BRIGHAM YOUNG UNIVERSITY GEOLOGY STUDIES Volume 42, Part I, 1997
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Triangulation in Utah 1871-1934
UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Bulletin 913 TRIANGULATION IN UTAH 1871-1934 J. G. STAACK Chief Topographic Engineer UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON: 1940 Tor sale by the Superintendent of Documents, Washington, D. C. Price 20 cents (paper) CONTENTS Page Introduction ______________________________________________________ 1 Scope of report------__-_-_---_----_------------ --__---__ _ 1 Precision __ _ ________________________ _ __________________ _ ___ 1 Instruments used._ _ _ _ _ _ _ _ _ 2 Station marks___- _ _.__ __ __ _ 2 Datum_-_-_-__ __________________________ ______ ______-___.__ 3 Methods of readjustment..._____.-.__..________.___._._...___.__ 4 Form of results__-.________________________ _.___-_____.______ 5 Arrangement__.______________________________ _ ___ _ ________ 6 Descriptions of stations._______________________________________ 6 Azimuths and distances.__ ____-_.._---_--_________ -____ __ __ ^ 7 Maps.__----__-----_-_---__-_--_-___-_-___-__-__-_-_-___.-.__ 7 Personnel_ _ __-----_-_-_---_---------_--__-____-__-_.--_.___ . 7 Projects 9 Uinta Forest Reserve, 1897-98_ 9 Cottonwood and Park City special quadrangles, 1903____ _ 19 Iron Springs special quadrangle, 1905____________________________ 22 Northeastern Utah, 1909.. -_. 26 Eastern Utah, 1910 - . 30 Logan quadrangle, 1913._________-__-__'_--______-___:_____.____ 42 Uintah County, 1913___-__. 48 Eastern Utah, 1914.. ... _ _ .. 55 Northern Utah, 1915 (Hodgeson)_____-___ __-___-_-_-__-_--. _. 58 Northern Utah, 1915 <Urquhart)_. -
Inventory, Assessment and Preliminary Management Planning for Utah’S Sovereign Land Along the Bear River
INVENTORY, ASSESSMENT AND PRELIMINARY MANAGEMENT PLANNING FOR UTAH’S SOVEREIGN LAND ALONG THE BEAR RIVER Plan B Thesis Project Matthew Coombs, M.S. Bioregional Planning Utah State University College of Natural Resources Department of Environment and Society 2017 ii Copyright © Matthew S. Coombs 2017 All Rights Reserved Maps throughout this document were created using ArcGIS® software by Esri. ArcGIS® and ArcMap™ are the intellectual property of Esri and are used herein under license. Copyright © Esri. All rights reserved. For more information about Esri® software, please visit www.esri.com. iii ABSTRACT Inventory, Assessment and Preliminary Management Planning for Utah’s Sovereign Land along the Bear River by Matthew S. Coombs, Master of Science in Bioregional Planning Utah State University, 2017 Major Professor: Richard E. Toth Department: Environment and Society The Utah Division of Forestry, Fire and State Lands (FFSL) is responsible for the management of state-owned sovereign land in Utah, which includes the bed and banks of the Bear River in Cache and Box Elder Counties. The purpose of this project is to provide relevant background information and data to support the future development of a comprehensive management plan for the Bear River. This project develops a methodology and process to describe the Bear River Corridor, summarizes and integrates existing information regarding important biophysical and socio- cultural attributes of the river, delineates lands along the river into identified management classes, and recommends management goals and objectives to be carried forward into the future development of a comprehensive management plan. While this project is not the most comprehensive or detailed report for any individual attribute of the Bear River, it is currently the most comprehensive resource addressing sovereign lands along the Bear River. -
