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Cunningham Falls State Park

State park in Maryland, United States

Cunningham Falls State Park

Summary

State park in Maryland, United States

FieldValue
nameCunningham Falls State Park
photoCunningham Falls State Park - lower falls - 4.JPG
photo_captionThe longest cascading waterfall in Maryland
photo_altWaterfall
photo_width280
mapUSA Maryland
map_captionLocation in Maryland
map_width280
relief1
labelCunningham Falls State Park
locationFrederick County, Maryland, United States
nearest_townThurmont, Maryland
coordinates
coords_ref
area6157 acre
elevation1273 ft
established1954
designationMaryland state park
administratorMaryland Department of Natural Resources
website

Cunningham Falls State Park is a public recreation area located west of Thurmont, Maryland, in the United States. The state park is the home of Cunningham Falls, the largest cascading waterfall in Maryland, a 43 acre man-made lake, and the remains of a historic iron furnace. The park is one of several protected areas occupying 50-mile-long Catoctin Mountain; it is bordered on its north by Catoctin Mountain Park and on its south by Frederick Municipal Forest.

History

Before the arrival of European settlers, Native Americans used the Catoctin Mountain area for hunting and fishing and also quarried it for rhyolite to make projectile points. During the 19th century, settlers began cutting the area's forests for charcoal to power the Catoctin Iron Furnace. "Charcoal flats"—square areas measuring approximately 25 by, cut flat into the hillsides and linked by mule trails—were used to build charcoal kilns. The charcoal flats can still be seen in the park.

Over two hundred years of abuse of the forest led to the destruction of the land. In the 1930s, after years of clearcutting for the making of charcoal, mountain farming, and timber harvesting, the land was purchased by the Federal government. Beginning in 1935, workers with the Works Progress Administration and the Civilian Conservation Corps began constructing the Catoctin Recreational Demonstration Area to transform the area for recreational use. The site's northern portion was transferred to the National Park Service on November 14, 1936, and renamed and reorganized on July 12, 1954, as Catoctin Mountain Park. The southern 5000 acre were transferred to Maryland as Cunningham Falls State Park.

Features

View from the top of Cunningham Falls

Known locally as McAfee Falls, after a family of early settlers, 78 ft Cunningham Falls was apparently named after a photographer from Pen Mar Park who frequently photographed the falls.

An old homestead can be seen above the falls. There is an abandoned iron mine located in the park in addition to the ruins of the third Catoctin iron furnace, owned and constructed by Jacob Kinkel, in the 1850s-1860s.

Activities and amenities

Recreational activities include hiking, hunting, swimming, boating, fishing, and camping. Big Hunting Creek, one of Maryland's premier trout streams, flows through the park.

Campgrounds are featured in the park's William Houck Area and Manor Area, with the former including numerous campsites, a camp store, and a handful of mini cabins, while the latter includes 31 campsites. Camp hosts are volunteers through the Maryland Park Service.

References

References

  1. {{cite gnis. 583992. Cunningham Falls
  2. "Cunningham Falls State Park". Maryland Department of Natural Resources.
  3. "DNR Lands Acreage Report". Maryland Department of Natural Resources.
  4. "Big Hunting Creek". Maryland Department of Natural Resources.
  5. (April 22, 2003). "Source Water Assessment for Cunningham Falls State Park". Maryland Department of the Environment.
  6. Strain, Paula M.. (1993). "The Blue Hills of Maryland". Potomac Appalachian Trail Club.
  7. "Cunningham Falls". The Historical Marker Database.
  8. Miller, Jennifer. (2011). "The Demonstration Succeeds". National Park Service.
Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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