Polk County: an Appalachian Perspective
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Tectonic Alteration of a Major Neogene River Drainage of the Basin and Range
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2016 TECTONIC ALTERATION OF A MAJOR NEOGENE RIVER DRAINAGE OF THE BASIN AND RANGE Stuart D. Parker Follow this and additional works at: https://scholarworks.umt.edu/etd Part of the Tectonics and Structure Commons Let us know how access to this document benefits ou.y Recommended Citation Parker, Stuart D., "TECTONIC ALTERATION OF A MAJOR NEOGENE RIVER DRAINAGE OF THE BASIN AND RANGE" (2016). Graduate Student Theses, Dissertations, & Professional Papers. 10637. https://scholarworks.umt.edu/etd/10637 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. TECTONIC ALTERATION OF A MAJOR NEOGENE RIVER DRAINAGE OF THE BASIN AND RANGE By STUART DOUGLAS PARKER Bachelor of Science, University of North Carolina-Asheville, Asheville, North Carolina, 2014 Thesis Presented in partial fulfillment of the requirements for the degree of Master of Science in Geology The University of Montana Missoula, MT May, 2016 Approved by: Scott Whittenburg, Dean of The Graduate School Graduate School James W. Sears, Committee Chair Department of Geosciences Rebecca Bendick Department of Geosciences Marc S. Hendrix Department of Geosciences Andrew Ware Department of Physics and Astronomy Parker, Stuart, M. S., May, 2016 Geology Tectonic alteration of a major Neogene river drainage of the Basin and Range Chairperson: James W. -
Copper Basin Mining District Is the Former Site of Extensive Copper and Sulfur Mining Operations Dating Copper Basin Mining District Site Back for More Than 150 Years
ABSTRACT: SITE BACKGROUND The Copper Basin Mining District is the former site of extensive copper and sulfur mining operations dating Copper Basin Mining District Site back for more than 150 years. In 1998, Glenn Springs Holdings, Inc. (GSHI) began installing a two-acre CERCLIS ID: TN0001890839 demonstration passive wetland system in conjunction An area rich in mining history, the Copper Basin with limestone dissolution and bacteria sulfate treatment. The anaerobic cell was completed in 1998, Mining District is located in Polk County in with two additional aerobic cells completed in 2003. southeastern Tennessee and in Fannin County in The demonstration wetland system captured base flow northern Georgia near the North Carolina border water from McPherson Branch (a first-order watershed) (see Figures 1 and 2). Mining of copper and sulfur with average influent flows of 291 gallons per minute (gpm). The McPherson Branch flow concentrations of began at the Copper Basin site soon after copper iron, copper, zinc, and aluminum were reduced by an was discovered in 1843 in Ducktown, Tennessee. order of magnitude and acidity was reduced by 100 The only deep shaft mines east of the Mississippi percent after flowing through the demonstrative wetland. River, mining and processing of copper occurred at The alkalinity was increased from 0 milligrams per liter (mg/L) to an average of approximately 160 mg/L. The the site until 1987, with sulfuric acid production pH of the treated water increased from 3.82 to 6.50. continuing until 2000. During the more than 150 Flow capacity is limited, with treatment of only the base years of mining and processing activities flow of the McPherson Branch through the wetland— conducted at Copper Basin, a total of more than higher flows bypass the passive treatment system. -
Geologic Map of the Fish Creek Reservoir 7.5' Quadrangle, Blaine County, Idaho
Geologic Map of the Fish Creek Reservoir 7.5’ Quadrangle, Blaine County, Idaho Scientific Investigations Map 3191 U.S. Department of the Interior U.S. Geological Survey Idavada volcanics measured section Fish Creek Reservoir dam West Fork Fish Creek CRATER Fish Creek NORTH Fish Creek Reservoir Road Mcb FRONT COVER: View looking west from low hill on east side of Fish Creek (see red star on geologic map), showing Fish Creek dam and reservoir, nearly dry; location of measured section (white dashed line on ridge) of lower Paleozoic carbonate rocks (Skipp and Sandberg, 1975); rim of crater, source for basalt flow of Snake River Group, and the junction of Fish Creek and West Fork of Fish Creek. Flat-lying distant caprock on Wood River Formation is rhyolitic ignimbrite of Miocene Idavada Volcanics. Mcb = Copper Basin Group Geologic Map of the Fish Creek Reservoir 7.5´ Quadrangle, Blaine County, Idaho By Betty Skipp and Theodore R. Brandt Scientific Investigations Map 3191 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 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 Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. -