The Spence Shale Lagerstätte: an Important Window Into Cambrian Biodiversity
Downloaded from http://jgs.lyellcollection.org/ by guest on September 24, 2021 Accepted Manuscript Journal of the Geological Society The Spence Shale Lagerstätte: an Important Window into Cambrian Biodiversity Julien Kimmig, Luke C. Strotz, Sara R. Kimmig, Sven O. Egenhoff & Bruce S. Lieberman DOI: https://doi.org/10.1144/jgs2018-195 Received 31 October 2018 Revised 21 February 2019 Accepted 28 February 2019 © 2019 The Author(s). This is an Open Access article distributed under the terms of the Creative Commons Attribution 4.0 License (http://creativecommons.org/licenses/by/4.0/). Published by The Geological Society of London. Publishing disclaimer: www.geolsoc.org.uk/pub_ethics Supplementary material at https://doi.org/10.6084/m9.figshare.c.4423145 To cite this article, please follow the guidance at http://www.geolsoc.org.uk/onlinefirst#cit_journal Downloaded from http://jgs.lyellcollection.org/ by guest on September 24, 2021 The Spence Shale Lagerstätte: an Important Window into Cambrian Biodiversity 1* 1,2 1,3 4 1,2 Julien Kimmig , Luke C. Strotz , Sara R. Kimmig , Sven O. Egenhoff & Bruce S. Lieberman 1Biodiversity Institute, University of Kansas, Lawrence, KS 66045, USA 2 Department of Ecology & Evolutionary Biology, University of Kansas, Lawrence, KS, USA 3Pacific Northwest National Laboratory, Richland, WA 99354, USA 4Department of Geosciences, Colorado State University, Fort Collins, CO 80523, USA *Correspondence: [email protected] Abstract: The Spence Shale Member of the Langston Formation is a Cambrian (Miaolingian: Wuliuan) Lagerstätte in northeastern Utah and southeastern Idaho. It is older than the more well- known Wheeler and Marjum Lagerstätten from western Utah, and the Burgess Shale from Canada. -
Palaeoecology of the Early Cambrian Sinsk Biota from the Siberian Platform
Palaeogeography, Palaeoclimatology, Palaeoecology 220 (2005) 69–88 www.elsevier.com/locate/palaeo Palaeoecology of the Early Cambrian Sinsk biota from the Siberian Platform Andrey Yu. Ivantsova, Andrey Yu. Zhuravlevb,T, Anton V. Legutaa, Valentin A. Krassilova, Lyudmila M. Melnikovaa, Galina T. Ushatinskayaa aPalaeontological Institute, Russian Academy of Sciences, ul. Profsoyuznaya 123, Moscow 117997, Russia bA´rea y Museo de Paleontologı´a, faculdad de Ciences, Universidad de Zaragoza, C/ Pedro Cerbuna, 12, E-50009, Zaragoza, Spain Received 1 February 2002; accepted 15 January 2004 Abstract The Sinsk biota (Early Cambrian, Botoman Stage, Siberian Platform) inhabited an open-marine basin within the photic zone, but in oxygen-depleted bottom waters. Its rapid burial in a fine-grained sediment under anoxic conditions led to the formation of one of the earliest Cambrian Lagerst7tte. All the organisms of the biota were adapted to a life under dysaerobic conditions. It seems possible that the adaptations of many Cambrian organisms, which composed the trophic nucleus of the Sinsk Algal Lens palaeocommunity to low oxygen tensions allowed them to diversify in the earliest Palaeozoic, especially during the Cambrian. Nowadays these groups comprise only a negligible part of communities and usually survive in settings with low levels of competition. Nonetheless, the organization of the Algal Lens palaeocommunity was not simple, it consisted of diverse trophic guilds. The tiering among sessile filter-feeders was well developed with the upper tier at the 50 cm level. In terms of individuals, the community was dominated by sessile filter-feeders, vagrant detritophages, and diverse carnivores/scavengers. The same groups, but in slightly different order, comprised the bulk of the biovolume: vagrant epifaunal and nektobenthic carnivores/ scavengers, sessile filter-feeders, and vagrant detritophages. -
