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UID444249在线时间 小时注册时间2009-5-29最后登录1970-1-1主题帖子性别保密 
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JJ18确认是否为原文?考友们,叩谢!!!
| Earth’s surface consists of rigid plates that are constantly shifting and
 jostling one another. Plate movements
 Line are the surface expressions of motions
 (5) in the mantle—the thick shell of rock
 that lies between Earth’s crust and its
 metallic core. Although the hot rock of
 the mantle is a solid, under the tremendous
 pressure of the crust and
 (10) overlying rock of the mantle, it flows like
 a viscous liquid. The mantle’s motions,
 analogous to those in a pot of boiling
 water, cool the mantle by carrying hot
 material to the surface and returning
 (15) cooler material to the depths. When
 the edge of one plate bends under
 another and its cooler material is consumed
 in the mantle, volcanic activity
 occurs as molten lava rises from the
 (20) downgoing plate and erupts through the
 overlying one.
 Most volcanoes occur at plate
 boundaries. However, certain “misplaced”
 volcanoes far from plate
 (25) edges result from a second, independent
 mechanism that cools the deep
 interior of Earth. Because of its proximity
 to Earth’s core, the rock at the
 base of the mantle is much hotter than
 (30) rock in the upper mantle. The hotter the
 mantle rock is, the less it resists flowing.
 Reservoirs of this hot rock collect
 in the base of the mantle. When a
 reservoir is sufficiently large, a sphere
 (35) of this hot rock forces its way up
 through the upper mantle to Earth’s
 surface, creating a broad bulge in the
 topography. The “mantle plume” thus
 formed, once established, continues to
 (40) channel hot material from the mantle
 base until the reservoir is emptied.
 The surface mark of an established
 plume is a hot spot—an isolated
 region of volcanoes and uplifted terrain
 (45) located far from the edge of a surface
 plate. Because the source of a hot
 spot remains fixed while a surface
 plate moves over it, over a long period
 of time an active plume creates a chain
 (50) of volcanoes or volcanic islands, a
 track marking the position of the plume
 relative to the moving plate. The natural
 history of the Hawaiian island chain
 clearly shows the movement of the
 Pacific plate over a fixed plume.
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