DOCSLIB.ORG

Geology and Niineral Resources Freltiont County, Wyo

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

Bulletin 2 Series B Geology and NIineral Resources of a Portion of FrelTIOnt County, Wyo. c. E .•JAMISON I' State Geologist CHEYENNE, W"\"O. THE S. A. BRISTOL CO., PRINTERS AND BINDERS 19II J '. 'WYOMING STATE GEOLOGIST. BULLETIN 2, BERIES B. PLATE I BIG PoPO AGIE RIVER NEAR HEAD OF POPO AGIE CANYON. , . ~ ... ... -, ." CONTENTS PAGE Introduction ...................... 5 Acknowledgments ~. 6 History.. .. ..... .... 6 Bibliography ................................................... .12 Topography .. ......... .. 16 Drainage ......... .. 16 Climate.. .. 18 Plants and animals. .21 I rrigation and crops .. 22 Grazing.. .23 Resources ".......... ......... .23 Towns and villages. ........... 23 Geology .. 26 pre-Cambrian rocks 29 Cambrian System.. .29 Deadwood formation .. ........... .29 Ordovician System .. .................................. .30 Bighorn limestone. .30 Carboniferous System ......... .30 Madison limestone ...................... .30 AmBden formation ................ .. 31 . Tensleep sandstone. .......... .. 31 Embar formation .32 • Triassic System. 34 Chugwater formation .. .. 34 Jurassic System. .......... .. 37 Sundance formation. ................................... .. .37 Morrison formation ........ .39 Cretaceous System .. .............. .39 Lower Cretaceous rocks 39 Dakota sandstone. 39 Mancos group, ... .41 Fort Benton shales '. .42 Greenhorn limestone ...42 Niobrara formation, . .. 42 Fort Pierre shales.. .42 Mesaverde formation.. ................................. .. .44 Tertiary System ......... 45 Structural Geology ". 45 Wind River Mountains .45 Sage Creek district .46 Plunkett field .47 Dallas field .47 Lander valley 48 Geologic History. .48 Pre-Cambrian time ,.... .49 .. Cambrian sea 49 Ordovician sea .......... .. 49 Carboniferous sea.. .50 Triassic sea 50 • Jurassic sea .............. 50 Cretaceous conditions 51 Tertiary conditions... .52 -4- PAGE Mineral Resources .. ................... ..... 52 ~l ......~ History of development 53 Dallas field .. ....................... 53 Sage Creek field 56· Plunkett field .......... .. 59' Geologic relations. .61 Quality. ... .. .. ........ ... ....... ..... ..63 Yield ... 68- Pipe lines . ................ .. 69 Storage. ........................ 69 Practical suggestions ....................... 70, Origin. ............................................ 71 Organic theory _. 71 Inorganic theory. _. __ 72 Accumulation .. _. __ . _. _. _.. _. _. _73 Movement in porous rocks .......... _.-73 Places of accumulation ..... _. __ .. 75' Gold . _. _. _. _75 Coal ._....................... _ __ 81 Copper _. _.... __ .. _. ._.81 Iron Ore ___ ... ..82 Gilsonite _ __ .. 82 Building stones . _83 Gypsum _. __ _. _ . _. _. 84 Asbestos ___.. __ ... _ _.................. .._85 Clay .. .85 I Washakie Hot Spring _ _85 Surface waters. _ _._._ _ ._._.__86 '" Underground waters. _. _ 89- ILLUSTRATIONS. PLATE I. Big Popo Agie River above the "Sinks" Frontispiece PLATE II. Map showing area discussed. _. Facing page 6 PLATE III. Oil well in the Plunkett field. Washakie oil spring in the right middle ground Facing page 22 PLATE IV. The "Sinks"; Madison limestone. _ Facing page 30 PLATE V. Tensleep sandstone in Big Popo Agie canyon _ Facing page 32 PLATE VI. A-A canyon wall formed by Tensleep sandstone B-Juniper Butte, showing trough of the sec- ondary syncline in the Sage Creek Oil field .. Facing page 46· PLATE VII. Massive gypsum near the top of the Chugwater formation on Little Wind River .. __ . _. _ Facing page 50 PLATE VIII. Hogbapk of Dakota sandstone Facing page 52 PLATE IX. Diagram illustrating faulting in Sage Creek field Facing page 58 PLATE X. Oil wells in the: Plunkett field _ Facing page 60 PLATE XI. The Shoshone anticline in the Sage Creek field Facing page 66· PLATE XII. Crest of the Shoshone anticline, Plunkett field Facing page 74 PLATE XIII. General view of a portion of the South Pass dis- trict . .. Facing page 78- PLATE XIV. A-Old la-stamp mill driven by overshot water wheel. B-A part of the Big Popo Agie Falls .. Facing page 85 PLATE XV. Geologic map of a portion of Fremont County, Wyoming. ... In pocket (Geology and Mineral Resources of a Portion of Frenlont County, Wyoming By C. E. JAMISON INTRODUCTION. This report, based upon field work carried on during ,.. the summer of 1911, discusses an area of about 500 square miles, situated in the south central portion of· Fremont County, Wyoming, and extending from the vicinity of I • South Pass City, some 35 miles south of Lander, to Sage Creek, about 6 miles north of the Wind River Indian Agency. (Plate 2.) A portion of the oil fields embraced in this. area lies in the Wind River Indian Reservation, where work can be carried on only under lease from the Indian Council, subject to the rules and regulations of the Department of the Interior. The immediate cause for taking up the work in this .section was the large and increasing demand for infor­ mation in regard