Virginia State Route 9
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Virginia State Route 9
Virginia State Route 9 (SR 9) is a primary state highway in the U.S. state of Virginia. Known as Charles Town Pike, the state highway runs from the West Virginia state line near Mechanicsville, where the highway continues west as West Virginia Route 9 (WV 9), east to SR 7 and SR 7 Business in Paeonian Springs. SR 9 is the main east–west highway of northwestern Loudoun County, connecting Leesburg with Hillsboro and the West Virginia cities of Charles Town and Martinsburg. As a result, the state highway and its West Virginia continuation are a major, overburdened commuter route between the Eastern Panhandle of West Virginia and Washington, D.C. Route description SR 9 begins at the West Virginia state line at Keyes Gap, a wind gap on top of Blue Ridge Mountain. The highway continues west as WV 9 to Charles Town. SR 9 heads southeast as a two-lane undivided road, passing to the west of Purcell Knob as the highway descends Blue Ridge Mountain to the village of Me ...
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Virginia D6-V1
Virginia, officially the Commonwealth of Virginia, is a state in the Mid-Atlantic and Southeastern regions of the United States, between the Atlantic Coast and the Appalachian Mountains. The geography and climate of the Commonwealth are shaped by the Blue Ridge Mountains and the Chesapeake Bay, which provide habitat for much of its flora and fauna. The capital of the Commonwealth is Richmond; Virginia Beach is the most-populous city, and Fairfax County is the most-populous political subdivision. The Commonwealth's population was over 8.65million, with 36% of them living in the Baltimore–Washington metropolitan area. The area's history begins with several indigenous groups, including the Powhatan. In 1607, the London Company established the Colony of Virginia as the first permanent English colony in the New World. Virginia's state nickname, the Old Dominion, is a reference to this status. Slave labor and land acquired from displaced native tribes fueled the growi ...
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Clarke's Gap
Clarke's Gap, also known as Clarks Gap, is a pass through Catoctin Mountain west of Leesburg, Virginia. The gap has an elevation of . The gap is not a true wind gap, but rather a man-made railroad cut through a local saddle point between two ridges to the southeast and northwest created by the drainage of Dry Mill Branch of Tuscarora Creek to the east and an unnamed tributary of Catoctin Creek to the west. The original road between Alexandria and Winchester, known as Vestal's Gap or Braddock's Road passed through the gap beginning in the middle 18th century. Later, in the 1860s the Alexandria, Loudoun and Hampshire Railroad, predecessor of the Washington and Old Dominion Railroad was routed through the gap. The railroad christened the gap when it established a station there, naming it after a nearby landowner, Addison H. Clarke. Today, Dry Mill Road (Virginia State Route 699 (VA Route 699)) and the Washington and Old Dominion Trail still pass through the gap. VA Route 7 ...
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Virginia State Route 287
State Route 287 (SR 287) is a primary state highway in the U.S. state of Virginia. Known as Berlin Pike, the state highway runs from SR 7 Business in Purcellville north to the Maryland state line at the Potomac River near Lovettsville, where the highway continues as Maryland Route 17 (MD 17). SR 287 is the main north–south highway of the Catoctin Valley of northern Loudoun County. Route description SR 287 begins at a roundabout with SR 7 Business (Main Street) on the east side of Purcellville. The state highway heads north as a two-lane undivided road that passes between a residential subdivision and Patrick Henry College. At the north town limit of Purcellville, SR 287 meets SR 7 (Harry Byrd Highway) at a diamond interchange. Within this interchange, SR 287 parallels the Washington and Old Dominion Trail, whose western terminus is in Purcellville. The rail trail intersects the highway on its way east toward Leesburg immediately north of the interchange. S ...
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Catoctin Valley
The Catoctin Valley is a small valley, geographically and culturally associated with the larger Loudoun Valley in Loudoun County, Virginia. Geography The Catoctin Valley encompasses the northern part of the Loudoun Valley east of the Short Hill Mountain and west of Catoctin Mountain. Its northern border is the Potomac River, while its southern border is an intangible line running from the southern terminus of the Short Hill to the base of Catoctin Mountain, located approximately two miles north of Virginia State Route 7. Across the Potomac in Maryland, the valley continues on as the Middletown Valley, which historically has also been known as the Catoctin Valley. The valley contains the communities of Waterford, Lovettsville, Wheatland, Morrisonville and Taylorstown. The valley is approximately wide east to west and {{convert, 11, mi, km long north to south. The valley is drained by the Catoctin Creek and its tributaries. Transportation Virginia State Route 287, the ...
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Short Hill Mountain
Short Hill Mountain is a mountain ridge of the Blue Ridge Mountains in northwest Loudoun County, Virginia. Geography Short Hill rises sharply from the Piedmont countryside of the Loudoun Valley, northwest of Purcellville. It is a low-lying ridge, barely over in elevation. The mountain ridge extends northeast for approximately before descending to the Hillsboro Gap, through which the North Fork of Catoctin Creek flows and the town of Hillsboro is located. North of the gap, the ridge quickly achieves heights of greater than , and continues for , gradually gaining elevation, before dropping precipitously to the Potomac River. The portion of the mountain south of Hillsboro Gap is known as Signal Mountain for the Union Army signaling station located on its summit during the American Civil War. North of the Potomac, the ridge continues as South Mountain in Maryland and Pennsylvania. Short Hill is about east of the crest of the Blue Ridge Mountain, which forms the western bor ...
