The Geology of the Central Part of the Favant Range, Utah
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UMNP Mountains Manual 2017
Mountain Adventures Manual utahmasternaturalist.org June 2017 UMN/Manual/2017-03pr Welcome to Utah Master Naturalist! Utah Master Naturalist was developed to help you initiate or continue your own personal journey to increase your understanding of, and appreciation for, Utah’s amazing natural world. We will explore and learn aBout the major ecosystems of Utah, the plant and animal communities that depend upon those systems, and our role in shaping our past, in determining our future, and as stewards of the land. Utah Master Naturalist is a certification program developed By Utah State University Extension with the partnership of more than 25 other organizations in Utah. The mission of Utah Master Naturalist is to develop well-informed volunteers and professionals who provide education, outreach, and service promoting stewardship of natural resources within their communities. Our goal, then, is to assist you in assisting others to develop a greater appreciation and respect for Utah’s Beautiful natural world. “When we see the land as a community to which we belong, we may begin to use it with love and respect.” - Aldo Leopold Participating in a Utah Master Naturalist course provides each of us opportunities to learn not only from the instructors and guest speaKers, But also from each other. We each arrive at a Utah Master Naturalist course with our own rich collection of knowledge and experiences, and we have a unique opportunity to share that Knowledge with each other. This helps us learn and grow not just as individuals, but together as a group with the understanding that there is always more to learn, and more to share. -
Eocene Red Beds from NE Iraq: Constraints from Framework Petrography Muatasam M
University of Wollongong Research Online Faculty of Science, Medicine and Health - Papers Faculty of Science, Medicine and Health 2014 Provenance of Paleocene - Eocene red beds from NE Iraq: constraints from framework petrography Muatasam M. Hassan University of Wollongong, [email protected] Brian Jones University of Wollongong, [email protected] Solomon Buckman University of Wollongong, [email protected] Ali Ismael Al-Jubory Mosul University Fahad M. Al Gahtani University of Wollongong, [email protected] Publication Details Hassan, M. Mahmood., Jones, B. G., Buckman, S., Al-Jubory, A. & Al Gahtani, F. Mubarak. (2014). Provenance of Paleocene - Eocene red beds from NE Iraq: constraints from framework petrography. Geological Magazine, 151 (6), 1034-1050. Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Provenance of Paleocene - Eocene red beds from NE Iraq: constraints from framework petrography Abstract The er d-bed deposits in northern Iraq are situated in an active foreland basin adjacent to the Zagros Orogenic Belt, bound to the north by the Iranian plate thrust over the edge of the Arabian plate. The er d-bed successions are composed of alternating red and brown silty mudstones, purplish red calcareous siltstone, fine- ot coarse- grained pebbly sandstone and conglomerate. The er d beds in the current study can be divided into four parts showing a trend of upward coarsening with fine-grained deposits at the top. A detailed petrographic study was carried out on the sandstone units. The clastic rocks consist mainly of calcite cemented litharenite with rock fragments (volcanic, metamorphic and sedimentary), quartz and minor feldspar. -
Geology and Mineral Resources of Sierra Nacimiento and Vicinity, New
iv Contents ABSTRACT 7 TERTIARY-QUATERNARY 47 INTRODUCTION 7 QUATERNARY 48 LOCATION 7 Bandelier Tuff 48 PHYSIOGRAPHY 9 Surficial deposits 48 PREVIOUS WORK 9 PALEOTECTONIC SETTING 48 ROCKS AND FORMATIONS 9 REGIONAL TECTONIC SETTING 49 PRECAMBRIAN 9 STRUCTURE 49 Northern Nacimiento area 9 NACIMIENTO UPLIFT 49 Southern Nacimiento area 15 Nacimiento fault 51 CAMBRIAN-ORDOVICIAN (?) 20 Pajarito fault 52 MISSISSIPPIAN 20 Synthetic reverse faults 52 Arroyo Peñasco Formation 20 Eastward-trending faults 53 Log Springs Formation 21 Trail Creek fault 53 PENNSYLVANIAN 21 Antithetic reverse faults 53 Osha Canyon Formation 23 Normal faults 53 Sandia Formation 23 Folds 54 Madera Formation 23 SAN JUAN BASIN 55 Paleotectonic interpretation 25 En echelon folds 55 PERMIAN 25 Northeast-trending faults 55 Abo Formation 25 Synclinal bend 56 Yeso Formation 27 Northerly trending normal faults 56 Glorieta Sandstone 30 Antithetic reverse faults 56 Bernal Formation 30 GALLINA-ARCHULETA ARCH 56 TRIASSIC 30 CHAMA BASIN 57 Chinle Formation 30 RIΟ GRANDE RIFT 57 JURASSIC 34 JEMEZ VOLCANIC FIELD 59 Entrada Sandstone 34 TECTONIC EVOLUTION 60 Todilto Formation 34 MINERAL AND ENERGY RESOURCES 63 Morrison Formation 34 COPPER 63 Depositional environments 37 Mineralization 63 CRETACEOUS 37 Origin 67 Dakota Formation 37 AGGREGATE 69 Mancos Shale 39 TRAVERTINE 70 Mesaverde Group 40 GYPSUM 70 Lewis Shale 41 COAL 70 Pictured Cliffs Sandstone 41 ΗUMΑTE 70 Fruitland Formation and Kirtland Shale URANIUM 70 undivided 42 GEOTHERMAL ENERGY 72 TERTIARY 42 OIL AND GAS 72 Ojo Alamo Sandstone -
