Memorial to John J. Anderson 1930–2017 PETER D
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Hydrothermal Uranium Deposits Containing Molybdenum and Fluorite in the Marysvale Volcanic Field, West-Central Utah
Mineralium Deposita (199K) 33 : 4774'14 ( . srl'lllt!~r-V~rlag 199X ARTICLE C. G. Cunningham' J. D. Rasmussen' T. A. Stcycn R. O. Rye' P. D. Rowley S. B. Romberger' J. Selverstone Hydrothermal uranium deposits containing molybdenum and fluorite in the Marysvale volcanic field, west-central Utah Received: 23 June 1997 I Accepted: 15 October 1997 Abstract Uranium deposits containing molybdenum \9-1 ~ Ma in a I km2 area. above a cupola of a com and fluorite occur in the Central Mining Area. near posite, recurrent. magma chamber at least 24 x 5 km Marysvale, Utah. and formed in an epithermal vein across that fed a sequence of 21- to 14-Ma hypabyssal system that is part of a volcanic/hypabyssal complex. granitic stocks. rhyolite lava flows. ash-flow tuffs. and They represent a known. but uncommon. type of de volcanic domes. Formation of the Central Mining Area posit; relative to other commonly described volcanic began when the intrusion of a rhyolite stock. and re related uranium deposits. they are young. well-exposed lated molybdenite-bearing, uranium-rich. glassy rhyolite and well-documented. Hydrothermal uranium-bearing dikes, lifted the fractured roof above the stock. A quartz and fluorite veins are exposed over a 300 m breccia pipe formed and relieved magmatic pressures. vertical range in the mines. Molybdenum. as jordisite and as blocks of the fractured roof began to settle back (amorphous MoS2), together with fluorite and pyrite, in place, flat-lying, concave-downward. "pull-apart" increase with depth. and uranium decreases with depth. fractures were formed. Uranium-bearing, quartz and The veins cut 23-Ma quartz monzonite, 20-Ma granite. -
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 . -
Detrital Zircon U-Pb Provenance of the Colorado River: a 5 M.Y
Research Paper THEMED ISSUE: CRevolution 2: Origin and Evolution of the Colorado River System II GEOSPHERE Detrital zircon U-Pb provenance of the Colorado River: A 5 m.y. record of incision into cover strata overlying the GEOSPHERE; v. 11, no. 6 doi:10.1130/GES00982.1 Colorado Plateau and adjacent regions David L. Kimbrough1, Marty Grove2, George E. Gehrels3, Rebecca J. Dorsey4, Keith A. Howard5, Oscar Lovera6, Andres Aslan7, P. Kyle House8, 19 figures; 5 tables; 1 supplemental file and Philip A. Pearthree9 1Department of Geological Sciences, San Diego State University, 5500 Campanile Drive, San Diego, California 92182, USA CORRESPONDENCE: [email protected] 2School of Earth, Energy & Environmental Sciences, Stanford University, 450 Serra Mall, Building 320, Stanford, California 94305, USA 3Department of Geosciences, University of Arizona, 1040 4th Street, Tucson, Arizona 85721, USA CITATION: Kimbrough, D.L., Grove, M., Gehrels, 4Department of Geological Sciences, 1272 University of Oregon, Eugene, Oregon 97403-1272, USA G.E., Dorsey, R.J., Howard, K.A., Lovera, O., Aslan, 5U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025-3591, USA A., House, P.K., and Pearthree, P.A., 2015, Detrital 6Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, 595 Charles Young Drive East, Los Angeles, California 90095, USA zircon U-Pb provenance of the Colorado River: A 7Colorado Mesa University, 1100 North Avenue, Grand Junction, Colorado 81501, USA 5 m.y. record of incision into cover strata overlying the 8U.S. Geological Survey, 2255 N. Gemini Drive, Flagstaff, Arizona 86001, USA Colorado Plateau and adjacent regions: Geosphere, 9Arizona Geological Survey, 416 W. -
