The continental crust is less dense than the oceanic crust. That's the reason we find that the oceanic crust sinks (subducts) beneath the continental crust.
Continental crust is less dense than oceanic crust and so cannot sink below it.
short answer, no... the continental crust is too thick and bouyant to be subducted by thinner oceanic crust.
if stuff goes screwy however you can get oceanic crust thrust over continental crust which is called an ophiolite complex and is generally a bag of hurt
The oceanic crust is more dense than the continental crust and therefore it sinks under it.
We find oceanic crust sinking beneath continental crust because oceanic crust is generally more dense than continental crust.
because the oceanic crust is denser than the continental crust.
The oceanic crust (typically made of basalt) is denser than the continental crust (usually made of granite and other lighter rocks). Denser substances sink lower than less dense substances.
The three types of convergent plate boundaries are Oceanic-Oceanic, Continental-Continental, Continental-Oceanic.
Rift Valleys are the most common at oceanic-continental convergent boundaries.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
Oceanic-Oceanic, Oceanic-Continental, and Continental-Continental are all sub types of convergent plate boundaries.
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The three types of convergent boundaries are when two plates meet and two oceanic plate meet, or where an oceanic and continental plate meet.the three types of convergent boundaries are continent boundaries , continent - ocean boundaries, and last but not least............. ocean boundaries
The three types of convergent plate boundaries are Oceanic-Oceanic, Continental-Continental, Continental-Oceanic.
if i thing if gago abno yudipota ka
Rift Valleys are the most common at oceanic-continental convergent boundaries.
There are three types of convergent boundaries: Oceanic, continental, and continental-oceanic convergent boundaries. Continental-continental convergent boundaries form mountain ranges. Continental-oceanic boundaries result in subduction zones and the recycling of lithosphere. The continental side of the boundary may form a mountain range. Oceanic-oceanic form deep oceanic trenches and sometimes volcanoes.
Oceanic-Continental, Oceanic-Oceanic, and Continental-Continental.
There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.
There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.
Convergent oceanic - continental and oceanic - oceanic boundaries.
Oceanic-Oceanic, Oceanic-Continental, and Continental-Continental are all sub types of convergent plate boundaries.
Syncline folds are found in Convergent boundaries. (Oceanic - Oceanic, Continental-Continental, Oceanic-Continental)
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.