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Morgan County Relocation Package
Morgan County Relocation Package Long & Foster/Webber & Associates, Realtors® 480 W. Jubal Early Drive, Suite 100 Winchester, Virginia 22601 Office: 540-662-3484 - Toll Free: 800-468-6619 www.webberrealty.com TABLE OF CONTENTS INTRODUCTION ---------------------------------------------------------------------------------2 GOVERNMENT -----------------------------------------------------------------------------------3 TAXES ---------------------------------------------------------------------------------------------4-5 LICENSE ------------------------------------------------------------------------------------------5-6 IMPORTANT NUMBERS -----------------------------------------------------------------------7 HEALTH ------------------------------------------------------------------------------------------8-9 CLIMATE ------------------------------------------------------------------------------------------10 POPULATION --------------------------------------------------------------------------------10-11 CHURCHES ---------------------------------------------------------------------------------------12 TEMPORARY LODGING -----------------------------------------------------------------12-14 SHOPPING ----------------------------------------------------------------------------------------15 TRANSPORTATION ---------------------------------------------------------------------------16 SCHOOLS -------------------------------------------------------------------------------------17-18 LIBRARIES ---------------------------------------------------------------------------------------19 -
Determining the Geometry and Former Extent of the North Mountain Thrust from Fluid Inclusion and Microstructural Analysis
DETERMINING THE GEOMETRY AND FORMER EXTENT OF THE NORTH MOUNTAIN THRUST FROM FLUID INCLUSION AND MICROSTRUCTURAL ANALYSES Megan Castles A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE May 2010 Committee: Charles Onasch, Advisor James Evans John Farver ii ABSTRACT Charles Onasch, Advisor Fluid inclusion microthermometry, microstructural analysis, and vitrinite reflectance measurements were used to determine pressure and temperature conditions in several Paleozoic rock units in the Valley and Ridge province in order to determine the former extent and geometry of the North Mountain thrust sheet. Overburden thicknesses determined for the Devonian Hampshire/Catskill Formation, Mississippian Pocono Sandstone, and Pennsylvanian Pottsville Sandstone were found to be 5.5-6.0, 4.5-10.5, and 4.8-8.0 km, respectively. Differences in salinity and CH4 content between the Hampshire/Catskill Formation and the Pocono Sandstone and Pottsville Formation indicate that the Hampshire/Catskill Formation was affected by fluids from a different source than the younger units. These fluids were also cooler than those in overlying units, which explains why the older Hampshire/Catskill Formation yielded lower overburden thicknesses. All units experienced considerably greater overburdens than can be explained stratigraphically, which supports the model of Evans (1989) that the North Mountain thrust once extended over these rocks so that the large overburdens are of tectonic origin. iii This paper is dedicated to my family and loved ones. Especially my parents Kevin and Mary Castles who have always had faith in my abilities and pride in my accomplishments, I could not have completed this project without their love and support. -
US Geological Survey Karst Interest Group Proceedings, Fayetteville
Prepared In Cooperation with the Department of Geosciences at the University of Arkansas U.S. Geological Survey Karst Interest Group Proceedings, Fayetteville, Arkansas, April 26-29, 2011 Scientific Investigations Report 2011-5031 U.S. Department of the Interior U.S. Geological Survey Prepared in Cooperation with the Department of Geosciences at the University of Arkansas U.S. Geological Survey Karst Interest Group Proceedings, Fayetteville, Arkansas, April 26–29, 2011 Edited By Eve L. Kuniansky Scientific Investigations Report 2011–5031 U.S. Department of the Interior U.S. Geological Survey i U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia 2011 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Kuniansky,E.L., 2011, U.S. Geological Survey Karst Interest Group Proceedings, Fayetteville, Arkansas, April 26-29, 2011, U.S. Geological Survey Scientific Investigations Report 2011-5031, 212p. Online copies of the proceedings area available at: http://water.usgs.gov/ogw/karst/ Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. -
National Register of Historic Places Inventory -- Nomination Form Owner
