The Yampa Bed—A Regionally Extensive Tonstein in the Williams

Total Page:16

File Type:pdf, Size:1020Kb

The Yampa Bed—A Regionally Extensive Tonstein in the Williams The Yampa Bed—A Regionally Extensive Tonstein in the Williams Fork Formation, Northwestern Piceance Creek and Southern Sand Wash Basins, Colorado Contributions to Stratigraphy Scientific Investigations Report 2008–5033 U.S. Department of the Interior U.S. Geological Survey Cover. Excavated exposure of the Yampa Bed at the type locality, south of Craig, Colo. Yampa Bed is about 38 in. thick. Note 24-in. shovel for scale. The Yampa Bed—A Regionally Extensive Tonstein in the Williams Fork Formation, Northwestern Piceance Creek and Southern Sand Wash Basins, Colorado By Michael E. Brownfield and Edward A. Johnson Contributions to Stratigraphy Scientific Investigations Report 2008–5033 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2008 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 Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Suggested citation: Brownfield, M.E., and Johnson, E.A., 2008, The Yampa Bed—A regionally extensive tonstein in the Williams Fork Formation, northwestern Piceance Creek and southern Sand Wash Basins: U.S. Geological Survey Scientific Investigations Report 2008–5033, 32 p. iii Contents Abstract ...........................................................................................................................................................1 Introduction.....................................................................................................................................................1 Geologic Setting .............................................................................................................................................4 Cretaceous Paleogeography ..............................................................................................................4 Stratigraphy of Upper Cretaceous Rocks in Northwestern Colorado .........................................7 Mesaverde Group in the Yampa Coal Field ......................................................................................7 Detailed Stratigraphy of Coal-Bearing Upper Cretaceous Rocks .........................................................7 Iles Formation ........................................................................................................................................7 Tow Creek Sandstone Member ...............................................................................................12 Double-Ledge Sandstone .........................................................................................................12 Trout Creek Sandstone Member .............................................................................................12 Williams Fork Formation ....................................................................................................................12 Sub-Twentymile Sandstone ............................................................................................12 Twentymile Sandstone Member .....................................................................................13 Big White Sandstone .......................................................................................................13 Three White Sandstones .................................................................................................13 Depositional Setting of the Mesaverde Group .......................................................................................13 Origin, Description, and Distribution of the Yampa Bed ........................................................................14 Yampa Coal Field .................................................................................................................................17 Eckman Park Measured Section .............................................................................................17 Fish Creek Canyon Measured Section ...................................................................................18 Ute Gulch Measured Section ..................................................................................................19 Eagle Mine Measured Section ................................................................................................19 Lay, Colo., Measured Section ..................................................................................................19 Danforth Hills Coal Field.....................................................................................................................19 Piceance and Sand Wash Basins ........................................................................................................... 19 Geophysical Log Response ........................................................................................................................23 Yampa Bed as a Correlation Tool ..............................................................................................................26 Summary........................................................................................................................................................30 Acknowledgments .......................................................................................................................................30 References Cited..........................................................................................................................................30 Plates 1. Subsurface Correlations of Coal and Related Rocks of the Upper Cretaceous Iles and Williams Fork Formations in the Yampa Coal Field, Northeastern Colorado A. Coal correlations of the middle coal group along cross section A-A’ B. Coal correlations of the middle coal group along cross section B-B’ C. Lithologic interpretation of drill hole H–36–H iv 2. Subsurface Correlations of Coal and Related Rocks of the Iles and Williams Fork Formations in the Danforth Hills Coal Field, Northwestern Colorado A. Location map showing public drill holes and line of section A-A’ in the Danforth Hills coal field B. Subsurface correlations of coal and related rocks in the Iles and Williams ForkFormations in the Danforth Hills coal field Figures 1. Geologic map and major