Trout Pond

What is Trout Pond?

Trout Pond, historically known as Old Pond, holds the distinction of being West Virginia's sole natural lake. It is a significant karst feature, originating from a sinkhole that has been replenished by a network of mountain streams flowing from Long Mountain. Located within the Trout Pond Recreation Area (TPRA) of the George Washington National Forest near Wardensville, Hardy County, it represents a unique hydrological phenomenon.

Geological Formation and Behavior

The formation of Trout Pond is directly linked to the geological makeup of the region, which is characterized by layers of limestone. Rainfall has slowly eroded these subterranean limestone layers, creating conical holes and caverns. While many sinkholes form and exist, Trout Pond's unique position allowed it to maintain a stable, lake-like status for an extended period. However, recent geological activity, specifically suspected shifts in the underlying limestone cavern, have drastically altered its behavior. Since July 2002, officials have observed significant drops in water levels, with the pond draining almost dry within a month due to these underground structural changes. While it can regenerate during prolonged wet periods, it tends to empty again as soon as dry spells occur.

Recreation and Management

The Trout Pond Recreation Area, established in the late 1970s, provides facilities for visitors, including a designated swimming area, lakeside trails, and fifty campsites, operating seasonally from early May through late October. Trout Pond has a history of being stocked with trout, which contributed to its current name. This practice was temporarily halted due to erosion of the banks caused by fishermen, highlighting the challenges in managing natural attractions that are also popular recreational sites.