Stratigraphy of the Cretaceous Rocks and the Tertiary Ojo Alamo Sandstone, Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah

Total Page:16

File Type:pdf, Size:1020Kb

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 boundary of Cretaceous rocks -------------­ 5 Lower part of the Mesaverde Group in the Lower Cretaceous rocks -----------------------­ 7 Black Mesa area --------------------­ 34 Burro Canyon Formation --------------------­ 7 Toreva Formation -------------------­ 35 Lower (?) and Upper Cretaceous rocks ------------ 9 Wepo Formation ------:----------------­ 38 Dakota Sandstone --------------------~-------­ 9 Yale Point Sandstone ------------------ 40 Upper Cretaceous rocks -------------------------- 13 Upper part of the Mesaverde Group -------­ 40 Mancos Shale -------------------------------­ 13 Point Lookout Sandstone ------------­ 42 Lower part of Mancos Shale -------------­ 15 Menefee Formation ------------------­ 44 Upper part of Mancos Shale --------------- 22 Post-Menefee rocks in the Chuska Moun- Mesaverde Group ----------------------------- 24 tains area -------------------------- 46 Lower part of the Mesaverde Group in San Cliff House Sandstone ----------------- 48 Juan Basin -----------------------­ 25 Lewis Shale ---------------------------------­ 50 Gallup Sandstone --------------------­ 25 Pictured Cliffs Sandstone ---------------------- 51 Gallup Sandstone south of the Chuska Fruitland Formation -------------------------­ 52 Mountains ---------------------- 25 Kirtland Shale ------------------------------- 53 Gallup Sandstone. Dileo Coal Mem- Tertiary Ojo Alamo Sandstone -------------------- 55 ber eq~i:va:len:t~, a-nd~ st~-l;l:Y,:' s~n!i~.tq~~­ . ~~e:ren~e.f:!, ~·~te~ ..,,..,......,-,...,....,.,.,.,,.,...,...,,.,_,..""""·"'<:" ________________ _ 58 of Sears, Hunt, and Hendricks · Index -------------------------------------------- 63 (1941) --------------~---------- 29 Age assignment and correlation ___ _ 30 > ILLUSTRATIONS Page PLATE 1. Generalized geologic map of the Cretaceous and some related rocks, Navajo and Hopi Indian Reser­ vations and adjacent areas -------------------------------------------------------------In pocket 2. Fence diagram of Dakota Sandstone and younger Cretaceous rocks in the Navajo country ________ In pocket FIGURE 1. Map showing Bureau of Indian Affairs administration districts and 15-minute quadrangles -------- E3 2. Index map showing location of the Navajo and Hopi Indian Reservations and the additional area studied ---------------------------------------------------------------------------------- 5 3. Chart showing nomenclature of the Upper Cretaceous rocks in the Navajo country ---------------- 6 4. Photograph of the Burro Canyon Formation in southeast Utah ---------------------------------- 8 5. Photograph of Dakota Sandstone, near Steamboat, in southeastern Black Mesa --------------------- 10 6. Map showing generalized distribution and thickness of the Dakota Sandstone -------------------- 11 7. Time-lithologic-correlation chart of the Cretaceous rocks in the Navajo country, Arizona and New Mexico -----------------·------------------------------------------·---------------------- 14 8. Diagrammatic cross section showing intertonguing relationships of the Mesaverde Group and related formations and the Mancos Shale in western San Juan Basin ---------------------------- 16 9. Map showing generalized distribution and thickness of the Mancos Shale ------------------------- 18 10-12. Photographs: 10. Limestone unit of Greenhorn age near road between Shiprock and Bitlabito --------------- 19 11. Juana Lopez Member of the Mancos Shale along road between Shiprock and Bitlabito ---- 20 12. Gallup Sandstone at The Hogback 2% miles northeast of Gallup -------------------------- 26 111 IV CONTENTS Page 13. ·Map showing generalized" distribution and thickness of the Toreva Formation and the Gallup Sand­ stone and related units ------------------------------------------------------------------- E28 14. Photograph showing the Gallup Sandstone along road to Sanostee ------------------------------ 29 15. Map showing generalized distribution and thickness of the Crevasse Canyon and Wepo Formations __ 33 16-21. Photographs: 16. Dalton Sandstone Member and related rocks --------------------------------------------- 34 17. Toreva Formation at the south end of Third Mesa ------------------------------------ 35 18. Lower tongue of the Toreva Formation near Blue Point ----------------------------.--- 36 J ...;. 