Ad
related to: rift geometry symbol chart printable free blank contracts agreements word
Search results
Results from the WOW.Com Content Network
The following table lists many specialized symbols commonly used in modern mathematics, ordered by their introduction date. The table can also be ordered alphabetically by clicking on the relevant header title.
Continental-continental divergent/constructive boundary Oceanic divergent boundary: mid-ocean ridge (cross-section/cut-away view). In plate tectonics, a divergent boundary or divergent plate boundary (also known as a constructive boundary or an extensional boundary) is a linear feature that exists between two tectonic plates that are moving away from each other.
A passive margin forms by sedimentation above an ancient rift, now marked by transitional lithosphere. Continental rifting forms new ocean basins. Eventually the continental rift forms a mid-ocean ridge and the locus of extension moves away from the continent-ocean boundary. The transition between the continental and oceanic lithosphere that ...
Accommodation zones may be located where older crustal structures intersect the rift axis. In the Gulf of Suez rift, the Zaafarana accommodation zone is located where a shear zone in the Arabian-Nubian Shield meets the rift. [6] Rift flanks or shoulders are elevated areas around rifts. Rift shoulders are typically about 70 km wide. [7]
As the rift valley aged, extensive deformation developed on both sides of the lake, converting them into asymmetric full grabens. [8] A generalized cross section of the Albuquerque Basin from east to west. Note the half-graben geometry, Paleozoic and Mesozoic sediments that existed pre-rift, and the large (up to 28%) amount of extension. [11]
The elements of a polytope can be considered according to either their own dimensionality or how many dimensions "down" they are from the body.
Rift valley – Linear lowland created by a tectonic rift or fault; Rôche moutonnée – Rock formation created by the passing of a glacier; Sandur – Plain formed from glacier sediment transported by meltwater; Side valley – Valley with a tributary to a larger river
The Midcontinent Rift System (MRS) or Keweenawan Rift is a 2,000 km (1,200 mi) long geological rift in the center of the North American continent and south-central part of the North American plate. It formed when the continent's core, the North American craton , began to split apart during the Mesoproterozoic era of the Precambrian , about 1.1 ...
Ad
related to: rift geometry symbol chart printable free blank contracts agreements word