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[GRE真题] 历年GRE考试真题精选系列十七

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发表于 2012-8-15 12:45:20 | 显示全部楼层 |阅读模式
Scattered around the globe are more than one  
0 g/ w( d1 h: [/ T3 X1 bhundred regions of volcanic activity known as hot  
* c& c0 v: I( u5 B& R9 wspots. Unlike most volcanoes, hot spots are rarely  ) T7 u9 k4 F- K* }, h! M5 U
found along the boundaries of the continental and  1 v2 P( H; G( h8 {+ b$ |
oceanic plates that comprise the Earth’s crust; most  / j( G0 @9 [0 e
hot spots lie deep in the interior of plates and are  2 e' {  {2 g# c3 _) f0 F8 h
anchored deep in the layers of the earth’s surface.  ) R1 m+ i. [  q: T( a
Hot spots are also distinguished from other volcanoes  ' O9 T  A, G# g7 O
by their lavas, which contain greater amounts of  . a( U- V% U( U5 {/ ^1 Y: Q
alkali metals than do those from volcanoes at plate  
1 l' u! ?& |. q( Bmargins.
2 X) Q3 p; o6 B' [# d; H" A   In some cases, plates moving past hot spots have  ( F! O4 W4 l% b' L: a. u$ j
left trails of extinct volcanoes in much the same way  4 a5 J" `1 @9 s' j. |* y: i( O2 C
that wind passing over a chimney carries off puffs of  
" S5 Y2 s) P7 M* Wsmoke. It appears that the Hawaiian Islands were  , G6 [2 F  v3 s6 ^0 z4 U
created in such a manner by a single source of lava,  
( x% G2 Y5 H+ m, ?- l4 Gwelling up from a hot spot, over which the Pacific  
& d9 C6 H9 k- e7 }- ^- aOcean plate passed on a course roughly from the east  
# G- n; c) O4 P% ltoward the northwest, carrying off a line of volcanoes  
  U$ ~& q0 e0 b! M8 tof increasing age. Two other pacific island chains—
. ?  g; W$ m$ w" O$ R) v0 H, Othe Austral Ridge and the Tuamotu Ridge—parallel  $ S1 H$ i1 y  E$ H7 p& z
the configuration of the Hawaiian chain; they are also  
' O# ^3 [/ N1 S/ t8 z& z. m% ?% Laligned from the east toward the northwest, with the  
/ F' R; S; P5 Rmost recent volcanic activity near their eastern  ; D8 @/ g1 R, D  Y, _! H. O& Z1 C
terminuses.
' _  n1 y2 S" |& A7 @- [   That the Pacific plate and the other plates are  
. c  @- W3 J& k+ o  }0 _moving is now beyond dispute; the relative motion of  0 G4 ]8 E* M  l5 p0 X
the plates has been reconstructed in detail. However,  / c- L& d2 C7 H) E) {' V$ g
the relative motion of the plates with respect to the  
7 y% q$ h1 z# v; zEarth’s interior cannot be determined easily. Hot  & M7 c* }7 |$ H( e6 B; w" m4 L4 _
spots provide the measuring instruments for resolving  
  T# b7 C6 p  s3 O- D. b: \% q8 xthe question of whether two continental plates are  
) I4 X9 t- n/ b6 Q: Vmoving in opposite directions or whether one is sta-
+ y: {7 U/ g# B0 Z) H6 U% K, `  C2 ]tionary and the other is drifting away from it. The  
" d- E0 i/ m6 W# P! umost compelling evidence that a continental plat is  & ]; f  h& C* e: C
stationary is that, at some hot spots, lavas of several  8 u2 \# b5 r& Y1 J, k: ?
ages are superposed instead of being spread out in  
: G0 w. h* f* _chronological sequence. Of course, reconstruction of  ) J) o( }! T5 C5 |
plate motion from the tracks of hot-spot volcanoes  0 T2 {) `3 E* p) ]
assumes that hot spots are immobile, or nearly so.  . H* p% B( ~) l/ \
Several studies support such an assumption, including  
+ {# y- @  M! T# k9 X9 none that has shown that prominent hot spots through-
8 Q2 \5 [; h4 g# E. D; Xout the world seem not to have moved during the past  
0 M9 r9 ^* M5 k/ M& Zten million years.
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 楼主| 发表于 2012-8-15 12:45:21 | 显示全部楼层