Water Resources of Parowan Valley, Iron County, Utah
Prepared in cooperation with the Utah Department of Natural Resources Water Resources of Parowan Valley, Iron County, Utah Scientific Investigations Report 2017–5033 U.S. Department of the Interior U.S. Geological Survey Cover photograph: Parowan Valley looking east toward the Red Cliffs. Photograph by Tom Marston, U.S. Geological Survey, November 2013. Water Resources of Parowan Valley, Iron County, Utah By Thomas M. Marston Prepared in cooperation with the Utah Department of Natural Resources Scientific Investigations Report 2017–5033 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. Geological Survey William H. Werkheiser, Acting Director U.S. Geological Survey, Reston, Virginia: 2017 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://store.usgs.gov/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Marston, T.M., 2017, Water resources of Parowan Valley, Iron County, Utah: U.S. Geological Survey Scientific -
Interim Geologic Map of the Southwestern Quarter of the Beaver 30' X 60' Quadrangle Utah Department of Natural Resources
Plate 1 UTAH GEOLOGICAL SURVEY Utah Geological Survey Open-File Report 686DM a division of Interim Geologic Map of the Southwestern Quarter of the Beaver 30' x 60' Quadrangle Utah Department of Natural Resources 113°00'00" 112°52'30" 112°45'00" 112°37'30" 112°30'00" b E E E E E ! ! E ! E ! E E ! ! E E ! ! ! ! F ! E ! 38°15'00" ! ! 38°15'00" ! ! ! ! ! ! ! ! ! ! ! ! ! ! Tm (Ticl) QTs Qms *c ! Qal1 1 Ppk ! Qat ! Tm (Jn) E QTs Qal1 ! Qaf1 Qaf3 Tm (Tdv) Qat1 ! E ! E Qal1 Tm (Tlk) ! Pt M Tm (Tdv) ! Qaf ! E E 4 ! Qaf2 ! Qat1 E Qms A ! ! E ! E ! Qal1 Tm ! ! R ! Qal1 ! ! Tm ! E ! ! Qat1 ! Qaf1 31 K ! ! ! ! ! ! ^m ! ! A ! Pp ! 1 ! ! Qat ! (Tda) G ! ! ! ! ! (Tdv) ! E ! E ! E ! U ! ! ! E 1 E ! ! Qat ! ! ! N ! ! Tm (Tdv) ! ! ! ! E ! ! ! ! T ! ! QTs ! ! Qat2 2 ! Qaf ! ! Tm ! E E ! ! Qaf2 Tm (Tdv) ! ! ! Qaf1 Qat1 ! ! ! Tm (Tlk) ! E E ! ! E Tm (Ticl) ! ! Qat1 ! ! E ! ! ! ! ! ! (Tda) b ! Qat1 ! E ! ! Qaf3 ! ! ! Qaf1 ! ! E ! 7 ! E ! E ! ! ! ! Qaf3 Pt E 1 ! ! Qaf ! ! Tm (Tin) Tb Qat2 ! ! ! ! ^cm ! ! E E 1 ! ! ! Qaf ! Qaf2 Qaf3 ! ! ! E Qaf3 ! E ! Tm (Tlk) ! ! ! ! ! ! ! ! Ppk E ! ! E ! ! ! ! ! ! ! E 3 ! Qaf E Qaf3 ! ! 1 ! E Qaf ! ! E ! ! ! ! ! ! E ! ! ! ! Qaf1 ! ! ! ! ! ! ! ! Tm (Tlb) ! ! ! ! ! E ! Tm (Tdb) ! ! ! ! E Tm ! ! ! E Qaf2 ! E ! ! Tm (Tda) E ! ! ! ! 2 ! ! Qaf Pq ! E ! ! ! E E ! ! E ! ! ! ! ! ! ! ! Tm (Tdv) E Qaf3 ! ! ! (Tin) ! Qaf2 ! ! ! E ! E ! Qaf2 E ! ! ! ! ! ! Qaf2 ! Tm (Tdv) ! ! ! ! ! E ! ! ! Tm E ! ! Qat1 ! ! Tm (Tdv) ! Qaf1 ! ! E ! ! ! ! E ! E ! Qal ! 2 ! ! ! E E! ! Tm (Tda) ! ! ! ! ! Tm (Tdv) ! ! ! ! ! ! E E E ! ! E ! ! ! ! Tm (Tdv) ! ! -
Mount Belknap and Red Hills Marysvale Volcanic Field
Mount Belknap and Red Hills Calderas and Associated Rocks, Marysvale Volcanic Field, West-Central Utah GEOLOGICAL SURVEY BULLETIN 1468 Mount Belknap and Red Hills Calderas and Associated Rocks, Marysvale Volcanic Field, West-Central Utah By C. G. CUNNINGHAM and T.A. STEVEN GEOLOGICAL SURVEY BULLETIN 1468 Description of the rocks, eruptive history, and inferred subvolcanic environment associated with the formation of the J1ount Belknap and Red Hills calderas UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1979 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress Cataloging in Publication Data Cunningham, C. G. Mount Belknap and Red Hills calderas and associated rocks, Marysvale volcanic field, west-central Utah. (Geological Survey Bulletin 1468) Bibliography: p. Supt. of Docs. no.: I 19.3:1468 1. Calderas-Utah-Marysvale region. 