Blue River Valley Stratigraphic Chart
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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 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%. -
Pennsylvanian Minturn Formation, Colorado, U.S.A
Journal of Sedimentary Research, 2008, v. 78, 0–0 Research Articles DOI: 10.2110/jsr.2008.052 DEPOSITS FROM WAVE-INFLUENCED TURBIDITY CURRENTS: PENNSYLVANIAN MINTURN FORMATION, COLORADO, U.S.A. 1 2 2 3 2 M. P. LAMB, P. M. MYROW, C. LUKENS, K. HOUCK, AND J. STRAUSS 1Department of Earth & Planetary Science, University of California, Berkeley, California 94720, U.S.A. 2Department of Geology, Colorado College, Colorado Springs, Colorado 80903, U.S.A. 3Department of Geography and Environmental Sciences, University of Colorado, Denver, Colorado, 80217-3363 U.S.A. e-mail: [email protected] ABSTRACT: Turbidity currents generated nearshore have been suggested to be the source of some sandy marine event beds, but in most cases the evidence is circumstantial. Such flows must commonly travel through a field of oscillatory flow caused by wind-generated waves; little is known, however, about the interactions between waves and turbidity currents. We explore these interactions through detailed process-oriented sedimentological analysis of sandstone event beds from the Pennsylvanian Minturn Formation in north-central Colorado, U.S.A. The Minturn Formation exhibits a complex stratigraphic architecture of fan-delta deposits that developed in association with high topographic relief in a tectonically active setting. An , 20–35-m- thick, unconformity-bounded unit of prodelta deposits consists of dark green shale and turbidite-like sandstone beds with tool marks produced by abundant plant debris. Some of the sandstone event beds, most abundant at distal localities, contain reverse- to-normal grading and sequences of sedimentary structures that indicate deposition from waxing to waning flows. In contrast, proximal deposits, in some cases less than a kilometer away, contain abundant beds with evidence for deposition by wave- dominated combined flows, including large-scale hummocky cross-stratification (HCS). -
8.4.0 Wolford Mountain Site C 8.4.1 Location And
8.4.0 WOLFORD MOUNTAIN SITE C 8.4.1 LOCATION AND TOPOGRAPHY Wolford Mountain Site C is located on Muddy Creek, 5 miles north of Kremmling, Colorado and 3.8 miles upstream from Site A'. The dam site is a 250-foot wide canyon with sides that rise steeply to a height of approximately 80 feet. At that point, the left abutment is relatively flat for about 500 feet, continuing east to the base of Wolford Mountain. The right abutment slopes gently upwards towards Highway U.S. 40, located 0.7 miles west of the site. Figure 8.4.1 presents a plan view of the Wolford Mountain Site C. A 120-foot high dam at Site C would impound a reservoir of 60,000 af capacity with a water surface elevation of 7485 feet. This is 10 feet higher than the water surface elevation proposed for an alternative reservoir at Site A'. Approximately 1900 acres would be occupied by the reservoir and lake shore area. An area-capacity curve is presented on Figure 8.4.2. 8.4.2 PRIOR STUDIES Wolford Mountain Site C has been under investigation by the CRWCD. A report titled "Rock Creek Dam Project", prepared by Morrison-Knudsen Engineers, Inc. (1986) for the River District, considered three reservoir capacities for this Muddy Creek Site: 60,000, 46,800 and 30,400 af. The feasibility report illustrates a preliminary design for the selected 46,800 af size. Information from this report has been liberally incorporated into this section on Wolford Mountain Site C. The report titled "Seismotectonic Hazard Evaluation, Rock Creek Project Near Kremmling, Grand And Routt Counties, Colorado", was prepared by Michael West and Associates (1986) for Morrison-Knudsen Engineers as part of their study for the CRWCD. -
Vol. 7 National Family Farm Discovery Dox