to the several oil fields tributary to Lander, and especial attention was given to the Sage Creek and Plunkett fields. Field work was commenced June 10, 1911, with L. 1VI. Trask as field assistant and Oscar Woolery • as teamster, and was closed at Lander July 2l. The oil bearing area is divided naturally into three fields, known as the Dallas field (Popo Agie field of Knight*; * Knight, W. C., The Petroleum of the Shoshone Anticlinal; School of Mines., Univ. of Wyoming, Petroleum series-Bulletin No.2,. Laramie, Wyo., 1897. -6-' Little Popo Agie district of Woodruff*), the Plunkett field (Lander field of Knight; Big Popo Agie district of Woodruff), and the Sage. Creek field (Shoshone field of Knight; Little Wind River district of Woodruff). The names Dallas, Plunkett and Sage Creek are here used because it is by these names the various oil fields are best known to the residents of the Lander district. On account of the small amount of time that could be devoted' to the entire district, no detailed study of the geology of the mining camps was made. As a large pro­ portion of the mines are idle and filled with water, the descriptions of most of them are based on information supplied by residents of the district. ACKNOWLEDGMENTS. I . The writer is indebted to Mr. Chas. Swanson of Lander, <> to Mr. Jas. MacFarlane of South Pass City, and to Capt. O. M. Beck of Atlantic City, for information and assistance in the South Pass mining district; to Mr. J. H. Sharp and Mr. Geo. D. Case of Lander, and. to all of the oil operators for information in regard to the Lander district; to Mr. E. E. Jones, Assistant Engineer U. S. 1. S., for maps of the Wind River Indian Reservation; to Mr. E. W. Hains­ worth of Lander for maps of Fremont County; to Col. E. H. Power of Lander for' maps of the Dallas oil field; and to a lesser degree to nearly all of the residents of the Lander valley. J HISTORY. The first recorded visit of white men to this region a was in 1744, Sieur de la Verendrye having equipped and * Woodruff, E. G., The Lander Oil Field; U. S. Geo!. Survey Bulletin No. 452, 1911. WYOMING STATEJGEOLOGIST. BULLETIN 2, SERIES B. PLATE II rr~-I /'""" ./ I I -_..J "-! i '~ \ ll.I .J \ I o \ I I 4: Iw o I r-«-' ­ I \ ~ ~ (;--1I \ o Green Riv6r ).. 1 o Roc\:Springs -y 'J 0 E:vein'Oton oLarami6 __ ----=-:EYENNE I ~ -- o 0 MAP OF WYOMING, ,'HOWING AREA DISCUSSED. , • o -7- sent out an expedition from Canada for the purpose of trading with the Indians. This expedition reached the Wind River valley early in the year 1744, where they met the Shoshone Indians, who advised them that a band of the war-like Sioux were encamped at a pass in the moun­ tains-----:-probably South Pass. After exploring several of the canyons on the east flank of the Wind River Mountains the expedition returned to Canada, and no further e~plora­ tions were carried on from th.at quarter. The earliest extended knowledge of this region was probably that obtained by Gen. Wm. Ashley, Robt~ Camp­ bell, Wm. Sublette, Jim Bridger and others, who trapped I on all of the streams tributary to Big Wind River as early as 18!Z2, but the first authentic information given to the public was that which resulted from the explorations of .. Capt. Bonneville in 1833. Capt. Bonneville's first trip to this section, his visit to the "Tar Springs" in the Dallas oil field, and his discovery of the Washakie Hot Spring are described by Washington Irving* in the following language: "On the 25th of July, 1833, Capt. Bonneville struck his tents and set out on his route for the Big Horn, at the head of a party of fifty-six men. He proceeded along the south point of the Wind River Mountains, and t~rning to the north-east, soon came upon the waters of the Popo Agi'e. This stream takes its rise in the Wind River Moun­ tains. Its name, like most Indian names, is characteristic. Popo, in the Crow language, signifying head; Agie, river. It is the head of a long river, extending from the south end of the Wind River Mountains in a north-east direction, until it falls into the Yellowstone. Its course is generally through plains, but twice it is crossed by chains of moun­ tains; the first the Little Horn, the second the Big Horn. * The Rocky Mountains, or Scenes, Incidents and Adventures in the Far West. Philadelphia, 1837. -8- After it has forced its way through the first chain, it is called the Horn River; after the second chain, it is called the Big Hom River. Its passage through this 'last chain is rough and violent; making repeated falls, and rushing down long and furious rapids which threaten destruction to the navigator; though a hardy trapper is said to have shot down them in a canoe. "Proceeding dovvn the Popo Agie, Capt. Bonneville came again in full view of the 'Bluffs', as they are called, extending from the base of the 'Vind River Mountains far away to the east, and presenting to the eye a confusion of hills ·and cliffs of red sandstone, some peaked and angular, some round.
Recommended publications
  • Post-Carboniferous Stratigraphy, Northeastern Alaska by R

