Peter Coyote?
Tectonic plates.
Continents exist due to the movement of tectonic plates on Earth's surface. These plates constantly shift and collide, leading to the formation of continents over millions of years. The Earth's crust is divided into several large and small land masses, which we refer to as continents.
When two continents collide, it usually forms a convergent boundary. This often leads to the creation of mountain ranges due to the intense pressure and folding of the Earth's crust. Examples include the Himalayas formed by the collision of the Indian Plate with the Eurasian Plate.
Continental drift is an ongoing process, so the arrangement of continents will continue to change over millions of years. One possible scenario is that the continents may merge into a supercontinent, similar to past supercontinents like Pangaea, before eventually breaking apart again due to tectonic plate movements.
When continents collide, they can either merge together to form a larger landmass or create mountains due to the intense pressure and folding of the Earth's crust. This process, known as continental collision, can lead to the formation of mountain ranges like the Himalayas when two continental plates collide. Additionally, it can also cause earthquakes, volcanic activity, and the rearrangement of land and sea boundaries.
when continents collide you bum your pet hamster
When continents collide, they can form mountain ranges, such as the Himalayas. The immense pressure and heat generated during the collision can cause the Earth's crust to fold and uplift, leading to the formation of high peaks. Additionally, the collision can also result in the creation of deep oceanic trenches and volcanic activity.
Tectonic plates.
Europe and Asia
Continents exist due to the movement of tectonic plates on Earth's surface. These plates constantly shift and collide, leading to the formation of continents over millions of years. The Earth's crust is divided into several large and small land masses, which we refer to as continents.
When two continents collide, mountains called "fold mountains" are formed. This process is known as orogeny, and examples of such mountains include the Himalayas and the Alps. The collision forces the rocks to compress and fold, creating vast mountain ranges.
When two continents collide, it usually forms a convergent boundary. This often leads to the creation of mountain ranges due to the intense pressure and folding of the Earth's crust. Examples include the Himalayas formed by the collision of the Indian Plate with the Eurasian Plate.
c) two continents collide. Mountain formation typically occurs when two tectonic plates collide, causing the crust to rise and form mountain ranges. This process is common when continents converge, leading to the compression and uplift of the Earth's crust, resulting in the formation of mountains.
Continental drift is an ongoing process, so the arrangement of continents will continue to change over millions of years. One possible scenario is that the continents may merge into a supercontinent, similar to past supercontinents like Pangaea, before eventually breaking apart again due to tectonic plate movements.
When continents collide, they can either merge together to form a larger landmass or create mountains due to the intense pressure and folding of the Earth's crust. This process, known as continental collision, can lead to the formation of mountain ranges like the Himalayas when two continental plates collide. Additionally, it can also cause earthquakes, volcanic activity, and the rearrangement of land and sea boundaries.
Continents grow through a process called continental drift, where tectonic plates move and collide. As plates converge, they can create mountain ranges and add landmass to existing continents. This process takes millions of years to occur.
When two plates carrying continents collide, they can buckle upward to form mountain ranges through a process known as continental collision. This occurs as the crust shortens and thickens, leading to the upward deformation of the land. If one plate subducts beneath the other, it can also lead to the downward bending of the crust in the form of trenches or subduction zones.