New Approaches to Understanding the Mechanics of Burgess Shale-Type Deposits: from the Micron Scale to the Global Picture Robert Gaines Pomona College
Claremont Colleges Scholarship @ Claremont Pomona Faculty Publications and Research Pomona Faculty Scholarship 1-1-2005 New Approaches to Understanding the Mechanics of Burgess Shale-type Deposits: From the Micron Scale to the Global Picture Robert Gaines Pomona College Mary L. Droser University of California - Riverside Recommended Citation Gaines, R.R., and Droser, M.L., 2005, New Approaches to Understanding the Mechanics of Burgess Shale-type Deposits: From the Micron Scale to the Global Picture, The eS dimentary Record, v. 3, n. 2, p. 4-8. http://www.sepm.org/pages.aspx?pageid=37 This Article is brought to you for free and open access by the Pomona Faculty Scholarship at Scholarship @ Claremont. It has been accepted for inclusion in Pomona Faculty Publications and Research by an authorized administrator of Scholarship @ Claremont. For more information, please contact [email protected]. The Sedimentary Record platforms, at sharp shelf-slope breaks (Conway New Approaches to Morris, 1998; Rees, 1986). Classic models for the Burgess Shale have considered the deposi- tional environment to be fully anoxic, due to Understanding the the exquisite preservation of fossils, and the dark color of the mudrocks (e.g., Conway Morris, 1986). This implies that the faunas Mechanics of Burgess were transported, yet some assemblages of fos- sils, such as the well-known Ogygopsis trilobite beds in the Burgess Shale and horizons that Shale-type Deposits: contain delicate sponges, clearly occur in situ. Important questions, key to a first-order understanding the biotas in an ecological sense, have remained: Can discrete, paleoeco- From the Micron Scale to logically meaningful assemblages be resolved from within the homogeneous sediments? the Global Picture Were bottom water oxygen conditions suffi- Robert R. -
Stromatolites in the Todilto Formation? Dana S
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/56 Stromatolites in the Todilto Formation? Dana S. Ulmer-Scholle, 2005, pp. 380-388 in: Geology of the Chama Basin, Lucas, Spencer G.; Zeigler, Kate E.; Lueth, Virgil W.; Owen, Donald E.; [eds.], New Mexico Geological Society 56th Annual Fall Field Conference Guidebook, 456 p. This is one of many related papers that were included in the 2005 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. -
The Geology of New Mexico As Understood in 1912: an Essay for the Centennial of New Mexico Statehood Part 2 Barry S
Celebrating New Mexico's Centennial The geology of New Mexico as understood in 1912: an essay for the centennial of New Mexico statehood Part 2 Barry S. Kues, Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico, [email protected] Introduction he first part of this contribution, presented in the February Here I first discuss contemporary ideas on two fundamental areas 2012 issue of New Mexico Geology, laid the groundwork for an of geologic thought—the accurate dating of rocks and the move- exploration of what geologists knew or surmised about the ment of continents through time—that were at the beginning of Tgeology of New Mexico as the territory transitioned into statehood paradigm shifts around 1912. Then I explore research trends and in 1912. Part 1 included an overview of the demographic, economic, the developing state of knowledge in stratigraphy and paleontol- social, cultural, and technological attributes of New Mexico and its ogy, two disciplines of geology that were essential in understand- people a century ago, and a discussion of important individuals, ing New Mexico’s rock record (some 84% of New Mexico’s surface institutions, and areas and methods of research—the geologic envi- area is covered by sediments or sedimentary rocks) and which were ronment, so to speak—that existed in the new state at that time. advancing rapidly through the first decade of the 20th century. The geologic time scale and age of rocks The geologic time scale familiar to geologists working in New The USGS did not adopt the Paleocene as the earliest epoch of the Mexico in 1912 was not greatly different from that used by modern Cenozoic until 1939. -
Revision of the Lower Part of the Tertiary System in the Central and \Vestern Uinta Basin, Utah______