    Post-Carboniferous Stratigraphy, Northeastern Alaska by R

    Post-Carboniferous Stratigraphy, Northeastern Alaska By R. L. DETTERMAN, H. N. REISER, W. P. BROSGE,and]. T. DUTRO,JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 886 Sedirnentary rocks of Permian to Quaternary age are named, described, and correlated with standard stratigraphic sequences UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Detterman, Robert L. Post-Carboniferous stratigraphy, northeastern Alaska. (Geological Survey Professional Paper 886) Bibliography: p. 45-46. Supt. of Docs. No.: I 19.16:886 1. Geology-Alaska. I. Detterman, Robert L. II. Series: United States. Geological Survey. Professional Paper 886. QE84.N74P67 551.7'6'09798 74-28084 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02687-2 CONTENTS Page Page Abstract __ _ _ _ _ __ __ _ _ _ _ _ _ _ _ _ _ _ _ __ __ _ _ _ _ _ _ __ __ _ _ __ __ __ _ _ _ _ __ 1 Stratigraphy__:_Continued Introduction __________ ----------____ ----------------____ __ 1 Kingak Shale ---------------------------------------- 18 Purpose and scope ----------------------~------------- 1 Ignek Formation (abandoned) -------------------------- 20 Geographic setting ------------------------------------ 1 Okpikruak Formation (geographically restricted) ________ 21 Previous work and acknowledgments ------------------ 1 Kongakut Formation ----------------------------------
  • Understanding and Mapping Variability of the Niobrara Formation

    Understanding and Mapping Variability of the Niobrara Formation

    UNDERSTANDING AND MAPPING VARIABILITY OF THE NIOBRARA FORMATION ACROSS WATTENBERG FIELD, DENVER BASIN by Nicholas Matthies A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Master of Science (Geology). Golden, Colorado Date________________ Signed:____________________________________ Nicholas Matthies Signed:____________________________________ Dr. Stephen A. Sonnenberg Thesis Advisor Golden, Colorado Date:_______________ Signed:____________________________________ Dr. Paul Santi Professor and Head Department of Geology and Geological Engineering ii ABSTRACT Wattenberg Field has been a prolific producer of oil and gas since the 1970s, and a resurgence of activity in recent years in the Niobrara Formation has created the need for a detailed study of this area. This study focuses on mapping regional trends in stratigraphy, structure, and well log properties using digital well logs, 3D seismic data, and core X-ray diffraction data. Across Wattenberg, the Niobrara is divided into the Smoky Hill Member (made up of A Chalk, A Marl, B Chalk, B Marl, C Chalk, C Marl, and Basal Chalk/Marl) and the Fort Hays Limestone Member. Directly beneath the Niobrara, the Codell Sandstone is the uppermost part of the Carlile Formation. Stratigraphic trends in these units are primarily due to differential compaction and compensational sedimentation. The largest structural trend is a paleo-high that runs east-west to northeast-southwest across the middle of the field. It has a relief of about 100 ft, and is 20 mi wide. The A Chalk and A Marl show evidence of submarine erosion over this area. Faults mapped from 3D seismic data are consistent with previously published data on a proposed polygonal fault system in the Denver Basin.
  • Hydrogeology and Stratigraphy of the Dakota Formation in Northwest Iowa

    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.
  • 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

    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%.

