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Fault-block mountain of the tilted type. [16] Sierra Nevada Mountains (formed by delamination) as seen from the International Space Station. When a fault block is raised or tilted, a block mountain can result. [17] Higher blocks are called horsts, and troughs are called grabens. A spreading apart of the surface causes tensional forces.
The Canadian Rocky Mountain foreland thrust and fold belt is a northeastward tapering deformational belt consisting of Mesoproterozoic, Paleozoic, and Mesozoic strata. The Lewis thrust sheet is one of the major structures of the foreland thrust and fold belt extending over 280 mi (450 km) from Mount Kidd near Calgary, AB in the Southeast Canadian Cordillera to Steamboat Mountain, located west ...
The Chaloctaca lived along the crest of the Santa Cruz Mountains around Loma Prieta Creek. They may have been a separate village community of one larger group with the Sayanta. They held kinship ties with the Sayanta, Achistaca, Cotoni, Partacsi of Santa Clara Valley, and Somontoc.
A mountain man is an explorer who lives in the wilderness and makes his living from hunting and trapping.Mountain men were most common in the North American Rocky Mountains from about 1810 through to the 1880s (with a peak population in the early 1840s).
Bryges or Briges (Greek: Βρύγοι or Βρίγες) is the historical name given to a people of the ancient Balkans. They are generally considered to have been related to the Phrygians, who during classical antiquity lived in western Anatolia. Both names, Bryges and Phrygians, are assumed to be variants of
Galtymore or Galteemore (Irish: Cnoc Mór na nGaibhlte, meaning 'big hill of the Galtees') is a mountain in the province of Munster, Ireland.At 917.9 metres (3,011 ft 6 in), it is one of Ireland's highest mountains, being the 12th-highest on the Arderin list, and 14th-highest on the Vandeleur-Lynam list.
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The Cedar Mountain Formation is the name given to a distinctive sedimentary geologic formation in eastern Utah, spanning most of the early and mid-Cretaceous. The formation was named for Cedar Mountain in northern Emery County, Utah , where William Lee Stokes first studied the exposures in 1944.