Colorado Stratigraphy Chart

Total Page:16

File Type:pdf, Size:1020Kb

Colorado Stratigraphy Chart Piceance Basin, Upper Arkansas, Denver- NW San Juan, Sand Wash Eagle North\Middle South Park Front Range Raton Southeast Geologic Ma Epoch San Juan San Luis Julesburg Era Paradox Basins Basin Basin Park Basins Basin Outcrops Basin Colorado History Volcanics Valleys Basin Period 0 Dotsero Volcano 1, 4-5 my basalt Raton basalt ows Mesa de Maya basalt ows Gravel Mtn Independence Mtn Tilt conglomerate Pleistocene/ Alamosa Ogallala Ogallala Rifting Pliocene Breeze Mtn (Yampa Stocks) Dry Gravels at Divide 8 Grand Mesa Volcanics Grouse Mtn Basalt Union Regional uplift Flat Tops Volcanics Santa Fe Miocene Goodenough Treasure Mtn Los Pinos Trump Wagon Tongue Martins Canyon Browns Park Browns Park Troublesome North Park Cedar Mtn 20 Neogene San Juan Volcanics Arikaree Spanish Peaks Creede San Juan Volcanics Healing Phase 2 Conejos Mt Cumulus Oligocene Mt Richthofen Bishop Cgl Pitch- Rabbit Ears Volcanics Central Colo- Tallahassee Brule West Elk Volcanics Pinnacle rado Volcanics Creek Cgl White River Group Gilbert Peak erosion surface Antero Castle Rock Cgl Chadron Devils Hole Castle Rock Rhyolite Two Buttes Mt Sopris White River Echo Park Telluride Cgl Wall Mountain Tu 39 Mile Volcanics Florissant (Wall Mtn Tu) Montezuma Larkspur Cgl 40 Chapter 7 Breckenridge Eocene Washakie/Bridger Laccolith Uinta Farisita Laramide Orogeny CENOZOIC Blanco Basin Huerfano-Cuchara Green River Coalmont Wasatch Poison Canyon San Jose Wasatch D2 Sequence Dawson Arkose Orogenic Paleogene gravels Molina Animas Middle Park Paleosol Raton Nacimiento/Animas Ft Union Ft Union South Park 60 Paleocene Green Mtn Cgl sub-Arapahoe Ohio Ck Cgl Moat Cgl Windy Gap D1 Sequence unconformity Raton Cgl Ch 6 Ojo Alamo Laramide Reinecker Ridge Cgl Laramie Arapahoe Cgl Denver sub-Ojo Alamo unconformity sub-Ohio Ck unconformity sub-Moat unconformity sub-Windy Gap unconformity Vermejo Williams Fork Lance/Williams Fork Laramie Pando Porphyry Laramie Kirtland Lion Cyn Fox Hills Laramie Richard Fox Hills Richard Fruitland Lion Cyn Fox Hills Fox Hills Trinidad Rollins Iles Fox Hills Larimer Larimer Cozzette Twentymile Lewis Rocky Ridge Rocky Ridge Pictured Clis Corcoran Hygiene Pierre Pierre Pierre Castlegate Kremmling Laramide Lewis Cli House Sego Trout Ck Terry Terry Pierre Pierre Meeker Tow Ck Laramide Lujane Pt Mancos Apache Creek Shale Hygiene Shale Hygiene 80 Menefee Sharon Springs Sharon Springs MV Sharon Spr Laramide Pierre Point Lookout Morapas Mancos Prairie Cyn Smoky Hill Smoky Hill Niobrara Smoky Hill Upper Mancos Smoky Hill Niobrara Niobrara Niobrara Niobrara Niobrara Niobrara Niobrara Ft Hays Ft Hays Juana Lopez Montezuma Juana Lopez Ft Hays Juana Lopez Ft Hays Juana Lopez Mancos Shale Juana Lopez Codell Codell Cretaceous Blue Hill Frontier Benton Benton Carlile Codell CarlileCarlile Carlile Codell Carlile Bridge Ck Cretaceous Benton