19. Toreva Formation and related rocks at Yale Point ------------------------------------ 37 20. Wepo Formation near the Cow Springs coal mine ------------------'------------------ 39 21. Northeast wall of Black Mesa, showing exposures of the Dakota Sandstone, Mancos Shale, Toreva and Wepo Formations and Yale Point Sandstone -------------------------- 40 22. Map showing generalized distribution of the upper part of the Mesaverde Group and thickness of the Menefee Formation ---------------------~------------------------------------------------- 41 23-29. Photographs: 23. Point Lookout Sandstone on Chimney Rock, southwestern Colorado ---------------------- 43 24. Hosta Tongue of the J;>oint Lookout Sandstone and related rocks on Mesa de los Lobos ___ _ 44 25. Post-Menefee rocks 3 miles west of Sheep Springs ---.---------------------------------- 48 26. Mesaverde Group in The Hogback at the San Juan River ------------------------------ 49 27. Pictured Cliffs Sandstone along the south side of the San Juan River ------------------- 51 28. Fruitland Formation, west of Bisti, at Hunter Wash ------------------------------------ 52 29. Lower conglomeratic part of the Ojo Alamo Sandstone in cliffs south of Farmington ------- 56 .; I ~, HYDROGEOLOGY OF THE 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, ARIZ·ONA, NEW MEXICO, AND UTAH By R. B. O'SuLLIVAN, C. A. REPENNING, E. C. BEAUMONT, and H. G. PAGE ABSTRACT In the northeastern part of the Navajo country, the Mancos Shale is about 2,200 feet thick and underlies the Point Look­ This study of Cretaceous rocks constitutes a part of the out Sandstone. In this area the Mancos i_s divided into upper ground-water investigation of the Navajo and Hopi Indian and lower parts by the Gallup Sandstone and related rocks Reservations. The Navajo and Hopi Indian Reservations of the Mesaverde Group. In the southeastern part of the cover about 25,000 square miles, and about one-third of this Navajo country, the Mancos Shale is about 600 feet thick area is underlain by Cretaceous rocks. The Navajo country-a and underlies the Gallup Sandstone. The Crevasse Canyon more general geographic term that encompasses the Navajo Formation of the Mesaverde Group overlies the Gallup and, and Hopi Indian Reservations-lies principally in northeast­ in ascending order, consists of the Dileo Coal Member, Dalton ern Arizona, but it also includes adjacent parts of north­ Sandstone Member, Bartlett Barren Member, and Gibson western New Mexico, southeastern Utah, and southwestern Coal Member. The upper part of the Mancos Shale is re­ Colorado. placed laterally by marginal marine and continental deposits Cretaceous rocks crop out primarily in two large areas­ into which two conspicuous tongues of Mancos Shale wedge San Juan Basin and Black Mesa-in the eastern and central out to the southwest. The lower, Mulatto Tongue of the parts of the Navajo country, respectively. These rocks are as Mancos wedges out into the Crevasse Canyon Formation. The much as 6,500 feet thick in the San Juan Basin and are about upper shale body-the Satan Tongue-lies above the Hosta 1,500 feet thick on Black Mesa. At several other places in the Tongue of the Point Lookout Sandstone, and where the Satan mapped area are thin isolated 1·emnants of Cretaceous rock. Tongue wedges out, the Hosta joins the main body of the The Lower Cretaceous Burro Canyon Formation, as much Point Lookout Sandstone. as 200 feet thick, is the oldest Cretaceous unit in the Navajo country. It occurs in a very limited area of extrem~ south­ On Black Mesa the Mancos Shale is as much as
Recommended publications
  • Emerging Oil and Gas Development in Northwestern New Mexico HORIZONTAL GALLUP / MANCOS PLAY
    Emerging Oil and Gas Development in Northwestern New Mexico HORIZONTAL GALLUP / MANCOS PLAY Gallup / Mancos Oil Play Northwestern New Mexico Bob Just, Petroleum Geologist, Ron Lloyd, Petroleum Geologist Robert Anderson, Branch Chief / Petroleum Geophysicist Assistant Secretary – Indian Affairs, Division of Energy and Mineral Development Introduction of the EnCana well have had cumulative production ranging from around 7,800 to 21,000 barrels of oil A new oil exploration play is beginning to develop and 114 million to 345 million cubic feet of gas. These in Sandoval and San Juan Counties, New Mexico. A production values are relatively poor except that Calgary based company (with offices in Denver, CO), water production is low, ranging from 1,000 to 3,400 Encana Oil and Gas (Encana) has recently horizontally barrels cumulative. It appears the horizontal portion drilled and produced oil from the Cretaceous age of the EnCana well is in the same zone as the older Gallup sandstone. These wells offset unleased Navajo vertical wells. allotted lands and it is anticipated that Encana and other oil and gas companies will be very interested in leasing Navajo allotment tracts as soon as possible. Early Play Development and Reported Results One of Encana’s wells, the Lybrook #H36-2307 (located in se se 32-23n- 7w, Figure 1) was reported flowing at a rate of 838 mcfgpd (natural gas) and 786 bopd (oil) from a lateral leg in the Gallup sandstone formation. Daily production through the initial 30-day period was around 440 barrels of oil per day. This well is a horizontal well with a 4,100 foot lateral section.
