Search results
Results from the WOW.Com Content Network
This paradoxically results in divergence which was only incorporated in the theory of plate tectonics in 1970, but still results in net destruction when summed over major plate boundaries. [2] Divergent boundaries are areas where plates move away from each other, forming either mid-ocean ridges or rift valleys. These are also known as ...
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 ...
Extensional tectonics is associated with the stretching and thinning of the crust or the lithosphere.This type of tectonics is found at divergent plate boundaries, in continental rifts, during and after a period of continental collision caused by the lateral spreading of the thickened crust formed, at releasing bends in strike-slip faults, in back-arc basins, and on the continental end of ...
This list covers all faults and fault-systems that are either geologically important [clarification needed] or connected to prominent seismic activity. [clarification needed] It is not intended to list every notable fault, but only major fault zones.
Includes country profiles, disaster profiles and a disaster list. "Natural Hazard Information from the Coastal Ocean Institute". Woods Hole Oceanographic Institution Particularly including articles on tsunamis, hurricanes and other storms. "Global Disaster Alert and Coordination System".
Plate tectonics. Continental drift; Earthquake; Oceanic trench; Phenomena associated with igneous activity. Geysers and hot springs; Bradyseism; Volcanic eruption; Earth's magnetic field; Exogenic phenomena Slope phenomena Slump; Landslide; Weathering phenomena Erosion; Glacial and peri-glacial phenomena Glaciation; Moraines; Hanging valleys ...
Unlike the West Coast, where tectonic plates meet at a boundary and create a seismic hazard that runs down the spine of the coast, the Northeast’s tectonic risk is rooted in ancient history ...
Seismotectonics is the study of the relationship between the earthquakes, active tectonics and individual faults of a region. It seeks to understand which faults are responsible for seismic activity in an area by analysing a combination of regional tectonics, recent instrumentally recorded events, accounts of historical earthquakes and geomorphological evidence.