Continental-continental convergence.
The collision of the Indian plate with the Asian plate created the Himalayas, Karakoram, and Hindu Kush mountain ranges. These are some of the highest and most geologically active mountain ranges in the world.
The Himalayas are not formed by subduction. They are the result of the Indian tectonic plate colliding with the Eurasian plate, causing the uplift of the mountain range. The other options (Mt. Fuji, Mt. Rainier, and Krakatoa) are associated with volcanic activity resulting from subduction processes.
A convergent plate boundary typically forms mountains when two tectonic plates collide, causing the leading edge of one plate to be forced upward and form mountain ranges. This process is known as orogeny and can result in the creation of large mountain systems such as the Himalayas.
When oceanic plates collide with continental plates, The oceanic plate goes under the Continental plate, creating friction deep in the earth, where the plates are rubbing against each other, creating magma, which rises to the surface and creates volcanic mountain ranges. The Andes mountain range is an example. I don't know if this will help you at all.
Mountain formation can result from tectonic plate interactions, particularly through processes like continental collision, subduction, and rifting. When two continental plates collide, they can push the Earth's crust upward, forming mountain ranges like the Himalayas. Subduction of an oceanic plate beneath a continental plate can also lead to volcanic mountain ranges, such as the Andes. Additionally, rifting can create uplifted mountain ranges as the crust pulls apart.
are the result of continental-continental convergence (:
Continental-continental convergence
It's the Himalayas - although "mountain" questions are more complicated than might be thought as there are underwater mountains. The Himalayas, in brief, are the result of the Indian plate pushing into the Asian plate forcing up the Himalayas.
The collision of the Indian plate with the Asian plate created the Himalayas, Karakoram, and Hindu Kush mountain ranges. These are some of the highest and most geologically active mountain ranges in the world.
The Himalayas.
The Andes mountain range was not formed as a result of continental-continental convergence; instead, it resulted from oceanic-continental convergence. Specifically, the Andes were created by the subduction of the Nazca Plate beneath the South American Plate. In contrast, the Himalayas, Alps, and Appalachians are primarily the result of continental-continental tectonic interactions.
The Himalayas began forming approximately 50 million years ago as a result of the collision between the Indian Plate and the Eurasian Plate. This tectonic activity caused the land to uplift, creating the mountain range that we see today. The process is ongoing, as the tectonic plates continue to converge, causing the Himalayas to rise gradually.
The Himalayas do not subduct; instead, they are the result of the collision between the Indian Plate and the Eurasian Plate. This collision caused the land to buckle and fold, resulting in the towering mountain range. While subduction occurs in other areas of the world where one tectonic plate sinks beneath another, the Himalayas are primarily a result of continental collision rather than subduction.
The Himalayas are not formed by subduction. They are the result of the Indian tectonic plate colliding with the Eurasian plate, causing the uplift of the mountain range. The other options (Mt. Fuji, Mt. Rainier, and Krakatoa) are associated with volcanic activity resulting from subduction processes.
Some examples of mountain ranges created by continental-continental convergence are the Himalayas (resulting from the collision of the Indian and Eurasian plates) and the Alps (formed by the collision of African and Eurasian plates).
A convergent plate boundary typically forms mountains when two tectonic plates collide, causing the leading edge of one plate to be forced upward and form mountain ranges. This process is known as orogeny and can result in the creation of large mountain systems such as the Himalayas.
The Andes