Greenhorn GreenhornGreenhorn Greenhorn Greenhorn Interior Seaway Graneros Mowry Mowry Mowry shales Graneros GranerosGraneros Graneros Graneros Dakota Grp Mowry Dakota Grp Dakota Grp Mowry Mowry Colorado Grp Mowry Colorado Grp Dakota Grp Dakota Grp 100 Dakota Grp Dakota Grp Horsetooth/J Dakota Grp Dakota Grp Dakota Grp Transgressive lags Lytle pebbles Van Bibber Dakota Dakota J Dakota J Dakota J Kassler/Ft. Collins Skull Ck Skull Ck Skull Ck Grp Skull Creek Grp Plainview Grp Plainview Grp Plainview Plainview Lytle Lytle Lytle Sevier Orogeny Burro Canyon Burro Canyon Lytle (Cedar Mountain in UT) Cretaceous 120 Chapter 5 Lower sub-Dakota unconformity sub-Dakota unconformity sub-Dakota unconformity sub-Dakota unconformity sub-Dakota unconformity sub-Dakota unconformity sub-Dakota unconformity sub-Dakota unconformity Basal conglomerates (e.g., Buckhorn) sub-Dakota unconformity sub-Dakota unconformity 140 Brushy Basin Salt Wash Brushy Basin Salt Wash Brushy Basin Tidwell Blu Morrison Morrison Morrison Tidwell Morrison Salt Wash Morrison Morrison Morrison Morrison Morrison Morrison Westwater Recapture Ck Junction Ck Junction Ck Upper J5 unconformity J5 unconformity J5 unconformity Ralston Creek Ralston Creek Ralston Creek J5 unconformity J5 unconformity J5 unconformity J5 unconformity J5 unconformity J5 unconformity J5 unconformity Wanakah Wanakah 160 Curtis Curtis Pony Express (Todilto in UT) Pony Express Entrada Entrada Entrada Entrada Entrada/Sundance Garo Sundance Entrada Entrada Middle Page Carmel San Rafael Grp Carmel San Rafael Grp Carmel San Rafael Grp MESOZOIC J2 unconformity J2 unconformity J2 unconformity J2 unconformity J2 unconformity J2 unconformity J2 unconformity J2 unconformity J2 unconformity Healing Phase 1 Navajo 180 Navajo Jurassic Navajo/Nugget Lower Kayenta Kayenta Glen Cyn Glen Cyn Glen Grp Cyn Glen Grp Cyn Wingate Wingate Glen Grp Canyon 200 J0 unconformity J0 unconformity J0 unconformity J0 unconformity Chapter 4 220 Upper Chinle Chinle Chinle Chinle Chinle Chinle Triassic Shinarump Gartra Gartra Gartra N Atlantic Opens, America driftsW 240 Tr3 unconformity Tr3 unconformity Tr3 unconformity Tr3 unconformity Middle Jelm Jelm Jelm Moenkopi Moenkopi Moenkopi Chugwater Lower Lykins Lykins Taloga Tr1 unconformity Tr1 unconformity Tr1 unconformity Ochoan State State Bridge Forelle Forelle Forelle 260 Bridge Day Creek Glendo White Rim Ss Lykins Falcon Guadalupian Minnekahta Whitehorse Grp Ancestral Rockies Kaibab Ls Orogeny Phosphoria Park City/S Canyon Creek S Canyon Ck Opeche Blaine Blaine Blaine Leonardian Organ Rock Cedar Hills Cedar Hills Lyons Stone Corral Glorieta Stone Corral 280 Sumner Schoolhouse Satanka/Owl Cyn Wellington Yeso Chase Permian Sangre Weber Ingleside Wolfcamp Council Grove Wolfcampian Weber de Weber Wabaunsee Cristo Wabaunsee Maroon Shawnee Crestone Shawnee Hermosa Maroon Maroon Cgl Fountain Lansing Lansing ASSEMBLES PANGEA 300 Elephant Canyon Jacque Mtn Jacque