Upper Cretaceous coal fields of northwestern Colorado .........2 2. Index map of Yampa coal field....................................................................................................3 3. Photograph of baked strata (clinker) above Trout Creek Sandstone Member of the Iles Formation ................................................................................................................................4 4. Stratigraphic column of Upper Cretaceous and Tertiary rocks, Yampa coal field ............5 5. Paleogeographic map of central part of North America during the late Campanian .......6 6. Geologic map of Yampa coal field..............................................................................................8 7. Cross section of Mesaverde Group in the Yampa coal field .................................................9 8. Cross section of Upper Cretaceous and Tertiary rocks in the Lower White River, Danforth Hills, and Yampa coal fields ......................................................................................10 9. Stratigraphic section of Eckman Park area ...........................................................................11 10–15. Photographs showing Yampa Bed 10. Excavated outcrop at type location .........................................................................................15 11. Drill core from Eagle Mine ........................................................................................................15 12. Closeup of excavated outcrop at type location .....................................................................16 13. Upper contact at type location .................................................................................................17 14. Lower contact at type location.................................................................................................17 15. Outcrop northeast of Eckman Park..........................................................................................18 16. Stratigraphic section in Fish Creek Canyon ...........................................................................20 17–20. Photographs showing Yampa Bed 17. Outcrop in Fish Creek Canyon ..................................................................................................21 18. Outcrop in Ute Gulch ..................................................................................................................21 19. Closeup in Ute Gulch ..................................................................................................................22 20. Outcrop south of Eagle Mine ....................................................................................................22 21. Outcrop of Yampa Bed and Peacock coal bed south
Recommended publications
  • Structural Interpretation of the Cherokee Arch, South
    STRUCTURAL INTERPRETATION OF THE CHEROKEE ARCH, SOUTH CENTRAL WYOMING, USING 3-D SEISMIC DATA AND WELL LOGS by Joel Ysaccis B. ABSTRACT The purpose of this study is to use 3-D seismic data and well logs to map the structural evolution of the Cherokee Arch, a major east-west trending basement high along the Colorado-Wyoming state line. The Cherokee Arch lies along the Cheyenne lineament, a major discontinuity or suture zone in the basement. Recurrent, oblique-slip offset is interpreted to have occurred along faults that make up the arch. Gas fields along the Cherokee Arch produce from structural and structural-stratigraphic traps, mainly in Cretaceous rocks. Some of these fields, like the South Baggs – West Side Canal fields, have gas production from multiple pays. The tectonic evolution of the Cherokee Arch has not been previously studied in detail. About 315 mi2 (815 km2) of 3-D seismic data were analyzed in this study to better understand the kinematic evolution of the area. The interpretation involved mapping the Madison, Shinarump, Above Frontier, Mancos, Almond, Lance/Fox Hills and Fort Union horizons, as well as defining fault geometries. Structure maps on these horizons show the general tendency of the structure to dip towards the west. The Cherokee Arch is an asymmetrical anticline in the hanging wall, which is mainly transected by a south-dipping series of east-west striking thrust faults. The interpreted thrust faults generally terminate within the Mancos to Above Frontier interval, and their vertical offset increases in magnitude down to the basement. Post-Mancos iii intervals are dominated by near-vertical faults with apparent normal offset.
    [Show full text]
  • 1 Revision 2 1 K-Bentonites
    1 Revision 2 2 K-Bentonites: A Review 3 Warren D. Huff 4 Department of Geology, University of Cincinnati, Cincinnati, OH 45221 USA 5 Email: [email protected] 6 Keywords: K-bentonite, bentonite, tephra, explosive volcanism, volcanic ash 7 Abstract 8 Pyroclastic material in the form of altered volcanic ash or tephra has been reported and described 9 from one or more stratigraphic units from the Proterozoic to the Tertiary. This altered tephra, 10 variously called bentonite or K-bentonite or tonstein depending on the degree of alteration and 11 chemical composition, is often linked to large explosive volcanic eruptions that have occurred 12 repeatedly in the past. K-bentonite and bentonite layers are the key components of a larger group of 13 altered tephras that are useful for stratigraphic correlation and for interpreting the geodynamic 14 evolution of our planet. Bentonites generally form by diagenetic or hydrothermal alteration under 15 the influence of fluids with high Mg content and that leach alkali elements. Smectite composition is 16 partly controlled by parent rock chemistry. Studies have shown that K-bentonites often display 17 variations in layer charge and mixed-layer clay ratios and that these correlate with physical 18 properties and diagenetic history. The following is a review of known K-bentonite and related 19 occurrences of altered tephra throughout the time scale from Precambrian to Cenozoic. 20 Introduction 21 Volcanic eruptions are often, although by no means always, associated with a profuse output 22 of fine pyroclastic material, tephra. Tephra is a term used to describe all of the solid material 23 produced from a volcano during an eruption (Thorarinsson, 1944).
