The plates get closer together.
Volcanos,,,, Mountain Building
they will form a mountain
Over time, they form a mountain range
The Himalayas are one of the youngest Mountain ranges in the world. So the to tectonic plates which collided to make the Himalayas are really still hitting each other, therefore making Mount Everest and other Mountains in the Himalayan range taller.
Volcanoes are not necessarily bigger than mountains. A volcano is a mountain that forms from the eruption of magma, while a mountain can be formed through various processes like tectonic plate movement. The size of a volcano or mountain can vary greatly, with some volcanoes being taller or larger than some mountains, and vice versa.
Yes. The Andes Mountain Range is above sea level. As the Pacific Plate slides under South America, the Andes continue growing taller. They may have grown higher with this latest earthquake in Chile.
When that happens a earthquake is produced.
I assume you meant a tectonic plate boundary? When a weaker plate collides with a stronger plate, the weaker plate may be subducted, (forced downwards) and into the mantle. When the Indian Plate collided with the European Plate, the Indian Plate was subducted beneath the European Plate, which raised the European plate and caused the formation of the Himalayas Mountain Range.
Mountains can vary in height due to differences in tectonic processes such as plate collisions, volcanic activity, and erosion. Taller mountains are typically formed at convergent plate boundaries where two continental plates collide, pushing the Earth's crust upwards to create massive mountain ranges like the Himalayas. Erosion rates also play a role in determining mountain height, as faster erosion can wear down mountains quicker and result in lower peaks.
either subduction (e.g. pacific ring of fire) or mountain building (e.g. himalayas)
an example of a convergent plate/boundary are mountain ranges
Mountain building occurs through the process of tectonic plates colliding or converging, causing the earth's crust to fold, fault, and uplift. This can result in the formation of mountain ranges and chains over millions of years as a result of tectonic forces pushing rock layers upwards.