International Geological Congress, XXVII Session, Estonian Soviet Socialist Republic, Excursions: 027, 028 Guidebook
INTERNATIONAL GEOLOGICAL CONGRESS XXVII SESSION ESTONIAN SOVIET SOCIAL1ST REPUBLIC Excursions: 027, 028 Guidebook 021 A +e \ \ �� Dz \ _(,/ \ POCCHHCKAR Ct/JCP\ RUSsiAN SFSR \ y n] Dt (. - � v$&.1/ATBHHCKA f1 CCP LATV/AN SSR 02 • 3 INTERNATIONAL GEOLOGICAL CONGRESS XXVII SESSION USSR MOSCOW 1984 ESTONIAN SOVIET SOCIAL1ST REPUBLIC Excursions: 027 Hydrogeology of the Baltic 028 Geology and minerai deposits of Lower Palaeozoic of the Eastern Baltic area Guidebook Tallinn, 1984 552 G89 Prepared for the press by Institute of Geology, Academy of Sciences of the Estonian SSR and Board of Geology of the Estonian SSR Editorial board: D. Kaljo, E. Mustjõgi and I. Zekcer Authors of the guide: A. Freimanis, ü. Heinsalu, L. Hints, P. Jõgar, D. Kaljo, V. Karise, H. Kink, E. Klaamann, 0. Morozov, E. Mustjõgi, S. Mägi, H. Nestor, Y. Nikolaev, J. Nõlvak, E. Pirrus, L. Põlma, L. Savitsky, L. Vallner, V. Vanchugov Перевод с русского Титул оригинала: Эстонская советехая сочиалистичесхая Республика. Экскурсии: 027, 028. Сводный путеводителъ. Таллии, 1984. © Academy of Sciences of the Estonian SSR, 1984 INTRODUCTION The geology of the Estonian Soviet Socialist Republic (Estonia) has become the object of excursions of the International Geo logical Congress for the second time. It happened first in 1897 when the excursion of IGC visited North Estonia (and the ter ritory of the present Leningrad District) under the guidance of Academician F. Schmidt. Such recurrent interest is justi fied in view of the classical development of the Lower Pa laeozoic in our region and the results of investigations ohtained by geological institutions of the republic. The excursions of the 27th IGC are designed, firstly, to provide a review of the stratigraphy, palaeontology and lithology of the Estonian Early Palaeozoic and associated useful minerals in the light of recent investigations (excursion 028), and, secondly, to give a survey of the problerus and some results of hydrogeology in a mare extensive area of the northwestern part of the Soviet Union (excursion 027). -
Cedar Breaks National Monument
Cedar Breaks National Monument 2004 Invasive Non-Native Plant Inventory Northern Colorado Plateau Inventory and Monitoring Network Final Report April 2005 Prepared by Steven Dewey and Kimberly Andersen Utah State University Cover photo: Bromus inermis invading a small drainage in Cedar Breaks National Monument. Photo by K. A. Andersen. Cedar Breaks National Monument 2004 Invasive Non-Native Plant Inventory Northern Colorado Plateau Inventory and Monitoring Network Final Report April 2005 Prepared by Steven Dewey and Kimberly Andersen Utah State University Report prepared for: Northern Colorado Plateau Inventory and Monitoring Network, National Park Service, 2282 S. West Resource Blvd., Moab UT 84532 by Utah State University Suggested citation: Dewey, S. A. and K. A. Andersen. 2005. An Inventory of Invasive Non-native Plants in Cedar Breaks National Monument (2004) - Final Report. Prepared for the National Park Service, Northern Colorado Plateau Network by Utah State University; Plants, Soils, and Biometeorology Department; Weed Science Research Project Report No. SD0515A, 29 pp. plus appendices. FINAL REPORT Inventory of Invasive Non-native Plants Conducted during 2004 in portions of Cedar Breaks National Monument, Northern Colorado Plateau Network of the National Park Service TABLE of CONTENTS INTRODUCTION…………………………………………………………………………. 1 BACKGROUND and JUSTIFICATION…………………………………………………...1 OBJECTIVES…….…………………………………………………………………………2 METHODS………………………………………………………………………………… 2 Selection of Inventory Areas and Target Species………………………………….. 2 -
