How do plate motions create mountains?
Plate tectonic processes create some of the world's most beautiful places. The North Cascades Mountains in Washington State are a continental volcanic arc. The mountains currently host some glaciers. There are many features left by the more abundant ice age glaciers. Changes in altitude make the range a habitable place for many living organisms.
Stress and Mountain Building
Many processes create mountains. Most mountains form along plate boundaries. A few mountains may form in the middle of a plate. For example, hotspot volcanoes.
Most of the world’s largest mountains form as plates collide at convergent plate boundaries. Continental crust is too buoyant to get pushed down into the mantle. So when the plates smash together, the crust crumples upward. This creates mountains. Folding and faulting in these collision zones makes the crust thicker.
The world’s highest mountain range, the Himalayas, is growing as India collides with Eurasia. About 80 million years ago, India was separated from Eurasia by an ocean ( Figure below ). As the plates collided, pieces of the old seafloor were forced over the Asian continent. This old seafloor is now found high in the Himalayas ( Figure below ).
As India rams into Eurasia, the Himalaya Mountains rise.
Oceanic Plate Subduction
Volcanic mountain ranges form when oceanic crust subducts into the mantle at convergent plate boundaries. The Andes Mountains are a chain of coastal volcanic mountains. They are forming as the Nazca plate subducts beneath the South American plate ( Figure below ).
Cotopaxi is in the Andes Mountains of Ecuador. The 19,300 foot tall mountain is the highest active volcano in the world.
Mid-ocean ridges form at divergent plate boundaries. As the ocean floor separates an enormous line of volcanoes is created.
Continents can also rift apart; a process called continental rifting . When continental crust is pulled apart, it breaks into blocks. These blocks of crust are separated by normal faults. This is known as block faulting . The blocks slide up or down. The result is alternating mountain ranges and valleys. This topography is known as basin-and-range ( Figure below ). The area near Death Valley, California is the center of a classic basin-and-range province ( Figure below ).
This diagram shows how a basin-and-range forms.
This photograph was taken from a basin with a range in the distance near Death Valley, California.
Here you can find a very quick animation of movement of blocks in a basin-and-range setting: http://earthquake.usgs.gov/learn/animations/animation.php?flash_title=Horst+%26amp%3B+Graben&flash_file=horstandgraben&flash_width=380&flash_height=210 .
- block faulting : Large blocks of rock that are separated by normal faults
- continental rifting : The process that causes continental crust to extend and thin.
- Converging or diverging plates cause mountains to grow.
- Subduction of oceanic crust beneath a continental or oceanic plate creates a chain of volcanoes.
- Tensional forces bring about block faulting. This creates a basin-and-range valleys and mountains.
Use the resource below to answer the questions that follow.
- Mountain Building at http://www.history.com/shows/how-the-earth-was-made/videos/mountain-building (2:14)
- What created the landscape we see today on Earth?
- What can cause mountains to form?
- How tall are the Alps?
- How were the Alps formed?
- Explain the forces that caused the Alps to form.
- Describe how plates create mountain ranges like the Himalayas.
- Diagram how pulling apart continental crust could create mountains and basins. What are the mountains and basins called?
- Why don't strike slip faults create mountains?