Revision of the Lower Part of the Tertiary System in the Central and \Vestern Uinta Basin, Utah_____ __________ GEOLOGICAL SURVEY BULLETIN 1405G Revision of the Lower Part of the Tertiary System in the Central and \Vfestern Uinta Basin, Utah By THOMAS D. FOUCH CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1405-C Correlation of lower Tertiary stratigraphic units recently penetrated in northeastern Utah UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Fouch, Thomas D. Revision of the lower part of the Tertiary system in the central and western Uinta Basin, Utah. (Contributions to stratigraphy) (Geological Survey Bulletin 1405-C) Bibliography: p. Supt. of Docs, no.: I 19.3:1405-C 1. Geology, Stratigraphic Tertiary. 2. Geology, Stratigraphic Nomenclature Utah Uinta Basin. I. Title. II. Series. III. Series: United States Geological Survey Bulletin 1405-C. QE75.B9 No. 1405-C [QE691] 557.3'08s [ 551.7'8'0979221] 75-619374 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D. C. 20402 Stock Number 024-001-02770-4 CONTENTS Page Abstract....................................................................................................................... Cl Introduction................................................................................................................ 1 North Horn Formation ............................................................................................. -
Paleosols in an Outcrop of Red Beds from the Upper Cretaceous Yaojia
Zhang et al. Journal of Palaeogeography (2020) 9:20 https://doi.org/10.1186/s42501-020-00069-7 Journal of Palaeogeography ORIGINAL ARTICLE Open Access Paleosols in an outcrop of red beds from the Upper Cretaceous Yaojia Formation, southern Songliao Basin, Jilin Province, NE China Li Zhang1, Zhi-Dong Bao2*, Chang-Min Zhang1, Lu-Xing Dou2, Ping Fu3, Jia-Hong Zhao3, Wu-Xue Wang3 and Yu Ji3 Abstract Paleosols in an outcrop of fluvial–lacustrine red beds have been recognized in the Upper Cretaceous Yaojia Formation in southern Songliao Basin, Songyuan City, Jilin Province, NE China. They are recognized in the field by pedogenic features, including root traces and burrows, soil horizons and soil structures. Root traces are remnants of small herbaceous plants, elongating and branching downwards in the red paleosols. They are filled by calcite, analcime, and clay minerals in spaces created by the decay of the plant roots. Burrows are found near the root traces with backfilled cells made by soil-dwelling insects. Soil horizons include calcic horizons (Bk horizon) with continuous calcareous layers, argillic horizons (Bt horizon) with clay films and dark brown to black iron-manganese cutans, vertic horizons (Bw horizon) with slickensided claystone, and deformed soil structure and gleyed horizons (Bg horizon) with mottles and reticulate mottles. Soil structures of the paleosols include pseudo-anticlinal structures, subangular blocky structures, and angular blocky structures. The micro-pedogenesis characteristics are also observed, including micrite pedogenic minerals and clay skins. Based on the pedogenic features above, paleosols types including Aridisol, Alfisol, and Vertisol are interpreted in the red beds of the Yaojia Formation. -
Scipio Irrigation Company Ivie Creek Pipeline Project - Watersmart
Draft Environmental Assessment Scipio Irrigation Company Ivie Creek Pipeline Project - WaterSMART PRO-EA-16-026 Upper Colorado Region Provo Area Office Provo, Utah U.S. Department of the Interior Bureau of Reclamation Provo Area Office Provo, Utah May 2017 Mission Statements The mission of the Department of the Interior protects and manages the Nation’s natural resources and cultural heritage; provides scientific and other information about those resources; and honors its trust responsibilities or special commitments to American Indians, Alaska Natives, and affiliated island communities. The mission of the Bureau of Reclamation is to manage, develop, and protect water and related resources in an environmentally and economically sound manner in the interest of the American public. Draft Environmental Assessment Scipio Irrigation Company Ivie Creek Pipeline Project – WaterSMART Upper Colorado Region Provo Area Office Provo, Utah Interdisciplinary Team Leader Jared Baxter Bureau of Reclamation Provo Area Office 302 East 1860 South Provo, UT 84606 801-379-1081 [email protected] U.S. Department of the Interior Bureau of Reclamation Provo Area Office Provo, Utah May 2017 Contents Page Chapter 1 Purpose of and Need for Proposed Action ...................................... 1 1.1 Introduction .......................................................................................... 1 1.2 Background .......................................................................................... 1 1.3 Purpose of and Need for Proposed Action .......................................... -
A History of Beaver County, Utah Centennial County History Series
