Convergant boundries hit eachother and wrinkle like a wet graham cracker. This forms the mountains
The Pontic Mountains are formed by convergent boundaries, where the Eurasian plate subducts beneath the Anatolian plate. This collision causes uplift and deformation of the Earth's crust, resulting in the formation of mountain ranges like the Pontic Mountains.
No, divergent boundaries do not cause the formation of mountains. Instead, mountains are typically formed at convergent boundaries where tectonic plates collide. Divergent boundaries are where plates move away from each other, creating rifts and oceanic ridges.
Oceanic-continental convergent boundaries form mountains with a volcanic origin, such as the Andes in South America. Oceanic-oceanic convergent boundaries create volcanic island arcs, like the Japanese archipelago.
Mountains are typically formed by tectonic plate movements, where one plate is pushed up over another, creating uplifted landforms. The boundaries where tectonic plates meet, such as convergent or collision boundaries, often lead to the formation of mountain ranges through processes like folding, faulting, and volcanic activity. These boundaries can also experience intense seismic activity, leading to the further formation and growth of mountains over time.
Mountains.
convergent
The mountains that are associated with convergent plate boundaries are mountain ranges or mountain belts. Examples of a mountain range is the Andes.
usually it is mountains
Earthquakes and volcanoes are hazards typically associated with convergent boundaries where tectonic plates collide. Mountains can also form at convergent boundaries due to the collision of plates. Trenches are associated with subduction zones at convergent boundaries where one plate is forced beneath another. Mudslides are not directly related to convergent boundaries.
Compression stress is found at convergent boundaries, where two tectonic plates are moving towards each other. This stress can result in the formation of mountains, deep ocean trenches, and volcanic arcs.
Convergent boundary mountains are formed where two tectonic plates collide, causing one plate to be forced beneath the other in a process called subduction. This collision can lead to the formation of mountain ranges due to the intense pressure and folding of the Earth's crust. The Himalayas are a notable example of convergent boundary mountains, formed by the collision of the Indian Plate with the Eurasian Plate.
Underwater volcanoes and mountains can form at both convergent and divergent boundaries.