Broad River Basin Have Captivated Tourists T and Ecologists Alike
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CEMOZOIC DEPOSITS in the SOUTHERN FOOTHILLS of the SANTA CATALINA MOUNTAINS NEAR TUCSON, ARIZONA Ty Klaus Voelger a Thesis Submi
Cenozoic deposits in the southern foothills of the Santa Catalina Mountains near Tucson, Arizona Item Type text; Thesis-Reproduction (electronic) Authors Voelger, Klaus, 1926- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 25/09/2021 10:53:10 Link to Item http://hdl.handle.net/10150/551218 CEMOZOIC DEPOSITS IN THE SOUTHERN FOOTHILLS OF THE SANTA CATALINA MOUNTAINS NEAR TUCSON, ARIZONA ty Klaus Voelger A Thesis submitted to the faculty of the Department of Geology in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in the Graduate College, University of Arizona 1953 Approved; , / 9S~J Director of Thesis ^5ate Univ. of Arizona Library The research on which this thesis is based was com pleted by Mr. Klaus Voelger of Berlin, Germany, while he was studying at the University of Arizona under the program of the Institute of International Education. The final draft was written after Mr. Voelgerf s return to his home in the Russian-occupied zone of Berlin. Difficulties such as a shortage of typing paper of uniform grade and the impossibility of adequate supervision and advice on matters of terminology, punctuation, and English usage account for certain details in which this thesis may depart from stand ards of the Graduate College of the University of Arizona. These details are largely mechanical, and it is felt that they do not detract appreciably from the quality of the research nor the clarity of presentation of the results. -
Cultural Heritage the Mountains and Foothills of North Carolina Have Over Many Centuries Fostered a Rich Mosaic of Cultural Heritage
Western North Carolina Vitality Index Cultural Heritage www.wncvitalityindex.org The mountains and foothills of North Carolina have over many centuries fostered a rich mosaic of cultural heritage. The birthplace of the Cherokee’s advanced early civilization, the region is home today to the Eastern Band of Cherokee Indians, which continues to preserve many facets of traditional Cherokee culture. Beginning in the eighteenth century, European and African settlers moved into the mountains. The relative isolation of mountain life helped these settlers refine and preserve many traditions, most notably handmade crafts, traditional music, and local agricultural practices. Today, these distinctive cultural legacies are celebrated as living traditions, providing employment to master artists and tradition bearers and drawing tourists from across the globe to experience the region’s craft galleries, music halls, festivals, museums, farms, and local cuisine. photo courtesy of Blue Ridge National this project has been funded by Heritage Area a project of Blue Ridge National Heritage Area Designation A National Heritage Area is a place designated by the United States Congress where natural, cultural, historic, and recreational resources combine to form a cohesive, nationally distinctive landscape arising from patterns of human activity shaped by geography. Currently, there are 49 National Heritage Areas across the United States, where each area shares how their people, resources, and histories come together to provide experiences that “tell America’s story” and to encourage the community to join together around a common theme and promote the cultural, natural, and recreational benefits of the area. In November 2003, Western North Carolina (WNC) was designated the Blue Ridge National Heritage Area in recognition of the region’s agriculture, craft heritage, traditional music, the distinctive living traditions of Cherokee culture, and rich natural heritage, and their significance to the country. -
Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region. -
Geologic Framework of the Catalina Foothills, Outskirts of Tucson (Pima County, Arizona)
