Hocking Hills State Park, Ohio, USA
Ohio can boast of having the country's best campground, with Hocking Hills State Park finishing ahead of other go-to camping destinations such as Yellowstone National Park. Among the park's famous features is Old Man's Cave, Ash Cave Gorge and several waterfalls, while the 9,238-acre Hocking State Forest is adjacent to the park. Also included in its Top 100 Campgrounds. The Hockhocking enters the county from Good Hope Township in the northwest and then flows southwest, touches Marion Township, continues through Falls and Green Townships, and exits the county through northwestern Starr Township. The river is then in Athens County.
Tappan is owned and operated by the Muskingum Watershed Conservancy District, while the other three locations are owned and operated by the Ohio Department of Natural Resources' Division of Parks and Recreation. In describing its selection of Hocking Hills, Tripleblazer.com is quoted by as saying: "Located in the heart of Ohio's stunning Hocking Hills region, the campground beat out hundreds of camping sites across America, including the famed Yosemite National Park, which came in second, and Mount Rainier National Park, which is ranked No. 14.
Hocking Hills State Park is a non-contiguous state park in the Hocking Hills region of Hocking County, Ohio, United States; it is contiguous with the Hocking State Forest. Within the park are several spectacular features based around rock formations, including Old Man's Cave, a narrow, deep gorge featuring waterfalls; Rock House, a cliffed area with a rock shelter; Cantwell Cliffs, a broad gorge at the head of a hollow with a unique stone stairway; and Ash Cave, a large rock shelter with a small waterfall, and Cedar Falls, a larger waterfall south of Old Man's Cave
History
The name, Hocking Hills
Hocking County was named after the Hockhocking River. Hockhocking, in the Delaware tongue, signifies a bottle. In Shawnee, Wea-tha-Kagh-Qua-sepe, meant bottle river. The Hockhocking River had a waterfall of nearly 20 feet located about 6 or 7 miles northwest of Lancaster. Above the falls, the creek was very narrow and straight, forming the "bottle" neck.
History of the Park
More than 330 million years ago, the Hocking Hills State Park area was relatively level and was covered by the waters of the Atlantic Ocean. For millions of years, the ocean’s currents deposited immense amounts of sand and gravel. After millions of years, the ocean receded, and the sandy layers bonded with silica to form the Black Hand Sandstone that underlies the area. It formed like a sandwich, with a hard top and bottom and a soft middle layer. When the Appalachian Mountains arose, form and feature were cast upon the area and created Hocking Hills State Park.
Hocking Hills State Park was hemmed in by the ancient north-flowing Teahs River to the west, and the then north-flowing Hocking to the east. The "slump rocks" in the gorges today are what’s left of the hard top layer. In just a few centuries, the rushing waters of the glacier carved the soft middle layer of sandstone into the myriad dimples and wrinkles that decorate the cliffs and grottos today. Early settlers in Muskingum County found an ancient black human handprint on a cliff that is part of this same sandstone formation. That is the same "Black Hand Sandstone" that is seen in six areas of the Hocking Hills State Park
Nature of the Area
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.
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