2. Volcanic ash, tuff, etc.-Utah-Marysvale region. I. Steven, Thomas August, 191 7-joint author. II. Title. III. Series: United States Geological Survey Bulletin 1468 QE75.B9 No. 1468 ( QE461] 557.3'08s 78-21191 [551.2'1'0979246) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock No. 024-001-03175-2 CONTENTS Page Abstract_ 1 Introduction _________ _ 2 Acknowledgments_ 4 Geologic setting __________ _ 4 Mount Belknap Volcanics ____ _ 6 Outflow facies ___________________ _ 7 Lower heterogeneous member _ 7 Joe Lott 'iliff Member 9 Red Hills 'fuff Member 11 Crystal-rich tuff member -
Application to Neogene Bimodal Igneous Rocks and Mineral Resources in the Great Basin
Development of an igneous rock database with geologic functions: Application to Neogene bimodal igneous rocks and mineral resources in the Great Basin Douglas B. Yager1*, Albert H. Hofstra1*, Katheryn Fifarek2*, and Ank Webbers3* 1Central Mineral and Environmental Resources Science Center, U.S. Geological Survey, Denver Federal Center, Box 25046, MS 973, Denver, Colorado 80225, USA 2Department of Geology, Mailcode 4324, Southern Illinois University, Carbondale, Illinois 62901, USA 3516 Orchard Way, Louisville, Colorado 80027, USA ABSTRACT and various subsamples. Absolute radiomet- INTRODUCTION ric age determinations on samples from geo- Geologists routinely use sample data logic features and expert interpretations of Now that GIS is fully implemented for (descriptive, qualitative, quantitative) to relative age relationships between different Windows-based software platforms on personal characterize a hierarchy of larger geologic features may be captured and used together computers and has interoperability with rela- features that each have their own indepen- to constrain the ages of undated features. tional databases, a new realm for data investiga- dent attributes, use physical relationships Such age information is linked to features tion, display, and analysis is available to earth between geologic features to establish their of various scales in the hierarchy. Common scientists. GIS enables data to be input, man- relative ages, combine this information with attributes that are shared between the rela- aged (in a database management -
West-Central Utah AVAILABILITY of BOOKS and MAPS of the U.S
Isotopic Ages and Stratigraphy of Cenozoic Rocks of the Marysvale Volcanic Field and Adjacent Areas, West-Central Utah AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the current-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Survey publications re leased prior to the current year are listed in the most recent annual "Price and Availability List." Publications that may be listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" may no longer be available. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices listed below. BY MAIL OVER THE COUNTER Books Books and Maps Professional Papers, Bulletins, Water-Supply Papers, Tech Books and maps of the U.S. Geological Survey are available niques of Water-Resources Investigations, Circulars, publications over the counter at the following U.S. Geological Survey offices, all of general interest (such as leaflets, pamphlets, booklets), single of which are authorized agents of the Superintendent of Docu copies of Earthquakes & Volcanoes, Preliminary Determination of ments. Epicenters, and some miscellaneous reports, including some of the foregoing series that have gone out of print at the Superintendent of Documents, are obtainable by mail from • ANCHORAGE, Alaska-Rm. -
