Ordovician) at Wequiock Creek, Eastern Wisconsin
    ~rnooij~~~mij~rnoo~ ~oorn~rn~rn~~ rnoo~~rnrn~rn~~ Number 35 September, 1980 Stratigraphy and Paleontology of the Maquoketa Group (Upper Ordovician) at Wequiock Creek, Eastern Wisconsin Paul A. Sivon Department of Geology University of Illinois Urbana, Illinois REVIEW COMMITTEE FOR THIS CONTRIBUTION: T.N. Bayer, Winona State College University, Winona Minnesota M.E. Ostrom, Wisconsin Geological Survey, Madison, Wisconsin Peter Sheehan, Milwaukee Public Museum· ISBN :0-89326-016-4 Milwaukee Public Museum Press Published by the Order of the Board of Trustees Milwaukee Public Museum Accepted for publication July, 1980 Stratigraphy and Paleontology of the Maquoketa Group (Upper Ordovician) at Wequiock Creek, Eastern Wisconsin Paul A. Sivon Department of Geology University of Illinois Urbana, Illinois Abstract: The Maquoketa Group (Upper Ordovician) is poorly exposed in eastern Wisconsin. The most extensive exposure is found along Wequiock Creek, about 10 kilometers north of Green Bay. There the selection includes a small part of the upper Scales Shale and good exposures of the Fort Atkinson Limestone and Brainard Shale. The exposed Scales Shale is 2.4 m of clay, uniform in appearance and containing no apparent fossils. Limestone and dolomite dominate the 3.9 m thick Fort Atkinson Limestone. The carbonate beds alternate with layers of dolomitic shale that contain little to no fauna. The shales represent times of peak terrigenous clastic deposition in a quiet water environment. The car- bonates are predominantly biogenic dolomite and biomicrite. Biotic succession within single carbonate beds includes replacement of a strophomenid-Lepidocyclus dominated bottom community by a trep- ostome bryozoan-Plaesiomys-Lepidocyclus dominated community. Transported echinoderm and cryptostome bryozoan biocalcarenites are common.
    [Show full text]