GEOLOGY and UNDERGROUND WATERS J of SOUTH DAKOTA (

Total Page:16

File Type:pdf, Size:1020Kb

GEOLOGY and UNDERGROUND WATERS J of SOUTH DAKOTA ( DEPARTMENT OF THE INTEEIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIEECTOE WATER-SUPPLY PAPER 227 GEOLOGY AND UNDERGROUND WATERS j OF SOUTH DAKOTA ( BY N. H. DARTON i ' WASHINGTON GOVEBNMENT PBINTING OFFICE 1909 CONTENTS. Page. Introduction.............................................................. 7 Geography and topography.................................................. 8 Geology of the Black Hills region............................................ 8 General relations....................................................... 8 Cambrian system....................................................... 10 Deadwood sandstone............................................... 10 Ordovician system..................................................... 11 Whitewood limestone............................................... 11 Carboniferous system................................................... 11 General outline................................................... 11 Englewood limestone............................................... 12 Pahasapa limestone................................................. 12 Minnelusa sandstone................................................ 13 Opeche formation.................................................. 14 Minnekahta limestone............................................. 14 Triassic (?) system..................................................... 15 Spearfish formation................................................. 15 Jurassic system......................................................... 16 Sundance formation............................................... 16 Unkpapa sandstone................................................. 17 Cretaceous system..................................................... 17 Morrison shale..................................................... 17 Lakota sandstone.................................................. 18 Minnewaste limestone.............................................. 18 Fuson formation.................................................... 19 Dakota sandstone............. .................................... 20 Benton group...............................'...................... 20 Graneros shale................................................ 20 Greenhorn limestone........................................... 21 Carlile shale.................................................. 21 Niobrara formation....'............................................ 22 Pierre shale........................................................ 22 Fox Hills'sandstone............................... ^................ 24 Tertiary system....................................................... 24 White River group................................................. 24 Geology of south-central South Dakota....................:.................. 26 General relations....................................................... 26 Tertiary deposits....................................................... 26 Geology of northwestern South Dakota..................................... 1. 27 General outline...............................................^ ......... 27 Fort Union, Laramie (?), and Fox Hills formations....................... 28 Post-Eocene..........'................................................ 31 Geology of eastern South Dakota........................................... 32 General structure....................................................... 32 Archean and Algonkian rocks........................................... 33 Paleozoic to Jurassic................................................... 40 3 4 CONTENTS. Geology of eastern South Dakota Continued. Page. Cretaceous system..................................................... 41 Dakota sandstone.................................................. 41 Benton group..................................................... 48 Niobrara formation................................................ 53 Pierre shale........................................................ 56 Fox Hills sandstone.....:.......................................... 58 Tertiary deposits. .................................................... 58 Quaternary deposits................................................... 58 Underground waters........................................."............... 59 General conditions.................................................... 59 Water horizons........................................................ 61 Dakota and associated sandstones................................... 61 Sandstones of the Benton group..................................... 62 Minnelusa sandstone.............................................. 62 Fox Hills and overlying sandstones................................. 63 Deadwood sandstone............................................... 63 ,Chadron formation................................................. 63 Deep wells and well prospects in South Dakota.......................... 64 Introductory statement. .......................................... 64 Aurora County. .................................................. 65 Beadle County.................................................... 68 Bonhomme County............................................... 69 Brookings County.^............................................... 72 Brown County..................................................... 72 Brule County.......................................... '. .......... 74 Buffalo County................................................... 75 Butte County. ................................................... 76 Belle Fourche and vicinity.................................... 78 United States Reclamation Service............................ 79 Orman well................................................... 80 Chambers ranch. ............................................. 81 Vale......................................................... 81 Campbell County.....'............................................. 81 Charles Mix County.........:...................................... 82 Cheyenne Indian Reservation..................................... 84 Clark County..................................................... 85 Raymond..................................................... 85 Clark. ..........................:............................ 86 Clay County...................................................... 86 Codington County................................................. 87 Custer County..................................................... 87 Davidson County................................................. 