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Recent Fossil Finds in the Indian Islands Group, Central Newfoundland
Current Research (2006) Newfoundland and Labrador Department of Natural Resources Geological Survey, Report 06-1, pages 221-231 RECENT FOSSIL FINDS IN THE INDIAN ISLANDS GROUP, CENTRAL NEWFOUNDLAND 1W.D. Boyce, P.Geo. and 2W.L. Dickson, P.Geo. 1Regional Geology Section 2Mineral Deposits Section ABSTRACT During the 2004 and 2005 field seasons a number of fossiliferous exposures of the Indian Islands Group rocks were exam- ined. The results of these fossil surveys are presented here. The occurrence of the bryozoan Stictopora scalpellum (Lonsdale, 1839) in many outcrops of the Silurian Indian Islands Group definitively dates these exposures as latest Wenlock (late Home- rian). Several richly fossiliferous localities yield faunas indicative of Wenlock, late Wenlock (Homerian), and middle Ludlow (late Gorstian to early Ludfordian) ages. INTRODUCTION Dudley, West Midlands, England, of late Homerian (latest Wenlock) age (Snell, 2004, page 6, Text-Figure 4). There is as yet no comprehensive, integrated lithostrati- graphic–biostratigraphic scheme for the Silurian shelly fau- Boyce (2004, page 7) identified Ptilodictya scalpellum nas of the Indian Islands Group (IIG). Furthermore, apart Lonsdale, 1839 from a sawdust-filled quarry near Glenwood from this report, the most extensive recent paleontological (JOD-2003-113 and LD05-0064 - see Plates 2 and 3) as well studies of the area remain those of Boyce et al. (1993), as from drill core at the Beaver Brook antimony mine Boyce and Ash (1994) and Donovan et al. (1997). (2004F016 - see Plate 4). During the summers of 2004 and 2005, Stictopora scalpellum (Lonsdale, 1839) was also iden- In 2004, a total of six days was spent in the field with tified from a number of additional IIG outcrops, including: G.C. -
Hydrogeology and Stratigraphy of the Dakota Formation in Northwest Iowa
WATER SUPPLY HYDROGEOLOGY AND J.A. MUNTER BULLETIN G.A. LUDVIGSON NUMBER 13 STRATIGRAPHY OF THE B.J. BUNKER 1983 DAKOTA FORMATION IN NORTHWEST IOWA Iowa Geological Survey Donald L. Koch State Geologist and Director 123 North Capitol Street Iowa City, Iowa 52242 IOWA GEOLOGICAL SURVEY WATER-SUPPLY BULLETIN NO. 13 1983 HYDROGEOLOGY AND STRATIGRAPHY OF THE DAKOTA FORMATION IN NORTHWEST IOWA J. A. Munter G. A. Ludvigson B. J. Bunker Iowa Geological Survey Iowa Geological Survey Donald L. Koch Director and State Geologist 123 North Capitol Street Iowa City, Iowa 52242 Foreword An assessment of the quantity and quality of water available from the Dakota (Sandstone) Formation 1n northwest Iowa is presented in this report. The as sessment was undertaken to provide quantitative information on the hydrology of the Dakota aquifer system to the Iowa Natural Resources Council for alloca tion of water for irrigation, largely as a consequence of the 1976-77 drought. Most area wells for domestic, livestock, and irrigation purposes only partial ly penetrated the Dakota Formation. Consequently, the long-term effects of significant increases in water withdrawals could not be assessed on the basis of existing wells. Acquisition of new data was based upon a drilling program designed to penetrate the entire sequence of Dakota sediments at key loca tions, after a thorough inventory and analysis of existing data. Definition of the distribution, thickness, and lateral and vertical changes in composition of the Dakota Formation has permitted the recognition of two mem bers. Additionally, Identification of the rock units that underlie the Dakota Formation has contributed greatly to our knowledge of the regional geology of northwest Iowa and the upper midwest. -
Stratigraphic Succession in Lower Peninsula of Michigan
