Cameron to Milford ROD.Pdf
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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 . -
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) ! ! -
BRIGHAM YOUNG UNIVERSITY GEOLOGY STUDIES Volume 42, Part 11, 1997
BRIGHAM YOUNG UNIVERSITY GEOJ (3GY GEOLOGICAL SOCIETY OF AMERICA 1997 ANNUAL MEETING SALT LAKE CITY, UTAH PART2 TWO EDITED BY PAUL KARL LINK AND BART J. KOWALLIS VOLUME 42 1997 MESOZOIC TO RECENT GEOLOGY OF UTAH Edited by Paul Karl Link and Bart J. Kowallis BRIGHAM YOUNG UNIVERSITY GEOLOGY STUDIES Volume 42, Part 11, 1997 CONTENTS Triassic and Jurassic Macroinvertebrate Faunas of Utah: Field Relationships and Paleobiologic Significance ........................................ Carol M. Tang and David J. Bottjer Part 2: Trace fossils, hardgrounds and ostreoliths in the Carmel Formation (Middle Jurassic) of southwestern Utah ...........................................Mark A. Wilson Part 3: Low-diversity faunas of the Middle Jurassic Carmel Formation and their paleobiological implications ................................Carol M. Tang and David J. Bottjer Part 4: Paleoecology of Lower Triassic marine carbonates in the southwestern USA ....................... ......................................................David J. Bottjer and Jennifer K. Schubert Structure and Kinematics of a Complex Impact Crater, Upheaval Dome, Southeast Utah .........................Bryan J. Kriens, Eugene M. Shoemaker, and Ken E. Herkenhoff Stratigraphy, and structure of the Sevier thrust belt, and proximal foreland-basin system in central Utah: A transect from the Sevier Desert to the Wasatch Plateau ...................T. E Lawton, D. A. Sprinkel, F! G. DeCelles, G. Mitra, A. J. Sussman,, and M. l? Weiss Lower to Middle Cretaceous Dinosaur Faunas of the Central Colorado Plateau: A Key to Understanding 35 Million Years of Tectonics, Sedimentology, Evolution, and Biogeography ..................... James I. Kirkland, Brooks Britt, Donald L. Burge, Ken Carpenter, Richard Cifelli, Frank DeCourten, Jeffrey Eaton, Steve Hasiotis, and Tim Lawton Sequence Architecture, and Stacking Patterns in the Cretaceous Foreland Basin, Utah: Tectonism versus Eustasy ........................................ -
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. -
GEOLOGIC MAP of the RICHFIELD 30' X 60' QUADRANGLE
113°00' 3 0000m 112°00' R 10 W 3 E 1 600 1 600 00 FEET (SOUTH) R 9 W 34 3 3 3 4 R 21/2 W 1 850 000 FEET (CENTRAL) R 2 W 39°00' 1 625 1 625 45' R 8 W 1 650 1 675 1 675 R 7 W 6 1 700 1 700 R 6 W 30' 1 725 1 725 R 5 W 8 1 750 R 4 W 1 775 9 15' 1 800 1 800 R 3 W 0 1 825 1 825 39°00' -Cpm -Cdh 16 -Cdh Qaf2 QTaf Tf 55 Tf Qlg -Cp Tf Qdg Qdg Tht Qgt Tg 12 Qaf P Toc QTaf 1 -Cdh QTlf Qlf P - Qac 850 000 Qaf1 Qlg Qlg/Toc Toc Cum Kc Qal1 B -Cp -Cpm Qls Qgt FEET -Cpm 12 12 Qal1 Qac Qac Qgt Qac Tf Tse Tg Qaf2 - Qaf2 -Cop 18 -Cpm Cp Tf (SOUTH) Qla - Qla Jn TKn Cp Tf B Toc -Cpm 8 Qaf2 Tg -Cdh -Cdh QTlf Qdg Qlg -Cum 10 Qaf2 - Qaf2 QTaf - Cdh Toc TKn Tse Cpm -Cpm - -Cpm -Cdh Qdg Qed/Qvb3 Toc Qgt Qac Qac -Cpm Cp Tf QTlf Qla Qed/Qlf Qaf2 Toc -Cop Qed Qvb Qac B 1 Qac QTaf Qaf2 T 21 S -Cdh Toc Qaf2 QTaf QTaf -Cp 25 -Ccm Tf -Cdh TKn Qgt Qaf2 -Cp P -Cum Qal QTaf - -Cp QTlf Qac 1 B Cpm Toc Tg Tg Tflr Qaf2 T 21 S -Cdh -Cw Qed Qlf Qlg Qlg - 72 Tflr Qaf2 -Cp 12 Qla P Cum - - - -Cdh Qlf Qdg Qla Qmu Ct Cop Qac Tg Cw -Cp Tf Qaf1 Tflw - Tg Cp 11 -Cdh Tflr - -Cp TRm Qac Qac Cpm Qlg 5 -Ct Kc Qlg Qlf Toc Qaf 30 Tflr Tflw QTaf -Ccm 14 Qed/Qvb 2 - -Cdh QTlf 1 Toc TRcu Qac 10 Qac Cw B B Tht 20 TRcs 35 Qaf2 Tg 20 Qaf2 Qvb1 Kc 5 - Qlf/Qvb2 Qpm Tflr Tg Cdh - Qlg Qdf 30 Jn Qac QTaf -Cpm Cdh P -Cdh Qac -Cum TKn Qaf Qla P 20 Qaf2 1 - 18 Qed Qlg TRcu Tflr -Cpm Cdh Qed/Qlg Qed/Qlf Qed/ -Cum Qac 225 000 - -Ccm Qaf2 TRcs Qaf Cdh Qlf/ Tflr FEET 2 24 -Cw -Ccm Qed/Qll -Ccm QTlf Qed/ Qvb4 Qal2 30 Qac Qac -Cdh Qla Qed/Qvb1 Toc Tflw Tg (CENTRAL) Qdg Ktm 5 Qll Toc TRm Qac TKn Tg Qal B Qac -