89 Day County....................................................... 90 Andover..................................................... 91 Pierpoint. ................................................... 91 Webster....................................................... 91 Deuel County. ................................................... 92 Douglas County. ................................................. 92 Edmunds County................................................. 92 Fall River County................................................ 94 Edgemont..................................................... 95 Minnekahta................................................... 99 Ardmore...................................................... 100 CONTENTS. 5 Underground waters Continued. Page. Deep wells and well prospects in South Dakota Continued. Fall River County Continued. Argentine.................................................... 100 Hot Springs................................................... 101 Faulk County. ................................................... 101 Grant County...................................................... 102 Gregory County................................................... 103 Hamlin County................................................... 104 Hand County...................................................... 104 Hanson County.................................................... 106 Hughes County.................................................... 108 Hutchinson County................................................ 109 Hyde County..........................!........................... Ill Jerauld County.................................................... 112 Kingsbury County................................................ 113 Lake County..................................................... 117 Lawrence County.................................................. 118 Lincoln County.................................................... 118 Lyman County..................................................... 119 Wells opposite Chamberlain.................................... 119 McClure well................................................. 120 Capa......................................................... 120 Kennebec.....................................................'. 121 Vivian....................................................... 121 Draper....................................................... 121 Murdo McKenzie............................................. 121 McCook County................................................... 122 McPherson County................................................. 122 Marshall County.................................................. 123 Meade County..................................................... 124 Wells north of Sturgis.......................................... 124 Fort Meade.................................................... 125 Miner County...................................................... 126 Minnehaha County................................................
Recommended publications
  • Floods in North and South Dakota Frequency and Magnitude
    UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY FLOODS IN NORTH AND SOUTH DAKOTA FREQUENCY AND MAGNITUDE By John A. McCabe and Orlo A. Crosby Prepared in cooperation with the NORTH DAKOTA STATE HIGHWAY DEPARTMENT AND THE SOUTH DAKOTA DEPARTMENT OF HIGHWAYS Open-file report Bismarck, North Dakota May 1959 DEC 15 1967 PREFACE This report was prepared by the U. S. Geological Survey in cooperation with the North Dakota State Highway Department and the South Dakota Department of Highways. The work was performed under the supervision of H. M. Erskine. District Engineer, Surface Water Branch. Water Resources Division, U. S. Geological Survey. The authors were assisted by R. E. West. Advice and review were furnished by the Floods Section. Surface Water Branch, Washington. D. C. The streamflow records used in this report were collected and compiled by the U. S. Geological Survey co­ operating with the following agencies: the North Dakota State Engineer and State Water Conservation Commission; pthe South Dakota State Engineer, State Geologist. State Fish and Game Commission, and State Water Resources Commission; the Corps of Engineers, Department of the Army; the Department of State; the Bureau of Reclamation and the Fish and Wildlife Service, Department of the Interior; the Soil Conservation Service, Department of Agriculture; and others. CONTENTS Page Page Abstract. .................. 1 Gaging-station records--Continued Introduction ................. 1 Red River of the North basin--Continued Description of the area .......... 1 Sheyenne River at West Fargo, Physiography ............ 1 N. Dak. (13). ........... 41 Climate ............... 1 Maple River at Mapleton, N. Dak. (14) . 42 Causes of floods ............. 1 Rush River at Amenia, N.
    [Show full text]
  • South Dakota to Nebraska
    Geological Society of America Special Paper 325 1998 Lithostratigraphic revision and correlation of the lower part of the White River Group: South Dakota to Nebraska Dennis O. Terry, Jr. Department of Geology, University of Nebraska—Lincoln, Lincoln, Nebraska 68588-0340 ABSTRACT Lithologic correlations between type areas of the White River Group in Nebraska and South Dakota have resulted in a revised lithostratigraphy for the lower part of the White River Group. The following pedostratigraphic and lithostratigraphic units, from oldest to youngest, are newly recognized in northwestern Nebraska and can be correlated with units in the Big Badlands of South Dakota: the Yellow Mounds Pale- osol Equivalent, Interior and Weta Paleosol Equivalents, Chamberlain Pass Forma- tion, and Peanut Peak Member of the Chadron Formation. The term “Interior Paleosol Complex,” used for the brightly colored zone at the base of the White River Group in northwestern Nebraska, is abandoned in favor of a two-part division. The lower part is related to the Yellow Mounds Paleosol Series of South Dakota and rep- resents the pedogenically modified Cretaceous Pierre Shale. The upper part is com- posed of the unconformably overlying, pedogenically modified overbank mudstone facies of the Chamberlain Pass Formation (which contains the Interior and Weta Paleosol Series in South Dakota). Greenish-white channel sandstones at the base of the Chadron Formation in Nebraska (previously correlated to the Ahearn Member of the Chadron Formation in South Dakota) herein are correlated to the channel sand- stone facies of the Chamberlain Pass Formation in South Dakota. The Chamberlain Pass Formation is unconformably overlain by the Chadron Formation in South Dakota and Nebraska.
