Land Use This Chapter Describes the Proposed Land Use Plan for Garrett County
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Loudoun County African-American Historic Architectural Resources Survey
Loudoun County African-American Historic Architectural Resources Survey Lincoln "Colored" School, 1938. From the Library of Virginia: School Building Services Photograph Collection. Prepared by: History Matters, LLC Washington, DC September 2004 Sponsored by the Loudoun County Board of Supervisors & The Black History Committee of the Friends of the Thomas Balch Library Leesburg, VA Loudoun County African-American Historic Architectural Resources Survey Prepared by: Kathryn Gettings Smith Edna Johnston Megan Glynn History Matters, LLC Washington, DC September 2004 Sponsored by the Loudoun County Board of Supervisors & The Black History Committee of the Friends of the Thomas Balch Library Leesburg, VA Loudoun County Department of Planning 1 Harrison Street, S.E., 3rd Floor Leesburg, VA 20175 703-777-0246 Table of Contents I. Abstract 4 II. Acknowledgements 5 III. List of Figures 6 IV. Project Description and Research Design 8 V. Historic Context A. Historic Overview 10 B. Discussion of Surveyed Resources 19 VI. Survey Findings 56 VII. Recommendations 58 VIII. Bibliography 62 IX. Appendices A. Indices of Surveyed Resources 72 B. Brief Histories of Surveyed Towns, Villages, Hamlets, 108 & Neighborhoods C. African-American Cemeteries in Loudoun County 126 D. Explanations of Historic Themes 127 E. Possible Sites For Future Survey 130 F. Previously Documented Resources with Significance to 136 Loudoun County’s African-American History 1 Figure 1: Map of Loudoun County, Virginia with principal roads, towns, and waterways. Map courtesy of the Loudoun County Office of Mapping. 2 Figure 2. Historically African-American Communities of Loudoun County, Virginia. Prepared by Loudoun County Office of Mapping, May 15, 2001 (Map #2001-015) from data collected by the Black History Committee of the Friends of Thomas Balch Library, Leesburg, Va. -
Thenorthforkofbenscre
TTHHEE NNOORRTTHH FFOORRKK OOFF BBEENNSS CCRREEEEKK COLDWATER CONSERVATIION PLAN February 2014 PREPARED BY THE SOMERSET CONSERVATIION DIISTRIICT 1 Acknowledgements This plan was funded and developed by a grant awarded to the Somerset Conservation District by the Cold Water Heritage Partnership, which is a multifaceted joint venture between the Pennsylvania State Council of Trout Unlimited, The Foundation for Pennsylvania Watersheds, The Pennsylvania Department of Conservation and Natural Resources and The Pennsylvania Fish and Boat Commission. Author: Greg Shustrick, Somerset County Watershed Specialist GIS mapping: Amanda Deal Kind regards to the following contributors for their assistance with the plan development: o Mr. Richard Lorson, PFBC SW Region 8 Area Fisheries Manager o Mr. Michael Depew, PFBC Fisheries Biologist o Mr. Scott Alexander, PADEP Biologist o Mr. Len Lichvar, Somerset Conservation District Manager o Mr. Drew Walker, Somerset Conservation District Intern o Ms. Amanda Deal, Environmental Consultant o Ms. Samantha Kutskel, Coldwater Resource Specialist, PATU / CWP o Mr. James Shustrick, Public Volunteer o Mr. Chris Mahla, Public Volunteer o Mr. Travis Rudge, Public Volunteer o Mr. Andy Fresch, Public Volunteer o The Mountain Laurel Chapter of Trout Unlimited o The Greater Johnstown Water Authority o The Bens Creek Canoe Club SOMERSET CONSERVATION DISTRICT, 6024 GLADES PIKE, SOMERSET, PA 15501 www.somersetcd.com , 814.445.4652 X 5 [email protected] *Digital copies of this plan can be downloaded on the District’s website -
Route of Meriwether Lewis from Harpers Ferry, Va. to Pittsburgh, Pa