INSIDE ▲ the California Arc: Thick Granitic Batholiths, Eclogitic Residues, Lithospheric-Scale Thrusting, and Magmatic Flare-Ups, P
Vol. 11, No. 11 A Publication of the Geological Society of America November 2001 INSIDE ▲ The California Arc: Thick Granitic Batholiths, Eclogitic Residues, Lithospheric-Scale Thrusting, and Magmatic Flare-Ups, p. 4 Mihai Ducea Rocky Mountain Section Meeting, p. 14 Cordilleran Section Meeting, p. 16 COLORADO CONVENTION CENTER IMPORTANT DATES FIELD TRIP CO-CHAIRS Mid-November Pardee Keynote Symposia and Eric A. Erslev Topical Session proposal forms (970) 491-5661 available at www.geosociety.org fax 970-491-6307 December 3, 2001 Short Course proposals due [email protected] January 17, 2002 Keynote and Topical Session proposals due Jerry Magloughlin April 2002 Call for Papers in April issue of (970) 491-1812 GSA Today fax 970-491-6307 June 2002 Registration and housing infor- [email protected] mation in June issue of GSA Today HOT TOPICS CHAIR July 16, 2002 Abstracts due Steve Getty (710) 389-6512 Field Trip proposals are still being accepted. fax 719-389-6910 Exhibit Space is available. Call Brenda Martinez [email protected] at 1-800-472-1988 for an Exhibitor Prospectus. GSA TECHNICAL PROGRAM OFFICER Nancy Carlson For more information, contact: (303) 357-1061 [email protected] TECHNICAL PROGRAM CHAIR John W. Geissman GSA SHORT COURSE PROGRAM OFFICER (505) 277-3433 Edna Collis fax 505-277-8843 (303) 357-1034 [email protected] [email protected] For More Information (303) 447-2020 " 1-800-472-1988 " fax 303-357-1070 [email protected] " www.geosociety.org Contents GSA TODAY (ISSN 1052-5173) is published monthly by The Geological Vol. 11, No. 11 November 2001 Society of America, Inc., with offices at 3300 Penrose Place, Boulder, Colorado. -
Oligocene Caldera Complex and Calc-Alkaline Tuffs and Lavas of the Indian Peak Volcanic Field, Nevada and Utah
Oligocene caldera complex and calc-alkaline tuffs and lavas of the Indian Peak volcanic field, Nevada and Utah MYRON G. BEST US. Geological Survey and Department of Geology, Brigham Young University, Provo, Utah 84602 ERIC H. CHRISTIANSEN Department of Geology, Brigham Young University, Provo, Utah 84602 RICHARD H. BLANK, JR. US. Geological Survey, Denver, Colorado 80225 ABSTRACT eruptive sequence consists of several cooling subject of recent controversy (Whitney and units of trachydacite tuff containing small to Stormer, 1985; Johnson and Rutherford, 1989; The Indian Peak volcanic field is represen- modest amounts of plagioclase and two Grunder and Boden, 1987). tative of the more than 50,000 km3 of ash- pyroxenes. Compared to contemporaneous volcanic flow tuff and tens of calderas in the Great These dominantly high-K calc-alkaline fields around the Colorado Plateaus to the east Basin that formed during the Oligocene-early rocks are a record of the biih, maturation, (Fig. l), the -10,000 km3 of ash-flow deposits Miocene "ignimbrite flareup" in southwest- and death of a large, open, continental in the Indian Peak volcanic field is an order of ern North America. The field formed about magma system that was probably initiated magnitude greater than in the Marysvale field 32 to 27 Ma in the southeastern Great Basin and sustained by influx of mafic magma de- (Steven and others, 1984) but similar to that of and consists of the centrally positioned Indi rived from a southward-migrating locus of the San Juan (Steven and Lipman, 1976) and Peak caldera complex and a surrounding magma production in the mantle. -
