冰岛是由于“热区”里的物质从地底深处涌起,把部分海底山脊推到空中而形成的国家。
Iceland is the result of a "hotspot" in which material rises from deep within the Earth, pushing part of this ridge up into the air.
海底板块移动得离中部山脊越远,额外的热能给予板块的浮力就越大。
That extra thermal energy gives the ocean plates more buoyancy as they move farther away from the ridges.
随着这种新地壳的冷却,它会在自身重力的作用下凹陷下去,这个过程被称为“沉降”。因此,在距离海洋中部山脊越远的地方,海底就应该越深。
As the new crust cools, it sinks under its own weight-a process called subsidence-so the seafloor should be deeper the farther it is from a mid-ocean ridge.
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