(1) Himalayas -- Convergent between continental-continental collision of Indo-Australian and Eurasian plates.
(2) Aleutian islands -- Convergent between oceanic-oceanic collision of Pacific plate beneath North American plate.
(3) Andes Mountains -- Convergent between oceanic-continental collision of Pacific plate beneath South American plate.
(4) San Andreas Fault (Zone) -- Transform boundary (sometimes called a conservative boundary) between Pacific and North American plates.
(5) Iceland -- Divergent boundary along the Mid-Atlantic Ridge arm of the Mid-Ocean Ridge, separating North America to the west and Eurasia to the east. *Also* a large hot spot, which is what brought Iceland to the surface, rather than remaining undersea.
(6) Japan -- Convergent boundary between Pacific plate beneath North American plate (yes, Japan is on the North American plate).
(7) Mount St. Helens -- Convergent boundary between Juan de Fuca beneath North Americna plate.
Convergent boundaries build mountains (technically divergent do too, but no one ever thinks about them -- but they're lots and lots of small volcanoes)
Continental-continental --> crust slams together like two buses, neither plate can subduct, rock squirts up and out, you get the Himalayas (Indo-Australian and Eurasia)
Oceanic-oceanic --> crust meets and the older, denser, cooler one subducts. It reaches a depth that it melts, the new magma rises to the surface, pops out as a volcanic lava flow. Thousands of flows later, you have dry volcanic islands poking out of the surface. Because this is happening along a plane, you get a whole chain - an volcanic island arc like the Aleutians (Pacific plate below North American plate)
Oceanic-continental --> crust meets and the oceanic will *always* subduct. Just like oceanic-oceanic, it melts and rises and pops out, but this time on a dry continental surface. Again, thousands of flows later, you have a volcano. Again, as it's on a plane, you get a whole mountain range.
The Aleutian Islands are associated with the state of Alaska.
Mount Wrangell is situated on a convergent plate boundary, specifically where the Pacific Plate is subducting beneath the North American Plate. This boundary is associated with the formation of the Aleutian Islands and the Alaska Range of mountains.
Oceanic-Continental Convergence - Andean-Type - the Andes MountainsOceanic-Oceanic Convergence - Aleutian-Type - island arcsContinental-Continental Convergence - the Appalachian Mountains
Kauai is in the Hawaiian-Aleutian Time Zone (Hawaii-Aleutian Standard Time, HST).
No, Redoubt Volcano is not part of an island arc. It is located in the Aleutian Range in Alaska and is associated with the Aleutian volcanic arc, which is a chain of volcanoes formed by the subduction of the Pacific Plate beneath the North American Plate.
The Aleutian Islands are associated with the state of Alaska.
A chain of volcanic mountains
The Aleutian Range.
Aleutian type mountains are formed by the subduction of the Pacific Plate under the North American Plate along the Aleutian Trench. This subduction leads to the volcanic activity in the region, forming a chain of volcanic islands known as the Aleutian Islands. As the Pacific Plate sinks beneath the North American Plate, magma rises to the surface, creating the characteristic volcanic peaks of the Aleutian Mountains.
There are rocky mountains, plains and such others
The Near Islands and the Islands of Four Mountains are groups of small islands within the Aleutian Islands (the "tail" of the Alaska Peninsula). The Near Islands are the westernmost in the Aleutian Island chain.
Himalayas: Continental-continental North American Cordillera: Terrane accretion Aleutian: Oceanic-oceanic Andes: Near an active continental margin _______________________________ Himalayas: Two continents colliding Grand Tetons: Plates spreading Aleutian: Two ocean plates colliding. Andes: Near a subduction zone
Mount Wrangell is situated on a convergent plate boundary, specifically where the Pacific Plate is subducting beneath the North American Plate. This boundary is associated with the formation of the Aleutian Islands and the Alaska Range of mountains.
The chain of islands is the = Aleutian Islands =
The Aleutian Islands.
Convergent boundary Convergent boundary
aleutian trench