    [Show full text]
  • Ron Blakey, Publications (Does Not Include Abstracts)
    Ron Blakey, Publications (does not include abstracts) The publications listed below were mainly produced during my tenure as a member of the Geology Department at Northern Arizona University. Those after 2009 represent ongoing research as Professor Emeritus. (PDF) – A PDF is available for this paper. Send me an email and I'll attach to return email Blakey, R.C., 1973, Stratigraphy and origin of the Moenkopi Formation of southeastern Utah: Mountain Geologist, vol. 10, no. 1, p. 1 17. Blakey, R.C., 1974, Stratigraphic and depositional analysis of the Moenkopi Formation, Southeastern Utah: Utah Geological Survey Bulletin 104, 81 p. Blakey, R.C., 1977, Petroliferous lithosomes in the Moenkopi Formation, Southern Utah: Utah Geology, vol. 4, no. 2, p. 67 84. Blakey, R.C., 1979, Oil impregnated carbonate rocks of the Timpoweap Member Moenkopi Formation, Hurricane Cliffs area, Utah and Arizona: Utah Geology, vol. 6, no. 1, p. 45 54. Blakey, R.C., 1979, Stratigraphy of the Supai Group (Pennsylvanian Permian), Mogollon Rim, Arizona: in Carboniferous Stratigraphy of the Grand Canyon Country, northern Arizona and southern Nevada, Field Trip No. 13, Ninth International Congress of Carboniferous Stratigraphy and Geology, p. 89 109. Blakey, R.C., 1979, Lower Permian stratigraphy of the southern Colorado Plateau: in Four Corners Geological Society, Guidebook to the Permian of the Colorado Plateau, p. 115 129. (PDF) Blakey, R.C., 1980, Pennsylvanian and Early Permian paleogeography, southern Colorado Plateau and vicinity: in Paleozoic Paleogeography of west central United States, Rocky Mountain Section, Society of Economic Paleontologists and Mineralogists, p. 239 258. Blakey, R.C., Peterson, F., Caputo, M.V., Geesaman, R., and Voorhees, B., 1983, Paleogeography of Middle Jurassic continental, shoreline, and shallow marine sedimentation, southern Utah: Mesozoic PaleogeogÂraphy of west central United States, Rocky Mountain Section of Society of Economic Paleontologists and Mineralogists (Symposium), p.
