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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 .
A trench drain (also known as a channel drain, line drain, slot drain, linear drain, or strip drain) is a specific type of floor drain featuring a trough- or channel-shaped body. It is designed for the rapid evacuation of surface water or for the containment of utility lines or chemical spills.
The Kamchatka–Aleutian junction is located at the northern end of the Kuril–Kamchatka Trench.. The Kamchatka–Aleutian triple junction is a triple junction of tectonic plates, of the fault–fault–trench type, where the Pacific plate, the Okhotsk plate, and the North American plate meet. [1]
A French drain is a trench that diverts water away from an area where it's pooling to a lower elevation where it can be released, explains Mike Arnold, director of The Gardens at Texas A&M ...
The Ozernaya river drains the lake. The Kurile Lake caldera is filled by the Kurile crater lake, covering a surface area of 76 square kilometres (29 sq mi) [4] to 77.1 square kilometres (29.8 sq mi). [10] A lake existed already before the Kurile Lake caldera-forming eruption. [16]
The Kuril Islands lie along the seismically active convergent boundary between the Pacific plate and the Okhotsk plate (a microplate within the North American plate). [7] The trench that accommodates this subduction—the Kuril-Kamchatka Trench, accommodates the convergence at a rate of 80 mm (3.1 in)/yr, with rates increasing from north to south. [7]
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