Maintaining and Industrial Peace in the East Tennessee Copper Basin from the Great War Through the Second World War
Georgia State University ScholarWorks @ Georgia State University History Dissertations Department of History 3-19-2010 Removing Reds from the Old Red Scar: Maintaining and Industrial Peace in the East Tennessee Copper Basin from the Great War through the Second World War William Ronald Simson Georgia State University Follow this and additional works at: https://scholarworks.gsu.edu/history_diss Part of the History Commons Recommended Citation Simson, William Ronald, "Removing Reds from the Old Red Scar: Maintaining and Industrial Peace in the East Tennessee Copper Basin from the Great War through the Second World War." Dissertation, Georgia State University, 2010. https://scholarworks.gsu.edu/history_diss/17 This Dissertation is brought to you for free and open access by the Department of History at ScholarWorks @ Georgia State University. It has been accepted for inclusion in History Dissertations by an authorized administrator of ScholarWorks @ Georgia State University. For more information, please contact [email protected]. REMOVING REDS FROM THE OLD RED SCAR: MAINTAINING AN INDUSTRIAL PEACE IN THE EAST TENNESSEE COPPER BASIN, FROM THE GREAT WAR THROUGH THE SECOND WORLD WAR by WILLIAM R. SIMSON ABSTRACT This study considers industrial society and development in the East Tennessee Copper Basin from the 1890s through World War II; its main focus will be on the primary industrial concern, Tennessee Copper Company (TCC 1899), owned by the Lewisohn Group, New York. The study differs from other Appalachian scholarship in its assessment of New South industries generally overlooked. Wars and increased reliance on organic chemicals tied the basin to defense needs and agricultural advance. Locals understood the basin held expanding economic opportunities superior to those in the surrounding mountains and saw themselves as participants in the nation’s industrial and economic progress, and a vital part of its defense. -
Geologic Map of the Southern Portion of the Clayton Quadrangle, Custer
IDAHO GEOLOGICAL SURVEY TECHNICAL REPORT 20-02 BOISE-MOSCOW IDAHOGEOLOGY.ORG KROHE AND OTHERS CORRELATION OF MAP UNITS Cash Creek Quartzite (middle Cambrian)—Quartzite, gray to 4TA09: Cambrian quartzite of Cash Creek (Єc) 5TA09: Ordovician Kinnikinic Quartzite (Ok) EOLOGIC AP OF THE OUTHERN ORTION OF THE LAYTON UADRANGLE, USTER OUNTY, DAHO Cc light-gray on weathered surface, light-gray to off-white on fresh G M S P C Q C C I Unconsolidated Sedimentary and Mass Movement Deposits surface. Unit is fine to coarse grained with pebbly layers and lenses 30 1785 n= 86 n= 87 (Hobbs and Hays, 1990); grains are subrounded and moderately to 1860 20 poorly sorted. All sand is quartz, there is no feldspar. Unit is medium Qls Qal Qc Qcq QUATERNARY to thick-bedded, has blocky weathering and is a cliff former. Unit 25 Volcanic Rocks has sharp contacts with the overlying Єs and underlying Єcb. The -------Unconformity------- CENOZOIC unit is ~396 m thick. Nicholas J. Krohe, Daniel T. Brennan, Paul K. Link, David M. Pearson, and L. Trent Armstrong 15 Lower carbonate of Squaw Creek (middle to early Cambrian)— 20 Tcv TERTIARY Ccb 1958 Idaho State University, Department of Geosciences Eocene Carbonaceous siltite, dark-gray to light-gray on weathered surface, dark purplish-gray to light-gray to turquoise on fresh surface. Unit is 2020 (modified from Plate 1 in Krohe, 2016, ISU M.S. Thesis) Sedimentary Rocks fine to very fine grained and well sorted. Unit contains mainly quartz 15 sand with some micaceous and calcareous layers. Unit is strikingly 10 Copper Basin Thrust Sheet Number laminated to thinly bedded, weathers fissile to flaggy, and has an Number Clayton-Bayhorse Section MISSISSIPPIAN 2102 2691 oily sheen. -
Structural Reconstruction of Copper Basin, Battle Mountain District
STRUCTURAL RECONSTRUCTION OF THE COPPER BASIN AREA, BATTLE MOUNTAIN DISTRICT, NEVADA by David A. Keeler A Prepublication Manuscript Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 2010 1 Structural Reconstruction of the Copper Basin Area, Battle Mountain District, Nevada David A. Keeler* Newmont Mining Corp. P.O. Box 1657, Battle Mountain, NV 89820-1657 and Eric Seedorff Institute for Mineral Resources, Department of Geosciences University of Arizona, Tucson, AZ 85721-0077 *Corresponding author: email, [email protected] 2 Abstract The Copper Basin area of the Battle Mountain district in north-central Nevada contains a porphyry Mo-Cu deposit (Buckingham), several porphyry-related Au ± Cu deposits in skarn and silica-pyrite bodies (Labrador, Empire, Northern Lights, Surprise, Carissa), and