enow.com Web Search

Search results

  1. Results from the WOW.Com Content Network
  2. File:Active Margin.svg - Wikipedia

    en.wikipedia.org/wiki/File:Active_Margin.svg

    Main page; Contents; Current events; Random article; About Wikipedia; Contact us

  3. Continental margin - Wikipedia

    en.wikipedia.org/wiki/Continental_margin

    These active margins can be convergent or transform margins, and are also places of high tectonic activity, including volcanoes and earthquakes. The West Coast of North America and South America are active margins. [4] Active continental margins are typically narrow from coast to shelf break, with steep descents into trenches. [4] Convergent ...

  4. Wikipedia:WikiProject Maps/Conventions - Wikipedia

    en.wikipedia.org/wiki/Wikipedia:WikiProject_Maps/...

    Most of these conventions are supported by active groups of map makers, and have been created and improved through long and serious discussions. The main intentions are: to display efficiently selected data; to create screen, web, print, creation & share friendly maps; to create a wiki style free of nationalism issues.

  5. Accretionary wedge - Wikipedia

    en.wikipedia.org/wiki/Accretionary_wedge

    Active margins characterized by a significant proportion of fine-grained sediment within the incoming section, such as northern Antilles and eastern Nankai, exhibit thin taper angles, whereas those characterized by a higher proportion of sandy turbidites, such as Cascadia, Chile, and Mexico, have steep taper angles. Observations from active ...

  6. Seafloor spreading - Wikipedia

    en.wikipedia.org/wiki/Seafloor_spreading

    The driver for seafloor spreading in plates with active margins is the weight of the cool, dense, subducting slabs that pull them along, or slab pull. The magmatism at the ridge is considered to be passive upwelling, which is caused by the plates being pulled apart under the weight of their own slabs.

  7. Orogeny - Wikipedia

    en.wikipedia.org/wiki/Orogeny

    Orogeny (/ ɒ ˈ r ɒ dʒ ə n i /) is a mountain-building process that takes place at a convergent plate margin when plate motion compresses the margin. An orogenic belt or orogen develops as the compressed plate crumples and is uplifted to form one or more mountain ranges.

  8. Continental shelf - Wikipedia

    en.wikipedia.org/wiki/Continental_shelf

    Passive continental margins such as most of the Atlantic coasts have wide and shallow shelves, made of thick sedimentary wedges derived from long erosion of a neighboring continent. Active continental margins have narrow, relatively steep shelves, due to frequent earthquakes that move sediment to the deep sea.

  9. Category:Labelled map templates - Wikipedia

    en.wikipedia.org/.../Category:Labelled_map_templates

    Templates presenting maps to which labels have been added (e.g. using {{ Image label ...