STRATIGRAPHIC DOMINANT LITHOLOGY ERA PERIOD EPOCHNORTHSTAGES AMERICANBasin Margin Basin Center MEMBER FORMATIONGROUP SUCCESSION IN LOWER Quaternary Pleistocene Glacial Drift PENINSULA Cenozoic Pleistocene OF MICHIGAN Mesozoic Jurassic ?Kimmeridgian? Ionia Sandstone Late Michigan Dept. of Environmental Quality Conemaugh Grand River Formation Geological Survey Division Late Harold Fitch, State Geologist Pennsylvanian and Saginaw Formation ?Pottsville? Michigan Basin Geological Society Early GEOL IN OG S IC A A B L N Parma Sandstone S A O G C I I H E C T I Y Bayport Limestone M Meramecian Grand Rapids Group 1936 Late Michigan Formation Stratigraphic Nomenclature Project Committee: Mississippian Dr. Paul A. Catacosinos, Co-chairman Mark S. Wollensak, Co-chairman Osagian Marshall Sandstone Principal Authors: Dr. Paul A. Catacosinos Early Kinderhookian Coldwater Shale Dr. William Harrison III Robert Reynolds Sunbury Shale Dr. Dave B.Westjohn Mark S. Wollensak Berea Sandstone Chautauquan Bedford Shale 2000 Late Antrim Shale Senecan Traverse Formation Traverse Limestone Traverse Group Erian Devonian Bell Shale Dundee Limestone Middle Lucas Formation Detroit River Group Amherstburg Form. Ulsterian Sylvania Sandstone Bois Blanc Formation Garden Island Formation Early Bass Islands Dolomite Sand Salina G Unit Paleozoic Glacial Clay or Silt Late Cayugan Salina F Unit Till/Gravel Salina E Unit Salina D Unit Limestone Salina C Shale Salina Group Salina B Unit Sandy Limestone Salina A-2 Carbonate Silurian Salina A-2 Evaporite Shaley Limestone Ruff Formation -
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. -
Mechanical Properties of St. Peter Sandstone a Comparison of Field and Laboratory Results a Thesis Submitted to the Faculty of T
MECHANICAL PROPERTIES OF ST. PETER SANDSTONE A COMPARISON OF FIELD AND LABORATORY RESULTS A THESIS SUBMITTED TO THE FACULTY OF THE GRADUATE SCHOOL OF THE UNIVERSITY OF MINNESOTA BY MICHAEL EUGENE DITTES IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE DECEMBER, 2015 This thesis contains previously published material (Appendix E) in the “Journal of Geotechnical and Geoenvironmental Engineering” © 2002 ASCE. All other material © 2015 Michael E. Dittes All Rights Reserved. ACKNOWLEDGMENTS I would like to extend my thanks to those, who without their help I would not have been able to bring this project to completion. First and foremost, I thank Professor Joseph Labuz who took a chance on me, by offering me a TA-ship. Through my time in school, Joe helped me stay focused when I started to move off on tangents, offered timely advice, and over the years has become much more than my advisor. I am proud to think of him as a friend. Professors Andrew Drescher and Peter Huddleston also deserve special thanks for providing critical review of my work, and agreeing to sit on my thesis committee. To Ms. Tiffany Ralston who had an uncanny way of knowing what I needed to do, and how, before I knew myself. To Charles Nelson who helped me streamline my thesis project and helped me gain access to the Minnesota Library Archives construction site. To my fellow graduate students with whom I debated, joked and laughed, you helped me see things that I was missing. Your input was invaluable and you have my deep appreciation. -
Back Matter (PDF)
Index acritarchs 131 Carbonate Dagestan 259 Aeronian, recovery patterns 127-33 carbonate ramps, Frasnian-Famennian 135 Alaska, graptolites 119-26 Carboniferous Albian, Late, Albian-Cenomanian oceanic anoxic 'lesser mass extinction event' events (OAEs) 240-1 rugose corals ammonites 231 extinction 188-9 Campanian 299-308 recovery 192-7 desmoceratacean, E Russia, Sakhalin 299-308 survival interval 189-91 Santonian-Maastrichtian, stratigraphy 300-3 catastrophic mass extinction 54 see also goniatites Caucasus, N ammonoids foraminifera, Danian extinctions 337-42 early stages 164-8 locations 337 goniatite survival 163-85 Caucasus, NE Japan 306 foraminifera, Cenomanian-Turonian