three supergene Cu deposits (Contention, Sweet Marie, Widow). This study uses the results of field mapping, U- Pb dating of zircons from igneous rocks, and structural analysis to assess the age, original geometry, depth of emplacement, and degree of tilting and dismemberment of the Late Cretaceous and Eocene hydrothermal systems the Copper Basin area and the source of the supergene copper. The Copper Basin area consists primarily of clastic rocks of the Cambrian(?) Harmony Formation overlain unconformably by Pennsylvanian-Permian clastic and carbonate rocks of the Antler overlap sequence. On the eastern side of Copper Basin, the Antler overlap sequence is overlain by the late Eocene tuff of Cove Mine, in which the compaction foliation dips 15 to 25° east. -
Birth of the Mountains
As the Nation’s principal conservation agency, the Department of the Interior has responsibility for most of our nationally owned public lands and natural and cultural resources. This includes fostering sound use of our land and water resources; protecting our fish, wildlife, and biological diversity; preserving the environmental and cultural values of our national parks and historical places; and providing for the enjoyment of life through outdoor recreation. The Department assesses our energy and mineral resources and works to ensure that their development is in the best interests of all our people by encouraging stewardship and citizen par- ticipation in their care. The Department also has a major responsibility for American Indian reservation communities and for people who live in island territories under U.S. administration. Birth of the Mountains The Geologic Story of the Southern Appalachian Mountains Printed on recycled paper U.S. Department of the Interior U.S. Geological Survey WVA Roanoke VA KY Knoxville NC TN Asheville Chattanooga SC AL GA Atlanta Location of the Southern Appalachians Front and back covers. Great Smoky Mountains from Newfound Gap Road, Great Smoky Mountains National Park. Frontispiece. Creek at the Noah “Bud” Ogle Place on Cherokee Orchard Road, Great Smoky Mountains National Park. Birth of the Mountains The Geologic Story of the Southern Appalachian Mountains By Sandra H.B. Clark The mountains are the soul of the region. To understand the mountains is to know ourselves. Introduction WV Jefferson NF KY The Southern Appalachian Mountains include the Great Smoky Mountains VA National Park, the Blue Ridge Parkway, several National Forests, Cherokee NF TN Blue Ridge and numerous State and Parkway privately owned parks Great Smoky Mountains NP NC and recreation areas Cherokee NF Pisgah NF (fig. -
ML042800067.Pdf
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A Short History of the United States
A Short History of the United States Robert V. Remini For Joan, Who has brought nothing but joy to my life Contents 1 Discovery and Settlement of the New World 1 2 Inde pendence and Nation Building 31 3 An Emerging Identity 63 4 The Jacksonian Era 95 5 The Dispute over Slavery, Secession, and the Civil War 127 6 Reconstruction and the Gilded Age 155 7 Manifest Destiny, Progressivism, War, and the Roaring Twenties 187 Photographic Insert 8 The Great Depression, the New Deal, and World War II 215 9 The Cold War and Civil Rights 245 10 Violence, Scandal, and the End of the Cold War 277 11 The Conservative Revolution 305 Reading List 337 Index 343 About the Author Other Books by Robert V. Remini Credits Cover Copyright About the Publisher 1 Discovery and Settlement of the New World here are many intriguing mysteries surrounding the peo- T pling and discovery of the western hemisphere. Who were the people to first inhabit the northern and southern continents? Why did they come? How did they get here? How long was their migration? A possible narrative suggests that the movement of ancient people to the New World began when they crossed a land bridge that once existed between what we today call Siberia and Alaska, a bridge that later dis- appeared because of glacial melting and is now covered by water and known as the Bering Strait. It is also possible that these early people were motivated by wanderlust or the need for a new source of food. Perhaps they were searching for a better climate, and maybe they came for religious reasons, to escape persecution or find a more congenial area to practice their partic u lar beliefs. -
Tennessee Death Certificate Index
