Yes, because of the huge compressional forces when two plates collide. This can happen at either a continental-continental boundary or a continental-oceanic boundary.
Type - SubductionFeature - Trenches or Volcanic mountainsType - CollisionFeature - Folded mountains
No. Sea floor trenches are found at convergent boundaries. divergen boundaries form mid-ocean ridges.
lithosphere plates collide forming the folded mountains!
Mountain building (orogenesis) normally occurs at convergent plate boundaries where plates are moving towards each other. However at divergent boundaries there is a possibility for the formation of horst and graben structures where the tensile stresses cause down thrown blocks of crust to occur bordered by up thrown blocks of crust (horst) which may appear to be mountains.
when plate boundaries converge folded mountains are formed.
Folded and volcanic mountains
Both were probably formed from convergent plate boundaries.
Type - SubductionFeature - Trenches or Volcanic mountainsType - CollisionFeature - Folded mountains
No. Sea floor trenches are found at convergent boundaries. divergen boundaries form mid-ocean ridges.
Folded mountains are created when plates move. Folded mountains occur at convergent boundaries where land is being pushed together. The pressure of the plate motion causes the land above to fold. This folding can happen in a number of different patterns. These folding patterns appear as domes, waves, or twists and turns. Occasionally, this happens at a divergent boundary where part of the adjacent land moves, causing the surface layers to buckle or fold. Folded mountains often have gentile slopes and a dome appearance.
lithosphere plates collide forming the folded mountains!
Mountain building (orogenesis) normally occurs at convergent plate boundaries where plates are moving towards each other. However at divergent boundaries there is a possibility for the formation of horst and graben structures where the tensile stresses cause down thrown blocks of crust to occur bordered by up thrown blocks of crust (horst) which may appear to be mountains.
It is folded and uplifted, or subducted into the mantle, depending on the type of convergent boundary.
two plates collide and then their edges crumble like a paper
No. A mid-ocean ridges is a divergent boundary. You find folded mountain at convergent plate boundaries.
when plate boundaries converge folded mountains are formed.
At distructive plate boundaries, and yes the Hymmalayas is an example of a fold mountain as are the Alps