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求教 TT GWD-20-25 关于火山那篇

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楼主
发表于 2006-10-29 12:44:00 | 只看该作者

求教 TT GWD-20-25 关于火山那篇


    

Q22 to Q25:


    

      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
tre-


    

mendous 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
con-


    

sumed 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 “mis-


    

placed” volcanoes far from plate


    

 (25)     edges result from a second, indepen-


    

dent mechanism that cools the deep


    

interior of Earth.  Because of its prox-


    

imity 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
flow-


    

ing.  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.


    

Q25:


    

According to the passage, a hot spot on Earth’s surface is
an indication of which of the following?


    

 


    
  1. An
         untapped reservoir of hot rock in the base of the mantle
  2. Volcanic
         activity at the edge of a plate
  3. Solid
         mantle rock under tremendous pressure
  4. The
         occurrence of a phenomenon unique to the Pacific plate
  5. A
         plume of hot mantle rock originating near Earth’s core

The given correct answer is E.  My question is how about A?  I didn't see much difference between A and E.  Could anyone help to explain?

Thanks!

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