Mtn Kansas City Kansas City Virgilian Maroon Eagle Valley Evaporite Gothic Marmaton Madera Minturn Fountain Marmaton Ouachita-Marathon-Sonoma and Alleghenian Orogenies Minturn Morgan Minturn Minturn Sharpsdale Missourian Round Valley Eagle Valley Cherokee Cherokee Desmoinesian Paradox salts Eagle Valley Evap Evaporite Atokan Belden Atoka Atoka Belden Belden Kerber Lower Hermosa Belden Glen Eyrie Morrow Morrow Chapter 3 Morrowan Uncompahgre Uncompahgre Keyes Keyes Ancestral Rockies Ancestral Ancestral Rockies Ancestral Rockies Ancestral Rockies Ancestral 320 Pennsylvanian Molas Chesterian Molas Molas Molas Molas pre-Pennsylvanian pre-Pennsylvanian pre-Pennsylvanian Meramecian pre-Pennsylvanian unconformity unconformity unconformity pre-Pennsylvanian pre-Pennsylvanian pre-Pennsylvanian pre-Pennsylvanian Carboniferous unconformity 340 unconformity unconformity unconformity unconformity Beulah Ste. Genevieve Osagean regression St. Louis St. Louis Mississippian Leadville Leadville Leadville Leadville Leadville Spergen Hardscrabble/ Spergen Kinder- Leadville Warsaw Leadville Warsaw hookian Gilman Gilman Kaskaskia Sequence Williams Cyn Osage Osage 360 PinyonPre Devonian Pk unconformityOuray Dyer Kinderhook Williams Chaee Grp Dyer Dyer Kinderhook Grp Grp Grp Misener Canyon Chaee Chaee Chaee Chaee Chaee Parting Parting Parting Elbert McCracken transgression Upper Ignacio 380 Aneth Middle Gore Fault Gore pre-Devonian pre-Devonian pre-Devonian pre-Devonian pre-Devonian pre-Devonian pre-Devonian pre-Devonian pre-Devonian Devonian 400 unconformity unconformity unconformity unconformity unconformity unconformity unconformity unconformity unconformity Lower PALEOZOIC 420 Pridoli Ludlow Wentlock Llandovery Silurian and Ordovician Gore Fault Gore 440 Silurian fossils in kimberlite pipes Chapter 2 west of Virginia Dale regression Upper Fault Dallas Creek/Ridgway Fremont Fremont Fremont Viola Fremont Ls Tippecanoe Sequence 460 Harding Harding Harding Harding Harding Ss Simpson Middle transgression sub-Harding unconformity sub-Harding unconformity sub-Harding unconformity sub-Harding unconformity sub-Harding unconformity regression Ordovician Manitou Laurentia Margin Passive Lower Manitou Manitou Manitou Manitou Manitou/Arbuckle Manitou/ ?Cambro-Ordovician 480 Arbuckle Arbuckle strata removed by Sauk Sequence pre-Devonian Dotsero Dotsero Dotsero sub-Manitou unconformity? unconformity Furongian Sawatch Sawatch/ Sawatch/Reagan Lodore Lodore Sawatch Sawatch Sawatch Sawatch/Reagan Reagan Tintic 500 transgression Series 3 Series 2 520 Cambrian Terren- The Great The Great The Great The Great The Great The Great The Great The Great The Great Unconformity Unconformity Unconformity Unconformity Unconformity Unconformity Unconformity Unconformity Unconformity euvian 540 Uinta Mt Grp 780-720 Ma Tava 800-680 Ma Proterozoic Uncompahgre Basement Rocks, mainly 1.1–1.8 Ga 1.7-1.4 Ga Owiyukuts Complex Ch 1 Oct. 30, 2018 2.4 Ga.
