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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.
Rimini, (/ ˈ r ɪ m ə n aɪ /) is a ghost town in Lewis and Clark County, Montana, United States. It is one of the oldest mining districts in the state. It was established when silver lodes were discovered in 1864. Other names for the district were Lewis and Clark, Tenmile, Vaughn, Colorado, and Bear Gulch. [3] It was the site of Camp Rimini.
It is intended to be a complete list of the properties and districts on the National Register of Historic Places in Granite County, Montana, United States. The locations of National Register properties and districts for which the latitude and longitude coordinates are included below, may be seen in a map. [1]
In First Chance Gulch in western Montana, the town is located 11 miles up the Garnet Range Road, in mountains and forest. The town is at approximately 6,000 feet (1,800 m) elevation. The nearest city is Missoula , approximately 20 miles (32 km) to the west.
Bear Gulch Limestone: 324 Ma: Montana, US A limestone-rich geological lens in central Montana. It is renowned for its unusual and ecologically diverse fossil composition of chondrichthyans, the group of cartilaginous fish containing modern sharks, rays, and chimaeras.
The bear gulch limestone is a fossil deposit from the Big Snowy Mountains of Montana. It is a smaller part of the larger St. louis limestone, which dates to the middle carboniferous. During the time, the area was a series of mudflats and lagoons with brackish and freshwater. [7] Many theories have been put forth for the preservation.
†Paratarrasius hibbardi Carboniferous Bear Gulch, Montana †Pegmatrea – or unidentified related form †Pelagiella †Peltabellia †Peltabellia willistoni – type locality for species †Pennireptepora; Fossilized theca of the Carboniferous blastoid echinoderm ("sea bud") Pentremites †Pentremites †Perditocardinia †Pericyclus
'bear paws', [4] Crow: Daxpitcheeischikáate, lit. 'bear's little hand', [5] and Gros Ventre: ʔɔɔwɔ́hʔoouh, lit. 'there are many buttes'. [6] While highway signs designate the range as the Bears Paw Mountains, historically, the names Bearpaw Mountains and Bear Paw Mountains also have been used, including on early state maps of the region.