This article possibly contains original research .(January 2014) |
Beaver Valley, Delaware and Pennsylvania | |
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Coordinates: 39°50′21″N75°33′51″W / 39.83917°N 75.56417°W | |
Country | United States |
State | Delaware and Pennsylvania |
County | New Castle and Delaware |
Township | Chadds Ford and Concord |
Elevation | 203 ft (62 m) |
Time zone | UTC-5 (Eastern (EST)) |
• Summer (DST) | UTC-4 (EDT) |
Area codes | 302, 484, 610 |
GNIS feature ID | 216027 [1] |
Beaver Valley (formerly known as Chandler's Hollow) straddles the Pennsylvania and Delaware border in Delaware County, PA and New Castle County, DE. An unincorporated place name, it is traversed by several streams which drain to Beaver Run which itself empties into the Brandywine River. It is approximately bounded by US Route 202 to the east, The Brandywine River to the west, Thompsons Bridge Road to the south, and Smithbridge Road to the north, with Beaver Valley Road encircling a large portion of the valley.
The majority of the lands in Beaver Valley have been owned for decades by The Woodlawn Trustees, which designated in the early 1970s all of its Brandywine Hundred and Delaware County holdings in Beaver Valley and elsewhere as a wildlife refuge. In 2012, The Woodlawn Trustees submitted development plans to Concord Township Supervisors in Delaware County for the purpose of constructing approximately 500 housing units and a 225,000 square foot national retail store, all of which would adjoin the First State National Historical Park in Chadds Ford Township, Delaware County, Pennsylvania and New Castle County, Delaware.
Roughly half of Beaver Valley lies in southeastern Pennsylvania in Concord and Chadds Ford Townships, in Delaware County, Pennsylvania. The other half is situated in northern Delaware in The Brandywine Hundred in New Castle County. The historic Brandywine River runs along Beaver Valley's western border and one of Pennsylvania and Delaware's most heavily traveled roads, Route 202, forms its eastern border. Much of Beaver Valley falls within the First State National Monument declared by President Obama in March 2013 (later redesignated the First State National Historical Park) and which represents Delaware County's and the state of Delaware's only representation in the National Park Service.
Across the Brandywine to the west sits the thousand acre Granogue, a du Pont estate occupied as of January, 2014 by Irenee du Pont. Other former du Pont lands became Brandywine Creek State Park, which adjoins Beaver Valley in the south. The only cave known to exist in the state of Delaware lies 200 feet west of the intersection of Beaver Valley and Beaver Dam Roads in the heart of the valley. Featuring The Brandywine Valley and Beaver Valley in their April print and online editions, National Geographic magazine highlighted the historic importance of this area. [2] John Thomas Scharf, an early chronicler of the area, described Beaver Valley as
“...a hamlet on Beaver Run where that stream crosses the Pennsylvania line. The place is also locally known as Chandler’s Hollow, being situated in a deep vale, through which flows the run to mingle its waters with those of the Brandywine, a short distance below. Amor Chandler had the first store at Beaver Valley In 1835 Charles and Martin Palmer were in trade. Lewis Talley followed later and with some partners manufactured shoes in connection with the store. John Chandler was also in trade, and since 1876, A. H. Chandler has been a merchant here These merchants have also been postmasters of the Beaver Valley office The hamlet has about a dozen and shops." [3]
Beaver Valley falls within the Piedmont plateau, a region located between the Atlantic Coastal Plain and the Appalachian Mountains. The Piedmont of Pennsylvania is divided into three distinct sections: the Piedmont Uplands, the Piedmont Lowlands, and the Gettysburg-Newark Lowlands. Beaver Valley is located on the upland section of the Piedmont wherein the oldest exposed rocks in Pennsylvania can be found. [4] These rocks have a complex history and a vast array of different minerals. Much of the rock was altered (squeeze and/or melted) during the formation of Rodinia during the Grenville orogeny. [4] One result of this metamorphism was the creation of significant deposits of mica which can be found in the National Historical Park near the intersection of Ramsey Road and Thompsons Bridge Road. In fact, mica was quarried there by early settlers, partly for use in early windows. These rocks eventually provided the platform or base for the later deposition of eroded sediment that consolidated into main bedrock referred to as the Wissahickon Formation, the particular variety of which in Beaver Valley is called the Mt. Cuba Wissahickon Formation. Characterized by assorted metamorphic and sedimentary rock types, Beaver Valley's bedrock provides the parent material for soils which include of a mix of gneiss and schist with subordinate amphibolite and pegmatite. [4] Erosion and chemical weathering of the Wissahickon bedrock give regional soils particular chemical characteristics that support diversified farming. Most upland Piedmont soils are fertile, [4] and Beaver Valley is no exception with local farmers planting a variety of crops on lands leased to them by The Woodlawn Trustees.
Up until the mid-twentieth century and despite ample historical evidence that Delaware Indians used it for shelter, the National Speleological Society maintained that Delaware was the only state in the union lacking a cave. [5] In 1958, a local resident, George Jackson, added this cave to the national cave files. [6] The cave was the focus of research in the 1940s when the Archeological Society of Delaware conducted a dig which revealed conclusively that Indians had used it for shelter and storage. [5] Sitting just 100 feet from the Pennsylvania border this small cave extends just 56 feet to its furthest reach, but has become one of the most researched caves in the United States relative to its size. Jack Speece notes that the cave has gone by many names in its history. Indian Cave, Beaver Valley Rock Shelter, and Wolf Rock Cave preceded the now more commonly accepted "Beaver Valley Cave." [5]
Abutting intensive development on its northerly and easterly borders, Beaver Valley's forests are reminiscent of an earlier age, and while they are in the process of slowly healing from 200 years of agricultural and milling operations, they are beginning to resemble again what the Lenni Lenape had known. Primarily deciduous forests consisting of native tulip poplar, sycamore, beech, red and white oak, cherry, ash, walnut, American hornbeam (Carpinus caroliniana), and one documented American Chestnut, Beaver Valley's woods are among the most extensive and mature in southeastern Pennsylvania. [4] Several patches offer “interior forest” conditions, critical nesting habitat for several neotropical migrant songbird species. Many of these tracts lie at least one hundred meters from any canopy fragmenting feature like roads, power lines, or fields and offer hundreds of migratory and sedentary bird species some of the last remaining unspoiled habitat in Southeastern Pennsylvania, increasingly found in short supply and degraded quality. [4]
Beaver Valley is a critical part of the Brandywine and Delaware River watersheds. At least one of its streams remains cold enough and pure enough to hold a small population of native brook trout, at the extreme southern edge of their range. [4] The once teeming population of minnows, salamanders, and crawfish supported a feral population of mink (gone wild from a failed ranching experiment), native populations of weasels, and substantial populations of skunk and raccoons. Continued efforts to improve the quality of Beaver Run have made the return of its eponymous mammal more likely. A significant number of old fields are very early in the long process of reverting from past agricultural uses to meadow although several large fields in Beaver Valley are still leased to local farmers for hay production. The forest was likely selectively cut for fuel wood and timber several times since colonial times, however much of the existing forests have been standing for well over 100 years. Some of the trees were likely considered less desirable for lumber and fuel or were less accessible due to steep slopes. While the Beaver Valley Woods is not considered virgin forest, some individual trees may be 200–300 years old or older. [4]
Before the Beaver Valley was settled by Europeans, it was traversed by Lenni Lenape, traveling from their summer camp at the “Big Bend” of the Brandywine River to Naaman's Creek – pausing at Beaver Valley Cave to seek rest and shelter, to store produce and supplies. According to a local historian, “in the late 17th and 18th centuries, Beaver Valley’s lands were taken up by Europeans, many Quaker, many coming with William Penn in pursuit of their personal peaceable kingdoms. The lands were cleared, surveyed, and domesticated into the dispersed family farms that characterized settlement patterns in the region. These farms were “mixed” – producing a variety of products (especially grain) for home use, and export to Colonial America's largest city, Philadelphia, and from there to Europe and the West Indies. Conestoga Wagons rumbled by on the “great road” (today, 202), en route to mills and ports, including those in the new town of Wilmington, stopping for rest and refreshment at the taverns that stood at each intersection of Beaver Valley and the Great Road – The Nine Ton in Pennsylvania and another in Delaware.” [7]