    [Show full text]
  • Hydrogeology and Stratigraphy of the Dakota Formation in Northwest Iowa
    WATER SUPPLY HYDROGEOLOGY AND J.A. MUNTER BULLETIN G.A. LUDVIGSON NUMBER 13 STRATIGRAPHY OF THE B.J. BUNKER 1983 DAKOTA FORMATION IN NORTHWEST IOWA Iowa Geological Survey Donald L. Koch State Geologist and Director 123 North Capitol Street Iowa City, Iowa 52242 IOWA GEOLOGICAL SURVEY WATER-SUPPLY BULLETIN NO. 13 1983 HYDROGEOLOGY AND STRATIGRAPHY OF THE DAKOTA FORMATION IN NORTHWEST IOWA J. A. Munter G. A. Ludvigson B. J. Bunker Iowa Geological Survey Iowa Geological Survey Donald L. Koch Director and State Geologist 123 North Capitol Street Iowa City, Iowa 52242 Foreword An assessment of the quantity and quality of water available from the Dakota (Sandstone) Formation 1n northwest Iowa is presented in this report. The as sessment was undertaken to provide quantitative information on the hydrology of the Dakota aquifer system to the Iowa Natural Resources Council for alloca tion of water for irrigation, largely as a consequence of the 1976-77 drought. Most area wells for domestic, livestock, and irrigation purposes only partial ly penetrated the Dakota Formation. Consequently, the long-term effects of significant increases in water withdrawals could not be assessed on the basis of existing wells. Acquisition of new data was based upon a drilling program designed to penetrate the entire sequence of Dakota sediments at key loca tions, after a thorough inventory and analysis of existing data. Definition of the distribution, thickness, and lateral and vertical changes in composition of the Dakota Formation has permitted the recognition of two mem bers. Additionally, Identification of the rock units that underlie the Dakota Formation has contributed greatly to our knowledge of the regional geology of northwest Iowa and the upper midwest.
    [Show full text]
  • Variability of Nanopore Systems in the Lincoln Limestone, Denver-Julesburg Basin, Colorado, Usa
    VARIABILITY OF NANOPORE SYSTEMS IN THE LINCOLN LIMESTONE, DENVER-JULESBURG BASIN, COLORADO, USA By Brandon Franklin Werner Chase B.A., University of Colorado, Boulder, 2016 Undergraduate Thesis submitted to the Faculty of the Undergraduate School of the University of Colorado’s Department of Geological Sciences 2016 Committee: David Budd – Geological Sciences – Advisor Charles Stern – Geological Sciences Tyler Lansford - Classics ABSTRACT: With a shift to exploiting unconventional petroleum plays in the United States to support energy consumption, understanding the nanopore systems in those unconventional resources becomes important for future exploitation. The goal of this study is to characterize the pore systems of the Cretaceous Lincoln Limestone found in the Denver-Julesburg (DJ) Basin in order to test the hypothesis that lithologic variability has a control on pore characteristics and total porosity. The Lincoln Limestone represents a possible reservoir interval in close proximity to a source interval, the Hartland Shale, which directly overlies it, thus making it a potentially profitable future exploration target. Pore networks in the Lincoln were characterized using AR-milled rock surfaces run through a scanning electron microscope (SEM) for image capture, image analysis with Avizio 9 software, and mineralogical characterization by X- Ray fluorescence (XRF). Seven samples were chosen for analysis from a single core taken from one well in the DJ basin. Five of the samples span the roughly 70-90 ft thick Lincoln Limestone and the other two come from right above and right below the Lincoln. The seven samples span the range of lithologic and porosity variability in the Lincoln Limestone. They have normalized volumes of carbonate that range from 6.0% to 70.6% (mostly as calcite); clay content ranges from 14.8% to 55.2%.
    [Show full text]
  • 26 Petroleum Geology of the Basal Niobrara Sandstone
    PETROLEUM GEOLOGY OF THE BASAL NIOBRARA SANDSTONE WEST PUERTO CHIQUITO FIELD RIO ARRIBA COUNTY NEW MEXICO USA By Thomas A. Arthur 26 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: Thomas A. Arthur Signed: Dr. Stephen A. Sonnenberg Thesis Advisor Golden, Colorado Date ____________ Signed: Dr. John D. Humphrey, Department Head Department of Geology and Geological Engineering ii ABSTRACT The basal Niobrara sandstone in the eastern San Juan Basin is an important oil producing reservoir. The West Puerto Chiquito (WPC) Field has produced approximately 18 million barrels of oil from Fort Hays age equivalent sandstones. Most of the Late Cretaceous oil producing stratigraphic traps that have been identified in the Rocky Mountain region are associated with unconformities. The boundary between the Carlile Shale and Niobrara is a well- known regional unconformity that has been extensively studied on the west side of the San Juan Basin in association with large oil fields such as Bisti and Horseshoe. A study of well log correlation, outcrop, core and source rock analysis was conducted in order to identify the resource potential of the Niobrara sandstone in the eastern part of the San Juan Basin. The Niobrara Sandstone is encased within 2000 feet of organic-rich, thermally mature Mancos source rock. Core analyses, including petrographic thin sections help to characterize the porosity and permeability of this tight reservoir. Surface lineaments were studied in order to identify reservoir connectivity.
