Divergent (Constructive)
Convergent (Destructive)
Transform Fault (Conservative)
Active and passive margins describe the various characteristics of continental margins that are a result of plate tectonics. An active margin usually has numerous volcanoes and mountains, while a passive margin typically do not have these formations.
The three types of plate boundaries are divergent boundaries, where plates move away from each other; convergent boundaries, where plates move towards each other; and transform boundaries, where plates slide past each other horizontally.
A plate margin is the boundary where two tectonic plates meet. These margins can be divergent (moving apart), convergent (moving together), or transform (moving past each other).Plate margins are dynamic areas where geological activities like earthquakes and volcanic eruptions often occur.
The three types of plate boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past each other horizontally.
The four types of plate movements that can cause earthquakes are convergent boundaries, divergent boundaries, transform boundaries, and subduction zones. These movements can result in the buildup of stress within the Earth's crust, which may eventually be released in the form of an earthquake.
the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries
the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries
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Active and passive margins describe the various characteristics of continental margins that are a result of plate tectonics. An active margin usually has numerous volcanoes and mountains, while a passive margin typically do not have these formations.
Yes, earthquakes can occur at constructive margins where tectonic plates are moving apart. As the plates separate, tension builds up in the crust which can lead to faults slipping and causing earthquakes. However, earthquakes at constructive margins tend to be less frequent and less intense compared to those at other types of plate boundaries.
Two types of crust involved at constructive plate margins are oceanic and continental crust. Oceanic crust is formed when magma rises to the surface at mid-ocean ridges, creating new oceanic crust. Continental crust can also be involved at constructive plate margins when rifting occurs, leading to the formation of new continental crust.
Convergent boundaries can form between two oceanic plates, between one oceanic plate and one continental plate, or between two continental plates.
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earthquake, volcano
after earth
Three types of plate boundaries are spreading boundaries, colliding boundaries, and sliding boundaries. um actually they are divergent, convergent, and transform