A stray reference to Beaver Valley in 1694 refers to the lands bordering Beaver Run as “mill lands,” and surveyors laying out Beaver Valley Road in 1712 passed by “the mill that Chandler is building.” Until well into the 19th century, Beaver Run and its tributaries supported small mills – generally managed by their owners and from one to three workers that produced a range of products, from lumber, to tin, to flax, to paper. By the third quarter of the 19th century the Valley had become a thriving community of several hundred people organized around two schools, the mills, and the characteristic family farms of 40 to 120 acres. [8] [9] Many of the mills and dams in Beaver Valley were damaged or destroyed as the result of the flood of 1843. [10] [11]
The landscape of Beaver Valley in the Woodlawn Wildlife Refuge has more than a trace of these early European beginnings, some dating back to 1683. Stone and wood-framed 18th and 19th century dwellings and outbuildings – barns, corn cribs, cart sheds, and springhouses - dot the landscape, a unique manifestation of the regional rural heritage. Located less than 2 miles from the famous Brandywine Battlefield, the Delaware County Planning Commission has noted that the area has "high potential" for archaeological resources given that it has remained undeveloped since the Township's founding before 1683. [4]
The importance of these lands has been recognized by New Castle and Delaware Counties. [4] [12] New Castle County has recommended that the Delaware roadways that wind through Beaver Valley be designated National Scenic Highways while The Delaware County Planning Commission has encouraged the preservation and protection of the lands in the valley. [4] The United States federal government has weighed in, too, designating 1,100 acres in New Castle County and Chadds Ford, Delaware County as First State Historical Park, of which Beaver Valley constitutes a large part. [2] [13] The majestic character of the valley was effectively captured by the National Geographic in April 2013 when it described it as existing “at some indeterminate point in time... somewhere between the 18th and the 20th centuries.” [2] Beaver Valley looks much like it did when George Washington's Continental Army camped nearby, and an old legend in the valley tells of British troops commandeering supplies from locals during their march across the Brandywine Valley. According to local family history, The Redcoats made off with Robert Green's best mare, as he continued to plow.
Beaver Valley's population was 250 in 1890, [14] and was 241 in 1900. [15]
A part of Beaver Valley's history lives on in The Brandywine Summit Camp Meeting on Beaver Valley Road. Established barely one year after the end of the Civil War in 1866, it is one of the oldest continually operating camp meetings in Pennsylvania, becoming a summertime destination of middle class Methodists from Wilmington, DE to West Chester, PA in the late nineteenth century and throughout much of the twentieth. [16]
“It is a prime example of the American Methodist Camp Meeting Movement, a movement made popular in the decades following the Civil War. Its layout and architecture, featuring gabled cottages along avenues surrounding a central square containing a tabernacle, typifies the general design of camp meetings at that time. The wooded landscape of the camp was once part of the William Johnson farm, and the specific thirteen acres which comprise the district was once known as Johnson’s Woods. The Johnson farmhouse still stands on Route 202, substantially renovated, and houses the Brandywine Conference and Visitors Bureau.” [16]
Crisscrossing upland meadows and pristine streams, heavily wooded areas or lush valleys, Beaver Valley's extensive network of packed-earth paths offers a wide variety of terrain for a wide variety of recreational activities. [17] Bikers, hikers, horseback riders, runners, birders, artists, cross country skiers, and dog walkers can frequently be seen taking advantage of what Beaver Valley offers. [18]
