Question

Continental-continental plate collisions produce ____.

Question 1 options:
island arcs
rift valleys
deep-sea trenches
very tall mountain ranges

Answer 1

Continental-continental plate collisions result in the formation of very tall mountain ranges, such as the Alps and the Ural Mountains, through the process of mountain building.

Step-by-step explanation:

Continental-continental plate collisions produce very tall mountain ranges. This tectonic activity occurs when two continental plates push against each other with great force, causing the Earth's crust to buckle and fold. The process elevates parts of the crust to form mountain ranges. A well-known example of such a formation is the Alps, which were created by the collision of the African and Eurasian plates. Other notable mountain ranges formed by this geological process include the Ural Mountains, marking the boundary between Europe and Asia, and the Appalachian Mountains, which underwent several orogenies shaping their current form.

Unlike oceanic-continental collisions that can create deep-sea trenches or island arcs, like the Marianas Trench or the Japanese Archipelago, continental-continental collisions do not typically result in significant volcanic activity. Rather, the primary result is the impressive mountain-building phenomenon, as the terrestrial plates crumple up against each other.

Answer 2

Answer: very tall mountain ranges

Explanation:When there is a collision between two continental plates, they become crunched up and then the rock folds at the boundary where it becomes lifted up and this leads to the formation of mountains and mountain ranges.

When collision occurs between two continental plates, both plates cannot be subducted because of their increased bouyancy. So when this collision occurs, features like subduction zone, trench and wedge do not occur. This type of collision occurs when the sea becomes narrower until both plates collide.

After the occurence of the collision, oceanic lithosphere breaks off and then sinks down into the mantle. The subduction zone then becomes inactive.

The two continents now welds together as they are being compressed together as time goes on.

The earth crust then becomes thickened by the under- thrusting of one continent under the other continent.

An example of this collision is the Himalayas where India collided with Asia.