Recommended publications
  • Analysis and Correlation of Growth
    ANALYSIS AND CORRELATION OF GROWTH STRATA OF THE CRETACEOUS TO PALEOCENE LOWER DAWSON FORMATION: INSIGHT INTO THE TECTONO-STRATIGRAPHIC EVOLUTION OF THE COLORADO FRONT RANGE by Korey Tae Harvey A thesis submitted to the Faculty and 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: ________________________ Korey Harvey Signed: ________________________ Dr. Jennifer Aschoff Thesis Advisor Golden, Colorado Date ___________________________ Signed: _________________________ Dr. Paul Santi Professor and Head Department of Geology and Geological Engineering ii ABSTRACT Despite numerous studies of Laramide-style (i.e., basement-cored) structures, their 4-dimensional structural evolution and relationship to adjacent sedimentary basins are not well understood. Analysis and correlation of growth strata along the eastern Colorado Front Range (CFR) help decipher the along-strike linkage of thrust structures and their affect on sediment dispersal. Growth strata, and the syntectonic unconformities within them, record the relative roles of uplift and deposition through time; when mapped along-strike, they provide insight into the location and geometry of structures through time. This paper presents an integrated structural- stratigraphic analysis and correlation of three growth-strata assemblages within the fluvial and fluvial megafan deposits of the lowermost Cretaceous to Paleocene Dawson Formation on the eastern CFR between Colorado Springs, CO and Sedalia, CO. Structural attitudes from 12 stratigraphic profiles at the three locales record dip discordances that highlight syntectonic unconformities within the growth strata packages. Eight traditional-type syntectonic unconformities were correlated along-strike of the eastern CFR distinguish six phases of uplift in the central portion of the CFR.
    [Show full text]
  • Stratigraphy of the Project Area
    I BRITISH &! COLUMBLA Ministry of Employment and Investment ENERGY AND MINERALS DIVISION Hon. Dan Miller. Minister Geological Survey Branch THE STIKINE PROJECT GEOLOGY OF WESTERN TELEGRAPH CREEK MAP AREA, NORTHWESTERN BRITISH COLUMBIA (NTS 104G/5,6, llW, 12 AND 13) By Derek A. Brown1 , Michael H. Gunning2 and Charles J. Greig3 Appendix 3 - Conodont identifications by "I. Orchard, Geological Survey of Canada 1. Geological Surve Branch, British Colunlhia Ministry of Employment andYlnvestment 2. Department of Geology, University of Western Ontario, London, Ontario 3. C.G. Greig and Associates Ltd., Penticton, B.C. BULLETIN 95 Canadian Cataloguing in Publication Data Brawn. Derek Anlhony. 1959- The Stikine project : geology of western Telegraph Creek map area. nonhwenlem British Columbia (NTS.lMG15. 6, IIW. 12and 13) Issued by Geological Survey Branch. Includes bibliographical references: p ISBN 0-7726-2502-6 1, Geology -British Columbia -Telegraph Creek Region 2. Geochemistry - British Columbia - Telegraph Creek VICTORIA Region. 3. Geology. Economic - British Columbia - BRITISH COLUMBIA Telegraph Creek Region. 4. Mines and mineral resources - CANADA British Columbia - Telegraph Creek Region. 1. Gunning. Michael H. 11. Greig.Charles James, 1956- . 111. British Columbia. Ministry of Employment and Investmenl. IV. MAY 1996 BritishColumbia. Geological Survey Branch. V. Title. VI. Title: Geology of western Telegraph Creek maparea, nanhwertern British Columbia (NTS 1WG15.6. 1 IW. 12 and 13). V11. Series: Bulletin (British Columbia. Ministry of Employment and Investment) ;95. QE187.B76 1996 557.11’185 (395-960208-9 Frontispiece. View north along the Scud Glacier. Ambition Mountainis underlain by Permian limestone and metavolcanic rocks. Ministry of Emp/oyment and Inveshent TABLE OF CONTENTS CHAPTER 1 Chemistry .....................