This Report Is Preliminary and Has Not Been Reviewed for Conformity with U.S
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY GUIDEBOOK TO THE LATE CENOZOIC GEOLOGY OF THE BEAVER BASIN, SOUTH-CENTRAL UTAH by Michael N. Machette Open-File Report 82-850 1982 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature CONTENTS Page Introduction.......................................................... 1 Late Cenozoic geology of the Beaver basin............................. 1 Lower basin-fill deposits and volcanic rocks........................ 3 Upper basin-fill deposits........................................... 5 Surficial deposits.................................................. 7 Soi1 Devel opment...................................................... 10 Late Cenozoic structural development of the Beaver basin.............. 14 Potential uranium mineralization in the Beaver basin.................. 15 Road log of the Beaver basin.......................................... 16 Stop 1: Table Grounds surface and overview of the Beaver basin...... 16 Stop 2: Buried soil on scarp colluvium and gravel of Last Chance Bench................................................ 20 Stop 3: Soil on old fan alluvium near North Creek................... 21 Stop 4: Soil on old piedmont-slope alluvium at 1-15 (optional)...... 23 Stop 5: Soils on middle and young alluvium of Indian Creek.......... 26 Stop 6: Last Chance Bench, overview of upper Cenozoic deposits and structure...................................... 28 Stop 7: Relation between -
Water Resources of Beaver Valley, Utah
Water-Supply Paper No. 217 tai.{J; DEPAETMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR WATER RESOURCES OP BEAVER VALLEY, UTAH BY WILLIS T. LEE WASHINGTON GOVERNMENT PRINTING OFFICE 1908 CONTENTS. Page. Introduction _______________________________ 5 Location and extent of the area examined_-_-_____ 5 Purpose and scope of work_ _________________ _ __ 5 Cooperation __________________________ _-____ __ 6 Geography ___________________ ______________-- 6 Plateau province ______________________________- 6 Basin province ________________________________ 6 Deserts ___________________________________ 6 Isolated basins _____________________________ 8 Residual lakes___________________. ______ ,___ 8 Drainage __________________________________ 9 Geology ___________________ ___________ __________ 9 Formations_________________________________ 9 Granite ____________________________________ 9 Paleozoic sediments ________________________ 11 Effusive rocks________________________________ 11 Younger sediments_____________________ 12 Structure _____________________________________ 13 Water supply______________________________________ 15 Precipitation __________..________..____________ 15 Surface waters _____________________________ 17 Source______________________________________ 17 Measurements of flow_______________________ 18 Utilization ___________________________________ 19 Underground waters ______________________________ 19 Springs ___________________________________ 19 Number and distribution_______________________ -
Tungsten Deposits in Beaver County, Utah
UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director Bulletin 945-D TUNGSTEN DEPOSITS IN BEAVER COUNTY, UTAH BY S. W. HOBBS Strategic Minerals Investigations, 1944 (Pages 81-111) UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1945 For sale by the Superintendent of Documents, U. S. Government Printing Office, Washington 25, D. C- Price 65 cents CONTENTS Page Abstract................................................. 81 Introduction............................................. 82 Location, accessibility, and transportation.......... 82 History of the area.................................. 82 Previous work........................................ 83 Field work........................................... 83 Geology.................................................. 84 Topography and regional setting...................... 84 Rocks................................................. 84 Sedimentary rocks................................ 85 Igneous rocks.................................... 85 Structure............................................ 86 Tungsten deposits........................................ 87 Cupric nines Co. tungsten deposit.................... 87 Geology.......................................... 88 Sedimentary rocks............................ 88 Igneous rocks................................ 88 Structure.................................... 88 Contact metamorphlsm......................... 89 Occurrence of scheelite...................... 89 Distribution, grade, and volume -
Implications of Thrust and Detachment Faulting for the Structural Geology of Thermo Hot Springs Region, Beaver County, Utah
GRC Transactions, Vol. 36, 2012 Implications of Thrust and Detachment Faulting for the Structural Geology of Thermo Hot Springs Region, Beaver County, Utah Warren V. Anderson1, 2, Ronald L. Bruhn2, and Joseph N. Moore1 1Energy & Geoscience Institute, Salt Lake City UT, USA 2Department of Geology and Geophysics, University of Utah, Salt Lake City UT Keywords 1. Geological Background Thermo Hot Springs, Sevier geothermal anomaly, Cave Canyon detachment, southern Mineral Mountains, Black Mountains The Sevier geothermal anomaly of southwestern Utah en- compasses a broad region of enhanced heat flow with seven known high-temperature geothermal resource areas (Mabey ABSTRACT and Budding, 1987, 1994). The anomaly covers the transition between the Colorado Plateau and the eastern Basin and Range This report presents data and conclusions concerning the role Province, where the Paleozoic miogeocline was collapsed east- of low-angle faulting in the formation of Thermo Hot Springs and ward by thrust faulting during the Cretaceous to early Tertiary the effects it may have on fluid flow and production. The conclu- (Cowan and Bruhn, 1992). The subsequent history included sions are that Thermo Hot Springs is formed by a low-angle normal widespread igneous activity, and extension initiated during or detachment fault that places Mesozoic and upper Paleozoic mid-Tertiary time and continuing to the present. Thrust faults sedimentary rock in the upper plate over underlying metamorphic are exposed throughout mountain blocks of the region, but there rock and granite. The Mesozoic section is overlain by a se- quence of Tertiary to Quaternary volcanic and sedimentary deposits. High-angle normal faults offset the sedimentary and volcanic section, and in some, if not all, cases penetrate and offset the low-angle detachment fault. -
Mineral Resource Potential of the Richfield I°X2° Quadrangle, West
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Mineral resource potential of the Richfield I°x2° quadrangle, west-central Utah Thomas A. Steven I and Hal T. Morris 2 Open-File Report 84-521 1984 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. 1Denver, Colo. 2Menlo Park, Calif. Contents Abstract ............................................................... 1 Introduction............................................................. 2 CUSMAP products.......................................................... 2 Outline of geology....................................................... 4 Older Precambrian rocks............................................. 