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Lookout Mountain Caverns (Lookout Mountain Cave, or Lower Cave) is the second-longest known cave in Hamilton County, Tennessee. [ citation needed ] Its mapped length of 2.481 miles (3.993 kilometers) places it at 361st on the United States Long Caves List.
There are at least 121 named trails in Lewis and Clark County, Montana according to the U.S. Geological Survey, Board of Geographic Names. A trail is defined as: "Route for passage from one point to another; does not include roads or highways (jeep trail, path, ski trail)." [1]
There are at least 75 named trails in Carbon County, Montana according to the U.S. Geological Survey, Board of Geographic Names. A trail is defined as: "Route for passage from one point to another; does not include roads or highways (jeep trail, path, ski trail)." [1]
Talus caves are usually short, although the longest have up to several kilometers of explorable passages. [1] Examples of long talus caves include Bodagrottorna [] in Hälsingland, Sweden, with 2,600 metres (8,500 ft) of passage, [8] [5] the Touchy Sword of Damocles cave in New York, United States with over 4,000 metres (13,000 ft) of passage, [2]: 55 [9] and Merrills-Barn Door-And-The Hole ...
(1997) Hearing on H.R. 588, to amend the National Trails System Act to create a new category of long-distance trails to be known as National Discovery Trails, to authorize the American Discovery Trail as the first trail in that category, and for other purposes; and H.R. 1513 a bill to amend the National Trails System Act to designate the ...
Trail building was expanded in the early 1930s, including a tunnel for the High Peaks Trail. [27] Bear Gulch Reservoir. In 1933, a Civilian Conservation Corps camp was established for about 200 men who worked on additions to the trail network. [28] [29] After lengthy legal proceedings, the old mining claims were incorporated into the monument ...
The Bear Gulch Limestone is commonly considered to be part of the Heath Formation, the youngest formation in the Big Snowy Group of central Montana. [1] [14] [2] [15] Some authors instead consider the Bear Gulch Limestone to be an early member of the Tyler Formation, a patchy but widespread unit of Carboniferous limestone and terrestrial sediments.
An 1883 map shows this town at the headwaters of a creek, which branches off of the Bear Butte Creek, below Sturgis. The map is rather inaccurate, but it shows the town about 4 + 1 ⁄ 2 miles (7.2 km) S-W of Sturgis, on a line between Sturgis and Lead. Sheridan: Golden City: Pennington: fall 1875-after 1930: Barren (submerged) Submerged under ...