  • 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
  • Stratigraphy of the Upper Cretaceous Fox Hills Sandstone and Adjacent

    Stratigraphy of the Upper Cretaceous Fox Hills Sandstone and Adjacent

    Stratigraphy of the Upper Cretaceous Fox Hills Sandstone and AdJa(-erit Parts of the Lewis Sliale and Lance Formation, East Flank of the Rock Springs Uplift, Southwest lo U.S. OEOLOGI AL SURVEY PROFESSIONAL PAPER 1532 Stratigraphy of the Upper Cretaceous Fox Hills Sandstone and Adjacent Parts of the Lewis Shale and Lance Formation, East Flank of the Rock Springs Uplift, Southwest Wyoming By HENRYW. ROEHLER U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1532 Description of three of/lapping barrier shorelines along the western margins of the interior seaway of North America UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1993 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Library of Congress Cataloging-in-Publication Data Roehler, Henry W. Stratigraphy of the Upper Cretaceous Fox Hills sandstone and adjacent parts of the Lewis shale and Lance formation, east flank of the Rock Springs Uplift, southwest Wyoming / by Henry W. Roehler. p. cm. (U.S. Geological Survey professional paper ; 1532) Includes bibliographical references. Supt.ofDocs.no.: I19.16:P1532 1. Geology, Stratigraphic Cretaceous. 2. Geology Wyoming. 3. Fox Hills Formation. I. Geological Survey (U.S.). II. Title. III. Series. QE688.R64 1993 551.7T09787 dc20 92-36645 CIP For sale by USGS Map Distribution Box 25286, Building 810 Denver Federal Center Denver, CO 80225 CONTENTS Page Page Abstract......................................................................................... 1 Stratigraphy Continued Introduction................................................................................... 1 Formations exposed on the east flank of the Rock Springs Description and accessibility of the study area ................
  • Niobrara Total Petroleum System in the Southwestern Wyoming Province

    Niobrara Total Petroleum System in the Southwestern Wyoming Province

    Chapter 6 Niobrara Total Petroleum System in the Southwestern Wyoming Province By Thomas M. Finn and Ronald C. Johnson Volume Title Page Chapter 6 of Petroleum Systems and Geologic Assessment of Oil and Gas in the Southwestern Wyoming Province, Wyoming, Colorado, and Utah By USGS Southwestern Wyoming Province Assessment Team U.S. Geological Survey Digital Data Series DDS–69–D U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director U.S. Geological Survey, Denver, Colorado: Version 1, 2005 For sale by U.S. Geological Survey, Information Services Box 25286, Denver Federal Center Denver, CO 80225 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Manuscript approved for publication May 10, 2005 ISBN= 0-607-99027-9 Contents Abstract ……………………………………………………………………………………… 1 Introduction …………………………………………………………………………………… 1 Acknowledgments ……………………………………………………………………………
  • This Is a Digital Document from the Collections of the Wyoming Water Resources Data System (WRDS) Library

    This Is a Digital Document from the Collections of the Wyoming Water Resources Data System (WRDS) Library