Route of Meriwether Lewis from Harpers Ferry, Va. to Pittsburgh, Pa. July 8 – July 15, 1803 by David T. Gilbert National Park Service Harpers Ferry, West Virginia May 5, 2003 (Revised September 28, 2015) Introduction The route which Meriwether Lewis traveled from Harpers Ferry, Virginia to Pittsburgh, Pennsylvania, between July 8 and July 15, 1803, has not been well documented 1. The only primary source we have is a letter Lewis penned to President Jefferson from Harpers Ferry on July 8, 1803: I shall set out myself in the course of an hour, taking the route of Charlestown, Frankfort, Uniontown and Redstone old fort to Pittsburgh, at which place I shall most probably arrive on the 15th.2 Route of Meriwether Lewis July 8-July 15, 1803 Pittsburgh R Elizabeth E V I Petersons R Brownsville Pennsylvania O I H (Redstone old fort) O Uniontown Farmington POT OMA Cumberland C R IV Grantsville E M R O Maryland Forks of N Cacapon Harpers O N Fort Ashby Ferry G Brucetown A (Frankfort) H E Gainesboro L A Winchester R I West Virginia V Charles Town E R Virginia 1. With the exception of quoted primary sources, this document uses the contemporary spelling, Harpers Ferry, and not the 19th century spelling, Harper’s Ferry. Harpers Ferry was part of Virginia until June 20, 1863, when the state of West Virginia was created by Presidential Proclamation. 2. Meriwether Lewis to Thomas Jefferson, July 8, 1803, quoted in Donald Jackson,Letters of the Lewis and Clark Expedition, With Related Documents, 1783-1854 (Champaign, Illinois: University of Illinois Press, 1979), 106-107. -
1 I-68/I-70: a WINDOW to the APPALACHIANS by Dr. John J
I-68/I-70: A WINDOW TO THE APPALACHIANS by Dr. John J. Renton Dept. of Geology & Geography West Virginia University Morgantown, WV Introduction The Appalachian Mountains are probably the most studied mountains on Earth. Many of our modern ideas as to the origin of major mountain systems evolved from early investigations of the Appalachian region. The Appalachians offer a unique opportunity to experience the various components of an entire mountain system within a relatively short distance and period of time. Compared to the extensive areas occupied by other mountain systems such as the Rockies and the Alps, the Appalachians are relatively narrow and can be easily crossed within a few hours driving time. Following I-68 and I-70 between Morgantown, WV, and Frederick, Maryland, for example, one can visit all of the major structural components within the Appalachians within a distance of about 160 miles. Before I continue, I would like to clarify references to the Allegheny and Appalachian mountains. The Allegheny Mountains were created about 250 million years ago when continents collided during the Alleghenian Orogeny to form the super-continent of Pangea (Figure 1). As the continents collided, a range of mountains were created in much the same fashion that the Himalaya Mountains are now being formed by the collision of India and Asia. About 50 million years after its Figure 1 1 creation, Pangea began to break up with the break occurring parallel to the axis of the original mountains. As the pieces that were to become our present continents moved away from each other, the Indian, Atlantic, and Arctic oceans were created (Figure 2). -
Cumberland Narrows: Portal to the National Road
12 m o u n t a i n d i s c o v e r i e s The Cumberland Narrows: Portal to the National Road Written by: Dan Whetzel New Photography by: Lance C. Bell he Cumberland Narrows has played an important events that occurred there have dimmed with the passing part Tin Western Maryland history, as it provided a natural of time. Cumberland’s Narrows is unique because it break in the Appalachian Mountains that stretched combines natural history with political, economic, and north/south through the region. Formed thousands of military events that have determined the course of our years ago, the Narrows is a one mile water gap dominated nation since 1755. To trace those recorded events, we at the lowest elevation by Will’s Creek and transportation need to turn back the clock to early European explorers arteries, while its higher elevations feature the spectacular and entrepreneurs who established themselves in lands beauty of Tuscarora and Juniata sandstone rock forma- formerly occupied by members of the Shawnee Tribe. tions. According to a geological report filed in 1978, Topography and abundant natural resources were key it was speculated the Narrows resulted from forces reasons Europeans migrated to Western Maryland during generated in the formation of the Eastern Appalachian the mid 18th century. The Ohio Trading Company con- Mountains. A stream began eroding the water gap structed a significant settlement in the area, a storehouse across Will’s Mountain and surrounding weaker rocks about one mile from the Narrows, at the confluence of were eroded into the valley, thereby causing a 900- foot Will’s Creek and the Potomac River. -