    [Show full text]
  • Stratographic Coloumn of Iowa
    Iowa Stratographic Column November 4, 2013 QUATERNARY Holocene Series DeForest Formation Camp Creek Member Roberts Creek Member Turton Submember Mullenix Submember Gunder Formation Hatcher Submember Watkins Submember Corrington Formation Flack Formation Woden Formation West Okoboji Formation Pleistocene Series Wisconsinan Episode Peoria Formation Silt Facies Sand Facies Dows Formation Pilot Knob Member Lake Mills Member Morgan Member Alden Member Noah Creek Formation Sheldon Creek Formation Roxana/Pisgah Formation Illinoian Episode Loveland Formation Glasford Formation Kellerville Memeber Pre-Illinoian Wolf Creek Formation Hickory Hills Member Aurora Memeber Winthrop Memeber Alburnett Formation A glacial tills Lava Creek B Volcanic Ash B glacial tills Mesa Falls Volcanic Ash Huckleberry Ridge Volcanic Ash C glacial tills TERTIARY Salt & Pepper sands CRETACEOUS "Manson" Group "upper Colorado" Group Niobrara Formation Fort Benton ("lower Colorado ") Group Carlile Shale Greenhorn Limestone Graneros Shale Dakota Formation Woodbury Member Nishnabotna Member Windrow Formation Ostrander Member Iron Hill Member JURASSIC Fort Dodge Formation PENNSYLVANIAN (subsystem of Carboniferous System) Wabaunsee Group Wood Siding Formation Root Formation French Creek Shale Jim Creek Limestone Friedrich Shale Stotler Formation Grandhaven Limestone Dry Shale Dover Limestone Pillsbury Formation Nyman Coal Zeandale Formation Maple Hill Limestone Wamego Shale Tarkio Limestone Willard Shale Emporia Formation Elmont Limestone Harveyville Shale Reading Limestone Auburn
    [Show full text]
  • UNITED STATES DISTRICT COURT AUG 0 5 2016 Owner, Operator, And
    Case 5:16-cv-05068-JLV Document 1 Filed 08/05/16 Page 1 of 6 PageID #: 1 FILED UNITED STATES DISTRICT COURT AUG 0 5 2016 DISTRICT OF SOUTH DAKOTA i WESTERN DIVISION 'CLfcfiK KARRIE K. YANKTON, CIVIL FILE NO. Plaintiff, V. COMPLAINT UNITED STATES OF AMERICA, Defendants. COMES NOW the Plaintiff Karrie K. Yankton, by and through legal counsel, and for her complaint, states as follows: 1. Plaintiff, Karrie K. Yankton is Native American and a member of the Oglala Sioux Tribe, residing in Pine Ridge, Oglala Lakota County, South Dakota. 2. At all times relevant hereto, the Department of Health and Human Services, a federal agency of the Defendant United States government, was and is now the owner, operator, and/or manager of the Pine Ridge Indian Health Service (IHS) Hospital in Pine Ridge, Oglala Lakota County, South Dakota. The Pine Ridge Indian Health Service Hospital is located within the exterior boundaries of the Pine Ridge Sioux Indian Reservation, and is legally obligated to provide health care services to Native Americans by statutory and treaty mandates. .nJRISDICTION 3. At all times relevant hereto, the United States, the Unites States Department of Health and Human Services, and the Pine Ridge IHS Hospital, are legally obligated to provide health care services to Native Americans by statutory and treaty mandates. The Oglala Sioux Tribe and the Department of Health Human Services are covered under the Federal Tort Claims Case 5:16-cv-05068-JLV Document 1 Filed 08/05/16 Page 2 of 6 PageID #: 2 Act(FTCA). A recent FTCA administrative claim was filed on June 4, 2012, naming those entities, and was denied on January 23, 2014.
