Red Rock Pass (Idaho)

Template:Short description Template:Infobox mountain pass Red Rock Pass is a low mountain pass in the western United States in southeastern Idaho, located in southern Bannock County, south of Downey. It is geologically significant as the spillway of ancient Lake Bonneville. It is traversed by U.S. Route 91 at an elevation of Template:Convert above sea level,<ref>MSRmaps.com – topo map – Red Rock Pass – accessed 2009-08-19</ref> 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 Template:Convert in length.<ref>"Idaho for the Curious", by Cort Conley, ©1982, Template:ISBN, p.505</ref> At one time the pass was Template:Convert higher, where the shoreline of Pleistocene Lake Bonneville stood.

The pass takes its name from the red limestone cliffs which border it.<ref>Template:Cite book</ref> Red Rock Pass has a surface deposit of calcareous silty alluvium with topsoil of dark grayish brown silt loam.<ref>Template:Cite web</ref>

Bonneville flood

{{#invoke:Labelled list hatnote|labelledList|Main article|Main articles|Main page|Main pages}} It is believed that during the last 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.<ref> Univ. of Utah Media – Lake Bonneville – accessed 2009-08-19</ref>

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, and almost 180 times the average flow rate of Niagara Falls (85,000 cfs). The speed of flow was approximately Template:Convert, and though peak flow lasted only a few days, voluminous discharges may have continued for at least a year.