Boundary juvenile ornament 169 Event 259--64 morphological sequence 169 location map 260 protoconch size 166, 181 Cauvery Basin, oceanic anoxic events (OAEs) 238 recovery, Sakhalin 304, 306 Cenomanian-Turonian Boundary Event taxonomic diversity, dynamics 305 dinoflagellate cyst assemblages recovery, England, Amphipora-bearing limestone 135-61 oceanic anoxic events 279-97 angiosperms, origination, extinction and diversity 73 England, S 267 Anisian Stage 223, 224 food chain recovery 265-77 Lazarus taxa 227 foraminifera 237-44, 259-64 Annulata Event, Devonian 178 Milankovitch rhythms 246 Apterygota 65 oceanic anoxic events (OAEs) archaeocyaths 82, 86 India, SE, Cauvery Basin 237-44 Ashgill, correlation of biotic events 129 NE Caucasus 259-64 Atavograptus atavus Zone 124 Spain, Menoyo section 245-58 Avalonian plate 125 Turonian lithological logs, England, SE 280-2 Changxingian -
Geological-Geotechnical Studies for Siting the Superconducting Super Collider in Illinois: Results of Drilling Large- Diameter Test Holes in 1986
LIBRARY. «-*/ f ion a JUN 1 2 1997 !L (jcul. ourWEY ; QoJ> 2«AAX-W f&S: EGN 124 GEOLOGICAL-GEOTECHNICAL STUDIES FOR SITING THE SUPERCONDUCTING SUPER COLLIDER IN ILLINOIS: RESULTS OF DRILLING LARGE- DIAMETER TEST HOLES IN 1986 / \ / 3 S z^rf / / y s > ',',',',', ' ', ', ', / ',',',',',, / ^ / / / zrzzzrzzzzz zrzzzzzzzzz. ^/^ ^ * / / / / ^7 R. C. Vaiden / / / / s^r M. J. Hasek / ; ; / ; / / / / /^7 / / / / / y C. R. Gendron * ^ / / ^ 7 ' '. /. /. B. B. Curry - '.', ; / / / ^ — A. M. Graese / / s / s z 5^^ ^ ^ R. A. Bauer /7777 > v v y y -Mum 1988 iiUN 1 3 ENVIRONMENTAL GEOLOGY NOTES 124 ''l. STATE GEOiOfiMKiip Department of Energy and Natural Resources ILLINOIS STATE GEOLOGICAL SURVEY LIBRARY. Vaiden, Ft. C. Geological-geotechnical studies for siting the Superconducting Super Collider in Illinois: results of drilling large-diameter test holes in 1986/ by R. C. Vaiden ... et al.—Champaign, IL: Illinois State Geological Survey, 1988. 57 p.; 28 cm. — (Environmental Geology Notes; 124) Bibliography: p. 42-44. 1. Geology— Illinois—Kane County. 2. Geology— Illinois—DuPage County. 3. Hydrogeology— Illinois—Kane County. 4. Hydrogeol- ogy— Illinois—DuPage County. 5. Geophysical exploration— Illinois, Northeastern. 6. SSC. I. Title. II. Series. Printed by authority of the State of Illinois 1 1988 1 1500 ILLINOIS STATE GEOLOGICAL SURVEY 3 3051 00005 5016 GEOLOGICAL-GEOTECHNICAL STUDIES FOR SITING THE SUPERCONDUCTING SUPER COLLIDER IN ILLINOIS: RESULTS OF DRILLING LARGE- DIAMETER TEST HOLES IN 1986 ILLINOIS STATE GEOLOGICAL SURVEY Morris W. Leighton, Chief Natural Resources Building 61 5 East Peabody Drive Champaign, Illinois 61820 R. C. Vaiden M. J. Hasek C. R. Gendron B. B. Curry A. M. Graese R. A. Bauer 1988 ENVIRONMENTAL GEOLOGY NOTES 124 JUN13i U. -
UPPER IOWA RIVER WATERSHED: PHASE 4: Ridgeway 7.5' Quadrangle
Surficial Geology of the Ridgeway (Iowa) 7.5' Quadrangle LEGEND 92°0'0"W 91°57'30"W 91°55'0"W 91°52'30"W CENOZOIC Qpsr 43°22'30"N Qal Qal Qal Qpsr D Qps Qal QUATERNARY SYSTEM 43°22'30"N Qal Qpsr Qpsr Qal Om Om Qps Qwa2 Qps Qal Om Om Qal Qwa2 Om Qal Od Qps Od Qal Owd Qps Owd Qpsr Qpsr HUDSON EPISODE Om Owd Qpsr Qal - Alluvium (De Forest Formation-Undifferentiated) One to four meters (3 – 13 ft) of massive to weakly stratified, grayish brown to brown Qal Qal Qal loam, silt loam, clay loam, or loamy sand overlying less than three meters (10 ft) of poorly to moderately well sorted, massive to moderately Qwa2 Om Owd Qps Qal well stratified, coarse to fine feldspathic quartz sand, pebbly sand, and gravel and more than three meters (10 ft) of pre-Wisconsin or late Qpsr Om Qpsr Wisconsin Noah Creek Formation sand and gravel. Also includes colluvium derived from adjacent map units in stream valleys, on hillslopes, Owd Qpsr Qpsr Owd Qal Owd and in closed depressions. Seasonal high water table occurs in this map unit. Owd Qnw2 Od D Qal Qnw2 Qal D D Qal D Qnw2 Qnw2 Om Owd Od Qpsr Qpsr D Qnw2 D HUDSON AND WISCONSIN EPISODE Om D D Om D Qpsr Om D Odpg Owd D D Qps Od Qnw2 – Sand and Gravel (Noah Creek Formation) Two to eighteen meters (6.5-59 ft) of yellowish brown to gray, poorly to well sorted, Om Owd Qps D DD Qnw2 Qps D Qpsr massive to well stratified, coarse to fine feldspathic quartz sand, pebbly sand and gravel with few intervening layers of silty clay. -