    [Show full text]
  • RE-EVALUATION, Mileposts 149 to 161
    RE-EVALUATION, Mileposts 149 to 161 Interstate 25 Improvements through the Colorado Springs Area Environmental Assessment PALEONTOLOGY TECHNICAL MEMO April 2012 Prepared for: CDOT Region 2 Prepared by: Doug Eberhart, Telephone (719) 520-5800 Introduction The Colorado Department of Transportation (CDOT) has prepared this technical memorandum to update findings with regards to the paleontological resources described in the original 2004 I-25 Environmental Assessment (EA) with regard to the portion of the Proposed Action between Woodmen Road (Exit 149) in Colorado Springs and State Highway 105 in Monument (Exit 161). The purpose of the EA’s Proposed Action is to relieve existing traffic congestion and address project future congestion on I-25 within the Colorado Springs Urbanized Area. The I-25 EA originally evaluated impacts for the widening of I-25 between South Academy Boulevard (Exit 135) and SH 105, together with reconstruction of various I-25 interchanges within this corridor. Page 2-10 of the EA stated that, “Consistent with projected traffic demand in the I-25 corridor, the conceptual phasing for the Proposed Action calls for: (1) initially six-laning through central Colorado Springs, then (2) six-laning in northern El Paso Figure 1. I -25 EA Re -evaluation Project Vicinity County, and finally (3) adding HOV [High-Occupancy Vehicle] lanes through central Colorado Springs and widening to six lanes south to South Academy Boulevard.” For the year 2012, CDOT has received funding to begin the second phase, meaning to widen I-25 to six lanes in northern El Paso County. The EA calls for eventually widening I-25 all the way to SH105.
    [Show full text]
  • Abdullin Colostate 0053N 11378.Pdf (3.002Mb)
    THESIS GEOPHYSICAL CONSTRAINTS ON THE FLEXURAL SUBSIDENCE OF THE DENVER BASIN Submitted by Ayrat Abdullin Department of Geosciences In partial fulfillment of the requirements For the Degree of Master of Science Colorado State University Fort Collins, Colorado Fall 2012 Master’s Committee: Advisor: Dennis L. Harry Sven Egenhoff Michael Lefsky ABSTRACT GEOPHYSICAL CONSTRAINTS ON THE FLEXURAL SUBSIDENCE OF THE DENVER BASIN The Denver Basin is an asymmetric Laramide (Late Cretaceous through Eocene) foreland basin covering portions of eastern Colorado, northwestern Kansas, southwestern Nebraska, and southeastern Wyoming, USA. It is bordered on the west by the Rocky Mountain Front Range Uplift, a basement cored Laramide anticline bounded by thrust faults, and on the east by the Great Plains and stable North American craton. A ~400 mGal negative Bouguer gravity anomaly exists over the Denver Basin and Front Range Uplift, with its minimum located over the highest topography in the central part of the uplift, approximately 100 km west of the Denver Basin. This study examines three hypotheses concerning the isostatic state of the basin and adjacent Front Range Uplift. These hypotheses are that the modern shape of the basin is due to: 1) flexure of the lithosphere under the surface load of the current topography, or 2) flexure under a subsurface load beneath the Rocky Mountains, or 3) a combination of both surface and subsurface loads. To test these hypotheses, spectral analysis and forward gravity modeling was conducted along three profiles located in the northern, central, and southern parts of the basin. Bouguer gravity power spectra along the profiles reveal 5 major density interfaces interpreted to represent the base of the lithosphere (at depths of 132 to 153 km), base of the crust (45-55 km), a mid-crustal boundary (about 20 km), the top of Precambrian basement (1-2 km), and a boundary between the Pierre Shale and Niobrara Formations within the pre-Laramide sedimentary section (-1-0 km).
