An active continental margin primarily forms along actively converging boundaries of plates with one continental plate slipping underneath another. These areas are site of high levels of tectonic activity and as such the mountains formed in these areas are generally large volcanic mountains.
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its the Andes moutains you shmuck
apex
Fold mountains are formed at continent to continent convergent boundaries.
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Andes
Science
they have a continental rise
around the margins of the indian ocean
Convergent plate margins are characterized as collision zones between plates and may involve continental to continental crust, continental to oceanic crust, or oceanic to oceanic crust. Those that involve oceanic crust result in subduction of the more dense plate into the Earth's mantle. Continental to continental plate collisions result in uplift of the surface features and mountain building and the margin may eventually become welded together.
Plate tectonics.
Science
no.
Plate tectonics, (inter-continental plate collision).
They have a continental rise
Continental board-Continental deckcontinental fall
they have a continental rise
Passive continental margins are not areas of convergence. There is little volcanic and earthquake activity on passive margins. Active margins are areas of convergence where one plate is descending beneath another. They are associated with volcanic and earthquake activity.
around the margins of the indian ocean
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
continental rise
continental rise
A continental rise.