4 Pre-orogenic sedimentary rocks...................................... 4 Sevier orogeny...................................................... 6 Synorogenic and post-orogenie sedimentary rocks..................... 7 Volcanic rocks...................................................... 8 Calc-alkalic igneous rocks..................................... 8 Bimodal igneous rocks of Miocene age........................... 10 Bimodal rocks of Pliocene and Pleistocene age.................. 12 Mineral Mountains batholith......................................... 12 Basin-Range tectonism and sedimentation............................. 13 Surficial deposits.................................................. 14 Mineral resources........................................................ 14 Syngenetic -
GEOLOGICAL SURVEY P ROFESSION a L PAPER 1149 Cenozoic Stratigraphic and Structural Framework of Southwestern Utah
GEOLOGICAL SURVEY P ROFESSION A L PAPER 1149 Cenozoic Stratigraphic and Structural Framework of Southwestern Utah By PETER D. ROWLEY, THOMAS A. STEVEN, JOHN J. ANDERSON,am/ CHARLES G. CUNNINGHAM GEOLOGICAL SURVEY PROFESSIONAL PAPER 1149 A summary of the Cenozoic sedimentary and volcanic stratigraphy of southwestern Utah, and the structures that controlled deposition of the strata and that displaced these strata 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 Main entry under title: Cenozoic Stratigraphic and Structural Framework of Southwestern Utah (Geological Survey Professional Paper 1149) Bibliography: p. 17 1. Geology, Stratigraphic Cenozoic. 2. Geology-Utah. I. Rowley, Peter D. II. Series: United States Geological Survey Professional Paper 1149 QE690.C438 551.7'8f09792 79-17228 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-03227-9 CONTENTS Page Abstract -- ——— — - —— - ——————— —— ———— ——— -- ———— ——— ———— -- 1 Introduction - —————— ———— - ———— —— — ——— —— - ———— ——— ———— —— 1 Acknowledgments — —— ————————— — ——— ———— ———— —————————————— 2 Stratigraphy - —————— ——— ———— —— - ————————— - ———— ——— ————————— 3 Lower Tertiary (and Upper Cretaceous?) sedimentary sequence ———————————————— 4 Middle Tertiary volcanic sequence —— —————— ——— ———— —————————————— 5 Early (pre-Needles Range Formation) -
Intrusive Rock Database for the Digital Geologic Map of Utah
Intrusive Rock Database for the Digital Geologic Map of Utah C.J. Nutt1 and Steve Ludington2 Open-File Report 03-486 Version 1.0 2003 U.S. Department of the Interior Gail A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1U.S. Geological Survey, Denver, CO 80225 3U.S. Geological Survey, Menlo Park, CA 94025 1 Introduction and Background Digital geologic maps offer the promise of rapid and powerful answers to geologic questions using Geographic Information System software (GIS). Using modern GIS and database methods, a specialized derivative map can be easily prepared. An important limitation can be shortcomings in the information provided in the database associated with the digital map, a database which is often based on the legend of the original map. The purpose of this report is to show how the compilation of additional information can, when prepared as a database that can be used with the digital map, be used to create some types of derivative maps that are not possible with the original digital map and database. This Open-file Report consists of computer files with information about intrusive rocks in Utah that can be linked to the Digital Geologic Map of Utah (Hintze et al., 2000), an explanation of how to link the databases and map, and a list of references for the databases. The digital map, which represents the 1:500,000-scale Geologic Map of Utah (Hintze, 1980), can be obtained from the Utah Geological Survey (Map 179DM).