Intermountain Trails
Intermountain Trails USDA Forest Service—Intermountain Region August 2014 Volume 3, Issue 6 Forest In Focus: Uinta-Wasatch-Cache National Forest Forest Supervisor—Dave Whittekiend In this issue: The Uinta-Wasatch-Cache National Forest Forest in Focus 1 was recently recognized as the National Volunteer Program Unit of the Year. The Forest Supervisor Message forest hosted over 12,000 volunteers for a total of 83,196 hours of work. This volunteer Trail Stories workforce accomplishes a wide variety of work on the ground, from naturalist walks to Trail Stories 2 Notch Mountain trail construction and maintenance. Without Capitol this dedicated unpaid workforce, many of the Improvement Uinta-Wasatch-Cache Forest Supervisor, services our public expects and enjoys would Project Dave Whittekiend not exist. This incredible volunteer program is made possible by the dedicated and passionate National Public 3 Lands Day employees of the Uinta-Wasatch-Cache. Our volunteer coordinators are continuously making connections with people and projects. It could be linking Safety Tip dedicated hunters to a guzzler installation or showing a prospective Eagle Scout a Mount Naomi 4 trailhead in need of improvement. The UWC volunteer coordinators and the rest Wilderness of the employees on the forest are always willing to figure out how to include volunteers in managing this incredible resource we call the uinta-Wasatch-Cache National Forest. Uinta‐Wasatch‐Cache Wellsville 5 NaƟonal Forest Mountain 857 West South Jordan Parkway Wilderness South Jordan, Utah hƩp://www.fs.usda.gov/uwcnf/ High Uintas 6 Wilderness TRAIL STORIES Notch Mountain Capitol Improvement Project-see page 2 1 Notch Mountain Capitol Improvement Project Trail Stories Through the use of a State of Utah, Recreation Trails Program grant, the Heber-Kamas Ranger District has made significant improvements to the Notch Mountain Trail in the first year of the multi-year grant. -
Distribution of the Native Trees of Utah Kimball S
Brigham Young University Science Bulletin, Biological Series Volume 11 | Number 3 Article 1 9-1970 Distribution of the native trees of Utah Kimball S. Erdman Department of Biology, Slippery Rock State College, Slippery Rock, Pennsylvania Follow this and additional works at: https://scholarsarchive.byu.edu/byuscib Part of the Anatomy Commons, Botany Commons, Physiology Commons, and the Zoology Commons Recommended Citation Erdman, Kimball S. (1970) "Distribution of the native trees of Utah," Brigham Young University Science Bulletin, Biological Series: Vol. 11 : No. 3 , Article 1. Available at: https://scholarsarchive.byu.edu/byuscib/vol11/iss3/1 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Brigham Young University Science Bulletin, Biological Series by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. MU3. CCy.P. ZOOL. LIBRARY DEC 41970 Brigham Young University HARVARD Science Bulletin UNIVERSITY) DISTRIBUTION OF THE NATIVE TREES OF UTAH by Kimball S. Erdman BIOLOGICAL SERIES—VOLUME XI, NUMBER 3 SEPTEMBER 1970 BRIGHAM YOUNG UNIVERSITY SCIENCE BULLETIN BIOLOGICAL SERIES Editor: Stanley L. Welsh, Department of Botany, Brigham Young University, Provo, Utah Members of the Editorial Board: Tipton, Zoology Vernon J. Feeeon L. Anderson, Zoology Joseph R. Murdock, Botany WiLMER W. Tanner, Zoology Ex officio Members: A. Lester Allen, Dean, College of Biological and Agricultural Sciences Ernest L. Olson, Chairman, University Publications The Brigham Young University Science Bulletin, Biological Series, publishes acceptable papers, particularly large manuscripts, on all phases of biology. Separate numbers and back volumes can be purchased from Pubhcation Sales, Brigham Young University, Provo, Utah. -