Case: 19-70115, 08/13/2019, ID: 11396549, DktEntry: 36-7, Page 1 of 233 No. 19-70115 UNITED STATES COURT OF APPEALS FOR THE NINTH CIRCUIT NATIONAL FAMILY FARM COALITION, et al., Petitioners, v. UNITED STATES ENVIRONMENTAL PROTECTION AGENCY, et al., Respondents, and MONSANTO COMPANY, Intervenor-Respondent. ON PETITION FOR REVIEW FROM THE UNITED STATES ENVIRONMENTAL PROTECTION AGENCY PETITIONERS’ EXCERPTS OF RECORD VOLUME VII of IX ______________________ CENTER FOR FOOD SAFETY CENTER FOR BIOLOGICAL George A. Kimbrell DIVERSITY Sylvia Shih-Yau Wu Stephanie M. Parent Amy van Saun PO Box 11374 2009 NE Alberta St., Suite 207 Portland, OR 97211 Portland, OR 97211 T: (971) 717-6404 T: (971) 271-7372 [email protected] [email protected] [email protected] [email protected] Counsel for Petitioners Case: 19-70115, 08/13/2019, ID: 11396549, DktEntry: 36-7, Page 2 of 233 INDEX TO PETITIONERS’ EXCERPTS OF RECORD VOLUME I Admin. R. ER Date 1 Document Description Doc. No. Page No. 2 11/1/2018 M.8 Registration Decision for the ER 0001 Continuation of Uses of Dicamba on Dicamba Tolerant Cotton and Soybean 11/1/2018 M.9 Approval Master Label for EPA ER 0025 Registration No. 524-617, Primary Brand Name: M1768 Herbicide Alternate Brand Name: XtendiMax® With VaporGrip® Technology 11/5/2018 M.4 Notice of Conditional Registration ER 0065 and Approved Master Label for EPA Registration No. 524-617, Primary Brand Name: M1768 Herbicide Alternate Brand Name: XtendiMax® With VaporGrip® Technology 11/5/2018 M.3 Notice of Conditional Registration ER 00121 EPA Reg Number 352-913 DuPont FeXapan Herbicide Decision 545658 and Approved Label 11/1/2018 M.5 Notice of Conditional Registration ER 0167 EPA Registration Number 7969- 345 Engenia Herbicide Decision No. -
Geologic Map of the Southern Espanola Basin
GEOLOGIC MAP OF THE SOUTHERN ESPAÑOLA BASIN, SANA FE COUNTY, NEW MEXICO By Daniel J. Koning and Adam S. Read October, 2010 OPEN-FILE REPORT 531 DESCRIPTION OF MAP UNITS Descriptive terminology Below are descriptions of the units depicted on the geologic map. Grain sizes follow the Udden- Wentworth scale for clastic sediments (Udden, 1914; Wentworth, 1922) and are based on field estimates. Pebbles are subdivided as shown in Compton (1985). The term “clast(s)” refers to the grain size fraction greater than 2 mm in diameter and the term “matrix” refers to the particles less than 2 mm in size. Clast percentages are based on percent volume and were estimated in the field with the aid of percentage charts. Descriptions of bedding thickness follow Ingram (1954). Colors of unconsolidated sediment are based on visual comparison of dry samples to the Munsell Soil Color Charts (Munsell Color, 1994). Soil horizon designations and descriptive terms follow those of the Soil Survey Staff (1992). Birkeland (1999), and Birkeland et al. (1991). Stages of pedogenic calcium carbonate morphology follow those of Gile et al. (1966) and Birkeland (1999). Metric units are used in this report (see Table 1 for conversion of English units to metric units). The divisions of geologic time used in this report are provided below (Table 2). Table 1. Factors for conversion of metric units to English units _______________________________________________________ Multiply By To obtain _______________________________________________________ centimeters (cm) 0.3937 inches -
Carbon and Strontium Isotope Stratigraphy of the Permian from Nevada and China: Implications from an Icehouse to Greenhouse Transition
Carbon and strontium isotope stratigraphy of the Permian from Nevada and China: Implications from an icehouse to greenhouse transition Dissertation Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Kate E. Tierney, M.S. Graduate Program in the School of Earth Sciences The Ohio State University 2010 Dissertation Committee: Matthew R. Saltzman, Advisor William I. Ausich Loren Babcock Stig M. Bergström Ola Ahlqvist Copyright by Kate Elizabeth Tierney 2010 Abstract The Permian is one of the most important intervals of earth history to help us understand the way our climate system works. It is an analog to modern climate because during this interval climate transitioned from an icehouse state (when glaciers existed extending to middle latitudes), to a greenhouse state (when there were no glaciers). This climatic amelioration occurred under conditions