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Water Gap
A water gap is a gap that flowing water has carved through a mountain range or mountain ridge and that still carries water today. Such gaps that no longer carry water currents are called wind gaps. Water gaps and wind gaps often offer a practical route for road and rail transport to cross the mountain barrier. Geology A water gap is usually an indication of a river that is older than the current topography. The likely occurrence is that a river established its course when the landform was at a low elevation, or by a rift in a portion of the crust of the earth having a very low stream gradient and a thick layer of unconsolidated sediment. In a hypothetical example, a river would have established its channel without regard for the deeper layers of rock. A later period of uplift would cause increased erosion along the riverbed, exposing the underlying rock layers. As the uplift continued, the river, being large enough, would continue to erode the rising land, cutting thr ...
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Hillsboro Gap
Hillsboro Gap, also known as the Gap in the Short Hill is a water gap in the Short Hill Mountain formed by the North Fork of the Catoctin Creek in Loudoun County, Virginia. The gap derives its name from the town of Hillsboro, which is nestled in the gap. Virginia State Route 9 passes through the gap in the town. In colonial times the main road between Alexandria and Winchester Winchester is a City status in the United Kingdom, cathedral city in Hampshire, England. The city lies at the heart of the wider City of Winchester, a local government Districts of England, district, at the western end of the South Downs Nation ..., Vestal's Gap Road, passed through the gap. That road eventually became the Charles Town Pike and modern day Route 9. The gap poses a substantial barrier to the widening of the congested road as the historic town completely fills the gap and as such Route 9 would have to be routed around or over the Short Hill Mountain to be widened. References *Scheel, ...
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Catoctin Creek (Virginia)
Catoctin Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed August 15, 2011 tributary of the Potomac River in Loudoun County, Virginia, with a watershed of . Agricultural lands make up 67 percent and forests 30 percent of Catoctin Creek's watershed. It is the main drainage system for the northern Loudoun Valley, including all of the Catoctin Valley. Course The main arteries consist of the Catoctin and its North and South Forks. North Fork Catoctin Creek The North Fork Catoctin Creek, long, begins at Purcellville Reservoir east of the Blue Ridge Mountains in the Between the Hills valley, near the West Virginia border. State Route 9 follows the north fork westward as it flows through Hillsboro Gap in Short Hill Mountain at Hillsboro. From Wheatland the North Fork flows northeast. South Fork Catoctin Creek The source of the South Fork Catoctin Creek is just east of the Blue Ridge's Wilson Gap on the We ...
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Between The Hills
Between the Hills is a small valley in northwest Loudoun County, Virginia, distinct from, but associated with, the greater Loudoun Valley. Geography The Between the Hills valley encompasses the area of Loudoun that lies west of Short Hill Mountain and east of the Blue Ridge Mountain. The area includes the communities of Neersville and Loudoun Heights. Between the Hills can be divided into two sections; the upper and lower valley. The upper valley encompasses the area north of the Hillsboro Gap in the Short Hill, while the lower valley encompasses the area south of the gap. The valley ranges from wide at its largest, just south of the Hillsboro gap to wide at its smallest, east of Purcell Knob in the upper valley and is approximately long. The main waterways of Between the Hills are the North Fork of Catoctin Creek, which drains the lower valley before flowing through the Hillsboro gap into the Catoctin Valley, and Piney Run, which drains the upper valley and flows north ...
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Purcell Knob
Purcell Knob is a spur of the Blue Ridge Mountain in Loudoun County, Virginia. The peak is just northeast of the main ridge at Keyes Gap and southeast of the village of Neersville. Purcell Knob is notable for exposure of the sericitic phyllite base of the Paleozoic The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ' ... Loudoun Formation in its antiformal syncline. References Mountains of Virginia Mountains of Loudoun County, Virginia Blue Ridge Mountains {{LoudounCountyVA-geo-stub ...
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Blue Ridge Mountain
Blue Ridge Mountain, also known as Blue Mountain, is the colloquial name of the westernmost ridge of the Blue Ridge Mountains in northern Virginia and the Eastern Panhandle of West Virginia. The Appalachian Trail traverses the entire length of the mountain along its western slope and crest. Geography The mountain extends from the Potomac River in the north to Chester Gap in the south. Along this section of the Blue Ridge Mountains, Blue Ridge Mountain comprises the sole ridge of the chain in the immediate vicinity and contains few spur ridges or peaks. The notable exceptions are the Bull Run and Catoctin mountains, which lie approximately to the east across the Loudoun Valley, and Short Hill Mountain, located to the east, which runs parallel to the Blue Ridge for near its northern terminus. To the west of the mountain is the lower Shenandoah Valley. Blue Ridge Mountain is noticeably lower in elevation than other sections of the Blue Ridge Mountains in Virginia. The southern ...
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