GEOLOGIC FRAMEWORK OF THE CATALINA FOOTHILLS, OUTSKIRTS OF TUCSON (PIMA COUNTY, ARIZONA) W.R. DICKINSON Emeritus, Dept. of Geosciences University of Arizona ARIZONA GEOLOGICAL SURVEY CONTRIBUTED MAP CM-99-B MAY 1999 31 p., scale 1 :24,000 TIus report is preliminary and has not been edited or reviewed for confonnity with Arizona Geological Survey standards. ARIZONA GEOLOGICAL SURVEY CONTRIBUTED MAP CM-99-B (31 pp., 1 Plate) Geologic Framework of the Catalina Foothills, Outskirts of Tucson (Pima County, Arizona) [Text and Legend to Accompany 1:24,000 Map] William R. Dickinson, Department of Geosciences, University of Arizona May 1999 Introduction and Purpose Past geologic maps and accounts of the sedimentary, geomorphic, and structural geology of the piedmont of the Santa Catalina Mountains in the outskirts of Tucson by Voelger (1953), Pashley (1966), Davidson (1973), Creasey and Theodore (1975), Banks (1976), Anderson (1987), Pearthree et al. (1988), McKittrick (1988), and Jackson (1989) raised questions about the sedimentary evolution of the foothills belt that were left open or unresolved. Multiple dissected alluvial fans and pediments overlie much older faulted and tilted strata to form Cenozoic sedimentary assemblages of considerable stratigraphic and structural complexity. As a contribution to improved understanding of urban geology in the Tucson metropolitan area, systematic geologic mapping of the piedmont belt was undertaken to establish the overall geologic framework of the Catalina foothills (~ 175 2 km ) at a common scale (1 :24,000). The area studied extends from Oracle Road on the west to the vicinity of Rinconado Road on the east, and from the Rillito River and Tanque Verde Wash northward to the limit of bedrock exposures at the base of the Santa Catalina Mountains. -
History of the Broad River Development from Henderson Island to Hampton Island
History of the Broad River Development From Henderson Island to Hampton Island Prepared For: South Carolina Electric & Gas Company 220 Operation Way Cayce, South Carolina 29033-3701 Prepared By: 521 Clemson Road Columbia, South Carolina 29229 December 2016 TABLE OF CONTENTS INTRODUCTION 2 DEVELOPMENTAL HISTORY 3 Early Settlement 3 The Revolutionary War 4 Civil War 5 Reconstruction – 20th Century 7 HYDROELECTRIC DEVELOPMENT 9 HISTORIC SITES 14 Parr Shoals 14 Fairfield Pumped Storage 19 Lyles Ford 22 REFERENCES 23 INTRODUCTION The existing Federal Energy Regulatory Commission (FERC) license for the Parr Hydroelectric Project (FERC Project No. 1894) expires on June 30, 2020. As a result, cultural resources investigations were conducted to assist the South Carolina Electric & Gas Company (SCE&G) in complying with the FERC relicensing process for the Parr Hydroelectric Project. The Parr Hydroelectric Project is located in central South Carolina along the Broad River in eastern Newberry County and western Fairfield County. The project includes both the Parr Shoals Development and the Fairfield Pumped Storage Facility Development. The total project area encompasses 4,400 acres on the Broad River and its tributaries between Henderson Island to the north and Hampton Island to the south, and Monticello Reservoir. As part of the FERC relicensing process, a Phase I cultural resources survey of the Parr Hydroelectric Project was completed in 2013 and 2014. Additional Phase II archaeological investigations were conducted in 2016 at two archaeological sites, 38NE8 and 38NE10. As a result of these investigations, four resources were identified as being eligible for inclusion in the National Register of Historic Places (NRHP): the Parr Shoals Development, the Fairfield Pumped Storage Facility, Lyles Ford; and archaeological site 38NE8. -
South Carolina Landform Regions (And Facts About Landforms) Earth Where Is South Carolina? North America United States of America SC