Form No. 10-300 REV. (9/77) UNITED STATES DEPARTMENT OF THE INTERIOR NATIONAL PARK SERVICE NATIONAL REGISTER OF HISTORIC PLACES INVENTORY -- NOMINATION FORM SEE INSTRUCTIONS IN HOWTO COMPLETE NATIONAL REGISTER FORMS ___________ TYPE ALL ENTRIES - COMPLETE APPLICABLE SECTIONS JLNAME it jTXlViJ-j ..• '»A*?4 N^- '1'^..--fe *|C-'H £*1-.>--w * «L' ^>---" .&^..,iLa; .:. rf(\ HISTORIC HLstsrie Res0arbes of BexteLey G^uaty, West Virginia .(?ar^Lal Inveateryt %st©ripal and Arehiteotural Properties) AND/OR COMMON * ~T~ —————— . LOCATION eatisty limits of Berkeley Cofcaty and tfeat part of tjbe Pofcowac VTRiET&NOM^ER 41iat borders'-6n the a©4nty line* Note* %taership of til© is CITY, TOWN CONGRESSIONAL DISTRICT VICiNITYOF STATE 'CODE COUNTY ' CODE 003 CATEGORY OWNERSHIP STATUS RRESENTUSE _^PUBlilC ,) : ^-OCCUPIED; X-AGRICULTURE JEMUSEUM 1 .! ,= -; _LPRIV.ATE;r ' :; ^^-UNOCCUPIEd X^COMMERCIAL JCPARK -',. ^.STRUCTURE v -JSBQTHU 4 , -iWORK IN -PROGRESS X_EDUCATIONAL ? r JtPRIVATE RESIDENCE _SITE , . PUBMCACpUISKTIONM ACCESSIBLE X-ENTCRTAINMENT JCRELIGIOUS OBJECT -...- A lulNiPRdCESS ; i» ... ±^YES: RESTRICTED 3£_GOVERNMENT SCIENTIFIC Ifeltiple Resottrces BEING^GONSIDERED ? <*vYES: UNRESTRICTED ^INDUSTRIAL » ^TRANSPORTATION - '-- • --> > ,-' •(»•?.-* v •« r'::»•» --. ;..| •. i . - , '-'_NO.- - .-'A • 3C_M4LITARY OTHER: OWNER OF PRO1ERTY NAME vi<'r STREET & NUMBER' *'• CITY. TOWN v VICINITY OF LOCATION OF LEGAL DESCRIPTION COURTHOUSE. REGISTRY OF DEEDa STREET &'NUMBER CITY, TOWN STATE Marti usfcurg, West Virginia REPRESENTATION Iltf.EXISTING SURVEYS Berkeley -
Inf-1 Chapter 4
CHAPTER 4 – PUBLIC UTILITIES AND INFRASTRUCTURE Introduction Infrastructure is typically limited to those services found in an urban setting made available under finite conditions. These services include water, sewer, solid waste, electricity, communications, and other related utilities. Most of these services are regulated by the Public Service Commission for rates to the customer and by State Environmental Authorities for capacity limitations and expansion. This arrangement governs the regulated cost to the consumer as well as the physical impacts expansion of such services may have on the community and environment. This chapter provides an overview of the historic methods of provision and regulation of these services, as well as the current trends experienced by each. It also outlines existing and projected deficiencies in order to establish goals for both corrective measures and adequate realistic projections to ensure that services are extended appropriately for the foreseeable future. Water A water system is defined by the West Virginia Department of Health as any water system or supply which regularly supplies or offers to supply, piped water to the public for human consumption, if serving at least an average of 25 individuals per day for at least 60 days per year, or which has at least 15 service connections. In Morgan County, there are three distinct methods by which water is provided. They include: public systems owned and operated by a government entity, community systems typically owned by an association of users and maintained by private contract, and private wells that are owned and operated to serve a limited number of customers or larger single user that still meets the above criteria. -
GPS/Tachymetry) and GIS
Ecological Assessment of Springs and Spring Brooks in the Swiss National Park: Combining Fieldwork with Geodesy (GPS/Tachymetry) and GIS Diploma Thesis by Michael Döring Written at the Swiss Federal Institute for Environmental Science and Technology (EAWAG) Supervised by Dr. Urs Uehlinger PD Dr. Christopher T. Robinson (EAWAG, Switzerland) Diploma Professor: Prof. Dr. Thomas Schmitt (Ruhr Universität Bochum, Germany) Table of contents Table of contents I SUMMARY......................................................................................................................1 II ZUSAMMENFASSUNG ................................................................................................3 1 INTRODUCTION...........................................................................................................5 1.1 HISTORY .......................................................................................................................5 1.2 STUDIES ON SPRINGS.....................................................................................................5 1.3 ECOLOGY OF SPRINGS ...................................................................................................6 1.4 OBJECTIVES OF THE STUDY ...........................................................................................8 2 DESCRIPTION OF THE STUDY AREA ....................................................................9 2.1 GEOGRAPHICAL SITUATION ..........................................................................................9 2.2 SWISS NATIONAL -
Gazetteer of West Virginia