历年GRE考试真题精选系列十七

Beyond acting as frames of reference, hot spots  4 f$ z- r0 e0 P
apparently influence the geophysical processes that  / y* L7 Y$ k) M" X& c. {3 s
propel the plates across the globe. When a continental  
8 g# d! y' S$ N7 }4 b3 x% N4 j2 i& uplate comes to rest over a hot spot, material welling  7 t% F- x% k: Y9 |
up from deeper layers forms a broad dome that, as it  
: G9 }- E- X, u! bgrows, develops deep fissures. In some instances, the  - n0 S% v; k7 j; F3 P$ r5 A% r: J
continental plate may rupture entirely along some of  
* @( a; x( i0 N* _( L% y" }# Sthe fissures so that hot spot initiates the formation  . e% X* i( \, ]1 I
of a new ocean. Thus, just as earlier theories have  
; c/ b& W4 @2 k# F5 H  {) w- ?5 [4 Gexplained the mobility of the continental plates, so  
% i) s! Y, i: ?" B; qhot-spot activity may suggest a theory to explain their  + {8 [- L% y: N6 L4 @
mutability. % c  N7 U: }! o- Q$ Y- \
  ) S& i( l8 i6 j8 n" R/ r/ X
20. The primary purpose of the passage is to  & w1 C7 n8 d/ g! s5 \& h. f
   (A) describe the way in which hot spots  , z+ T0 L7 D0 b# X$ ]( @! H5 @
     influence the extinction of volcanoes  
1 K4 ]! k! `  q& d+ J" c$ j) a   (B) describe and explain the formation of the  / w$ O7 h+ _) T, j" C3 ?/ I
     oceans and continents  8 L# `$ K, h% h, U: f$ M9 s6 W& Z( C
   (C) explain how to estimate the age of lava  1 K6 p1 z  Z4 m
     flows from extinct volcanoes  / f: c' J3 M  A
   (D) describe hot spots and explain how they  
+ z, T# c8 R$ y. \5 _1 A     appear to influence and record the  
, L7 J/ E* |. C4 l4 G     motion of plates $ [+ m6 Q$ z( @5 E
   (E) describe the formation and orientation of  
. l4 h6 U. a  p+ l: `# w     island chains in the Pacific Ocean  
0 g. |$ z6 \2 s9 ?6 M; C  ; i7 m6 K  ^; |" R* N, g( Q; ~/ R0 d) W5 n
21. According to the passage, hot spots differ from  
: W/ Z. j1 H( r% l/ `0 Q( bmost volcanoes in that hot spots ; e+ l* M2 {! q$ C" A
   (A) can only be found near islands
/ q5 h( s! ^" i4 k8 _( g/ _6 b   (B) are active whereas all other volcanoes are  
1 y  D2 O0 I8 H     extinct / H6 z$ C( d8 Q
   (C) are situated closer to the earth’s surface  - |, p$ r8 a2 J7 Q$ n) L
   (D) can be found along the edges of the plates  . S  E& b% U  n7 B. v. G7 j
   (E) have greater amounts of alkali metals in  0 n" [# [* H' p* b3 T6 U
     their lavas
0 F+ Y+ k: w/ T% G1 {( v$ ^  ) J7 p; P" ~0 ^$ a7 \7 T" f9 m' {
22. It can be inferred from the passage that evidence  / l6 e4 \& y" [9 w
for the apparent course of the Pacific plate has  
. a( B; M) @! b0 Ebeen provided by the  
& c: c7 s. x8 `3 K   (A) contours of the continents. : Y# S2 T% ^0 g; m9 h
(B) dimensions of ocean hot spots  5 R+ d  b# V/ ?) F
   (C) concurrent movement of two hot spots  ( I' i0 Q) _+ K0 X. Z" o
   (D) pattern of fissures in the ocean floor  
8 S' b( m/ G* o5 w: h   (E) configurations of several mid-ocean island  
- C$ ^8 o8 a! e/ A- T' [# h3 T; Qchains
, A- q* }; M" w3 t4 `- u/ _  ) p& H1 M2 I- F# Z- V# b
23. It can be inferred from the passage that the  
; O1 h' M6 p9 v  p" F  spreading out of lavas of different ages at hot  / {/ G! }& I, u
  spots indicates that a    e" D& U: @6 s4 S
   (A) hot spot is active
# ~0 _8 z; A% v7 V. c  u# T" t   (B) continental plate has moved  
! W5 l& C6 X9 u* s/ m   (C) continental rupture is imminent  * \1 ^4 S  I: m8 ?
   (D) hot spot had been moving very rapidly  
" a- x& v5 t  y1 o" G- l8 }   (E) volcano contains large concentrations of  
6 V0 f: Q) E% u0 @3 h6 I     alkali metals
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 楼主| 发表于 2012-8-15 12:45:22 | 显示全部楼层