SCSouth Carolina Landform Regions (and facts about Landforms) Earth Where is South Carolina? North America United States of America SC Here we are! South Carolina borders the Atlantic Ocean. SC South Carolina Landform Regions Map Our state is divided into regions, starting at the mountains and going down to the coast. Can you name these? Blue Ridge Mountains Landform Regions SC The Blue Ridge Mountain Region is only 2% of the South Carolina land mass. Facts About the Blue Ridge Mountains . ◼ It is the smallest of the landform regions ◼ It includes the state’s highest point: Sassafras Mountain. ◼ The Blue Ridge Mountains are part of the Appalachian Mountain Range Facts About the Blue Ridge Mountains . ◼ The Blue Ridge Region is mountainous and has many hardwood forests, streams, and waterfalls. ◼ Many rivers flow out of the Blue Ridge. Blue Ridge Mountains, SC Greenville Spartanburg Union Greenwood Rock Hill Abbeville Piedmont Landform Regions SC If you could see the Piedmont Region from space and without the foliage, you would notice it is sort of a huge plateau. Facts About the Piedmont Region . ◼ The Piedmont is the largest region of South Carolina. ◼ The Piedmont is often called The Upstate. Facts About the Piedmont Region . ◼ It is the foothills of the mountains and includes rolling hills and many valleys. ◼ Piedmont means “foot of the mountains” ◼ Waterfalls and swift flowing rivers provided the water power for early mills and the textile industry. Facts About the Piedmont Region . ◼ The monadnocks are located in the Piedmont. ◼ Monadnocks – an isolated or single hill made of very hard rock. -
Water Quality
3. Existing Conditions and WaterEnvironmental Quality Consequences 3.6 Water Quality 3.6.1 CHANGES TO THIS CHAPTER SINCE THE DEIS Since the Draft Environmental Impact Statement (DEIS) the acreage of water resources in the project area have been updated to reflect the design changes resulting in the Refined Recommended Preferred Alternative (RPA); impacts resulting from the Refined RPA; and reflect the impacts to impervious and pervious surface areas of the Refined RPA. 3.6.2 HOW IS WATER QUALITY ASSESSED? The Clean Water Act (CWA) of 1972 requires that each state set water quality standards for all contaminants in surface waters. These standards are typically based on criteria recommended by the US Environmental In South Carolina, the SCDHEC Protection Agency (USEPA). The CWA also regulates the discharge of is responsible for monitoring pollutants into our state’s waters. In South Carolina, the USEPA has and regulating water quality delegated the responsibility of monitoring and regulating water quality for the USEPA. to the Department of Health and Environmental Control (SCDHEC). Many factors can affect water quality, including pesticides, heavy metals, livestock waste, litter, oils and grease, and other chemicals. Water from rain and runoff collect these pollutants and carry them into creeks and rivers. Natural resources and processes can also affect water quality. The amount of tree cover over streams and rivers can affect the temperature of the water, thereby affecting the habitat for other plants, fish, and insects. Additionally, sediment from erosion can wash downstream and impact the depth and important substrate within the stream. Existing Conditions and Environmental Consequences Water Quality FEIS May 2019 Page 3-237 3. -
New Particle Formation Infrequently Observed in Himalayan Foothills – Why?
Atmos. Chem. Phys., 11, 8447–8458, 2011 www.atmos-chem-phys.net/11/8447/2011/ Atmospheric doi:10.5194/acp-11-8447-2011 Chemistry © Author(s) 2011. CC Attribution 3.0 License. and Physics New particle formation infrequently observed in Himalayan foothills – why? K. Neitola1, E. Asmi1, M. Komppula2, A.-P. Hyvarinen¨ 1, T. Raatikainen1,3, T. S. Panwar4, V. P. Sharma4, and H. Lihavainen1 1Finnish meteorological Institute, Helsinki, Finland 2Finnish meteorological Institute, Kuopio, Finland 3Georgia Institute of Technology, Atlanta, Georgia, USA 4Energy and Resource Institute, New Delhi, India Received: 10 December 2010 – Published in Atmos. Chem. Phys. Discuss.: 29 April 2011 Revised: 29 July 2011 – Accepted: 16 August 2011 – Published: 19 August 2011 Abstract. A fraction of the Himalayan aerosols originate 1 Introduction from secondary sources, which are currently poorly quan- tified. To clarify the climatic importance of regional sec- Secondary particle formation from gaseous precursors is ondary particle formation in the Himalayas, data from 2005 largely recognised as an important worldwide mechanism in- to 2010 of continuous aerosol measurements at a high- creasing the number of atmospheric particles (Kulmala et al., altitude (2180 m) Indian Himalayan site, Mukteshwar, were 2004; Spracklen et al., 2006, 2009). While in the atmo- analyzed. For this period, the days were classified, and the sphere, these particles are affected by several physical and particle formation and growth rates were calculated for clear chemical processes influencing the particle climatic proper- new particle formation (NPF) event days. The NPF events ties, such as their scattering and absorbing characteristics and showed a pronounced seasonal cycle. The frequency of the their ability to act as Cloud Condensation Nuclei (CCN). -