A half dozen horse farms exist throughout the valley and horseback riders make good use of the farms’ proximity to the trails. On any given day, several mountain bike clubs in the area will ride en masse in colorful array. [19] Birders frequent the valley, also, to take in the hundreds of migratory and sedentary bird species stopping or living in Beaver Valley. A calm summer evening will draw artists to the fields at the eastside of the valley, and their paintings ornament the walls of many a restaurant and business in the Brandywine Valley. A number of hiking clubs and recreational meetup groups schedule hikes in the valley on a regular basis in every season. [20] A short loop through a part of the valley might take a dog walker a half-hour while more serious hikers can wander for several hours through The Woodlawn Wildlife Refuge, Brandywine State Park, The First State National Historical Park, and beyond. On a summer ride or hike down to the river, one might witness a flotilla of kayakers or rafters drifting down to Thompson's Bridge [21] [22] [23] or a pace line of cyclists racing along Brandywine Creek Drive. Several cycling and hiking groups help maintain the trails in the wildlife refuge and can frequently be seen with chainsaws clearing fallen trees. [24]
In the early 20th century, William Poole Bancroft, a wealthy Wilmington philanthropist, saw the city spreading beyond its borders and recognized the urgent need to protect the lands around Wilmington for future generations to enjoy. To that end, he created a corporation called “The Woodlawn Trustees” and charged it with fulfilling his vision of securing parkland for a future Wilmington. [25] Accordingly, throughout the first half of the 20th century, Woodlawn purchased thousands of acres of land north of Wilmington in The Brandywine Hundred and in Delaware County, Pennsylvania. From the 20s until the 60s, Woodlawn also developed more than a half dozen high income communities closer to Wilmington, DE, some of which include Alapocas, Edenridge, Woodbrook, and Tavistock. At some point in the late 60s or early 70s, The Woodlawn Trustees designated their remaining land holdings in and around Beaver Valley and The Brandywine Hundred as a wildlife refuge, installing hundreds of “Wildlife Refuge” signs at considerable expense around the perimeter of their lands. [26] In 2012, Woodlawn sold 1,100 acres of its wildlife refuge to The Mt. Cuba Center for approximately 21 million dollars. [27] The 1,100 acres were turned over to The National Park Service by The Mt. Cuba Center via The Conservation Fund, and in March, 2013, the Obama administration declared these lands as First State National Monument. [28] [29] Six months prior to these events, Woodlawn announced plans in mid 2012 to build approximately 500 homes and a 225,000 square foot retail "big box" store in Beaver Valley on 324 of the remaining 775 acres of the Woodlawn Wildlife Refuge on lands directly adjoining what would shortly become The First State National Monument, sparking widespread community opposition. [29]
The original plans were withdrawn, but the developers – Frank McKee and the Julian brothers, Richard and Frank – came back with new plans entitled "Vineyard Commons" which called for 161 houses spread across approximately 230 acres. The Concord Board of Supervisors approved the preliminary version of these plans in spite of widespread public opposition and a large quantity of evidence presented by The Beaver Valley Conservancy that the plans did not conform to Concord Township zoning, SALDO, and Stormwater codes. In late March 2015, The Beaver Valley Conservancy filed suit in Common Pleas Court in Media, Pennsylvania disputing the decision of the Concord Board of Supervisors on the grounds that they acted in bad faith, among other allegations. [30] The remaining ~60 acres of the originally disputed land is now equitably owned by Steven Wolfson who has indicated he intends to build residential housing. Those plans are known as "Concord Ventures" and call for ~166 apartments and 29 townhouses. In October 2016, a Delaware County Common Pleas Court judge sent the case back to the Concord Supervisors ordering them to hold evidentiary hearings and to apply environmental protection standards to the development per Pennsylvania's Environmental Rights Amendment to its constitution. Shortly after this court order, the developers agreed to sell their rights to the land to the Conservation Fund and the Mount Cuba Foundation, a deal which was finalized in May 2017 with the help of the Brandywine Conservancy and the Beaver Valley Conservancy. In mid January 2018, yet another meeting was held, the purpose being the possibility of approving the Concord Ventures. During the meeting, the project faced much opposition from adjacent residents to the indicated location and residents of Beaver Valley. Arguments were made that the project was 'unharmonious with the surrounding environment and residents', in conflict with the [PRD?] building requirements. Conclusion of the meeting resulted in disapproval of the project.