历年GRE考试真题精选系列十七

24. The passage suggests which of the following  6 ]/ }7 K1 M: h* Z6 E
   about the Hawaiian Islands, the Austral  
- a7 \! M4 U# H+ [; I* E   Ridge, and the Tuamotu Ridge? . y3 ~$ }+ s! k$ I, p
   (A) The three chains of islands are moving east-
; ?* F$ b, D; `, U% o- a' Eward.
- M- L! [8 I4 E# w   (B) All the islands in the three chains have  : ^+ x9 g) f5 U5 I) G: W
     stopped moving. 2 P* F5 j5 B8 b; `' n3 `1 L
   (C) The three islands chains are a result of the  " L" ~) M2 E( \0 l$ [
     same plate movement.
: J4 @! f2 m. E9 t. p   (D) The Hawaiian Islands are receding from  4 Y7 j* _6 ?: N3 s( K' E9 D) y
     the other two island chains at a relatively  % s$ ?$ S) L+ O- ~# W
     rapid rate. 6 [+ _& e6 D; R6 H3 ]/ R: _
   (E) The Austral Ridge and the Tuamotu Ridge  8 k5 p: z: V* k% x. E
     chains have moved closer together    V  y3 z2 Z+ d' C' m4 K
     whereas the Hawaiian Islands have  : d. G7 J* f, N+ b
     remained stationary.
4 l  \1 _1 z  D8 D  , I( a% H& f0 Z+ P  g1 I  c% A8 C* D
25. Which of the following, if true, would best    |# J- V2 c& r7 Z' X& F
   support the author’s statement that hot-spot  1 H7 k) \: I8 M- F8 D3 I0 \3 D' j& n
   activity may explain the mutability of  
8 }$ a2 C' j& T5 w, M   continental plates? ; p7 H( P3 m" [% y3 i
   (A) Hot spots move more rapidly than the  9 }( F, C4 I2 R
     continental and oceanic plates. 7 M* F! }# Z  _+ X$ }. D
   (B) Hot spots are reliable indicators of the age  
5 s9 h7 {3 J/ y     of continental plates. * L" s( w* y4 Z/ f; Z8 a
   (C) Hot spots are regions of volcanic activity  
( [; F& q4 c9 f     found only in the interiors of the  . |4 M+ n% P0 b$ n2 l
     continental plates. 5 {# s* x7 U( x7 U
   (D) The alignment of hot spots in the Pacific.  ; P0 @9 X8 M( i* O
     Ocean parallels the alignment of Pacific  1 ^7 [& \0 ^# x; i: y
     Ocean islands. $ @% Q: d) Z" W& `2 z0 h
   (E) The coastlines of Africa and South  3 ], P2 I: D5 {! K5 T6 y2 D  }/ }
     America suggest that they may once  
% ]$ V5 a! i( |. l7 S     have constituted a single continent that  
* M( m8 O) B0 X6 O* [) h     ruptured along a line of hot spots.   k4 r) s3 {* W+ y, q0 g6 l
  / Q. C- Z5 p) \% ^" w% a; R
26. The author’s argument that hot spots can be  , r1 Y/ ^( ^. c9 T4 U
   used to reconstruct the movement of continental  
& G* m- s& }+ e1 }. v" f6 n+ A# S   plates is weakened by the fact that  
& Q3 v5 d3 H) i* L' I   (A) hot spots are never found at the boundaries  6 I0 y# l; v# N; J
     of plates
# p" G% c9 @6 T1 Z. c   (B) only extinct volcanoes remain after a plate  0 z0 v' u5 R2 \, B9 S6 R- Q7 W
     moves over a hot spot
5 s; j& G. k/ \7 x5 Z. ^5 F   (C) lava flow patterns for all hot spots have not  4 y3 a) Y2 p( \' n/ r& s9 H+ [# {
     been shown to be the same  
( _- V( r- E8 R  U% E0 K   (D) the immobility or near immobility of hot  8 n. f0 I+ b0 K2 K8 }" v) Q* F4 Z, _
     spots has not been conclusively proven  6 N( V3 _3 y% P. N( e" Q
   (E) the changing configurations of islands  
8 l+ E' H" u3 A: y! o: P     make pinpointing the locations of hot  $ t' l1 q* K8 I, Y: r* J
spots difficult  . B4 G2 d" E) _# g$ @
  
0 O, e& v( h) }  T' e0 X4 `  J27. The author’s style can best be described as  
2 G) B2 S; i( Q  u7 F- s   (A) dramatic  
  V$ i' }% \& Z( ]   (B) archaic  
# o+ e6 }. H) q  B/ Z& Z6 o   (C)esoteric  ( Z: {! {# s, k- O' G1 K( J
   (D) objective  * {, S' x/ I% N% f
   (E) humanistic  
% Q6 a7 N. y2 {5 T6 h, I20.D 21.E 22.E 23.B 24.C 25.E 26.D 27.D
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