Physiographic Map of Virginia Counties
Physiographic Map of FREDERICK Winchester CLARKE Virginia Counties LOUDOUN WARREN 2000 ARLINGTON FAUQUIER FAIRFAX C. Roberts & C.M. Bailey, College of William & Mary SHENANDOAHM RAPPAHANNOCK PRINCE F WILLIAM PAGE CULPEPER AP ML Modified from Virginia Division of Mineral Resources/ STAFFORD U.S. Geological Survey Map of Mineral Producing Localities ROCKINGHAM MADISON HIGHLAND Fredericksburg KING http://minerals.usgs.gov/minerals/pubs/state/985199mp.pdf RV GREENE GEORGE ORANGE WESTMORELAND 0 50 100 AUGUSTA ALBEMARLE SPOTSYLVANIA RICHMOND BATH Charlottesville CAROLINE miles GV LOUISA CU CU NORTHUMBERLAND KINGESSEX CL BM 0 50 100 ROCKBRIDGE nBR KING FLUVANNA HANOVER ALLEGHANY & LANCESTER kilometers NELSON WILLIAMQUEEN CL GOOCHLAND ACCOMACK HENRICO CU MIDDLESEX BM AMHERST BUCKINGHAM Richmond POWHATAN NEW GLOUCESTER BOTETOURT KENT MATHEWS CRAIG JAMES APPOMATTOX CHESTER CHARLES FIELD CITY CITY Lynchburg CUMBERLANDAMELIA CL YORK NORTHAMPTON GILES ROANOKE BEDFORD NEWPORT Roanoke PRINCE PRINCE NEWS BUCHANAN GEORGE RV MONTGOMERY CAMPBELL EDWARD NOTTOWAY DICKENSON BLAND SURRY HAMPTON TAZEWELL F DINWIDDIE AP PULASKI CHARLOTTE CU ISLE OF GV FRANKLIN SUSSEX WISE RUSSELL LUNENBURG WIGHT WYTHE FLOYD OP Norfolk BRUNSWICK SMYTH sBR VIRGINIA BEACH PITTSYLVANIA SOUTHAMPTON BM HALIFAX CHESAPEAKECL CARROLL MECKLENBURG PATRICK SCOTT WASHINGTON GRAYSON LEE HENRY GREEN- CL NANSEMOND SVILLE Appalachian Plateau Valley & Ridge Blue Ridge Piedmont Coastal Plain province province province province province AP- Rugged, well-dissected RV- Ridge & Valley nBR- northern Blue Ridge F- Foothills subprovince: CU- Upland subprovince: landscape with dendritic subprovince: long linear subprovince: rugged region region with broad rolling broad upland with low slopes drainage pattern. Elevation- ridges separated by linear with steep slopes narrow hills and moderate slopes. and gentle drainage divides. 1000'-3000' with High Knob valleys with trellis ridges, broad mountains, Elevation 400'-1000' with Steep slopes develop where dissected by stream erosion. -
Technical Memorandum
Technical Memorandum To: South Carolina Department of Natural Resources (DNR) South Carolina Department of Health and Environmental Control (DHEC) From: CDM Smith Date: January 2015 Subject: Methodology for Unimpaired Flow Development Saluda River Basin, South Carolina (Prepared as part of the South Carolina Surface Water Quantity Modeling Program) 1.0 Background and Objectives for Unimpaired Flows Unimpaired Flow (UIF) describes the natural hydrology of a river basin. UIFs quantify streamflows throughout a river basin in the absence of human intervention in the river channel, such as storage, withdrawals, discharges, and return flows. From this basis, modeling and decision making can be compared with pristine conditions. This memorandum explains the methods that will be employed to develop UIFs for South Carolina’s Saluda River basin. It describes data needs, methods for filling data gaps, and issues specific to the Saluda River basin. Once developed, UIFs will be input to the Simplified Water Allocation Model (SWAM) to evaluate surface water hydrology and operations throughout the basin. The UIFs for the Saluda Basin will extend from 1925-2013. UIFs will serve two purposes: ° UIFs will be the fundamental input to the model at headwater nodes and tributary nodes upstream of historic management activity, representing naturally occurring water in the riverways. Current and future management practices such as storage, withdrawals, and discharges will be superimposed on the UIFs. ° UIFs will provide a comparative basis for model results. The impacts of current and future management practices on flow throughout the river network can be compared to the natural conditions represented by the UIFs, and decisions about relative impacts can be well informed. -