    [Show full text]
  • 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.
    [Show full text]
  • Variability of Nanopore Systems in the Lincoln Limestone, Denver-Julesburg Basin, Colorado, Usa
    VARIABILITY OF NANOPORE SYSTEMS IN THE LINCOLN LIMESTONE, DENVER-JULESBURG BASIN, COLORADO, USA By Brandon Franklin Werner Chase B.A., University of Colorado, Boulder, 2016 Undergraduate Thesis submitted to the Faculty of the Undergraduate School of the University of Colorado’s Department of Geological Sciences 2016 Committee: David Budd – Geological Sciences – Advisor Charles Stern – Geological Sciences Tyler Lansford - Classics ABSTRACT: With a shift to exploiting unconventional petroleum plays in the United States to support energy consumption, understanding the nanopore systems in those unconventional resources becomes important for future exploitation. The goal of this study is to characterize the pore systems of the Cretaceous Lincoln Limestone found in the Denver-Julesburg (DJ) Basin in order to test the hypothesis that lithologic variability has a control on pore characteristics and total porosity. The Lincoln Limestone represents a possible reservoir interval in close proximity to a source interval, the Hartland Shale, which directly overlies it, thus making it a potentially profitable future exploration target. Pore networks in the Lincoln were characterized using AR-milled rock surfaces run through a scanning electron microscope (SEM) for image capture, image analysis with Avizio 9 software, and mineralogical characterization by X- Ray fluorescence (XRF). Seven samples were chosen for analysis from a single core taken from one well in the DJ basin. Five of the samples span the roughly 70-90 ft thick Lincoln Limestone and the other two come from right above and right below the Lincoln. The seven samples span the range of lithologic and porosity variability in the Lincoln Limestone. They have normalized volumes of carbonate that range from 6.0% to 70.6% (mostly as calcite); clay content ranges from 14.8% to 55.2%.
    [Show full text]
  • Rodents (Mammalia) from the Pilgrim Creek Local Fauna, Wyoming: a Mixed Eocene and Oligocene Assemblage (Duchesnean to Whitneyan)
    Paludicola 11(2):51-72 March 2017 © by the Rochester Institute of Vertebrate Paleontology RODENTS (MAMMALIA) FROM THE PILGRIM CREEK LOCAL FAUNA, WYOMING: A MIXED EOCENE AND OLIGOCENE ASSEMBLAGE (DUCHESNEAN TO WHITNEYAN) William W. Korth Rochester Institute of Vertebrate Paleontology, 265 Carling Road, Rochester, New York 14610 <[email protected]> ABSTRACT Previously, only the non-eomyid rodents from the Pilgrim Creek fauna of Wyoming have been described (Sutton and Black, 1975; Korth, 1981; Korth and Emry, 2013). This fauna has been considered as Chadronian in age since its first description. Twenty-seven species of rodents are recognized here from this fauna. There is a predominance of Chadronian species (13 taxa); however, the presence of three species known elsewhere from the Duchesnean (“Leptotomus” guildayi, Metanoiamys korthi, Griphomys cf. alecer), four from the Orellan (“Prosciurus” sp., cf. relictus, Eumys elegans, “Scottimus” viduus, Protosciurus sp., cf. P. mengi), and two from the Whitneyan (Leptodontomys douglassi, Ansomys sp., cf. A. cyanotephrus,) demonstrates that the fauna is clearly mixed with elements from four different horizons. INTRODUCTION either earlier or later horizons, demonstrating the evident mixing of faunas. Over 40 years ago, Sutton and Black (1975) _________________________________________ identified 11 species of rodents from the Pilgrim Creek fauna of Wyoming (Table 1). However, TABLE 1. Previously identified rodents from the Pilgrim Creek specimens of the family Eomyidae were not local fauna, Wyoming (Sutton and Black, 1975). described or listed. The locality from which the Ischyromyidae fossils were collected is in the Teton National Forest Ischyromys cf. veterior in Jackson County, Wyoming along Pilgrim Creek Cylindrodontidae (Sutton and Black, 1975).
