Hocking Hills State Park–Whispering Cave and Lodge
Whispering Cave and Lodge
Logan, Ohio 43138
Whispering Cave webpage
Whispering Cave trail map
Ash Cave webpage
Hocking Hills State Park webpage
Hocking Hills State Park map
Hocking Hills trail maps
Athens Area Outdoor Recreation Guide Hocking Hills State Park
eBird Bar Charts by Season
About Whispering Cave and Lodge
The Whispering Cave trail system is located near the cabins (and where the lodge stood). This newest trail leads to the second largest cave in the park system, Whispering Cave. It is a short jog off of the Hemlock Bridge Trail. The hiking area has a scenic overlook, hemlock-lined trails, and a huge recess cave. It runs 1.5 miles long and connects the lodge and cabin area to the midpoint of the Old Man’s Cave Gorge Trail. It has the first-ever swinging bridge at the park which connects the two points over Old Man’s Creek.
From Whispering Cave webpage
About Hocking Hills State Park
The natural history of this region is as fascinating as the caves are beautiful. Here, in these sandstones and shales, one can read Ohio’s history from the rocks. The scenic features of the six areas of the Hocking Hills State Park complex are carved in the Blackhand sandstone. This bedrock was deposited more than 350 million years ago as a delta in the warm shallow sea which covered Ohio at that time. Subsequent millions of years of uplift and stream erosion created the awesome beauty seen today.
The sandstone varies in composition and hardness from softer, loosely cemented middle zone to harder top and bottom layers. The recess caves at Ash Cave, Old Mans Cave, and Cantwell Cliffs are all carved in the softer middle zone. Weathering and erosion widened cracks found in the middle layer of sandstone at the Rock House to create that unusual formation.
Other features of the rock include cross-bedding, honeycomb weathering, and slump blocks. The first is noticeable as diagonal lines in the rock intersecting horizontal ones. It is actually the cross section of an ancient sandbar in the delta and was caused by changing ocean currents. Honeycomb weathering looks like the small holes in a beehive comb. They are formed by differential weathering which comes about when water, moving down through the permeable sandstone, washes out small pockets of loosely cemented sand grains. Finally, the huge slump blocks of rock littering the streams tumble from nearby cliffs when cracks widen to the extent that the block is no longer supported by the main cliff.
Although the glaciers never reached the park areas, their influence is still seen here in the form of the vegetation growing in the gorges. The glaciers changed the climate of all Ohio to a moist, cool environment. Upon their retreat, this condition persisted only in a few places such as the deep gorges of Hocking County. Therefore, the towering eastern hemlocks, the Canada yew and the yellow and black birch tell of a cool period 10,000 years ago.
From Hocking Hills State Park webpage
Restrooms and handicap accessible facilities at locations identified on Hocking Hills State Park map.