Stanton is an unincorporated community in New Castle County, Delaware, United States, near the confluence of the Red Clay and White Clay Creeks. It is located in the southern end of Mill Creek Hundred. It was a distinct census-designated place for the 1990 U.S. census.
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Glenville is a ghost town in Delaware, United States, at 39°42′45″N 75°38′24″W. The community consisted of a development on Bread and Cheese Island, on the east bank of the Red Clay Creek near its mouth, just south of Delaware Route 4 near Stanton. Located in the floodplain for Red Clay Creek, the subdivision has always been prone to flooding, such as flooding from Hurricane Floyd in 1999 and Tropical Storm Henri in 2003. After floods caused by Tropical Storm Henri on September 15, 2003, homeowners were bought out by the state and local government, and the community was abandoned in 2004. Demolition began in 2005. As of 2023, the remains of the town are fenced off to prevent trespassers.
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Springer-Cranston House is a historic home located at Marshallton, New Castle County, Delaware. It was built in the late-18th century, and is a 2+1⁄2-story, four-bay, coursed rubble stone dwelling with a two-story stuccoed stone service wing. It has a Georgian interior floor plan and gable roof. The house is constructed of local Brandywine granite. It was originally a one-story, stone dwelling roughly 24 feet by 18 feet, and subsequently enlarged and modified during the first half of the 19th century. The interior was modernized in the 1940s.
It was added to the National Register of Historic Places in 1994.
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Mill Creek is a 9.6-mile-long stream principally located in northern New Castle County, Delaware, a tributary of the White Clay Creek. It takes its name from the large number of mills located along it during the 18th and early 19th centuries.
It originates a short distance over the state line near Kaolin, Pennsylvania and flows east, then south into Delaware. It passes under the Lancaster Pike at Hockessin, where Swift Memorial Park has been laid out along the stream between Old Lancaster Pike and the Wilmington and Western Railroad tracks. Leaving Hockessin, the stream turns slightly to the west, and then sharply towards the southeast to flow through a deep, wooded gorge between suburban developments. Further down the gorge, Mill Creek passes through Limestone Hills Park, and then forms the western boundary of the DelCastle Recreation Area. Continuing south and passing under Limestone Road, the hills on either side diminish in height, and development increases, although the steep sides have protected the creek from direct encroachment. Passing through the neighborhood known as "Milltown", Lindell Park lies along the creek between Milltown Road and Kirkwood Highway. Below Kirkwood Highway, the valley begins to open, and the creek skirts Delaware Park and passes under the Wilmington and Christiana Turnpike just before it empties into the White Clay.
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Marshallton United Methodist Church is a historic United Methodist church located at 1105 Stanton Road in Marshallton, New Castle County, Delaware. The original portion was built in 1886 as a one-room, 30-foot by 50-foot center-aisle plan frame structure with a gable roof. It sits on a foundation of "Brandywine Granite", a commonly found local building stone. In 1922, a 30-foot by 45-foot gabled frame addition was added on the east side of the original building. At the same time, Gothic arched commemorative stained glass windows and a bell tower were added. A three-story brick educational building and fellowship hall were added between 1949 and 1957.
It was added to the National Register of Historic Places in 1986.
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Hershey Run is a 2.9-mile-long stream located in New Castle County, Delaware. It is a tributary of White Clay Creek.
It rises on the edge of the Belvedere subdivision on the outskirts of Newport, Delaware and flows southward along the western edge of that town. To the west of the run lies Bread and Cheese Island, cut off by a partly filled back channel between Hershey Run and Red Clay Creek. New Castle County's Pleasant Hills Park lies along the run in the vicinity of the junction with the back channel. At the southern end of the park, the run enters a tidal marsh which extends to its mouth, near the end of the White Clay.
The nearby Koppers railroad tie treatment plant heavily contaminated the run with creosote.