Merlin Brubaker, a DuPont chemist, lived in Beaver Valley on a 51-acre estate for more than 40 years from the late 30s to the mid 80s. Wanting to conserve his 51 acres in Beaver Valley, and having turned down more generous offers to develop his land, Mr. Brubaker approached Stephen Clark, president of Woodlawn, in the late 70s and asked if they would purchase his estate and protect it from development. Woodlawn agreed and allowed Mr. Brubaker to continue to live on his old estate for as long as he wanted. [31] In June 2014, Frank McKee builders and The Julian Brothers' Eastern States Construction announced that Dr. Brubaker's former estate would become the central part of a 171 house development—which several groups are opposing. Some of the groups that would like to see Beaver Valley remain a natural place include The Beaver Valley Preservation Alliance [ permanent dead link ], Save The Valley and The Beaver Valley Conservancy.
Brandywine may refer to:
Wilmington is the largest city in the U.S. state of Delaware. The city was built on the site of Fort Christina, the first Swedish settlement in North America. It lies at the confluence of the Christina River and Brandywine Creek, near where the Christina flows into the Delaware River. It is the county seat of New Castle County and one of the major cities in the Delaware Valley metropolitan area. Wilmington was named by Proprietor Thomas Penn after his friend Spencer Compton, Earl of Wilmington, who was prime minister during the reign of George II of Great Britain.
Concord Township is a township in Delaware County, Pennsylvania, United States. The population was 17,231 at the 2010 census. It contains the unincorporated communities of Concordville and Glen Mills.
Brandywine Creek is a tributary of the Christina River in southeastern Pennsylvania and northern Delaware in the United States. The Lower Brandywine is 20.4 miles (32.8 km) long and is a designated Pennsylvania Scenic River with several tributary streams. The East Branch and West Branch of the creek originate within 2 miles (3 km) of each other on the slopes of Welsh Mountain in Honey Brook Township, Pennsylvania, about 20 miles (32 km) northwest of their confluence.
Chadds Ford Township is an affluent township in Delaware County, Pennsylvania, United States. It is located about 25 miles (40 km) southwest of Philadelphia.
Brandywine Hundred is an unincorporated subdivision of New Castle County, Delaware. It is located to the north and northeast of the city of Wilmington. Hundreds were once used as a basis for representation in the Delaware General Assembly. Brandywine Hundred and North Wilmington are commonly used colloquial names for this area. However, while their names still appear on all real estate transactions, all other hundreds in Delaware presently have no meaningful use or purpose except as a geographical point of reference. In the 2010 census, Brandywine had 77,182 people.
Brandywine Creek State Park is a state park, located 3 miles (4.8 km) north of Wilmington, Delaware along the Brandywine Creek. Open year-round, it is 933 acres (378 ha) in area and much of the park was part of a Du Pont family estate and dairy farm before becoming a state park in 1965. It contains the first two nature preserves in Delaware. These nature preserves are Tulip Tree Woods and Freshwater Marsh. Flint Woods is a satellite area of the park and has become the park's third nature preserve. Flint Woods is home to species of rare song birds and an old-growth forest. The park's forests are part of the Northeastern coastal forests ecoregion.
Delaware Route 92 (DE 92) is a 8.83-mile-long (14.21 km) road in northern New Castle County, Delaware, that runs a short distance to the south of the Pennsylvania/Delaware state line for most of its length. The route runs from DE 100 near Montchanin east to U.S. Route 13 (US 13) in Claymont. The road is a two-lane rural road between the western terminus and US 202, passing through Brandywine Creek State Park and the Brandywine Valley section of First State National Historical Park. East of US 202, DE 92 is a four-lane divided highway called Naamans Road that passes through suburban areas to the north of Wilmington, with an interchange at Interstate 95 (I-95) in Claymont. DE 92 was first built as a state highway east of US 202 during the 1920s and 1930s. By 1968, the route was designated onto its current alignment. In the 1990s, DE 92 east of US 202 was widened into a divided highway.