Bulletin No. 233 Series F, Geography, 41 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIKECTOU A GAZETTEER OF WEST VIRGINIA I-IEISTRY G-AN3STETT WASHINGTON GOVERNMENT PRINTING OFFICE 1904 A» cl O a 3. LETTER OF TRANSMITTAL. DEPARTMENT OP THE INTEKIOR, UNITED STATES GEOLOGICAL SURVEY, Washington, D. C. , March 9, 190Jh SIR: I have the honor to transmit herewith, for publication as a bulletin, a gazetteer of West Virginia! Very respectfully, HENRY GANNETT, Geogwvpher. Hon. CHARLES D. WALCOTT, Director United States Geological Survey. 3 A GAZETTEER OF WEST VIRGINIA. HENRY GANNETT. DESCRIPTION OF THE STATE. The State of West Virginia was cut off from Virginia during the civil war and was admitted to the Union on June 19, 1863. As orig inally constituted it consisted of 48 counties; subsequently, in 1866, it was enlarged by the addition -of two counties, Berkeley and Jeffer son, which were also detached from Virginia. The boundaries of the State are in the highest degree irregular. Starting at Potomac River at Harpers Ferry,' the line follows the south bank of the Potomac to the Fairfax Stone, which was set to mark the headwaters of the North Branch of Potomac River; from this stone the line runs due north to Mason and Dixon's line, i. e., the southern boundary of Pennsylvania; thence it follows this line west to the southwest corner of that State, in approximate latitude 39° 43i' and longitude 80° 31', and from that corner north along the western boundary of Pennsylvania until the line intersects Ohio River; from this point the boundary runs southwest down the Ohio, on the northwestern bank, to the mouth of Big Sandy River. -
An Archaeological Investigation and Technological
AN ARCHAEOLOGICAL INVESTIGATION AND TECHNOLOGICAL ANALYSIS OF THE STOCKHOFF BASALT QUARRY , NORTHEASTERN OREGON By BRUCE RAYMOND WOMACK A thesis submitted in partial f ulfil l ment of the requirements for the degree of MASTER OF ARTS ~vASHINGTON STATE UNIVERS I TY Department of Anthropology 1977 r r r v r AN ARCHAEOLOGICAL INVESTIGATION AND TECHNOLOGICAL r ANALYSIS OF THE STOCKHOFF BASALT QUARRY, r NORTHEASTERN OREGON ABSTRACT r by Bruce Raymond Womack, M.A. Washington State University, 1977 r I Chairman: Frank C. Leonhardy J ~ i i The Stockhoff Basalt Quarry (35UN52) is located the Blue Mountains f in r ~ of northeastern Oregon, 19 km southeast of La Grande. The site lies along a r small tributary of Ladd Creek in the upper end of Ladd Canyon. During surface collection and excavation, over 700 basalt implements r and 3900 pieces of chipping detritus were recovered. A test excavation which r revealed the presence of basalt implements beneath a deposit of Mazama ash indicated exploitation of the site's lithic resources by 6700 B.P. The imple- r ments recovered from the site bear a strong technomorphological resemblance to implements of the Cascade Phase 8000-4500 B.P. This suggests that the r site's lithic resources may have been exploited as early as 8000 B.P. The r paucity of diagnostic lithic material post-dating the Cold Springs Horizon 6000-4000 B.P. suggests non-utilization of these resources after 4000 B.P. I r ( The Stockhoff site served aboriginal folk as a major source of lithic raw material for approximately 4000 years. -
Origin of the Tucannon Phase in Lower Snake River Prehistory
AN ABSTRACT OF THE THESIS OF Steven W. Lucas for the degree of Master of Arts in Interdisciplinary Studies in Anthropology, Anthropology, and Geography presented on September 29, 1994. Title: The Origin of the Tucannon Phase in Lower Snake River Prehistory. Abstract approved: Redacted for Privacy David R. Brauner Approximately 5,500 years ago a discreet period of wetter and cooler environmental conditions prevailed across the southern Columbia Plateau. This period was marked by the first prominent episodes of erosion to occur along the lower Snake River following the height of the Altithermal and eruption of Mt. Mazama during the mid post-glacial. In addition to the reactivation of small stream courses choked with debris and sediment, large stream channels began downcutting and scouring older terrace faces incorporated with large accumulations of Mazama ash. The resulting degradation of aquatic habitats forced concurrent changes within human economies adapted to the local riverine-environments. These adjustments reported for the Tucannon phase time period along the lower Snake River are notable and demonstrate the degree to which Cascade phase culture was unsuccessful in coping with environmental instability at the end of the Altithermal time period. This successionary event has demonstratively become the most significant post-glacial, qualitative change to occur in the lifeways of lower Snake River people prior to Euro-American influence. © Copyright by Steven W. Lucas September 29, 1994 All Rights Reserved Origin of the Tucannon Phase in Lower Snake River Prehistory By Steven W. Lucas A THESIS Submitted to Oregon State University in partial fulfillment of the requirements for the degree of Master of Arts in Interdisciplinary Studies Completed September 29, 1994 Commencement June 1995 Master of Arts in Interdisciplinary Studies thesis of Steven W. -