    [Show full text]
  • Stratigraphy of Cretaceous-Eocene Transition Beds in Eastern Montana and the Dakotas 1
    BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA VOL. 35. PP. 481-506, PLS. 23-25 SEPTEMBER 30, 1924 STRATIGRAPHY OF CRETACEOUS-EOCENE TRANSITION BEDS IN EASTERN MONTANA AND THE DAKOTAS 1 BY W. T. THOM, JR., AND C. E. DOBBIN (Presented before the Society December 28, 1923) CONTENTS Pago Introduction................................................................................................................... 4S1 Acknowledgments......................................................................................................... 483 Part I. Stratigraphy of the northern Plains...................................................... 483 General statement................................................................................................ 483 Lennep sandstone................................................................................................. 485 Fox Hills sandstone................................................................................................485 General statement....................................................................................... 485 Colgate sandstone member........................................................................ 490 Lance formation................................................................................................... 491 General statement........................................................................................ 491 Hell Creek member.....................................................................................491 Tullock member.......................................
    [Show full text]
  • 19Th Forum on Industrial Minerals Proceedings
    THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the “Content”) is governed by the terms set out on this page (“Terms of Use”). By downloading this Content, you (the “User”) have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario’s Ministry of Northern Development and Mines (MNDM) as a public service, on an “as-is” basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the “Owner”).
    [Show full text]
  • Geologic Characterization 111 Date 7/31/91 List of Appendices
    Characterization GEOLOGIC Prepared by ? TABLE OF CONTENTS Section Page 1.0 INTRODUCTION ....................................... 1 1.1 Purpose ........................................... 1 1.2 Scope of Characterization .............................. 1 1.2.1 Literature Search .... ........................... 1 1.2.2 Core Processing and Description ..................... 2 1.2.3 Reprocessing of Seismic Data ........................ 2 1.2.4 Grain Size Analysis .............................. 2 1.2.5 Geologic Report ................................ 3 1.3 Location and General Setting ...., ........................ 3 1.4 Previous Studies ...................................... 5 2.0 STRATIGRAPHY ....................................... 7 Precambrian ......................................... 2.1 7 2.2 Paleozoic And Mesozoic Sedimentary Section ................ 2.2.1 Fountain Formation (PennsylvanianPermian) ............ 7 2.2.2 Lyons Sandstone Formation (Permian) ................ 7 2.2.3 Lykins Formation (PermianrTriassic) ................. 10 2.2.4 Ralston Creek Formation (Jiurassic) .................. 10 2.2.5 Momson Formation (Jurassic) ...................... 10 2.2.6 Dakota Group (Lower Cretaceous) ................... 10 2.2.7 Benton Shale Formation (Lower/Upper Cretaceous) ....... 11 2.2.8 Niobrara Formation (Upper Cretaceous) ............... 11 2.2.9 Pierre Shale Formation (Upper Cretaceous) ............. 11 2.2.10 Fox Hills Sandstone Formation (Upper Cretaceous) ....... 12 2.2.1 1 Laramie Formation (Upper Cretaceous) ............... 12 2.2.12
    [Show full text]
  • Geologic Map of Washington - Northwest Quadrant
    GEOLOGIC MAP OF WASHINGTON - NORTHWEST QUADRANT by JOE D. DRAGOVICH, ROBERT L. LOGAN, HENRY W. SCHASSE, TIMOTHY J. WALSH, WILLIAM S. LINGLEY, JR., DAVID K . NORMAN, WENDY J. GERSTEL, THOMAS J. LAPEN, J. ERIC SCHUSTER, AND KAREN D. MEYERS WASHINGTON DIVISION Of GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 •• WASHINGTON STATE DEPARTMENTOF 4 r Natural Resources Doug Sutherland· Commissioner of Pubhc Lands Division ol Geology and Earth Resources Ron Telssera, Slate Geologist WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Ron Teissere, State Geologist David K. Norman, Assistant State Geologist GEOLOGIC MAP OF WASHINGTON­ NORTHWEST QUADRANT by Joe D. Dragovich, Robert L. Logan, Henry W. Schasse, Timothy J. Walsh, William S. Lingley, Jr., David K. Norman, Wendy J. Gerstel, Thomas J. Lapen, J. Eric Schuster, and Karen D. Meyers This publication is dedicated to Rowland W. Tabor, U.S. Geological Survey, retired, in recognition and appreciation of his fundamental contributions to geologic mapping and geologic understanding in the Cascade Range and Olympic Mountains. WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 Envelope photo: View to the northeast from Hurricane Ridge in the Olympic Mountains across the eastern Strait of Juan de Fuca to the northern Cascade Range. The Dungeness River lowland, capped by late Pleistocene glacial sedi­ ments, is in the center foreground. Holocene Dungeness Spit is in the lower left foreground. Fidalgo Island and Mount Erie, composed of Jurassic intrusive and Jurassic to Cretaceous sedimentary rocks of the Fidalgo Complex, are visible as the first high point of land directly across the strait from Dungeness Spit.