Paleontological Contributions
THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS July 24, 1984 Paper 111 EXCEPTIONALLY PRESERVED NONTRILOBITE ARTHROPODS AND ANOMALOCARIS FROM THE MIDDLE CAMBRIAN OF UTAH' D. E. G. BRIGGS and R. A. ROBISON Department of Geology, Goldsmiths' College, University of London, Creek Road, London SE8 3BU, and Department of Geology, University of Kansas, Lawrence, Kansas 66045 Abstract—For the first time arthropods with preserved soft parts and appendages are recorded from Middle Cambrian strata in Utah. Occurrences of four nontrilobite taxa are described, including Branchiocaris pretiosa (Resser) and Emeraldella? sp. from the Marjum Formation, Sidneyia? sp. from the Wheeler Formation, and Leanchoilia? hanceyi, n. sp., from the Spence Shale. A small specimen of the giant predator Anomalocaris nathorsti (Walcott) also is described from the Marjum Formation. These occurrences extend upward the observed stratigraphie ranges of Anomalocaris, Branchiocaris, and questionably Emeraldella and Sidneyia. Emeraldella, Leanchoilia, and Sidneyia hitherto have been recorded from only the Stephen Formation in British Columbia. Further evaluation indicates that Dicerocaris opisthoeces Robison and Rich- ards, 1981, is a junior synonym of Pseudoarctolepis sharpi Brooks and Caster, 1956. DURING RECENT years, intensive collecting has 1983). Although providing little new morpho- produced rare but diverse, soft-bodied or scler- logic data, the Utah specimens are important otized Middle Cambrian fossils from several because of new information they provide about -
Smithsonian Miscellaneous Collections
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 116, NUMBER 5 Cfjarle* £. anb Jfflarp "^Xaux flKHalcott 3Resiearcf) Jf tmb MIDDLE CAMBRIAN STRATIGRAPHY AND FAUNAS OF THE CANADIAN ROCKY MOUNTAINS (With 34 Plates) BY FRANCO RASETTI The Johns Hopkins University Baltimore, Maryland SEP Iff 1951 (Publication 4046) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION SEPTEMBER 18, 1951 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 116, NUMBER 5 Cfjarie* B. anb Jfflarp "^Taux OTalcott &egearcf) Jf unb MIDDLE CAMBRIAN STRATIGRAPHY AND FAUNAS OF THE CANADIAN ROCKY MOUNTAINS (With 34 Plates) BY FRANCO RASETTI The Johns Hopkins University Baltimore, Maryland (Publication 4046) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION SEPTEMBER 18, 1951 BALTIMORE, MD., U. 8. A. CONTENTS PART I. STRATIGRAPHY Page Introduction i The problem I Acknowledgments 2 Summary of previous work 3 Method of work 7 Description of localities and sections 9 Terminology 9 Bow Lake 11 Hector Creek 13 Slate Mountains 14 Mount Niblock 15 Mount Whyte—Plain of Six Glaciers 17 Ross Lake 20 Mount Bosworth 21 Mount Victoria 22 Cathedral Mountain 23 Popes Peak 24 Eiffel Peak 25 Mount Temple 26 Pinnacle Mountain 28 Mount Schaffer 29 Mount Odaray 31 Park Mountain 33 Mount Field : Kicking Horse Aline 35 Mount Field : Burgess Quarry 37 Mount Stephen 39 General description 39 Monarch Creek IS Monarch Mine 46 North Gully and Fossil Gully 47 Cambrian formations : Lower Cambrian S3 St. Piran sandstone 53 Copper boundary of formation ?3 Peyto limestone member 55 Cambrian formations : Middle Cambrian 56 Mount Whyte formation 56 Type section 56 Lithology and thickness 5& Mount Whyte-Cathedral contact 62 Lake Agnes shale lentil 62 Yoho shale lentil "3 iii iv SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL. -