    This is a digital document from the collections of the Wyoming Water Resources Data System (WRDS) Library. For additional information about this document and the document conversion process, please contact WRDS at [email protected] and include the phrase “Digital Documents” in your subject heading. To view other documents please visit the WRDS Library online at: http://library.wrds.uwyo.edu Mailing Address: Water Resources Data System University of Wyoming, Dept 3943 1000 E University Avenue Laramie, WY 82071 Physical Address: Wyoming Hall, Room 249 University of Wyoming Laramie, WY 82071 Phone: (307) 766-6651 Fax: (307) 766-3785 Funding for WRDS and the creation of this electronic document was provided by the Wyoming Water Development Commission (http://wwdc.state.wy.us) VOLUME 11-A OCCURRENCE AND CHARACTERISTICS OF GROUND WATER IN THE BIGHORN BASIN, WYOMING Robert Libra, Dale Doremus , Craig Goodwin Project Manager Craig Eisen Water Resources Research Institute University of Wyoming Report to U.S. Environmental Protection Agency Contract Number G 008269-791 Project Officer Paul Osborne June, 1981 INTRODUCTION This report is the second of a series of hydrogeologic basin reports that define the occurrence and chemical quality of ground water within Wyoming. Information presented in this report has been obtained from several sources including available U.S. Geological Survey publications, the Wyoming State Engineer's Office, the Wyoming Geological Survey, and the Wyoming Oil and Gas Conservation Commission. The purpose of this report is to provide background information for implementation of the Underground Injection Control Program (UIC). The UIC program, authorized by the Safe Drinking Water Act (P.L.
  • COSSMANNIANA Bulletin Du Groupe D'étude Et De Recherche Macrofaune Cénozoïque

    COSSMANNIANA Bulletin Du Groupe D'étude Et De Recherche Macrofaune Cénozoïque

    COSSMANNIANA Bulletin du Groupe d'Étude et de Recherche Macrofaune Cénozoïque Tome 3, numéro 4 Décembre 1995 ISSN 1157-4402 GROUPE D'ÉTUDE ET DE RECHERCHE MACROFAUNE CÉNOZOïQUE "Maisonpour tous" 26, rue Gérard Philippe 94120 FONTENAY-SOUS-SOIS Président . .. ... Jacques PONS Secrétaire .. PierreLOZOUET Trésorier . .. .. Philippe MAESTRATI Dessins de couverture : Jacques LERENARD Maquette et Édition: Jacques LERENARD [eau-Michel PACAUD Couverture: Campanile (Campanilopa) giganteum, d'après la figure 137-45 de l'tconographie (grossissement 3/8); et individu bréphiqu e (hauteur totale : 2 mm), muni de son périostracum et de sa protoconque (coll. LeRenard) . COSSMANNIANA, Paris, 3 (4), Décembre 1995, pp. 133-150, sans fig. ISSN: 1157-4402 . RÉVISION DES MOLLUSQUES PALÉOGÈNES DU BASSIN DE PARIS III - CHRONOLOGIE DES CRÉATEURS DE RÉFÉRENCES PRIMAIRES par Jacques ·LERENARD Laboratoire de Biologiedes Invertébrés Marins et Malacologie, Muséum.National d'Histoire Naturelle, 55,rue de Buffon- 75005 Paris - FRANCE RÉSUMÉ - La liste des 437 publications dans lesquelles ont été introduites des références primaires figurant dans la partie II (LERENARD & PACAUD, 1995, pp. 65-132) est donnée. Il s'agit de la première liste de l'ensemble des publications concernant des nouveaux noms ou des nouvelles espèces paléogènes de Mollusques du bassin de Paris. TITLE - Revision of the Paris Basin Paleogene MoIlusca. III: Chronological Iist of the authors of primary references. ABSTRACT - The 437 publications, in which the primary references cited in part II (LERENARD & PACAUD, 1995, pp. 65-132) have been introduced, are given. This constitutes the first list of aIl the publications that are conceming new species or new names of Paris Basin Paleogene Molluscan species.
  • Schmitz, M. D. 2000. Appendix 2: Radioisotopic Ages Used In