Basin Descriptions and Flow Characteristics of Ohio Streams
Ohio Department of Natural Resources Division of Water BASIN DESCRIPTIONS AND FLOW CHARACTERISTICS OF OHIO STREAMS By Michael C. Schiefer, Ohio Department of Natural Resources, Division of Water Bulletin 47 Columbus, Ohio 2002 Robert Taft, Governor Samuel Speck, Director CONTENTS Abstract………………………………………………………………………………… 1 Introduction……………………………………………………………………………. 2 Purpose and Scope ……………………………………………………………. 2 Previous Studies……………………………………………………………….. 2 Acknowledgements …………………………………………………………… 3 Factors Determining Regimen of Flow………………………………………………... 4 Weather and Climate…………………………………………………………… 4 Basin Characteristics...………………………………………………………… 6 Physiology…….………………………………………………………… 6 Geology………………………………………………………………... 12 Soils and Natural Vegetation ..………………………………………… 15 Land Use...……………………………………………………………. 23 Water Development……………………………………………………. 26 Estimates and Comparisons of Flow Characteristics………………………………….. 28 Mean Annual Runoff…………………………………………………………... 28 Base Flow……………………………………………………………………… 29 Flow Duration…………………………………………………………………. 30 Frequency of Flow Events…………………………………………………….. 31 Descriptions of Basins and Characteristics of Flow…………………………………… 34 Lake Erie Basin………………………………………………………………………… 35 Maumee River Basin…………………………………………………………… 36 Portage River and Sandusky River Basins…………………………………….. 49 Lake Erie Tributaries between Sandusky River and Cuyahoga River…………. 58 Cuyahoga River Basin………………………………………………………….. 68 Lake Erie Tributaries East of the Cuyahoga River…………………………….. 77 Ohio River Basin………………………………………………………………………. 84 -
U.S. Geological Survey Karst Interest Group Proceedings, San Antonio, Texas, May 16–18, 2017
A Product of the Water Availability and Use Science Program Prepared in cooperation with the Department of Geological Sciences at the University of Texas at San Antonio and hosted by the Student Geological Society and student chapters of the Association of Petroleum Geologists and the Association of Engineering Geologists U.S. Geological Survey Karst Interest Group Proceedings, San Antonio, Texas, May 16–18, 2017 Edited By Eve L. Kuniansky and Lawrence E. Spangler Scientific Investigations Report 2017–5023 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN ZINKE, Secretary U.S. Geological Survey William 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 https://www.usgs.gov/ or call 1–888–ASK–USGS (1–888–275–8747). For an overview of USGS information products, including maps, imagery, and publications, visit https://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: Kuniansky, E.L., and Spangler, L.E., eds., 2017, U.S. Geological Survey Karst Interest Group Proceedings, San Antonio, Texas, May 16–18, 2017: U.S. Geological Survey Scientific Investigations Report 2017–5023, 245 p., https://doi.org/10.3133/sir20175023. -
Hydrogeology and Ground-Water Monitoring of Coal-Ash Disposal Sites in a Karst Terrane Near Burnside, South-Central Kentucky
ISSN 0075-5591 Kentucky Geological Survey Donald C. Haney, State Geologist and Director University of Kentucky, Lexington Hydrogeology and Ground-Water Monitoring of Coal-Ash Disposal Sites in a Karst Terrane near Burnside, South-Central Kentucky Shelley Minns Hutcheson Lyle V.A. Sendlein James S. Dinger James C. Currens Arsin M. Sahba Report of Investigations 11 Series XI, 1997 DISCLAIMER The Kentucky Geological Survey provides online versions of its publications as a public service. Publications are provided as Adobe PDF (portable document format) files. Hard- copy versions are available for purchase by contacting the Survey at: Kentucky Geological Survey Publication Sales Office 228 Mining and Mineral Resources Building University of Kentucky Lexington, Kentucky 40506-0107 Phone: 606-257-5500 Fax: 606-257-1147 Selected KGS reports published before 1999 have been scanned and converted to PDF format. Scanned documents may not retain the formatting of the original publication. In addition, color may have been added to some documents to clarify illustrations; in these cases, the color does not appear in the original printed copy of the publication. Every effort has been made to ensure the integrity of the text. KGS maps and charts are supplied either whole or in part and some are too large to be printed on most plotters. Open-file reports are reproduced from the best available copy provided by the author, and have not undergone KGS technical or editorial review. The Kentucky Geological Survey disclaims all warranties, representations, or endorsements, expressed or implied, with regard to the information accessed from, or via, this server or the Internet.