    [Show full text]
  • Cozzette Sandstone, Book Cliffs, Colorado, U.S.A
    Journal of Sedimentary Research, 2015, v. 85, 459–488 Research Article DOI: http://dx.doi.org/10.2110/jsr.2015.26 TECTONICALLY CONTROLLED NEARSHORE DEPOSITION: COZZETTE SANDSTONE, BOOK CLIFFS, COLORADO, U.S.A. 1 2 2 ANDREW S. MADOF, NICHOLAS CHRISTIE-BLICK, AND MARK H. ANDERS 1Chevron Energy Technology Company, Houston, Texas 77002-7308, U.S.A. 2Department of Earth and Environmental Sciences and Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964-8000, U.S.A. e-mail: [email protected] ABSTRACT: The Book Cliffs of eastern Utah and western Colorado have been pivotal in the development of outcrop-based sequence stratigraphic concepts for nonmarine to shallow marine siliciclastic depositional settings. Prior studies in this area, and more generally in the Cretaceous western interior foreland basin of North America, have concluded that nearshore accumulation is controlled for the most part by the interaction between oscillatory eustatic change and longer-term regional patterns of flexural subsidence. New outcrop and subsurface evidence reported here from the eastern Book Cliffs suggests that three-dimensional tectonic tilting at length scales of up to , 50 km (31 mi) and timescales of less than , 200 kyr also strongly influenced sedimentation. Continental ice sheets are thought to have been small at the time. Documented patterns of accumulation are inconsistent with those expected from interactions of eustasy and regional flexure alone. The upper Campanian Cozzette Sandstone Member of the Mount Garfield Formation consists of twelve lithofacies arranged into six lithofacies assemblages, inferred to have been deposited in shallow marine, marginal marine, and nonmarine depositional environments.
    [Show full text]
  • KENNETH CARPENTER, Ph.D. Director and Curator Of
    KENNETH CARPENTER, Ph.D. Director and Curator of Paleontology Prehistoric Museum Utah State University - College of Eastern Utah 155 East Main Street Price, Utah 84501 Education May, 1996. Ph.D., Geology University of Colorado, Boulder, CO. Dissertation “Sharon Springs Member, Pierre Shale (Lower Campanian) depositional environment and origin of it' s Vertebrate fauna, with a review of North American plesiosaurs” 251 p. May, 1980. B.S. in Geology, University of Colorado, Boulder, CO. Aug-Dec. 1977 Apprenticeship, Smithsonian Inst., Washington DC Professional Museum Experience 1975 – 1980: University of Colorado Museum, Boulder, CO. 1983 – 1984: Mississippi Museum of Natural History, Jackson, MS. 1984 – 1986: Academy of Natural Sciences of Philadelphia, Philadelphia. 1986: Carnegie Museum of Natural History, Pittsburgh, PA. 1986: Oklahoma Museum of Natural History, Norman, OK. 1987 – 1989: Museum of the Rockies, Bozeman, MT. 1989 – 1996: Chief Preparator, Denver Museum of Nature and Science, Denver, CO. 1996 – 2010: Chief Preparator, and Curator of Vertebrate Paleontology, Denver Museum of Nature and Science, Denver, CO. 2006 – 2007; 2008-2009: Acting Department Head, Chief Preparator, and Curator of Vertebrate Paleontology, Denver Museum of Nature and Science, Denver, CO. 2010 – present: Director, Prehistoric Museum, Price, UT 2010 – present: Associate Vice Chancellor, Utah State University Professional Services: 1991 – 1998: Science Advisor, Garden Park Paleontological Society 1994: Senior Organizer, Symposium "The Upper Jurassic Morrison Formation: An Interdisciplinary Study" 1996: Scientific Consultant Walking With Dinosaurs , BBC, England 2000: Scientific Consultant Ballad of Big Al , BBC, England 2000 – 2003: Associate Editor, Journal of Vertebrate Paleontology 2001 – 2003: Associate Editor, Earth Sciences History journal 2003 – present: Scientific Advisor, HAN Project 21 Dinosaur Expos, Tokyo, Japan.