A HISTORY OF 'Beaver County Martha Sonntag Bradley UTAH CENTENNIAL COUNTY HISTORY SERIES A HISTORY OF 'Beaver County Martha Sonntag Bradley The settlement of Beaver County began in February 1856 when fifteen families from Parowan moved by wagon thirty miles north to Beaver Valley. The county was created by the Utah legislature on 31 January 1856, a week before the Parowan group set out to make their new home. However, centuries before, prehistoric peoples lived in the area, obtaining obsidian for arrow and spear points from the Mineral Mountains. Later, the area became home to Paiute Indians. Franciscan Friars Dominguez and Escalante passed through the area in October 1776. The Mormon settlement of Beaver devel oped at the foot of the Tushar Mountains. In 1859 the community of Minersville was es tablished, and residents farmed, raised live stock, and mined the lead deposits there. In the last quarter of the nineteenth century the Mineral Mountains and other locations in the county saw extensive mining develop ment, particularly in the towns of Frisco and Newhouse. Mining activities were given a boost with the completion of the Utah South ern Railroad to Milford in 1880. The birth place of both famous western outlaw Butch Cassidy and inventor of television Philo T. Farnsworth, Beaver County is rich in history, historic buildings, and mineral treasures. ISBN: 0-913738-17-4 A HISTORY OF 'Beaver County A HISTORY OF Beaver County Martha Sonntag Bradley 1999 Utah State Historical Society Beaver County Commission Copyright © 1999 by Beaver County Commission All rights reserved ISBN 0-913738-17-4 Library of Congress Catalog Card Number 98-61325 Map by Automated Geographic Reference Center—State of Utah Printed in the United States of America Utah State Historical Society 300 Rio Grande Salt Lake City, Utah 84101-1182 Contents ACKNOWLEDGMENTS vii GENERAL INTRODUCTION ix CHAPTER 1 Beaver County: The Places That Shape Us . -
This Article Appeared in a Journal Published by Elsevier. the Attached Copy Is Furnished to the Author for Internal Non-Commerci
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Palaeogeography, Palaeoclimatology, Palaeoecology 264 (2008) 100–122 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Microstratigraphy, trilobite biostratinomy, and depositional environment of the “Lower Cambrian” Ruin Wash Lagerstätte, Pioche Formation, Nevada Mark Webster a,⁎, Robert R. Gaines b, Nigel C. Hughes c a Department of the Geophysical Sciences, University of Chicago, 5734 South Ellis Avenue, Chicago, IL 60637, United States b Geology Department, Pomona College, 185 E. Sixth Street, Claremont, CA 91711, United States c Department of Earth Sciences, University of California, Riverside, CA 92521, United States ARTICLE INFO ABSTRACT Article history: The uppermost 43 cm of Dyeran strata at the Ruin Wash Lagerstätte (Chief Range, Lincoln County, Nevada) Received 13 November 2007 contain nonmineralized invertebrates and exceptionally preserved, articulated olenelloid trilobites. However, Received in revised form 4 March 2008 the environmental factors responsible for the preservation of olenelloids in this unusual state at Ruin Wash Accepted 3 April 2008 have received little study and are therefore poorly understood. -
Dinosaur Eggshells from the Lower Maastrichtian St. Mary River Formation of Southern Alberta, Canada
Canadian Journal of Earth Sciences Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern Alberta, Canada Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2017-0195.R1 Manuscript Type: Article Date Submitted by the Author: 13-Nov-2017 Complete List of Authors: Voris, Jared; University of Calgary, Geoscience; Zelenitsky, Darla; Department of Geoscience, Tanaka, Kohei; Nagoya Daigaku Hakubutsukan; University of Calgary, DepartmentDraft of Geoscience Therrien, François; Royal Tyrrell Museum of Palaeontology, Is the invited manuscript for consideration in a Special N/A Issue? : Keyword: eggshell, dinosaur, Cretaceous, Maastrichtian, Alberta https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 47 Canadian Journal of Earth Sciences 1 2 3 4 5 6 7 8 9 Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern 10 Alberta, Canada 11 12 Jared T. Voris, Darla K. Zelenitsky,Draft François Therrien, Kohei Tanaka 13 J. T. Voris, D. K. Zelenitsky, and K. Tanaka. Department of Geoscience, University of 14 Calgary, 2500 University Dr. NW, Calgary, AB T2N 1N4, Canada; [email protected], 15 [email protected], [email protected] 16 K. Tanaka. Nagoya University Museum, Nagoya University Furocho, Chikusa-Ku, Nagoya, 17 464-8601, Japan; [email protected] 18 F. Therrien. Royal Tyrrell Museum of Palaeontology, Box 7500, Drumheller, AB T0J 0Y0, 19 Canada.; [email protected] 20 1 https://mc06.manuscriptcentral.com/cjes-pubs Canadian Journal of Earth Sciences Page 2 of 47 1 2 Abstract–North America is known for its rich uppermost Cretaceous record of dinosaur egg 3 remains, although a notable fossil gap exists during the lower Maastrichtian.