Predictive Modeling: an Archeolgical Assessment of Duke Power Company's Proposed Cherokee Transmission Lines Veletta Canouts
University of South Carolina Scholar Commons Archaeology and Anthropology, South Carolina Research Manuscript Series Institute of 10-1981 Predictive Modeling: An Archeolgical Assessment of Duke Power Company's Proposed Cherokee Transmission Lines Veletta Canouts Follow this and additional works at: https://scholarcommons.sc.edu/archanth_books Part of the Anthropology Commons Recommended Citation Canouts, Veletta, "Predictive Modeling: An Archeolgical Assessment of Duke Power Company's Proposed Cherokee Transmission Lines" (1981). Research Manuscript Series. 173. https://scholarcommons.sc.edu/archanth_books/173 This Book is brought to you by the Archaeology and Anthropology, South Carolina Institute of at Scholar Commons. It has been accepted for inclusion in Research Manuscript Series by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. Predictive Modeling: An Archeolgical Assessment of Duke Power Company's Proposed Cherokee Transmission Lines Keywords Excavations, Duke Power Company, Transmission lines, Cherokee County, South Carolina, Archeology Disciplines Anthropology Publisher The outhS Carolina Institute of Archeology and Anthropology--University of South Carolina Comments In USC online Library catalog at: http://www.sc.edu/library/ This book is available at Scholar Commons: https://scholarcommons.sc.edu/archanth_books/173 PREDICTIVE MODELING: AN ARCHEOLOG~CAL ASSESSMENT OF DUKE POWER COMPANY'S PROPOSED CHEROKEE TRANSMISSION LINES by Veletta Canouts Research Manuscript Series 181 With Contributions by Paul E. Brockington, Jr. and Tommy Charles INSTITUTE OF ARCHEOLOGY AND ANTHROPOLOGY UNIVERSITY OF SOUTH CAROLINA COLUMBIA, SOUTH CAROLINA 29208 October 1981 The University of South Carolina offers equal opportunity in its employment, admissions and educational activities, in accordance with Title IX, Section 504 of the Rehabilitation Act of 1973 and other civil rights laws. -
A Photographic Field Guide to the Birds of India
© Copyright, Princeton University Press. No part of this book may be 4 BIRDS OF INDIAdistributed, posted, or reproduced in any form by digital or mechanical means without prior written permission of the publisher. INTRODUCTION Birds of the Indian subcontinent an overview by Carol and Tim Inskipp The Indian subcontinent has a great wealth of birds, making it a paradise for the birdwatcher. The classic Handbook of the Birds of India and Pakistan by Salim Ali and S Dillon Ripley, which covers the whole region and was first published in 1968-1975, lists over 1,200 species. With additional recording and following the more up-to-date nomenclature in the Howard and Moore Complete Checklist of Birds of the World edited by E. C. Dickinson (2003) the current species total for the subcontinent stands at 1,375 species – 13 per cent of the world’s birds. A further relevant reference is Birds of South Asia: the Ripley Guide by Pamela Rasmussen and John Anderton, which has adopted much narrower species Dr. Salim Ali limits and, consequently, the latest edition (2012) recognises 1451 species in the region. Note that less than 800 species are found in all of North America. The Indian subcontinent is species-rich partly because of its wide altitudinal range extending from sea level up to the summit of the Himalayas, the world’s highest mountains. Another reason is the region’s highly varied climate and associated diverse vegetation. The extremes range from the almost rainless Great Indian or Thar Desert, where temperatures reach over 55°C, to the wet evergreen forests of the Assam Hills where 1,300 cm of rain a year have bee recorded at Cherrapunji – one of the wettest places on Earth, and the Arctic conditions of the Himalayan peaks where only alpine flowers and cushion plants flourish at over 4,900 m.