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OCEANIC TRENCH

Aleutian Trench and Arc; Aleutian Trough; Alaska-Aleutian megathrust; Aleutian Megathrust; Alaskan/Aleutian Megathrust Fault; Alaska/Aleutian megathrust; Aleutian megathrust; Aleutian-Alaska megathrust; Alaskan megathrust; Alaska megathrust

Hawaii–Aleutian Time Zone

TIME ZONE USED IN HAWAII AND THE ALEUTIAN ISLANDS, CORRESPONDING TO UTC−10:00

Hawaii–Aleutian Standard Time; Hawaii Standard Time; Hawaiian Standard Time; Hawaii-Aleutian Standard Time Zone; Hawaii-Aleutian Time zone; Hawaii-Aleutian time; Hawaii Time Zone; Hawaiian time; Hawai'i-Aleutian Time Zone; Hawaii–Aleutian Daylight Time; HADT; Hawaii-Aleutian time zone; Hawaiian Time; Hawaii Time; Hawaii-Aleutian Time Zone; Hawaii-Aleutian Standard Time; Hawaii-Aleutian Daylight Time; Hawaiian Time Zone; Hawaiian Daylight Time; Aleutian Standard Time; Aleutian Daylight Time

The Hawaii–Aleutian Time Zone observes Hawaii–Aleutian Standard Time (HST) by subtracting ten hours from Coordinated Universal Time (UTC−10:00). The clock time in this zone is based on the mean solar time of the 150th meridian west of the Greenwich Observatory.

https://en.wikipedia.org/wiki/Hawaii–Aleutian_Time_Zone

Aleutian

WIKIMEDIA DISAMBIGUATION PAGE

Alutian; Aleutian (disambiguation)

·adj ·Alt. of Aleutic.

Aleutian Basin

Aleutian basin

The Aleutian Basin is an oceanic basin under the southwestern Bering Sea. While the northeastern half of the Bering Sea overlies the North American Plate in relatively shallow water, the Aleutian Basin consists of oceanic plate—the remnant of the Kula Plate that was mostly subducted under the North American Plate.

https://en.wikipedia.org/wiki/Aleutian_Basin

ويكيبيديا

Aleutian Trench

The Aleutian Trench (or Aleutian Trough) is an oceanic trench along a convergent plate boundary which runs along the southern coastline of Alaska and the Aleutian islands. The trench extends for 3,400 kilometres (2,100 mi) from a triple junction in the west with the Ulakhan Fault and the northern end of the Kuril–Kamchatka Trench, to a junction with the northern end of the Queen Charlotte Fault system in the east. It is classified as a "marginal trench" in the east as it runs along the margin of the continent. The subduction along the trench gives rise to the Aleutian Arc, a volcanic island arc, where it runs through the open sea west of the Alaska Peninsula. As a convergent plate boundary, the trench forms part of the boundary between two tectonic plates. Here, the Pacific Plate is being subducted under the North American Plate at a dip angle of nearly 45°. The rate of closure is 7.5 centimetres (3 in) per year.

https://en.wikipedia.org/wiki/Aleutian Trench