A Summary of 1Ertiary Volcanic Stratigraphy of the Southwestern High Plateaus and Acljacent Great Basin, Utah
A Summary of 1ertiary Volcanic Stratigraphy of the Southwestern High Plateaus and Acljacent Great Basin, Utah GEOLOGICAL SURVEY BULLETIN 1405-B A Summary of lertiary Volcanic Stratigraphy of the Southwestern High Plateaus and Aqjacent Great Basin, Utah By PETER D. ROWLEY, JOHN J. ANDERSON, and PAULL. WILLIAMS ' CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1405-B Stratigraphic setting of rocks of the south flank of the Marysvale volcanic pile and intertonguing regional ash-flow tuffs. of Great Basin sources, southwestern Utah UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1975 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Rowley, Peter D. A summary of Tertiary volcanic stratigraphy of the southwestern high plateaus and adjacent Great Basin, Utah. (Contributions to stratigraphy) (Geological Survey Bulletin 1405-B) Babliography: p. Supt. of Docs. no.: I 19.1405-B l. Geology, Stratigraphic-Tertiary. 2. Volcanism-The West. I. Anderson, John Jerome, 1930- joint author. II. Williams, Paul Lincoln, 1932- joint author. III. Title: A summary of Tertiary volcanic stratigraphy of the southwestern high plateaus ... IV. Series. V. Series: United States Geological Survey Bulletin 1405-B. QE75.B9 no. 1405-B (QE691) 557.3'08s (551.2'1] 75-619290 For sale by the Sup~rintendent of Documents, U.S. Government Printing Office Washington, D. C. 20402 Stock Number 024-001-02752-6 CONTENTS Page Metric-English equivalents....................................................................................... -
INTERIM GEOLOGIC MAP of the NORTHWESTERN QUARTER of the BEAVER 30' X 60' QUADRANGLE, BEAVER and PIUTE COUNTIES, UTAH
Utah Geological Survey Plate 1 a division of Utah Geological Survey Open-File Report 729DM Interim Geologic Map of the Northwestern Quarter of the Beaver 30' x 60' Quadrangle Utah Department of Natural Resources 113˚00' 112˚30' 38˚30' E MB Qal1 Qlae Xg Qs QTs SB 38˚30' Qaf3 Tm(Tbct) To Qaf2 QTs Trg Qaf1 SB E Tir Tm(To) Qms Tig To Tmj Qms Qaf3 Tig Qal1 Qaf1 QTs Tm(Tbc) Qafy Tig Qafy Qafo E Qs E E E Qaf1 E Qbr Qafy E Tic Tm SB E E Tm G (To) SB Tbct E E (Tbcd) G E — Tm G Qbk Qaf1 E E E Qs Tbc Qaf2 Tm(Tbc) (Tbc) E Trg Tbc E Tm Qafo SB Tm SB E Tic E E E Tic E (To) (Tbc) Qms Qaf3 Tm SB MNR ILE VILL MINERS E (Tbc) Tig QTs Trg QTs E E E Tm E (Tbc) Tbc E E Tm Tig Qrl (To) Tm(Tbc) G SB G E E Qms Xg E E QTs Tic MB Tmb Qaf1 E Tm Tmb Qes E (Tbcd) E E Tm(Tbc) Qms E E Tm(Tbc) Tm Tbc MB E SB (Tbc) Xg Qlae Tic E SB E Tbc Tm Tm(Tbcd) Tm(Tbc) E E QTs RL F To Qaf (Tbc) E E SB E 3 E Tbc E E E EE Tm(Tbc) Tm Qms E (Tbcd) SB MB E Tm(Tbcd) Tic Tig — E E Tbc Qs Qs E E SB Tig E Tmb Qaf2 Tig Tmv E QTs Tig Qbk Pq 32 Qll Tm(Tbcd) Qlg b E Qms QTs E E Qafy E Qaf3 Qrt Qms Qafy Tm(Tbcd) Qs Xg E E E Qafo E Qms E Tic E E FAUL T E E E Tbc E E QTs QTs Tic QTs E Tm(Tbcd) Tmv Trg b E Tbc Tmv Qlg Qaf1 — Trg 15 E E Pq QTs b Xg E Tig Qrd — — Tm(Tbc) 25 Qms E QTs — E Tic E E Tbc w Tig Qrt E Qaf1 E E E — E MB E Xg Qrd E E Qrl Qaf2 QTs Tmbl EE EE Qaf2 E E Qrt — E Pzc Qaf4 E Pq E E E E E E E E E Qrd Qaf Tbc Qaf2 1 — E QTs Tm(Tbc) E Qaf2 E QTs S B E Tir QTs Xg MB Qbk E Tmb E E Qaf2 Qaf2 Xg E Qal1 E Qaf1 Xg Trg Tir Tir Tic Qaf Qal1 Pzc 2 Qlg Tig E Xg Pq E Qaf Tmb Qms Tmv E 4 Tir Qaf