very similar to those that exist in modern times, including atmospheric CO2 levels and the presence of plants thriving in the terrestrial system. This analog to the modern system allows us to investigate the mechanisms that cause global warming. Scientist have learned that the distribution of carbon between the oceans, atmosphere and lithosphere plays a large role in determining climate and changes in this distribution can be studied by chemical proxies preserved in the rock record. There are two main ways to change the distribution of carbon between these reservoirs. Organic carbon can be buried or silicate minerals in the terrestrial realm can be weathered. These two mechanisms account for the long term changes in carbon concentrations in the atmosphere, particularly important to climate. -
Late Cretaceous Stratigraphy of Black Mesa, Navajo and Hopi Indian Reservations, Arizona H
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/9 Late Cretaceous stratigraphy of Black Mesa, Navajo and Hopi Indian Reservations, Arizona H. G. Page and C. A. Repenning, 1958, pp. 115-122 in: Black Mesa Basin (Northeastern Arizona), Anderson, R. Y.; Harshbarger, J. W.; [eds.], New Mexico Geological Society 9th Annual Fall Field Conference Guidebook, 205 p. This is one of many related papers that were included in the 1958 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Stratigraphy of the State Bridge Formation in the Woody Creek Quadrangle, Pit Kin and Eagle Counties, Colorado
Stratigraphy of the State Bridge Formation in the Woody Creek Quadrangle, Pit kin and Eagle Counties, Colorado By VAL L. FREEMAN CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1324-F UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY W. A. Radlinski, Acting Director Library of Congress catalog-card No. 77-169280 U.S. GOVERNMENT PRINTING OFFICE WASHINGTON : 1971 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 20 cents Stock Number 2401-1126 CONTENTS Page Abstract._____________________ __________________________________ Fl Introduction. ________________-_____-______-_-_--------_-_-_-__--_- 1 Paleogeography _ _____________-____________--__-_--_-____--_-_- 3 Nomenclature-__ __________________________--_---_-_-____--__-- 4 Maroon Formation-_______________________________________________ 5 State Bridge Formation_____-_-____-__-_--_-------__----------__-_- 6 Sandstone of the Fryingpan River.______________________________ 8 Sloane Peak Member_______________---__-_-__-_--------_--_-_- 9 Coarse unit of Toner Creek______________________----____- ___. 10 Comparison with its occurrence in other areas___________________ 10 Chinle Formation______________________________________________ 11 Selected stratigraphic sections_____________________________________ 11 1. Fryingpan River___________________-__--_-_-----___-___--_ 12 2. Box Canyon___-_______________________________ 13 3. Bionaz Gulch_____________________________________________ 14 4. Toner -
Fossil Fish Fauna from the Uppermost Graneros Shale (Upper Cretaceous) in Southeastern Nebraska
DePaul Discoveries Volume 1 Issue 1 Article 7 2012 Fossil Fish Fauna from the Uppermost Graneros Shale (Upper Cretaceous) in Southeastern Nebraska Kevin R. Jansen DePaul University, [email protected] Follow this and additional works at: https://via.library.depaul.edu/depaul-disc Part of the Life Sciences Commons, and the Physical Sciences and Mathematics Commons Recommended Citation Jansen, Kevin R. (2012) "Fossil Fish Fauna from the Uppermost Graneros Shale (Upper Cretaceous) in Southeastern Nebraska," DePaul Discoveries: Vol. 1 : Iss. 1 , Article 7. Available at: https://via.library.depaul.edu/depaul-disc/vol1/iss1/7 This Article is brought to you for free and open access by the College of Science and Health at Via Sapientiae. It has been accepted for inclusion in DePaul Discoveries by an authorized editor of Via Sapientiae. For more information, please contact [email protected]. Fossil Fish Fauna from the Uppermost Graneros Shale (Upper Cretaceous) in Southeastern Nebraska Acknowledgements Faculty Advisor: Dr. Kenshu Shimada, Department of Environmental Science and