    [Show full text]
  • Synoptic Taxonomy of Major Fossil Groups
    APPENDIX Synoptic Taxonomy of Major Fossil Groups Important fossil taxa are listed down to the lowest practical taxonomic level; in most cases, this will be the ordinal or subordinallevel. Abbreviated stratigraphic units in parentheses (e.g., UCamb-Ree) indicate maximum range known for the group; units followed by question marks are isolated occurrences followed generally by an interval with no known representatives. Taxa with ranges to "Ree" are extant. Data are extracted principally from Harland et al. (1967), Moore et al. (1956 et seq.), Sepkoski (1982), Romer (1966), Colbert (1980), Moy-Thomas and Miles (1971), Taylor (1981), and Brasier (1980). KINGDOM MONERA Class Ciliata (cont.) Order Spirotrichia (Tintinnida) (UOrd-Rec) DIVISION CYANOPHYTA ?Class [mertae sedis Order Chitinozoa (Proterozoic?, LOrd-UDev) Class Cyanophyceae Class Actinopoda Order Chroococcales (Archean-Rec) Subclass Radiolaria Order Nostocales (Archean-Ree) Order Polycystina Order Spongiostromales (Archean-Ree) Suborder Spumellaria (MCamb-Rec) Order Stigonematales (LDev-Rec) Suborder Nasselaria (Dev-Ree) Three minor orders KINGDOM ANIMALIA KINGDOM PROTISTA PHYLUM PORIFERA PHYLUM PROTOZOA Class Hexactinellida Order Amphidiscophora (Miss-Ree) Class Rhizopodea Order Hexactinosida (MTrias-Rec) Order Foraminiferida* Order Lyssacinosida (LCamb-Rec) Suborder Allogromiina (UCamb-Ree) Order Lychniscosida (UTrias-Rec) Suborder Textulariina (LCamb-Ree) Class Demospongia Suborder Fusulinina (Ord-Perm) Order Monaxonida (MCamb-Ree) Suborder Miliolina (Sil-Ree) Order Lithistida
    [Show full text]
  • Diachronous Development of Great Unconformities Before Neoproterozoic Snowball Earth
    Diachronous development of Great Unconformities before Neoproterozoic Snowball Earth Rebecca M. Flowersa,1, Francis A. Macdonaldb, Christine S. Siddowayc, and Rachel Havraneka aDepartment of Geological Sciences, University of Colorado, Boulder, CO 80309; bEarth Science Department, University of California, Santa Barbara, CA 93106; and cDepartment of Geology, The Colorado College, Colorado Springs, CO 80903 Edited by Paul F. Hoffman, University of Victoria, Victoria, Canada, and approved March 6, 2020 (received for review July 30, 2019) The Great Unconformity marks a major gap in the continental precisely because the Great Unconformities mark a large gap in geological record, separating Precambrian basement from Phan- the rock record, the erosion history leading to their formation erozoic sedimentary rocks. However, the timing, magnitude, cannot be investigated directly by study of preserved units. spatial heterogeneity, and causes of the erosional event(s) and/ Past work leads to at least four general models for the timing or depositional hiatus that lead to its development are unknown. and magnitude of pre-Great Unconformity continental erosion, We present field relationships from the 1.07-Ga Pikes Peak batho- which are depicted in Fig. 1. Some have proposed major erosion lith in Colorado that constrain the position of Cryogenian and of the continents associated with assembly of the supercontinent Cambrian paleosurfaces below the Great Unconformity. Tavakaiv Rodinia and mantle upwelling below it prior to 850 Ma (Hy- sandstone injectites with an age of ≥676 ± 26 Ma cut Pikes Peak pothesis 1) or with the early diachronous breakup of Rodinia granite. Injection of quartzose sediment in bulbous bodies indi- between 850 and 717 Ma (Hypothesis 2) (10–17).