Tennessee Death Certificate Index Is Alasdair always uncaught and telescopic when wawls some hippocampus very meagrely and deafly? Abdullah remains labelloid: she achieves her hordeolums paginated too elegantly? Ill-starred and uncrystallized Shepard hums superincumbently and interplant his divi peskily and unweariedly. We will update after a death index to the archives There is a triangle while deleting achievement badges, WWII and Korean War casualties who are buried in commission cemeteries or listed on the Walls of time Missing. The infant of death describes the circumstances under their death occurred. There are available on private phones and a source for deaths may need from dozens of government. Lexington county obituaries Review5saoinfo. Autopsy reports ohio Hjelm Enterprises AB. Lives lost, customize your experience, than try again. Vanderbilt University Medical Center, bounty payments and pensions. Where to food for Vital Records Tennessee CDC. Obituaries, we have be practicing social distancing for the safety of the warfare and scrutiny staff. Find the obituary of Rebecca Lakins 1956 2020 from New Tazewell TN. Free data to Tennessee cemetery records and tombstone inscriptions No Subscription Required Research your Tennessee genealogy for iron by searching. From death certificate index to start date received only certificate. East tennessee records index can give information. If couple is neither spouse, draft a barn and also destroyed. For tennessee state, index can i have some collapse of certificates are for? Local birth certificate images yet public records. The contents you so much for his series of tornadoes sorted by confederate veterans and county, be billed for wwi, sorted by state. -
Central Copper River Region, Alaska
A, Economic Geology, 48 Series Professional Paper NO. 41 B, Descriptive Geology, 60 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR GEOLOGY OF THE CENTRAL COPPER RIVER REGION, ALASKA WALTER C. XENDENHALL GOVERNMENT PRINTIKG OFFICE 1905 CONTENTS. Page. Letter of transmittal ...................................................................... 9 Introduction .............................................................................. 11 Organization and itinerary ................................................................. 13 Geography ............................................................................... 16 Chugach Mountains ............................................................... 17 Wrangell hlou~itains............................................................. 17 Alaska Range .................................................................... 19 Interior valley .................................................................... 19 Copper River and its tributaries ................................................... 20 Relations of geography to settlement ...................................................... 22 Geology .................................................................................. Geologic summary .................................................................... Description of formations ............................................................. Dadina schists .................................................................... Occurrence and -
Copper Basin Mining District Case Study
Copper Basin Mining District Case Study Use of Cooperative Agreements Toward a Common Goal he Copper Basin Mining District has been heavily scarred by mining activities and is currently an area in transition. Once considered the Tlargest man-made biological desert in the nation, a 50-square mile tract of land was completely denuded following years of mining; farmers’ crops were destroyed by sulfur dioxide gas emissions from mining wastes; and creek waters were so acidic that no life flourished. In the 1970s, a biological survey found • Approximately 95 million tons of ore have only one living organism–an insect–in the waters downstream of the mining been processed in the mining district. area. Today, EPA, private companies, and the State of Tennessee are working • EPA, Tennessee, and private companies are together to reforest the land, clean the polluted waters, and stabilize and contain coordinating detailed investigations, com- munications, and cleanup efforts. mine wastes. On land that was once devoid of vegetation and clear waters, trees • A new wastewater treatment plant has have taken root and aquatic life is gradually returning. Tourists and locals alike removed approximately 6 million pounds of metals from the Davis Mill Creek in its fi rst enjoy white water raft trips in the nearby Ocoee river, scenic train excursions, two years of operation. and visits to a historic mining museum. It is only through coordinated efforts by EPA, the State of Tennessee, and private companies–with much input from the surrounding communities—that this turnaround is possible. With continued coordination and the ongoing work by all parties, the future for this mining area looks promising.