Studies & Department of Biological Sciences This article is available in DePaul Discoveries: https://via.library.depaul.edu/depaul-disc/vol1/iss1/7 Jansen: Fossil Fish Fauna from the Uppermost Graneros Shale (Upper Cretaceous) in Southeastern Nebraska DEPAUL DISCOVERIES (2O12) Fossil Fish Fauna from the Uppermost Graneros Shale (Upper Cretaceous) in Southeastern Nebraska Kevin R. Jansen* Department of Environmental Science and Studies ABSTRACT The Graneros Shale is a rock deposited in the Late Cretaceous Western Interior Seaway of North America about 95 million years ago. Many fossil fish remains were collected from the uppermost portion of the Graneros Shale in southeastern Nebraska and were analyzed for their unique characteristics. -
U.S. Geological Survey Bulletin 1787-A-C
Sedimentology and Paleogeographic Significance of Six Fluvial Sandstone Bodies in the Maroon Formation, Eagle Basin, Northwest Colorado Sedimentology of an Eolian Sandstone from the Middle Pennsylvanian Eagle Valley Evaporite, Eagle Basin, Northwest Colorado Burial Reconstruction of the Early and Middle Pennsylvanian Belden Formation, Oilman Area, Eagle Basin, Northwest Colorado U.S. GEOLOGICAL SURVEY BULLETIN 1787-A-C Sedimentology and Paleogeographic Significance of Six Fluvial Sandstone Bodies in the Maroon Formation, Eagle Basin, Northwest Colorado By SAMUEL Y. JOHNSON Sedimentology of an Eolian Sandstone from the Middle Pennsylvanian Eagle Valley Evaporite, Eagle Basin, Northwest Colorado By CHRISTOPHER J. SCHENK Burial Reconstruction of the Early and Middle Pennsylvanian Belden Formation, Oilman Area, Eagle Basin, Northwest Colorado By VITO F. NUCCIO and CHRISTOPHER J. SCHENK U.S. GEOLOGICAL SURVEY BULLETIN 1787 EVOLUTION OF SEDIMENTARY BASINS-UINTA AND PICEANCE BASINS DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1987 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Johnson, Samuel Y. Evolution of sedimentary basins Uinta and Piceance basins. (U.S. Geological Survey bulletin ; 1787 A-C) Includes bibliographies. Contents: Sedimentology and paleogeographic significance of six fluvial sandstone bodies in the Maroon Formation, Eagle basin, northwest Colorado / by Samuel Y. Johnson Sedimentology of an eolian sandstone from the Middle Pennsylvanian Eagle Valley Evaporite, Eagle basin, northwest Colorado / by Christopher J. Schenk Burial reconstruction of the Early and Middle Pennsylvanian Belden Formation, Gilman area, Eagle basin, northwest Colorado / by Vito F. -
Inside: GSA Bookstore Update, a Special Insert, P
VOL. 14, NO. 6 A PUBLICATION OF THE GEOLOGICAL SOCIETY OF AMERICA JUNE 2004 Title Sponsor of the 2004 GSA Annual Meeting. Inside: GSA Bookstore Update, A Special Insert, p. 33 Limnogeology Division Award, p. 59 GeoMart Geoscience Directory, p. 62 VOLUME 14, NUMBER 6 JUNE 2004 GSA TODAY publishes news and information for more than 18,000 GSA members and subscribing libraries. GSA Today Cover Images: Upper left: “The Big Blue lead science articles should present the results of exciting new research or summarize and synthesize important problems or Marble,” courtesy of NASA. Lower left: Larson issues, and they must be understandable to all in the earth B Ice Shelf collapse. Image courtesy of NASA/ science community. Submit manuscripts to science editors GSFC/LaRC/JPL, MISR Team. View of the Keith A. Howard, [email protected], or Gerald M. Ross, Soyuz TMA-2 spacecraft docked to the cargo [email protected]. block on the International Space Station. GSA TODAY (ISSN 1052-5173 USPS 0456-530) is published 11 Image courtesy of the crew of ISS Expedition times per year, monthly, with a combined April/May issue, by The Geological Society of America, Inc., with offices at 3300 Penrose 7, NASA. Place, Boulder, Colorado. Mailing address: P.O. Box 9140, Boulder, CO 80301-9140, U.S.A. Periodicals postage paid at Boulder, Colorado, and at additional mailing offices. Postmaster: Send address changes to GSA Today, GSA Sales and Service, P.O. Box 9140, Boulder, CO 80301-9140. Copyright © 2004, The Geological Society of America, Inc. (GSA). Geoscience in a Changing World: Denver 2004 All rights reserved.