Delaware Route 100 (DE 100) is a state highway in New Castle County, Delaware. The route runs from DE 4 near Elsmere to the Pennsylvania border near Montchanin, where it continues into Pennsylvania as State Route 3100. The road runs through suburban areas of northern New Castle County. The route intersects DE 2 in Elsmere before forming separate concurrencies with DE 48 and DE 141 from west of Wilmington north to Greenville. In Greenville, there is an interchange with DE 52. North of Greenville, DE 100 continues by itself to the Pennsylvania border, intersecting DE 92 in Montchanin. DE 100 was first designated in the 1930s to run from DE 52 to the Pennsylvania border, where it connected to Pennsylvania Route 100 (PA 100) until the southern terminus of that route was truncated away from the state line in 2003. By the 1970s, it was extended south to DE 4. The route was realigned to follow parts of DE 48 and DE 141 by 1990.
Wilmington State Parks is a state park located in Wilmington, Delaware. Open year-round, the park is approximately 345 acres (140 ha) of land mostly situated along the Brandywine Creek. The state park is made up of a group of smaller parks that are administratively managed as a single unit.
U.S. Route 202 (US 202) is a US Highway running from New Castle, Delaware, northeast to Bangor, Maine. The southernmost section of the route in the U.S. state of Delaware passes through northern New Castle County. It runs from its southern terminus at an interchange with US 13/US 40 near the Wilmington Airport north to the Pennsylvania state line in Brandywine Hundred. The route passes east of the airport concurrent with Delaware Route 141 (DE 141) before coming to an interchange with Interstate 95 (I-95). At this point, US 202 heads northeast along with I-95 through Wilmington. Just north of Wilmington, US 202 splits from I-95 by running north on Concord Pike through the suburban Brandywine Hundred area to the Pennsylvania state line. US 202 is a multilane divided highway the entire length across Delaware, with the section concurrent with I-95 a freeway.
Tavistock is an unincorporated community in New Castle County, Delaware, United States. It is within ZIP Code Tabulation Area for 19803.
Edenridge is an unincorporated community in New Castle County, Delaware, United States in the Brandywine Hundred, north of Wilmington.
First State National Historical Park is a National Park Service unit which lies primarily in the state of Delaware but which extends partly into Pennsylvania in Chadds Ford. Initially created as First State National Monument by President Barack Obama under the Antiquities Act on March 25, 2013, the park was later redesignated as First State National Historical Park by Congress.
Brandywine Village was an early center of U.S. industrialization located on the Brandywine River in what is now Wilmington, Delaware.
The Beaver Valley Rock Shelter Site is the only formally recognized cave in the US state of Delaware. It is located in New Castle County near Wilmington and the state line with Pennsylvania.
William Poole Bancroft was an American industrialist who later became an important figure in the land conservation movement. His belief that the beauty of the Brandywine region should be protected against urban sprawl for future generations led to him purchasing large amounts of land which eventually became state and federally owned park land.
Alapocas Run State Park is a state park, located in Wilmington, Delaware, United States, along the Brandywine Creek and its Alapocas Run tributary. Open year-round, it is 415 acres (168 ha) in area. Much of the state park was created from land originally preserved by William Poole Bancroft in the early 1900s to be used as open space parkland by the city of Wilmington as it expanded. The park also includes the Blue Ball Barn, a dairy barn built by Alfred I. du Pont as part of his Nemours estate in 1914. In addition to walking trails, athletic fields, and playgrounds for children, one of the park's primary features is a rock climbing wall. The rock climbing wall is part of an old quarry across from historic Bancroft Mills on the Brandywine, and the quarry is also used for school educational programs centered on earth sciences.