2013001396 01396AJM:CMM 01/07/13 a RESOLUTION Urging the Governor to Create a Commission, Or Take Other Executive Action, To
2013001396 01396AJM:CMM 01/07/13 A RESOLUTION 1 Urging the Governor to create a commission, or take other 2 executive action, to rename Negro Mountain in Somerset County 3 to accurately reflect the history of the region and to update 4 related governmental maps, brochures, plaques and signs. 5 WEREAS, Negro Mountain is an approximately 30-mile long ridge 6 of the Allegheny Mountains that spans from Maryland north into 7 the Casselman River in Somerset County, Pennsylvania; and 8 WHEREAS, The highest point of Negro Mountain, rising 3,213 9 feet, is the highest point in Pennsylvania; and 10 WHEREAS, In 1756 during the French and Indian War, a battle 11 on Negro Mountain ensued between a band of volunteers led by the 12 English-born pioneer Thomas Cresap and Native Americans on the 13 mountain; and 14 WHEREAS, Historical reports of the account, including reports 15 written by Cresap himself, note that while crossing the 16 mountain, a party of Native Americans fired upon the volunteers 17 and mortally wounded one of the “Negroes.” A piece of a hollow 18 log was found and placed over the “Negro” to shelter him, and, 20 13 DO 13 96 1 throwing it of f, he said, “Save yourselves and never mind me; I 2 shall die soon”; and 3 WHEREAS, Cresap wrote an account of the expedition for 4 Benjamin Franklin’s “Pennsylvania Gazette” of June 17, 1756; and 5 WHEREAS, It is said that Negro Mountain took its name from 6 this battle, notably from the heroism of the “Negro” who gave 7 his life to protect the other volunteers; and 8 WHEREAS, In 1882, J. -
G-I-E-195 Bloomington Survey District
G-I-E-195 Bloomington Survey District Architectural Survey File This is the architectural survey file for this MIHP record. The survey file is organized reverse- chronological (that is, with the latest material on top). It contains all MIHP inventory forms, National Register nomination forms, determinations of eligibility (DOE) forms, and accompanying documentation such as photographs and maps. Users should be aware that additional undigitized material about this property may be found in on-site architectural reports, copies of HABS/HAER or other documentation, drawings, and the “vertical files” at the MHT Library in Crownsville. The vertical files may include newspaper clippings, field notes, draft versions of forms and architectural reports, photographs, maps, and drawings. Researchers who need a thorough understanding of this property should plan to visit the MHT Library as part of their research project; look at the MHT web site (mht.maryland.gov) for details about how to make an appointment. All material is property of the Maryland Historical Trust. Last Updated: 12-01-2003 G-I-E-195 Bloomington Survey District Bloomington Private 1800-1899 The town of Bloomington is located on the southeast side of Backbone Mountain where the Savage River drains into the North Branch of the Potomac River. Roughly half a square mile in area, the town is bounded by the Savage River to the north, the Potomac to the east and south, and by Bloomington U111 to the west. The historic district comprises about seven blocks at the northern end of town banded by Virginia Avenue to the south, Hampshire Avenue and the County Road to the west, the Baltimore and Ohio Railroad to the northeast, and North Branch and Hamill Avenues to the east. -
7 Sensitive Areas Garrett County’S Physical Landscape Is Characterized by Mountainous Ridges, Stream Valleys, Extensive Forests, and Productive Agricultural Areas
2008 Garrett County Comprehensive Plan 7 Sensitive Areas Garrett County’s physical landscape is characterized by mountainous ridges, stream valleys, extensive forests, and productive agricultural areas. The County is home to the four highest mountains in Maryland, the state’s first designated Scenic and Wild River (the Youghiogheny River), and the state’s largest freshwater lake (Deep Creek Lake). These features are scenic and recreational resources for the County’s residents and visitors, and many are also environmentally sensitive. The Planning Act of 1992 and subsequent legislation requires each comprehensive plan in Maryland to establish goals and policies related to sensitive environmental areas, specifically addressing: • Steep slopes, • Streams, wetlands, and their buffers, • 100-year floodplains, • The habitat of threatened or endangered species, • Agricultural and forest land intended for resource protection or conservation, and • Other areas in need of special protection. The County’s Sensitive Areas Ordinance (adopted in 1997) and Floodplain Management Ordinance (adopted in 1991) provide detailed guidance for development affecting these sensitive areas. This chapter updates the 1995 Plan’s description of the County’s sensitive areas, and, in conjunction with the Water Resources and Land Use chapters of this Plan, further strengthens policies to protect sensitive areas. This chapter includes a discussion of ridgelines as a sensitive area in need of protection. 7.1 Goals and Objectives The County’s sensitive areas goal is: Continue to protect Garrett County’s sensitive environmental resources and natural features. The objectives for achieving this goal are: 1. Limit development in and near sensitive environmental areas, including steep slopes, streams, wetlands, 100-year floodplains, and the habitats of threatened or endangered species. -
Regional Seismic Lines Across the Rome Trough and Allegheny Plateau of Northern West Virginia, Western Maryland, and Southwestern Pennsylvania
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I–2791 U.S. GEOLOGICAL SURVEY REGIONAL SEISMIC LINES ACROSS THE ROME TROUGH AND ALLEGHENY PLATEAU OF NORTHERN WEST VIRGINIA, WESTERN MARYLAND, AND SOUTHWESTERN PENNSYLVANIA By Christopher S. Kulander 1 and Robert T. Ryder 2 INTRODUCTION having thin-skinned structures with greater tectonic shortening. These provinces meet at a physiographic and structural boundary The study area for this investigation is the central Appalachian called the Allegheny structural front. The Rome trough, a north basin (see index map below). The northern West Virginia, west east-trending graben that involves basement, underlies the ern Maryland, and southwestern Pennsylvania parts of the cen Allegheny Plateau (fig. 2). Commonly, basement rocks in the tral Appalachian basin consist of complex structural geometries Rome trough are buried beneath at least 20,000 feet (ft) of and a thick Paleozoic sequence. Here, the basin coincides with Paleozoic strata (Shumaker, 1996). Little has been published that is related to the deep structure of 80˚ the Rome trough in northern West Virginia, western Maryland, and southwestern Pennsylvania. Wells drilled to basement are absent here and most of the multi-fold seismic data are propri etary. Although Ryder (1991) and Ryder and others (1992) con NY structed several detailed stratigraphic cross sections of Cambrian and Ordovician strata across parts of the Rome trough and Shumaker (1996) mapped basement structure along the entire PA NJ 40˚ Rome trough from central Kentucky to northeastern Pennsylvania, few interpreted, regional seismic-based geologic OH MD DE cross sections have been published in this area. The objective of this investigation is to interpret the structure and stratigraphy of 40˚ WV the Rome trough and Allegheny Plateau of northern West VA Virginia, western Maryland, and southwestern Pennsylvania KY based on three multi-fold seismic lines acquired by Amoco in the early 1980s. -
Geology and Mining Activities
IV-l IV GEOLOGY AND MINING ACTIVITIES 1. GEOLOGY All of the Youghiogheny Basin lies within the Applachian Plateaus Province. Some 30%, west of Chestnut Ridge, is in the Pittsburgh Plateaus Section of the province and the rest is in the Allegheny Mountain Section. A series of folds creates ridges and valleys which generally trend SW to NE. Folds east of Chestnut Ridge are closer and more uniform. West of Chestnut Ridge is more mountainous and includes Mt. Davis formed by the Negro Mountain Anticline, and which is the highest point in Pennsylvania, elev 3,213 ft. Prominent structural features are shown in Figure 1. Those of particular importance to mine drainage pollution are, from west to east: Important Important Structure Strata Group Coal Pigeon Creek Syncline Monongahela Pittsburgh Irwin Syncline Monongahela Pittsburgh Greensburg Syncline Monongahela Pittsburgh Latrobe Syncline Monongahela Pittsburgh Uniontown Syncline Monongahela Pittsburgh Ligonier Syncline Allegheny L. Kittanning Centerville Dome Allegheny L. Freeport Negro Mt. Anticline