Search results
Results from the WOW.Com Content Network
Laurel Caverns is the largest cave in the Commonwealth of Pennsylvania by volume and area. [3] Located in the community of Farmington , it sits on the Chestnut Ridge near Uniontown , [ 4 ] roughly 50 miles (80 km) southeast of Pittsburgh .
The Caverns at Natural Bridge; Clarks Cave; Dixie Caverns; Endless Caverns; Gap Cave; Grand Caverns, formerly "Weyer's cave" Indian Jim's Cave; Luray Caverns; Melrose Caverns; Natural Tunnel; Ogdens Cave; Shenandoah Caverns; Skyline Caverns; Stay High Cave; Unthanks Cave
It is the only tourist cave owned by the United States Forest Service and the only one owned by the federal government outside the National Park System. Blanchard Springs Caverns is a three-level cave system, all of which can be viewed on guided tours. The Dripstone Trail runs through the uppermost level of caverns for about a 0.5 miles (0.80 ...
Crater of Diamonds State Park is known for the 37.5-acre (15.2 ha) plowed field on which visitors can hunt for diamonds and other semi-precious gems. On average, two diamonds are found per day by park visitors. [3] A visitor center contains information about the geology of the park, a gift shop, and a cafe.
Plum Bayou Mounds Archeological State Park (), formerly known as "Toltec Mounds Archeological State Park", [3] also known as Knapp Mounds, Toltec Mounds or Toltec Mounds site, is an archaeological site from the Late Woodland period in Arkansas that protects an 18-mound complex with the tallest surviving prehistoric mounds in Arkansas.
The Big Room at Carlsbad Caverns National Park is the largest single cave chamber by volume in North America. It is accessible via a relatively flat 1.25 mile (2 km) trail.
The Little Maumelle River empties into the Arkansas River at Two Rivers Park approximately 6.6 miles (10.6 km) east of Pinnacle Mountain. The United States Board on Geographic Names once defined a mountain as any landform greater than 1,000 feet (305 m) of local relief and a hill as any landform less than 1,000 feet (305 m) of local relief.
The geology of Arkansas includes deep 1.4 billion year old igneous crystalline basement rock from the Proterozoic known only from boreholes, overlain by extensive sedimentary rocks and some volcanic rocks. The region was a shallow marine, riverine and coastal environment for much of the early Paleozoic as multi-cellular life became commonplace.