    Schmitz, M. D. 2000. Appendix 2: Radioisotopic Ages Used In

    Appendix 2 Radioisotopic ages used in GTS2020 M.D. SCHMITZ 1285 1286 Appendix 2 GTS GTS Sample Locality Lat-Long Lithostratigraphy Age 6 2s 6 2s Age Type 2020 2012 (Ma) analytical total ID ID Period Epoch Age Quaternary À not compiled Neogene À not compiled Pliocene Miocene Paleogene Oligocene Chattian Pg36 biotite-rich layer; PAC- Pieve d’Accinelli section, 43 35040.41vN, Scaglia Cinerea Fm, 42.3 m above base of 26.57 0.02 0.04 206Pb/238U B2 northeastern Apennines, Italy 12 29034.16vE section Rupelian Pg35 Pg20 biotite-rich layer; MCA- Monte Cagnero section (Chattian 43 38047.81vN, Scaglia Cinerea Fm, 145.8 m above base 31.41 0.03 0.04 206Pb/238U 145.8, equivalent to GSSP), northeastern Apennines, Italy 12 28003.83vE of section MCA/84-3 Pg34 biotite-rich layer; MCA- Monte Cagnero section (Chattian 43 38047.81vN, Scaglia Cinerea Fm, 142.8 m above base 31.72 0.02 0.04 206Pb/238U 142.8 GSSP), northeastern Apennines, Italy 12 28003.83vE of section Eocene Priabonian Pg33 Pg19 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 14.7 m above base of 34.50 0.04 0.05 206Pb/238U 14.7, equivalent to Ancona, northeastern Apennines, 13.6011 E section MAS/86-14.7 Italy Pg32 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 12.9 m above base of 34.68 0.04 0.06 206Pb/238U 12.9 Ancona, northeastern Apennines, 13.6011 E section Italy Pg31 Pg18 biotite-rich layer; MASS- Massignano (Oligocene GSSP), near 43.5328 N, Scaglia Cinerea Fm, 12.7 m above base of 34.72 0.02 0.04 206Pb/238U
  • Appendix 1 – Environmental Predictor Data

    Appendix 1 – Environmental Predictor Data

    APPENDIX 1 – ENVIRONMENTAL PREDICTOR DATA CONTENTS Overview ..................................................................................................................................................................................... 2 Climate ......................................................................................................................................................................................... 2 Hydrology ................................................................................................................................................................................... 3 Land Use and Land Cover ..................................................................................................................................................... 3 Soils and Substrate .................................................................................................................................................................. 5 Topography .............................................................................................................................................................................. 10 References ................................................................................................................................................................................ 12 1 OVERVIEW A set of 94 potential predictor layers compiled to use in distribution modeling for the target taxa. Many of these layers derive from previous modeling work by WYNDD1, 2, but a
  • Moneta Divide Map 6 Geologic

    Moneta Divide Map 6 Geologic

    Geologic Units Mesozoic - Paleozoic Cenozoic/Quaternary MzPz: Mesozoic and II Qa: Alluvium and D Paleozoic rocks Colluvium L___J Paleozoic/Permian Qt: Gravel, Pediment, II Pp: Phosphoria and Sand Deposits Formation and related - L___J rocks II Qs: Dune Sand and L___J Loess Paleozoic/Carboniferous Cenozoic/Tertiary PM : Tensleep Sandstone D and Amsden Formation Tim: Indian Meadows Formation P*M: Casper Formation and Madison Limestone -D Tm: Miocene rocks (N ,S) MD: Madison Tml: Lower Miocene Limestone rocks Mm : Madison Twr: White River - Limestone or Group Formation D -D (N) , or Madison ·- .... ---..:::-.::--------.... Limestone (S) ......... -- Twb : Wagon Bed --. - Formation --- --- Paleozoic/Cambrian Twdr: Wind River _r: Gallatin Limestone, Formation Gros Ventre Formation D and equivalents, and Tfu : Fort Union Formation Flathead Sandstone (N), or Cambrian rocks (S) Cenozoic - Mesozoic Pzr: Madison Limestone, Darby Formation , Bighorn TKu : Sedimentary Dolomite, Gallatin Rocks - Limestone, Gros Ventre Formation and Flathead Mesozoic/Cretaceous .. O_: Bighorn Dolomite, Kim: Lance Formation, D Gallatin Limestone, and D Fox Hills Sandstone, Gros Ventre Formation (TB) Meeteetse Formation Archaen Kml: Meeteetse .. Ugn: Oldest Twdr Formation and Lewis D Gneiss complex Shale Kmv: Mesaverde WVsv: Formation Metasedimentary and metavolcanic rocks Kc: Cody Shale - Wg : Granitic Rocks N ------ Fault Line ~ Mesozoic/Jurassic w KJ :Cloverly and Morrison Cl Project Features D Formations (N , S) . Jsg: Sundance and Production Area . Gypsum Spring D Formations Disposal Areas Mesozoic/Triassic D "cd: Chugwater and Treated Water Discharge D Dinwoody Formations ~ Pipeline Corridors Source: Geologic Units, USGS 1994 Product Pipeline (Upda ted 2013); USGS 2005 Corridor Disposal Area Water Pipeline Corridor Map6 Geologic Map Moneta Divide Natural Gas and Oil Development Project Draft Environmental Impact Statement April 2019 No warranty is made by the Bureau of Land Management for use ofthe data for purposes not intended by the BLM .