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Plate tectonics, mountain ranges, volcanoes, and earthquakes are geological phenomena that can be explained in terms of physical and chemical processes in the Earth's crust.	板块构造、山脉（山体形成）、火山和地震都是可以依据地壳内部的物理与化学作用来解释的地质现象。
Beneath the Earth's crust lies the mantle which is heated by the radioactive decay of heavy elements.	地壳之下是地幔，它的热量来源于某些重元素的放射性衰变。
The mantle is not quite solid and consists of magma which is in a state of semi-perpetual convection.	地幔并非完全固态，它主要由半永久对流状的岩浆构成。
This convection process causes the lithospheric plates to move, albeit slowly.	这一对流过程导致岩石圈板块移动，尽管移动的过程非常缓慢。
The resulting process is known as plate tectonics.	板块移动的过程被称为板块构造。
Plate tectonics might be thought of as the process by which the Earth is resurfaced.	板块构造可以理解成地球表面的重塑过程。
As the result of seafloor spreading, new crust and lithosphere is created by the flow of magma from the mantle to the near surface, through fissures, where it cools and solidifies.	作为海底扩张的结果，岩浆从地幔流经裂隙流向近地表面，在此冷却凝固后形成新的地壳和岩石层。
Through subduction, oceanic crust and lithosphere returns to the convecting mantle.	通过俯冲作用，大洋地壳和岩石圈返回对流的地幔之中。
Areas of the crust where new crust is created are called divergent boundaries, those where it is brought back into the Earth are convergent boundaries and those where plates slide past each other, but no new lithospheric material is created or destroyed, are referred to as transform (or conservative) boundaries Earthquakes result from the movement of the lithospheric plates, and they often occur near convergent boundaries where parts of the crust are forced into the Earth as part of subduction.	地壳中产生新地壳的区域称为离散型边界；地壳物质被带入地球深处的区域叫做汇聚型边界；板块相互滑过，既不产生也不破坏新岩石圈物质的区域则称之为转换型（或称守恒型）边界。地震源于岩石圈板块的运动，常发生在汇聚型边界附近，此处部分地壳在俯冲作用下被迫插入地球内部。
Volcanoes result primarily from the melting of subducted crust material.	火山主要是由俯冲带地壳物质的熔融引起。
Crust material that is forced into the asthenosphere melts, and some portion of the melted material becomes light enough to rise to the surface—giving birth to volcanoes.	被推挤进软流圈的地壳物发生熔融，部分熔融体因密度降低而上升至地表——因此催生出了火山。

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