    [Show full text]
  • Stratigraphy of the Cretaceous Rocks and the Tertiary Ojo Alamo Sandstone, Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah
    Stratigraphy of the Cretaceous Rocks and the Tertiary Ojo Alamo Sandstone, Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah GEOLOGICAL SURVEY PROFESSIONAL PAPER 521-E Prepared in cooperation with the Bureau of .Indian -L1Jfairs and the Navajo Tribe ;. ~:0 ..J :i.ui._lll{c,/1 II- Stratigraphy of the Cretaceous > Rocks and the Tertiary Ojo I Alamo Sandstone, Navajo and .. .... Hopi Indian Reservations, .. Arizona, New Mexico, and Utah By R. B. O'SULLIVAN, C. A. REPENNING, E. C. BEAUMONT, and H. G. PAGE HYDROGEOLOGY OF THE NAVAJO AND HOPI INDIAN RESERVATIONS, ARIZONA, NEW MEXICO, AND UTAH GEOLOGICAL SURVEY PROFESSIONAL PAPER 521-E Prepared in cooperation with the Bureau of Indian Affairs and the Navajo Tribe .I .. UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1972 ~· ·. UN.ITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY W. A. Radlinski, Acting Director Library of Congress catalog-card No. 76-180659 ·~ For sale by the Sup~rintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402- (paper cover) Stock Number 2401-1184 CONTENTS Page Page Abst1·act ------------------------------------------ El Upper Cretaceous rocks-Continued Introduction -------------------------------------­ 2 Mesaverde Group-Continued Location and land-net system ------------------ 2 Lower part of the Mesaverde Group in San Present work -------------------------------­ 3 Juan Basin-Continued Previous investigations and nomenclature ------ 5 Crevasse Canyon Formation ---------- E31 Lower
    [Show full text]
  • Geology Technical Report
    Geology Technical Report For the C-470 Corridor Revised Environmental Assessment January 2015 Submitted To: CDOT Region 1 2000 S. Holly Street Denver, CO 80222 Submitted By: Wilson & Company 1675 Broadway, Suite 200 Denver, CO 80202 C-470 Corridor Revised Environmental Assessment TABLE OF CONTENTS 2015 UPDATE TO THE 2005 REPORT............................................................. 1 1.0 INTRODUCTION............................................................................................... 2 2.0 AFFECTED ENVIRONMENT............................................................................. 2 2.1 Existing Conditions..................................................................................... 2 2.2 Geology…………………............................................................................. 2 2.2.1 Surficial Units………......................................................................... 3 2.2.2 Bedrock Units……………….............................................................. 4 2.2.3 Geologic Units……………................................................................. 4 2.2.4 Mineral Resources………………………………………….…………… 5 2.3 C-470 Corridor…………………………………………………....................... 6 2.3.1 Existing Pavement Condition………………………..…………………. 6 3.0 ENVIRONMENTAL CONSEQUENCES............................................................. 7 3.1 Methodology for Impact Evaluation............................................................ 7 3.2 Findings.....................................................................................................
    [Show full text]