Beaver Brook Antimony Mine Revisited: an Update on Operations and New Structural and Geological Observations
Current Research (2018) Newfoundland and Labrador Department of Natural Resources Geological Survey, Report 18-1, pages 123-152 BEAVER BROOK ANTIMONY MINE REVISITED: AN UPDATE ON OPERATIONS AND NEW STRUCTURAL AND GEOLOGICAL OBSERVATIONS H.A.I. Sandeman, C. Peddle1 and R. Newman2 Mineral Deposits Section 1Department of Earth Sciences, Memorial University of Newfoundland, St. John’s, NL, A1B 3X5 2Beaver Brook Antimony Mines Inc., 1 Mine Site Rd, Glenwood, NL, A0G 2K0 ABSTRACT Epithermal, fracture-controlled stibnite–quartz mineralization at Beaver Brook in central Newfoundland was discovered in 1989 during regional gold exploration surveys. Mineralization occurs along three zones (West, Central and East), disposed along a 4-km strike length outboard of the eastern margin of the Mount Peyton intrusive suite; the latter two zones have delin- eated reserves. The mine is in the East zone, where mineralization consists of massive stibnite veins, vein breccia, vug fillings and fracture coatings that occur in the hanging wall of an 065º-trending, steeply to moderately southeast-dipping fault. Gold abundances are typically low in the East zone stibnite–quartz ore, however, near the Central zone, diamond-drill hole (DDH) intercepts have yielded up to 26 g/t Au over 2 m, with and without coincident Sb. Beaver Brook Antimony Mine opened in 1997, but ceased after 8 months of operations. In 2007, after an ownership change, the mine was dewatered, reopened and processed ore until 2012. Exploration of the mine lease has continued through the acquisition of IP geophysical surveys, soil surveys and completion of a further 100 DDH throughout previously unexplored parts of the property. -
Paleozoic Lithostratigraphic Nomenclature for Minnesota
MINNESOTA GEOLOGICAL SURVEY PRISCILLA C. GREW, Director PALEOZOIC LITHOSTRATIGRAPHIC NOMENCLATURE FOR MINNESOTA John H. Mossier Report of Investigations 36 ISSN 0076-9177 UNIVERSITY OF MINNESOTA Saint Paul - 1987 PALEOZOIC LITHOSTRATIGRAPHIC NOMENCLATURE FOR MINNESOTA CONTENTS Abstract. Structural and sedimentological framework • Cambrian System • 2 Mt. Simon Sandstone. 2 Eau Claire Formation • 6 Galesville Sandstone • 8 Ironton Sandstone. 9 Franconia Formation. 9 St. Lawrence Formation. 11 Jordan Standstone. 12 Ordovician System. 13 Prairie du Chien Group. 14 Oneota Dolomite. 14 Shakopee Formation. 15 St. Peter Sandstone. 17 Glenwood Formation. 17 Platteville Formation. 18 Decorah Shale. 19 Galena Group • 22 Cummings ville Formation. 22 Prosser Limestone. 23 Stewartville Formation • 24 Dubuque Formation. 24 Maquoketa Formation. 25 Devonian System • 25 Spillville Formation • 26 Wapsipinicon Formation 26 Cedar Valley Formation • 26 Northwestern Minnesota. 28 Winnipeg Formation • 28 Red River Formation. 29 Acknowledgments • 30 References cited. 30 Appendix--Principal gamma logs used to construct the composite gamma log illustrated on Plate 1. 36 ILLUSTRATIONS Plate 1 • Paleozoic lithostratigraphic nomenclature for Minnesota • .in pocket Figure 1. Paleogeographic maps of southeastern Minnesota • 3 2. Map showing locations of outcrops, type sections, and cores, southeastern t1innesota • 4 3. Upper Cambrian stratigraphic nomenclature 7 iii Figure 4. Lower Ordovician stratigraphic nomenclature • • • • 14 5. Upper Ordovician stratigraphic nomenclature 20 6. Middle Devonian stratigraphic nomenclature. • • . • • 27 7. Map showing locations of cores and cuttings in northwestern Minnesota • • • • • • • • • • • • • • • • • • 29 TABLE Table 1. Representative cores in Upper Cambrian formations •••••• 5 The University of Minnesota is committed to the policy that all persons shall have equal access to its programs, facilities, and employment without regard to race, religion, color, sex, national orgin, handicap, age, veteran status, or sexual orientation. -
