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Rift (previously known as Rift: Planes of Telara, and as Heroes of Telara during alpha testing) is a fantasy free-to-play massively multiplayer online role-playing game developed by Trion Worlds. Rift takes place within the fantasy world of Telara. Two competing factions, composed of a selection of races and classes, battle each other and the ...
The Maui Hazard Zone numbers are a different scale from the island of Hawaiʻi's map. The lava flow hazard zones on Maui use a different scale. They can be compared to Hawai'i Island's lava zones. [4] [5] Maui Zone 1 - Includes the crater of Haleakalā and some rift zones, mainly areas that have experienced major eruptions in the last 1500 years.
Separation of the North and South American Plates in the Early-Mid Jurassic beginning with the rotation of the Yucatan Block, along with changes in sea level and thermal activity from the active rift, created a shallow marine basin wherein thick Jurassic salts and evaporites could be deposited. These evaporites overlay a thick transitional ...
A bathymetric map of the Mid-Atlantic Ridge (shown in light blue in the middle of the Atlantic Ocean). The Mid-Atlantic Ridge is a mid-ocean ridge (a divergent or constructive plate boundary) located along the floor of the Atlantic Ocean, and part of the longest mountain range in the world.
The Canadian Arctic Rift System is a branch of the Mid-Atlantic Ridge that extends 4,800 km (3,000 mi) into the North American continent. It is an incipient structure that diminishes in degree of development northwestward, bifurcates at the head of Baffin Bay and disappears into the Arctic Archipelago.
A rift is the result of pulling apart or extension of lithosphere, including the crust, caused by mantle upwelling where hotter asthenosphere magma rises up into the colder lithosphere to stretch and thin it. The internal dynamics of a rift system. The triple rift is thought to have begun in the Late Cretaceous epoch to the Paleogene period. At ...
Typical rift features are a central linear downfaulted depression, called a graben, or more commonly a half-graben with normal faulting and rift-flank uplifts mainly on one side. [4] Where rifts remain above sea level they form a rift valley , which may be filled by water forming a rift lake .
Map of Marie Tharp and Bruce Heezen, painted by Heinrich C. Berann (1977), showing the relief of the ocean floors with the system of mid-ocean ridges A mid-ocean ridge, with magma rising from a chamber below, forming new oceanic lithosphere that spreads away from the ridge Rift zone in Þingvellir National Park, Iceland.