    [Show full text]
  • Using Volcaniclastic Rocks to Constrain Sedimentation Ages
    Using volcaniclastic rocks to constrain sedimentation ages: To what extent are volcanism and sedimentation synchronous? Camille Rossignol, Erwan Hallot, Sylvie Bourquin, Marc Poujol, Marc Jolivet, Pierre Pellenard, Céline Ducassou, Thierry Nalpas, Gloria Heilbronn, Jianxin Yu, et al. To cite this version: Camille Rossignol, Erwan Hallot, Sylvie Bourquin, Marc Poujol, Marc Jolivet, et al.. Using vol- caniclastic rocks to constrain sedimentation ages: To what extent are volcanism and sedimentation synchronous?. Sedimentary Geology, Elsevier, 2019, 381, pp.46-64. 10.1016/j.sedgeo.2018.12.010. insu-01968102 HAL Id: insu-01968102 https://hal-insu.archives-ouvertes.fr/insu-01968102 Submitted on 2 Jan 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Accepted Manuscript Using volcaniclastic rocks to constrain sedimentation ages: To what extent are volcanism and sedimentation synchronous? Camille Rossignol, Erwan Hallot, Sylvie Bourquin, Marc Poujol, Marc Jolivet, Pierre Pellenard, Céline Ducassou, Thierry Nalpas, Gloria Heilbronn, Jianxin Yu, Marie-Pierre
    [Show full text]
  • Geology and Coal Resources of the Upper Cretaceous Fruitland Formation, San Juan Basin, New Mexico and Colorado
    Chapter Q National Coal Resource Geology and Coal Resources of the Assessment Upper Cretaceous Fruitland Formation, San Juan Basin, New Mexico and Colorado Click here to return to Disc 1 By James E. Fassett1 Volume Table of Contents Chapter Q of Geologic Assessment of Coal in the Colorado Plateau: Arizona, Colorado, New Mexico, and Utah Edited by M.A. Kirschbaum, L.N.R. Roberts, and L.R.H. Biewick U.S. Geological Survey Professional Paper 1625–B* 1 U.S. Geological Survey, Denver, Colorado 80225 * This report, although in the USGS Professional Paper series, is available only on CD-ROM and is not available separately U.S. Department of the Interior U.S. Geological Survey Contents Abstract........................................................................................................................................................Q1 Introduction ................................................................................................................................................... 2 Purpose and Scope ............................................................................................................................. 2 Location and Extent of Area............................................................................................................... 2 Earlier Investigations .......................................................................................................................... 2 Geography............................................................................................................................................
