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Cunningham Falls State Park
State park in Maryland, United States
State park in Maryland, United States
| Field | Value |
|---|---|
| name | Cunningham Falls State Park |
| photo | Cunningham Falls State Park - lower falls - 4.JPG |
| photo_caption | The longest cascading waterfall in Maryland |
| photo_alt | Waterfall |
| photo_width | 280 |
| map | USA Maryland |
| map_caption | Location in Maryland |
| map_width | 280 |
| relief | 1 |
| label | Cunningham Falls State Park |
| location | Frederick County, Maryland, United States |
| nearest_town | Thurmont, Maryland |
| coordinates | |
| coords_ref | |
| area | 6157 acre |
| elevation | 1273 ft |
| established | 1954 |
| designation | Maryland state park |
| administrator | Maryland 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

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