Allegheny L. Kittanning & Brookville Berlin Syncline Monongahela Pittsburgh & Allegheny L. Kittanning & U. Kittanning These geologic structures are discussed starting on page IV-4. A generalized tabulation of the stratigraphy is included in Table IV-A. The Washington Group is not included since this has been eroded away except on a few hilltops in the deepest syncline basins. IV-2 Table IV-A, Geologic Strata Age Group Thickness Members Thickness Pennsylvanian Monongahela 260-400’ Waynesburg Coal 3 -9’ Waynesburg Limestone 0-20’ Uniontown Sandstone 10-20’ Uniontown Coal 0 -2’ Uniontown Limestone 25-45’ Benwood Limestone 30-60’ Sewickley Sandstone 0-60’ SEWICKLEY COAL* 0-10’ Fishpot Limestone 5-30’ REDSTONE COAL* 1 -5’ Redstone Limestone 5-20’ Pittsburgh Sandstone 12-70’ PITTSBURGH COAL** 6 -14’ Pennsylvanian Conemaugh 500-750’ Little Pittsburgh Coal 0-l Connellsville Sandstone 5 -50’ Clarksburg Limestone 0 -7’ Morgantown Sandstone 5 -120’ Birmingham Shale 50 -60’ L. -
2019 Regular Session
HJ 10 Department of Legislative Services Maryland General Assembly 2019 Session FISCAL AND POLICY NOTE First Reader House Joint Resolution 10 (Delegate Mosby) Rules and Executive Nominations Commission to Rename Negro Mountain This joint resolution requires the Governor, in consultation with the Maryland State Archives (MSA), the Maryland Geological Survey (MGS), and the Department of Natural Resources (DNR), to establish a commission to rename Negro Mountain in Garrett County. By December 31, 2019, the commission must inform the Governor, the General Assembly, MSA, MGS, and DNR of the new name selected for the mountain. Fiscal Summary State Effect: Compliance with the joint resolution can be absorbed within existing budgeted resources. Local Effect: Potential minimal increase in local expenditures to change signs and maps. Small Business Effect: None. Analysis Background: Maryland has more than 60 mountain ranges and hills, which are located largely in the western portion of the State. Negro Mountain is a 30-mile long ridge of the Allegheny Mountains extending from Garrett County, Maryland to Somerset County, Pennsylvania. The mountain rises to an elevation of 3,075 feet above sea level. The U.S. Board on Geographic Names, which consists of representatives from several federal agencies, is charged with standardizing geographic names for use by the federal government. The board promulgates official geographic names and principles, policies, and procedures governing geographic name usage. According to the Maryland Department of Planning, the Maryland Geographic Names Authority within the Maryland Historical Trust coordinates naming activity between local, State, and federal agencies, reviews geographic name proposals, and makes recommendations to the board. -
How They Named the Western Maryland Mountains • Part III
56 m o u n t a i n d i s c o v e r i e s How They Named the Western Maryland Mountains • Part III If you stand high up on Wills Mountain in Cumberland, “Will” certainly doesn’t sound like an Indian name. you can look down on “The Narrows” mountain gap and But English settlers sometimes used nicknames for Indians imagine pioneer families in their covered wagons, driving they knew, probably because they found Indian names west through the gap in the early 1800s. You can picture hard to pronounce and spell. Lowdermilk didn’t mention runaway slaves as they may have traveled through the Narrows, Will’s tribe, nor call him a chief; but others later called hidden in wagons driven by black teamsters who were hauling him Chief Will. Lowdermilk presented Will as a benign cargo to Pennsylvania. You can imagine private coaches and fellow who gave “a kindly greeting” to English settlers stagecoaches rumbling through in the other direction, carrying and lived in “intimate friendship with them.” He said the presidents and other political leaders east to Washington. settlers gave Will “some trifl e as a pretended compensation” when they obtained grants to his land. He indicated that A 1755 map showed Wills Creek; and Charles Mason, Will died in the early 1780s and was buried on top of of the Mason-Dixon surveying team, mentioned “Will’s Creek Wills Knob, a hill near Wills Mountain. Mountain” in his 1760s journal. Early travellers used the Wills Creek name for what soon would be called Cumberland.