    [Show full text]
  • Fossil Amphibians and Reptiles from the Neogene Locality of Maramena (Greece), the Most Diverse European Herpetofauna at the Miocene/Pliocene Transition Boundary
    Palaeontologia Electronica palaeo-electronica.org Fossil amphibians and reptiles from the Neogene locality of Maramena (Greece), the most diverse European herpetofauna at the Miocene/Pliocene transition boundary Georgios L. Georgalis, Andrea Villa, Martin Ivanov, Davit Vasilyan, and Massimo Delfino ABSTRACT We herein describe the fossil amphibians and reptiles from the Neogene (latest Miocene or earliest Pliocene; MN 13/14) locality of Maramena, in northern Greece. The herpetofauna is shown to be extremely diverse, comprising at least 30 different taxa. Amphibians include at least six urodelan (Cryptobranchidae indet., Salamandrina sp., Lissotriton sp. [Lissotriton vulgaris group], Lissotriton sp., Ommatotriton sp., and Sala- mandra sp.), and three anuran taxa (Latonia sp., Hyla sp., and Pelophylax sp.). Rep- tiles are much more speciose, being represented by two turtle (the geoemydid Mauremys aristotelica and a probable indeterminate testudinid), at least nine lizard (Agaminae indet., Lacertidae indet., ?Lacertidae indet., aff. Palaeocordylus sp., ?Scin- cidae indet., Anguis sp., five morphotypes of Ophisaurus, Pseudopus sp., and at least one species of Varanus), and 10 snake taxa (Scolecophidia indet., Periergophis micros gen. et sp. nov., Paraxenophis spanios gen. et sp. nov., Hierophis cf. hungaricus, another distinct “colubrine” morphotype, Natrix aff. rudabanyaensis, and another dis- tinct species of Natrix, Naja sp., cf. Micrurus sp., and a member of the “Oriental Vipers” complex). The autapomorphic features and bizarre vertebral morphology of Perier- gophis micros gen. et sp. nov. and Paraxenophis spanios gen. et sp. nov. render them readily distinguishable among fossil and extant snakes. Cryptobranchids, several of the amphibian genera, scincids, Anguis, Pseudopus, and Micrurus represent totally new fossil occurrences, not only for the Greek area, but for the whole southeastern Europe.
    [Show full text]
  • Blue River Valley Stratigraphic Chart
    Blue River Valley Hydrogeologic Geologic Period Phase Stratigraphic Unit Unit Modern Alluvium and outwash deposits Alluvial Aquifer Quaternary Glacial deposits Glacial deposits Glaciation Older stream and outwash terrace Local perched deposits aquifer Troublesome Formation Local aquifer Neogene Extension Volcanic rocks Volcanics Paleogene Transition Paleogene and Cretaceous intrusive Crystalline rocks bedrock Laramide Pierre Shale Smoky Hill Member Fort Hayes Limestone Pierre confining Niobrara Niobrara Formation Cretaceous unit Interior Carlile Shale Seaway Greenhorn Limestone Graneros Shale Benton Group Dakota Sandstone Dakota Aquifer Morrison Formation Morrison Aquifer Jurassic Mesozoic Entrada Sandstone Entrada Aquifer Sandstones Chinle confining Triassic Chinle Formation unit Permian Maroon Formation Ancestral Maroon-Minturn Rocky Aquifer Mountains Minturn Formation Pennsylvanian Mississippian No strata Devonian Chaffee Group Paleozoic Silurian Mississippian- Carbonates Cambrian Ordovician Manitou Formation carbonate aquifer Dotsero Formation and Cambrian Sawatch Sandstone Crystalline rocks of igneous and Crystalline Precambrian Precambrian metamorphic origin in mountainous bedrock region Table 12a-05-01. Blue River Valley stratigraphic chart. Blue River Valley Unit Thickness Hydrogeologic Geologic Period Phase Stratigraphic Unit Physical Characteristics Hydrologic Characteristics (ft) Unit Well to poorly-sorted, uncemented sands, silts and gravels along modern Modern Alluvium and outwash deposits >35 Alluvial Aquifer streams and
    [Show full text]
  • Lands of the Lakota: Policy, Culture and Land Use on the Pine Ridge
    1 Lands of the Lakota: Policy, Culture and Land Use on the Pine Ridge Reservation Joseph Stromberg Senior Honors Thesis Environmental Studies and Anthropology Washington University in St. Louis 2 Abstract Land is invested with tremendous historical and cultural significance for the Oglala Lakota Nation of the Pine Ridge Indian Reservation. Widespread alienation from direct land use among tribal members also makes land a key element in exploring the roots of present-day problems—over two thirds of the reservation’s agricultural income goes to non-Natives, while the majority of households live below the poverty line. In order to understand how current patterns in land use are linked with federal policy and tribal culture, this study draws on three sources: (1) archival research on tribal history, especially in terms of territory loss, political transformation, ethnic division, economic coercion, and land use; (2) an account of contemporary problems on the reservation, with an analysis of current land policy and use pattern; and (3) primary qualitative ethnographic research conducted on the reservation with tribal members. Findings indicate that federal land policies act to effectively block direct land use. Tribal members have responded to policy in ways relative to the expression of cultural values, and the intent of policy has been undermined by a failure to fully understand the cultural context of the reservation. The discussion interprets land use through the themes of policy obstacles, forced incorporation into the world-system, and resistance via cultural sovereignty over land use decisions. Acknowledgements I would like to sincerely thank the Buder Center for American Indian Studies of the George Warren Brown School of Social Work as well as the Environmental Studies Program, for support in conducting research.
