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Tectonic_plate_boundaries.png (775 × 429 pixels, file size: 83 KB, MIME type: image/png) This is a file from the Wikimedia Commons . Information from its description page there is shown below.
These plates, called tectonic plates, can push against each other. Earthquakes are most common along fault lines, which are fractures that allow the plates to move.
This is an accepted version of this page This is the latest accepted revision, reviewed on 17 January 2025. Linear feature that exists between two tectonic plates that are moving away from each other This article needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. Find sources ...
The Motagua Fault has been responsible for several major earthquakes in Guatemala's history, including the 7.5 M w Guatemala 1976 earthquake, and is also notable for its significant visible fault trace. [4] The event caused 2 meters of vertical displacement and ruptured 230 km of the fault's length.
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While earthquakes are most common along the fault lines of tectonic plates—of which there are seven major ones in the world—the seismic quakes can actually hit anywhere, at any time, according ...
A series of earthquakes and aftershocks striking the border region between southeast Turkey and northwest Syria on Monday is feared to have killed 20,000 people.. The 7.8 magnitude earthquake ...
This is a list of tectonic plates on Earth's surface. Tectonic plates are pieces of Earth's crust and uppermost mantle , together referred to as the lithosphere . The plates are around 100 km (62 mi) thick and consist of two principal types of material: oceanic crust (also called sima from silicon and magnesium ) and continental crust ( sial ...