    [Show full text]
  • Mesaverde Group and Wasatch Formation - Piceance Basin, Colorado
    NONTRIBUTARY GROUNDWATER ASSESSMENT: MESAVERDE GROUP AND WASATCH FORMATION - PICEANCE BASIN, COLORADO Submitted to: OXY USA INC. AND OXY USA WTP LP Date: November 4, 2009 Norwest Corporation 950 South Cherry Street, Suite 800 Denver, CO 80246 Tel: (303) 782-0164 Fax: (303) 782-2560 Email [email protected] www.norwestcorp.com 004280 TABLE OF CONTENTS EXECUTIVE SUMMARY ..............................................................................................................1 1 INTRODUCTION.................................................................................................................1-1 2 CONCEPTUAL MODEL .....................................................................................................2-1 2.1 GEOLOGIC SETTING ....................................................................................................2-1 2.1.1 Mancos Shale ..............................................................................................2-1 2.1.2 Iles Formation ..............................................................................................2-2 2.1.3 Williams Fork Formation ..............................................................................2-2 2.1.4 Wasatch Formation......................................................................................2-3 2.2 HYDROLOGIC DATA .....................................................................................................2-3 3 HYDROLOGEOLOGIC PARAMETERS.............................................................................3-1
    [Show full text]
  • Mesozoic Stratigraphy at Durango, Colorado
    160 New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin, 2005, p. 160-169. LUCAS AND HECKERT MESOZOIC STRATIGRAPHY AT DURANGO, COLORADO SPENCER G. LUCAS AND ANDREW B. HECKERT New Mexico Museum of Natural History and Science, 1801 Mountain Rd. NW, Albuquerque, NM 87104 ABSTRACT.—A nearly 3-km-thick section of Mesozoic sedimentary rocks is exposed at Durango, Colorado. This section con- sists of Upper Triassic, Middle-Upper Jurassic and Cretaceous strata that well record the geological history of southwestern Colorado during much of the Mesozoic. At Durango, Upper Triassic strata of the Chinle Group are ~ 300 m of red beds deposited in mostly fluvial paleoenvironments. Overlying Middle-Upper Jurassic strata of the San Rafael Group are ~ 300 m thick and consist of eolian sandstone, salina limestone and siltstone/sandstone deposited on an arid coastal plain. The Upper Jurassic Morrison Formation is ~ 187 m thick and consists of sandstone and mudstone deposited in fluvial environments. The only Lower Cretaceous strata at Durango are fluvial sandstone and conglomerate of the Burro Canyon Formation. Most of the overlying Upper Cretaceous section (Dakota, Mancos, Mesaverde, Lewis, Fruitland and Kirtland units) represents deposition in and along the western margin of the Western Interior seaway during Cenomanian-Campanian time. Volcaniclastic strata of the overlying McDermott Formation are the youngest Mesozoic strata at Durango. INTRODUCTION Durango, Colorado, sits in the Animas River Valley on the northern flank of the San Juan Basin and in the southern foothills of the San Juan and La Plata Mountains. Beginning at the northern end of the city, and extending to the southern end of town (from north of Animas City Mountain to just south of Smelter Moun- tain), the Animas River cuts in an essentially downdip direction through a homoclinal Mesozoic section of sedimentary rocks about 3 km thick (Figs.
    [Show full text]
  • Of the International Committee for Coal and Organic Petrology – ICCP
    th 57 Annual Meeting of the International Committee for Coal and Organic Petrology – ICCP A B S T R A C T S 18-23rd September 2005 Patras, Greece Organizing Committee Assoc. Prof. Dr. Kimon Christanis, University of Patras Prof. Dr. Prodromos Antoniadis, National Technical University of Athens Prof. Dr. Andreas Georgakopoulos, University of Thessaloniki Dr. Cassiani Papanicolaou, Institute of Geology and Mineral Resources Dr. Stefanos Papazisimou, University of Patras Dr. Antonis Bouzinos, University of Patras Mr. Stavros Kalaitzidis, Ph.D. student, University of Patras Contents VASCONCELOS L., SIQUELA E. Variation of rank of World coals with age 7 JELONEK I., KRUSZEWSKA K., FILIPIAK P. Liptinite as an indicator of environ- 8 mental changes during coal seam formation as based on the seam no 207 profile (Upper Silesia, Poland) ZDRAVKOV A., KOSTOVA I., KORTENSKI J. Coal properties and depositional 9 environment of the Neogene Elhovo lignite, Bulgaria HACKLEY P., MARTÍNEZ M. Organic petrology of Paleocene Marcelina 10 formation coals, Paso Diablo Mine, Western Venezuela İNANER H., NAKOMAN E. Properties of lignite deposits in western Turkey 11 KARAYIĞIT A.I. Petrography and facies analysis of the Miocene Soma coals, 12 Manisa-Turkey NADER E., OPLUŠTIL S., SÝKOROVÁ I. Coal Facies and depositional environ- 13 ments of the 9th and 10th overlying coals of the Žacléř group (Duck- mantian, Intra-Sudetic Basin, Czech Republic) MAVRIDOU E., OIKONOMOPOULOS I., ANTONIADIS P. Reflectivity Measure- 14 ments in Lignite Deposits from Ptolemais Region (N. Greece) PAPAZISIMOU S., KALAITZIDIS S., CHATZIAPOSTOLOU A., SIAVALAS G., 15 CHRISTANIS K., VAGIAS, D. Coal-petrographic characteristics of the Pellana lignites (cores KP7 and KP13), Lakonia, Greece CUKALLA M., SERJANI A.
