Plate Tectonics and Geological Deformations Explained
Classified in Geology
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Divergent Boundaries
This occurs when a stream of magma rises to encounter a plate, breaking it up and separating it into two fragments.
Convergent Boundaries
These occur when two plates collide against each other.
Oceanic and Continental Plates
The oceanic plate sinks beneath the continental plate in a process called subduction.
Continental Plates
If two continental plates collide, they form intracontinental mountain ranges.
Two Oceanic Plates
When two oceanic plates collide, subduction occurs, with one sliding below the other to form a volcanic island arc.
Transform Boundaries
Plates slide laterally without climbing over one another, causing the formation of large faults.
Deformations and Scales
- Mesotectonics: Structures between 1m and 1km in length.
- Macrotectonics: