The primary source of energy for ecosystem processes is photosynthesis. Directly or indirectly, photosynthesis provides the energy for all forms of life in the biosphere.
Because the rock making up continental plates is generally lighter and less dense than oceanic rock, it is too light to get pulled under the earth and turned into magma. Instead, a collision between two continental plates crunches and folds the rock at the boundary, lifting it up and leading to the formation of mountains and mountain ranges.
<span>At some convergent boundaries, an oceanic plate collides with a continental plate. Oceanic crust tends to be denser and thinner than continental crust, so the denser oceanic crust gets bent and pulled under, or subducted, beneath the lighter and thicker continental crust. This forms what is called a subduction zone.
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Answer:
The correct answer is D, the Himalayan Mountains.
Explanation:
The Himalayas is a high mountain system in Asia. It is the highest mountain range on Earth and lies between the Indian subcontinent in the south and the Tibetan highlands in the north. The mountains stretch for a length of about 3000 kilometers from Pakistan to Burma and reach a width of up to 350 kilometers. In the Himalayas are ten of the fourteen highest mountains on earth, the peaks of which are more than 8000 meters high, including Mount Everest, which is 8848 m above sea level being the highest mountain on Earth. With its southern location and the Tibetan highlands rising up in the back of the Himalayas as an extensive high plateau, the Himalayas have a great influence on the climate of South and Southeast Asia.
Answer:
Glaciers not only transport material as they move, but they also sculpt and carve away the land beneath them. A glacier's weight, combined with its gradual movement, can drastically reshape the landscape over hundreds or even thousands of years. The ice erodes the land surface and carries the broken rocks and soil debris far from their original places, resulting in some interesting glacial landforms.