    [Show full text]
  • Basin-Margin Depositional Environments of the Fort Union and Wasatch Formations in the Buffalo-Lake De Smet Area, Johnson County, Wyoming
    U.S. DEPARTMENT OF INTERIOR GEOLOGICAL SURVEY Basin-Margin Depositional Environments of the Fort Union and Wasatch Formations in the Buffalo-Lake De Smet area, Johnson County, Wyoming By Stanley L. Obernyer Open-File Report 79-712 1979 Contents Page Abstract 1 Introduction 5 Methods of investigation 8 Previ ous work - 9 General geol ogy 10 Acknowledgments 16 Descriptive stratigraphy of the Fort Union and Wasatch Formations 18 Fort Union Formation- 18 Lower member 20 Conglomerate member 21 Wasatch Formation 30 Kingsbury Conglomerate Member 32 Moncrief Member 38 Coal-bearing strata Wasatch Formation 45 Conglomeratic sandstone sequence 46 The Lake De Smet coal bed 53 Very fine to medium-grained sandstone sequence 69 Fossil marker beds 78 Environments of Deposition 79 General 79 Alluvial fan environment 82 Braided stream environments 86 Alluvial valley environments 89 Tectonics and Sedimentation 92 Conglomerates and tectonics- 92 Coals and tectonics 98 Conclusions 108 References 111 11 ILLUSTRATIONS Plates Plate 1. Bedrock geologic map of the Buffalo-Lake De Smet area, Johnson County, Wyoming In pocket 2. Geologic cross sections along the Bighorn Mountain Front, Buffalo-Lake De Smet area, Johnson County, Wyoming In pocket FIGURES Page Figure 1. Location map sh wing the major structural units surround­ ing the Powder River Basin, Wyoming and Montana 7 2. Composite geologic section of the rocks exposed in in the Buffalo-Lake De Smet area- 11 3. Generalized geologic map of the Powder River Basin 12 4. Isopach map of the Fort Union and Wasatch Formations, Powder River Basin, from Curry (1971) 14 5. Generalized stratigraphic column of the conglomerate sequences 19 6.
    [Show full text]
  • 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 ................
    [Show full text]
  • Geologic Map and Upper Paleozoic Stratigraphy of the Marble Canyon Area, Cottonwood Canyon Quadrangle, Death Valley National Park, Inyo County, California
    Geologic Map and Upper Paleozoic Stratigraphy of the Marble Canyon Area, Cottonwood Canyon Quadrangle, Death Valley National Park, Inyo County, California By Paul Stone, Calvin H. Stevens, Paul Belasky, Isabel P. Montañez, Lauren G. Martin, Bruce R. Wardlaw, Charles A. Sandberg, Elmira Wan, Holly A. Olson, and Susan S. Priest Pamphlet to accompany Scientific Investigations Map 3298 2014 U.S. Department of the Interior U.S. Geological Survey Cover View of Marble Canyon area, California, showing dark rocks of Mississippian Indian Springs Formation and Pennsylvanian Bird Spring Formation overlying light rocks of Mississippian Santa Rosa Hills Limestone in middle distance. View is southeast toward Emigrant Wash and Tucki Mountain in distance. U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2014 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Suggested citation: Stone, P., Stevens, C.H., Belasky, P., Montanez, I.P., Martin, L.G., Wardlaw, B.R., Sandberg, C.A., Wan, E., Olson, H.A., and Priest, S.S., 2014, Geologic map and upper Paleozoic stratigraphy of the Marble Canyon area, Cottonwood Canyon quadrangle, Death Valley National Park, Inyo County, California: U.S. Geological Survey Scientific Investigations Map 3298, scale 1:24,000, 59 p., http://dx.doi.org/10.3133/sim3298.