Totoralia, a New Conical-Shaped Mollusk from the Middle Cambrian of Western Argentina
Geologica Acta, Vol.9, Nº 2, June 2011, 175-185 DOI: 10.1344/105.000001692 Available online at www.geologica-acta.com Totoralia, a new conical-shaped mollusk from the Middle Cambrian of western Argentina M.F. TORTELLO and N.M. SABATTINI CONICET-División Paleozoología Invertebrados, Museo de La Plata Paseo del Bosque s/nª, 1900 La Plata, Argentina. Tortello E-mail: [email protected] Sabatini E-mail: [email protected] ABS TRACT The new genus Totoralia from the Late Middle Cambrian of El Totoral (Mendoza Province, western Argentina) is described herein. It is a delicate, high, bilaterally symmetrical cone with a sub-central apex and five to seven prominent comarginal corrugations. In addition, its surface shows numerous fine comarginal lines, as well as thin, closely spaced radial lirae. Totoralia gen. nov., in most respects, resembles the Cambrian helcionellids Scenella BILLINGS and Palaeacmaea HALL and WHITFIELD. Although Scenella has been considered as a chondrophorine cnidarian by some authors in the past, now the predominant view is that it is a mollusk. Likewise, several aspects of Totoralia gen. nov. morphology indicate closer affinities with mollusks. The specimens studied constitute elevated cones that are rather consistent in height, implying that they were not flexible structures like those of the chondrophorines. The presence of a short concave slope immediately in front of the apex can also be interpreted as a mollusk feature. In addition, the numerous comarginal lines of the cone are uniform in prominence and constant in spacing, and are only represented on the dorsal surface of the shell; thus, they are most similar to the incremental growth lines of shells of mollusks. -
Cambrian Suspension-Feeding Tubicolous Hemichordates Karma Nanglu1* , Jean-Bernard Caron1,2, Simon Conway Morris3 and Christopher B
Nanglu et al. BMC Biology (2016) 14:56 DOI 10.1186/s12915-016-0271-4 RESEARCH ARTICLE Open Access Cambrian suspension-feeding tubicolous hemichordates Karma Nanglu1* , Jean-Bernard Caron1,2, Simon Conway Morris3 and Christopher B. Cameron4 Abstract Background: The combination of a meager fossil record of vermiform enteropneusts and their disparity with the tubicolous pterobranchs renders early hemichordate evolution conjectural. The middle Cambrian Oesia disjuncta from the Burgess Shale has been compared to annelids, tunicates and chaetognaths, but on the basis of abundant new material is now identified as a primitive hemichordate. Results: Notable features include a facultative tubicolous habit, a posterior grasping structure and an extensive pharynx. These characters, along with the spirally arranged openings in the associated organic tube (previously assigned to the green alga Margaretia), confirm Oesia as a tiered suspension feeder. Conclusions: Increasing predation pressure was probably one of the main causes of a transition to the infauna. In crown group enteropneusts this was accompanied by a loss of the tube and reduction in gill bars, with a corresponding shift to deposit feeding. The posterior grasping structure may represent an ancestral precursor to the pterobranch stolon, so facilitating their colonial lifestyle. The focus on suspension feeding as a primary mode of life amongst the basal hemichordates adds further evidence to the hypothesis that suspension feeding is the ancestral state for the major clade Deuterostomia. Keywords: Enteropneusta, Hemichordata, Cambrian, Burgess Shale Background no modern counterpart [11]. The coeval Oesia disjuncta Hemichordates are central to our understanding of Walcott [12] has been compared to groups as diverse as deuterostome evolution.