cutoff trench - определение. Что такое cutoff trench
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Что (кто) такое cutoff trench - определение

GEOGRAPHICAL OBJECT
Kuril Trench; Kamchatka Trench; Kurile Trench; Kuril-Kamchatka Trench
  • Map of earthquake locations, showing depth contours on top of downgoing slab
  • Topographic image of the northwest Pacific including the Kuril-Kamchatka Trench.

Meander cutoff         
  • Animation of the formation of an [[oxbow lake]]
  • View along the former Mississippi River riverbed at the [[Tennessee]]/[[Arkansas]] state line near [[Reverie, Tennessee]] (2007)
DISCONNECTED MEANDER LOOP OF A RIVER
Rincon (abandoned meander); Abandoned meander; Cutoff meander; Cutoff meander spur
A meander cutoff is a natural form of a cutting or cut in a river occurs when a pronounced meander (hook) in a river is breached by a flow that connects the two closest parts of the hook to form a new channel, a full loop. The steeper drop in gradient (slope) causes the river flow gradually to abandon the meander which will silt up with sediment from deposition.
Trench, Telford         
HUMAN SETTLEMENT IN THE UNITED KINGDOM
Trench, Shropshire
Trench is a suburb of the new town of Telford in the borough of Telford and Wrekin and ceremonial county of Shropshire, England, on the north side of the town, north of Oakengates.
Trench railways         
  • German troops loading for transport to the front about 1915.
  • A 0-8-0T Brigadelok preserved at Deutsches Dampflokomotiv-Museum.
SPECIAL NARROW GAUGE RAILWAY FOR WARFARE PURPOSES
Trench railway
Trench railways represented military adaptation of early 20th-century railway technology to the problem of keeping soldiers supplied during the static trench warfare phase of World War I. The large concentrations of soldiers and artillery at the front lines required delivery of enormous quantities of food, ammunition and fortification construction materials where transport facilities had been destroyed.

Википедия

Kuril–Kamchatka Trench

The Kuril–Kamchatka Trench or Kuril Trench (Russian: Курило-Камчатский жёлоб, Kurilo-Kamchatskii Zhyolob) is an oceanic trench in the northwest Pacific Ocean. It lies off the southeast coast of Kamchatka and parallels the Kuril Island chain to meet the Japan Trench east of Hokkaido. It extends from a triple junction with the Ulakhan Fault and the Aleutian Trench near the Commander Islands, Russia, in the northeast, to the intersection with the Japan Trench in the southwest.

The trench formed as a result of the subduction zone, which formed in the late Cretaceous, that created the Kuril island arc as well as the Kamchatka volcanic arc. The Pacific Plate is being subducted beneath the Okhotsk Plate along the trench, resulting in intense volcanism.

The maximum depth of the trench is reported in peer-reviewded academic papers as 9,600 meters.