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・ Red Rock Dam (Iowa)
・ Red Rock Entertainment
・ Red Rock Film Festival
・ Red Rock Folk Festival
・ Red rock hare
・ Red Rock Indian Band
・ Red Rock Island
・ Red Rock Job Corps Center
・ Red Rock Lake
・ Red Rock Lakes National Wildlife Refuge
・ Red Rock Lakes Wilderness
・ Red Rock Landing Conservation Area, Perry County, Missouri
・ Red Rock Mountain
・ Red Rock Mountain Natural Area Preserve
・ Red Rock Noodle Bar
Red Rock Pass
・ Red Rock Pass (Beaverhead County, Montana)
・ Red Rock Peak
・ Red Rock Pro Open
・ Red Rock railway station
・ Red rock rat
・ Red Rock Reserve
・ Red Rock Resort Spa and Casino
・ Red Rock Ridge
・ Red Rock River
・ Red Rock River (Montana)
・ Red Rock River (New South Wales)
・ Red Rock State Park
・ Red Rock Township
・ Red Rock Township, Mower County, Minnesota


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Red Rock Pass : ウィキペディア英語版
Red Rock Pass

Red Rock Pass is a low mountain pass in eastern Idaho, south of Downey in southern Bannock County. It is geologically significant as the spillway of ancient Lake Bonneville. It is located along highway US-91 at an elevation of 4785 feet (1458 m) above sea level,〔(MSRmaps.com ) – topo map – Red Rock Pass – accessed 2009-08-19〕 bounded by two mountain ranges; the Portneuf to the east and the Bannock to the west.

The pass was cut through resistant Paleozoic shale, limestone, and dolomite, and forms a narrow gap two miles (3 km) in length.〔"Idaho for the Curious", by Cort Conley, ©1982, ISBN 0-9603566-3-0, p.505〕
At one time the pass was 300 feet (100 m) higher, where the shoreline of Pleistocene Lake Bonneville stood.
Red Rock Pass has a surface deposit of calcareous silty alluvium with topsoil of dark grayish brown silt loam.〔http://casoilresource.lawr.ucdavis.edu/gmap/〕
== The Bonneville flood ==
(詳細はice age lava flows in the vicinity of Pocatello began to divert the Bear River through Lake Thatcher and then into Lake Bonneville. This sudden influx caused Bonneville to overflow at Red Rock about 14,500 years ago. This overflow caused a sudden erosion of unconsolidated material on the northern shoreline near Red Rock Pass. As the material gave way, Marsh Creek Valley, immediately downstream, was flooded from wall to wall, and the rapid discharge eroded the pass to its present level. The flood then flowed into the Snake River Plain, generally following the path of the present-day Snake River to its outlet in the Pacific Northwest.〔
(Univ. of Utah Media ) – Lake Bonneville – accessed 2009-08-19〕
The Bonneville Flood, as it is known, was a catastrophic event. The maximum discharge was about 15 million cubic feet per second (420,000 m³/s), or about three times the average flow of the Amazon River, the world's largest river. The speed of flow was approximately 16 mph (7 m/s), and though peak flow lasted only a few days, voluminous discharges may have continued for at least a year.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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