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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Relatively smooth waters helped trade and cultural exchange across the Mediterranean Sea. temperate climate provided for diverse and <span>abundant agriculture, substantial trade.</span>
The country in Europe that has marine west coast climate is Ireland
Explanation:
The marine west coast climate is one of the major climate types according to Koppen's climate classification. This climate type is mostly dictated by the sea. In Europe, the marine west coast climate can be found in a surprisingly high latitude, and the main reason for that are the warm ocean currents. The warm ocean currents of the Atlantic are running along the western coast of Europe, and they manage to have huge influence on the climate of the region.
- This climate type can be found at lower elevations and hills in Western Europe.
- The climate is warmer than it should be considering the latitude where this climate type is found in Europe.
- The summers are mild to warm, the springs and autumns mild to cold, while the winters are cold.
- The temperature extremes in both winter and summer are usually absent, and the climate is much more balanced.
- There is high amounts of precipitation throughout the whole year.
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When two oceanic plates collide, the younger of the two plates (because it is less dense)* will ride over the edge of the older plate. *(Oceanic plates grow more dense as they cool or move further away from the Mid-Ocean Ridge). The older, heavier plate bends and plunges steeply through the athenosphere, and descending into the earth, ir forms a trench that can be as much as 70 miles wide, more than a thousands miles long, and several miles deep.
C, take hundreds of millions of years to form!