    [Show full text]
  • Coal Resources of Western Colorado D
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/32 Upper Cretaceous (Campanian) coal resources of western Colorado D. Keith Murray, 1981, pp. 233-240 in: Western Slope (Western Colorado), Epis, R. C.; Callender, J. F.; [eds.], New Mexico Geological Society 32nd Annual Fall Field Conference Guidebook, 337 p. This is one of many related papers that were included in the 1981 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.
    [Show full text]
  • Geologic History and Hydrocarbon Potential of Late Cretaceous-Age, Low-Permeability Reservoirs, Piceance Basin, Western Colorado
    Geologic History and Hydrocarbon Potential of Late Cretaceous-Age, Low-Permeability Reservoirs, Piceance Basin, Western Colorado U.S. GEOLOGICAL SURVEY BULLETIN 1787-E Chapter E Geologic History and Hydrocarbon Potential of Late Cretaceous-Age, Low-Permeability Reservoirs, Piceance Basin, Western Colorado By RONALD C. JOHNSON A multidisciplinary approach to research studies of sedimentary rocks and their constituents and the evolution of sedimentary basins, both ancient and modern U.S. GEOLOGICAL SURVEY BULLETIN 1 787 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: 1989 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center, Box 25425 Denver, CO 80225 Any use of trade names in this report is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey. Library of Congress Cataloging-in-Publication Data Johnson, Ronald Carl, 1950- Geologic history and hydrocarbon potential of Late Cretaceous-Age, low-permeability reservoirs, Piceance Basin, western Colorado. (Evolution of sedimentary basins Uinta and Piceance Basins ; ch. E.) (U.S. Geological Survey bulletin ; 1787) Bibliography: p. Supt. of Docs, no.: I 19.3:1787-E 1. Geology Colorado Piceance Creek Watershed. 2. Gas, Natural Geology Colorado Piceance Creek Watershed. I. Title. II. Series. III. Series: U.S. Geological Survey bulletin ; 1787-E. QE75.B9 no. 1787-E 557.3
    [Show full text]
  • Grand Mesa, Uncompahgre, and Gunnison National Forests Coal
    Grand Mesa, Uncompahgre, and Gunnison National Forests Coal Resource and Development Potential Report (2004, revised 2006) ii TABLE OF CONTENTS I. Introduction .................................................................................................................... 1 Purpose and Scope .......................................................................................................... 1 Acknowledgments........................................................................................................... 1 II. Geologic Units............................................................................................................... 1 Description.................................................................................................................. 5 III. Coal Fields .................................................................................................................... 5 Carbondale Coal Field .................................................................................................... 6 Crested Butte Coal Field................................................................................................. 6 Grand Mesa Coal Field ................................................................................................... 8 Somerset Coal Field........................................................................................................ 8 Tongue Mesa Coal Field................................................................................................. 9 IV. Coal Characteristics
    [Show full text]