    [Show full text]
  • At Carowinds
    at Carowinds EDUCATOR’S GUIDE CLASSROOM LESSON PLANS & FIELD TRIP ACTIVITIES Table of Contents at Carowinds Introduction The Field Trip ................................... 2 The Educator’s Guide ....................... 3 Field Trip Activity .................................. 4 Lesson Plans Lesson 1: Form and Function ........... 6 Lesson 2: Dinosaur Detectives ....... 10 Lesson 3: Mesozoic Math .............. 14 Lesson 4: Fossil Stories.................. 22 Games & Puzzles Crossword Puzzles ......................... 29 Logic Puzzles ................................. 32 Word Searches ............................... 37 Answer Keys ...................................... 39 Additional Resources © 2012 Dinosaurs Unearthed Recommended Reading ................. 44 All rights reserved. Except for educational fair use, no portion of this guide may be reproduced, stored in a retrieval system, or transmitted in any form or by any Dinosaur Data ................................ 45 means—electronic, mechanical, photocopy, recording, or any other without Discovering Dinosaurs .................... 52 explicit prior permission from Dinosaurs Unearthed. Multiple copies may only be made by or for the teacher for class use. Glossary .............................................. 54 Content co-created by TurnKey Education, Inc. and Dinosaurs Unearthed, 2012 Standards www.turnkeyeducation.net www.dinosaursunearthed.com Curriculum Standards .................... 59 Introduction The Field Trip From the time of the first exhibition unveiled in 1854 at the Crystal
    [Show full text]
  • Rule Booklet
    Dig for fossils, build skeletons, and attract the most visitors to your museum! TM SCAN FOR VIDEO RULES AND MORE! FOSSILCANYON.COM Dinosaurs of North America edimentary rock formations of western North America are famous for the fossilized remains of dinosaurs The rules are simple enough for young players, but and other animals from the Triassic, Jurassic, and serious players can benefit Cretaceous periods of the Mesozoic Era. Your objective from keeping track of the cards that is to dig up fossils, build complete skeletons, and display have appeared, reasoning about them in your museum to attract as many visitors as possible. probabilities and expected returns, and choosing between aggressive Watch your museum’s popularity grow using jigsaw-puzzle and conservative plays. scoring that turns the competition into a race! GAME CONTENTS TM 200,000300,000 160,000 VISITORS VISITORS PER YEAR 140,000 VISITORS PER YEAR 180,000 VISITORS PER YEAR 400,000 VISITORS PER YEAR Dig for fossils, build skeletons, and 340,000 VISITORS PER YEAR RD COLOR ELETONS CA GENUS PERIODDIET SK FOSSIL VISITORSPARTS 360,000 VISITORS PER YEAR PER YEAR attract the most visitors to your museum! VISITORS PER YEAR PER YEAR Tyrannosaurus K C 1 4 500,000 Brachiosaurus J H 1 3 400,000 ON YOUR TURN: TM SCAN FOR VIDEO Triceratops K H 1 3 380,000 RULES AND MORE! Allosaurus J C 2 Dig3 a first360,000 card. If it is a fossil, keep it hidden. FOSSILCANYON.COM Ankylosaurus K H 2 If it3 is an340,000 action card, perform the action.
    [Show full text]
  • 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]
  • The Cretaceous System in Central Sierra County, New Mexico
    The Cretaceous System in central Sierra County, New Mexico Spencer G. Lucas, New Mexico Museum of Natural History, Albuquerque, NM 87104, [email protected] W. John Nelson, Illinois State Geological Survey, Champaign, IL 61820, [email protected] Karl Krainer, Institute of Geology, Innsbruck University, Innsbruck, A-6020 Austria, [email protected] Scott D. Elrick, Illinois State Geological Survey, Champaign, IL 61820, [email protected] Abstract (part of the Dakota Formation, Campana (Fig. 1). This is the most extensive outcrop Member of the Tres Hermanos Formation, area of Cretaceous rocks in southern New Upper Cretaceous sedimentary rocks are Flying Eagle Canyon Formation, Ash Canyon Mexico, and the exposed Cretaceous sec- Formation, and the entire McRae Group). A exposed in central Sierra County, southern tion is very thick, at about 2.5 km. First comprehensive understanding of the Cretaceous New Mexico, in the Fra Cristobal Mountains, recognized in 1860, these Cretaceous Caballo Mountains and in the topographically strata in Sierra County allows a more detailed inter- pretation of local geologic events in the context strata have been the subject of diverse, but low Cutter sag between the two ranges. The ~2.5 generally restricted, studies for more than km thick Cretaceous section is assigned to the of broad, transgressive-regressive (T-R) cycles of 150 years. (ascending order) Dakota Formation (locally deposition in the Western Interior Seaway, and includes the Oak Canyon [?] and Paguate also in terms of Laramide orogenic
    [Show full text]