    [Show full text]
  • A Revised Taxonomy of the Iguanodont Dinosaur Genera and Species
    ARTICLE IN PRESS + MODEL Cretaceous Research xx (2007) 1e25 www.elsevier.com/locate/CretRes A revised taxonomy of the iguanodont dinosaur genera and species Gregory S. Paul 3109 North Calvert Station, Side Apartment, Baltimore, MD 21218-3807, USA Received 20 April 2006; accepted in revised form 27 April 2007 Abstract Criteria for designating dinosaur genera are inconsistent; some very similar species are highly split at the generic level, other anatomically disparate species are united at the same rank. Since the mid-1800s the classic genus Iguanodon has become a taxonomic grab-bag containing species spanning most of the Early Cretaceous of the northern hemisphere. Recently the genus was radically redesignated when the type was shifted from nondiagnostic English Valanginian teeth to a complete skull and skeleton of the heavily built, semi-quadrupedal I. bernissartensis from much younger Belgian sediments, even though the latter is very different in form from the gracile skeletal remains described by Mantell. Currently, iguanodont remains from Europe are usually assigned to either robust I. bernissartensis or gracile I. atherfieldensis, regardless of lo- cation or stage. A stratigraphic analysis is combined with a character census that shows the European iguanodonts are markedly more morpho- logically divergent than other dinosaur genera, and some appear phylogenetically more derived than others. Two new genera and a new species have been or are named for the gracile iguanodonts of the Wealden Supergroup; strongly bipedal Mantellisaurus atherfieldensis Paul (2006. Turning the old into the new: a separate genus for the gracile iguanodont from the Wealden of England. In: Carpenter, K. (Ed.), Horns and Beaks: Ceratopsian and Ornithopod Dinosaurs.
    [Show full text]
  • The Cretaceous-Tertiary Boundary Interval in Badlands National Park, South Dakota
    The Cretaceous-Tertiary Boundary Interval in Badlands National Park, South Dakota Philip W. Stoffer1 Paula Messina John A. Chamberlain, Jr. Dennis O. Terry, Jr. U.S. Geological Survey Open-File Report 01-56 2001 U.S. DEPARTMENT OF THE INTERIOR Gale A. Norton, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director The Cretaceous/Tertiary (K-T) boundary study interval at the Rainbow Colors Overlook along Badlands Loop Road, North Unit of Badlands National Park. This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey (USGS) editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1345 Middlefield Road, Menlo Park, CA 94025 http://geopubs.wr.usgs.gov/open-file/of01-056/ ABSTRACT A marine K-T boundary interval has been identified throughout the Badlands National Park region of South Dakota. Data from marine sediments suggest that deposits from two asteroid impacts (one close, one far away) may be preserved in the Badlands. These impact- generated deposits may represent late Maestrichtian events or possibly the terminal K-T event. Interpretation is supported by paleontological correlation, sequence stratigraphy, magnetostratigraphy, and strontium isotope geochronology. This research is founded on nearly a decade of NPS approved field work in Badlands National Park and a foundation of previously published data and interpretations. The K-T boundary occurs within
    [Show full text]