An Account Of Tectonic Activity

there are three main types of headquarters border; constructive, poisonous and conservative, each with different processes that follow. At a constructive margin, the two menages involved are usually moving isolated from each other, thus creating a gap in the lithosphere and allowing magma from the mantle to well up in between. This process of the magma welling up creates new land mass as the magma cools to form busybodied igneous rock. A landform that is usually associated with this type of graduated table limit point is a rift valley; a rift valley is a large raftyon like feature at which the ground within has collapsed due to the separation of the two lithospheric plates. These can be volatile places, emitting poisonous gasses such as henry Sulphide and Sulphur. An example of a rift valley which is lifelessness in the process of development is the East African time out Valley, which stretches out for miles along the Eastern side of Africa.
Conservative plate boundaries are completely different to both constructive and destructive; land is neither created nor destroyed. At a conservative or transform boundary, the plates are sliding olden one another.



This causes a huge amount of friction to build up a huge amount of pressure, which is retained as potential slide fastener; when the pressure becomes too much, the energy is released and the pates quickly jolt past each other in the form of an earthquake. These can be very destructive to structures and can cause a consentaneous series of other problems which may cause death or destruction. One of the landforms which are usually associated with this type of boundary is strike-slip faults. These are large cracks in the lithosphere which appear perpendicular to the plate boundary; they can be very long and sometimes quite wide. One of the most well-known conservative plate boundaries is the San Andreas Fault which runs along the western coast of the U.S.A, from San Francisco to Los Angeles, and down into Mexico. There have been many major and minor earthquakes...If you want to captivate a full essay, order it on our website: Ordercustompaper.com



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