Basin-Centered Gas Systems of the U.S. by Marin A
Basin-Centered Gas Systems of the U.S. By Marin A. Popov,1 Vito F. Nuccio,2 Thaddeus S. Dyman,2 Timothy A. Gognat,1 Ronald C. Johnson,2 James W. Schmoker,2 Michael S. Wilson,1 and Charles Bartberger1 Columbia Basin Western Washington Sweetgrass Arch (Willamette–Puget Mid-Continent Rift Michigan Basin Sound Trough) (St. Peter Ss) Appalachian Basin (Clinton–Medina Snake River and older Fms) Hornbrook Basin Downwarp Wasatch Plateau –Modoc Plateau San Rafael Swell (Dakota Fm) Sacramento Basin Hanna Basin Great Denver Basin Basin Santa Maria Basin (Monterey Fm) Raton Basin Arkoma Park Anadarko Los Angeles Basin Chuar Basin Basin Group Basins Black Warrior Basin Colville Basin Salton Mesozoic Rift Trough Permian Basin Basins (Abo Fm) Paradox Basin (Cane Creek interval) Central Alaska Rio Grande Rift Basins (Albuquerque Basin) Gulf Coast– Travis Peak Fm– Gulf Coast– Cotton Valley Grp Austin Chalk; Eagle Fm Cook Inlet Open-File Report 01–135 Version 1.0 2001 This report is preliminary, has not been reviewed for conformity with U. S. Geological Survey editorial standards and stratigraphic nomenclature, and should not be reproduced or distributed. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U. S. Government. 1Geologic consultants on contract to the USGS 2USGS, Denver U.S. Department of the Interior U.S. Geological Survey BASIN-CENTERED GAS SYSTEMS OF THE U.S. DE-AT26-98FT40031 U.S. Department of Energy, National Energy Technology Laboratory Contractor: U.S. Geological Survey Central Region Energy Team DOE Project Chief: Bill Gwilliam USGS Project Chief: V.F. -
Henrystommel
Volume 35, Special Issue 1992 A Tribute to Henry Stommel Most human history has not afforded men much chance to pursue rich or the a their curiosity, except as a hobby of the within refuge of monastery. We can count ourselves fortunate to live in a society and at a time when we are actually paid to explore the universe. Henry Stommel, 1974 Vicky Cullen Editor Lisa Clark Assistant Editor InternationalOceqnusPerspectives on Our Ocean Environment Frisbee Kathy Sharp Volume 35, Special Issue 1992 ISSN 0029-8182 Business & Advertising Coordinator Barbara Gaffron K.I. Faith Hampshire Jeanne Young Editorial Assistants Ellen Schneider Editorial Intern Jayne Doucette Computer Graphics * * * 1930 The views expressed in Oceanus are those of the authors and do not necessarily reflect those of Oceanus Magazine or its publisher, the Woods Hole Oceanographic Institution. Published Quarterly as a Benefit of the Woods Hole Oceanographic Institution Editorial responses and advertising inquiries are welcome. Please write: Affiliates Program Oceanus Magazine Woods Hole Oceanographic Institution Guy W. Nichols, Chairman of the Board of Trustees Woods Massachusetts Hole, 02543, James M. Clark, President of the Corporation or (508) 457-2000, ext. 2386. telephone: Charles A. Dana, III, President of the Associates Members within the US, Canada, and Mexico, Craig E. Dorman, Director of the Institution please write: Oceanus Subscriber Service Sallie K. Riggs, Director of Communications Center, P.O. Box 6419, Syracuse, NY 13217- 6419, or telephone, toll free: 1-800-825-0061 forsubscription-related questions. Individual Editorial Advisory Board rate, $25 Students, membership per year; D. Baker $20; Libraries and Institutions, $35.