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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  
- ~9 K, F* O1 l4 r$ Ohundred regions of volcanic activity known as hot  
/ N: Y# }& G' r! G5 w* J3 q/ gspots. Unlike most volcanoes, hot spots are rarely  
6 D+ i1 V7 {( I) `- ifound along the boundaries of the continental and  & y, f+ r5 i0 E
oceanic plates that comprise the Earth’s crust; most  8 y1 W4 T( _7 j/ I+ C0 Y
hot spots lie deep in the interior of plates and are  # e. G$ V' t8 q0 o
anchored deep in the layers of the earth’s surface.  + q  ~+ {) l* n5 U! L. [7 L6 B& D3 |7 w
Hot spots are also distinguished from other volcanoes  
4 J; |5 r' j9 o4 {% I5 z# Z8 eby their lavas, which contain greater amounts of  
$ y( D/ ?/ O7 a- T* j+ ~alkali metals than do those from volcanoes at plate  1 J0 U% Y3 J4 g6 R
margins.
" D! I9 L0 x; f/ ~# ?   In some cases, plates moving past hot spots have  
1 \9 U; N  }7 sleft trails of extinct volcanoes in much the same way  7 U" K( m( P+ G* `, L
that wind passing over a chimney carries off puffs of  
$ {) m9 d8 L4 m* ?) i8 u  @% ]smoke. It appears that the Hawaiian Islands were  ; W' z$ L; j; [1 Q
created in such a manner by a single source of lava,  
; m  K8 P6 _3 L# X2 Twelling up from a hot spot, over which the Pacific  
% G3 R; x; K6 W- ?, n( ZOcean plate passed on a course roughly from the east  % r- E- K: |5 E$ \2 X' ^# `
toward the northwest, carrying off a line of volcanoes  / W6 D# [* r/ _3 P
of increasing age. Two other pacific island chains—
" L3 K' V% z7 l1 e( ~( q$ ethe Austral Ridge and the Tuamotu Ridge—parallel  % |) Z) U/ U4 p& |$ ~; Q
the configuration of the Hawaiian chain; they are also  ; @  H! d/ ]. x# c, a
aligned from the east toward the northwest, with the  ! c+ N! I9 h( J! D" Y8 V3 w9 t
most recent volcanic activity near their eastern  
. N" L1 l7 ^  b" R. w8 Q' Tterminuses. & Q% M+ [. D9 F* v$ h
   That the Pacific plate and the other plates are  
& k' E& H( F' q# _# mmoving is now beyond dispute; the relative motion of  5 Q1 I( W5 z; Z; H  }
the plates has been reconstructed in detail. However,  
5 l& M$ d4 f! t- Pthe relative motion of the plates with respect to the  ; X3 N* u/ w3 y" V0 x
Earth’s interior cannot be determined easily. Hot  2 @! ~0 o- j7 |% F2 G. X
spots provide the measuring instruments for resolving  ' W0 j* p& a- ~
the question of whether two continental plates are  
, T' M/ A: L, [1 `9 O9 Q& Zmoving in opposite directions or whether one is sta- - P- g* u  }5 ?! K# W
tionary and the other is drifting away from it. The  
* T& k! h, U+ V0 Z# S8 m' r1 T; ymost compelling evidence that a continental plat is  ( _% p( O0 n3 u; n
stationary is that, at some hot spots, lavas of several  ( S0 s7 h. r& ]) M3 S/ j6 ^1 B3 M
ages are superposed instead of being spread out in  ) K7 p. e6 S  O! b; c6 d
chronological sequence. Of course, reconstruction of  
% b9 I$ u5 P' L; q, d6 ^5 U3 ]plate motion from the tracks of hot-spot volcanoes  
, g$ K$ x& f3 |/ o* ]assumes that hot spots are immobile, or nearly so.  * P& a' A' b1 ~/ w  w
Several studies support such an assumption, including  
$ w( v/ [) k2 vone that has shown that prominent hot spots through- 6 D% V. r; ~8 {6 |$ H5 B' a
out the world seem not to have moved during the past  
+ j% Q7 p# [; `/ r! Vten 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  ) m$ c+ p) c, f: F+ l/ |7 |
apparently influence the geophysical processes that  
: l! F. k, Z$ v9 q6 jpropel the plates across the globe. When a continental  
+ y. C" t$ p5 Q  W; i( V) Uplate comes to rest over a hot spot, material welling    Z# L& q6 N& Y! S
up from deeper layers forms a broad dome that, as it  
& E$ ~3 U1 J3 h' E9 agrows, develops deep fissures. In some instances, the  
8 b; c% O  n* qcontinental plate may rupture entirely along some of  ; k( P* k+ U& @$ H) `: A
the fissures so that hot spot initiates the formation  1 M4 [0 N& C0 ?- D4 X- K# [4 v* S
of a new ocean. Thus, just as earlier theories have  : B- }( T% G6 Q& o2 o: f" j& B* I
explained the mobility of the continental plates, so  
$ d7 h; {8 s1 }  Zhot-spot activity may suggest a theory to explain their  7 |  w1 M1 J+ ?1 r4 ~$ G
mutability.
3 g4 d+ k" @! c( n5 x    W! f* _) h4 H5 x! R, ~# N
20. The primary purpose of the passage is to  " W4 {% ?- ~- H+ i8 G# F
   (A) describe the way in which hot spots  
7 e( N  N5 {. q! k     influence the extinction of volcanoes  
( m9 b( S' j. A/ _: l   (B) describe and explain the formation of the  , A! P9 H3 i. B6 b
     oceans and continents  
# t' u8 F0 x6 z- d   (C) explain how to estimate the age of lava  / e4 ^2 @- C; K& q0 c3 F& e( z
     flows from extinct volcanoes  # ]2 \9 b6 D) }1 U
   (D) describe hot spots and explain how they  
* u0 }5 z. L8 g4 m: W7 d$ E# V- v     appear to influence and record the  
' c! S7 j3 ?( Z. p     motion of plates ' C  }% ~8 X! e+ E
   (E) describe the formation and orientation of  ' a: }0 j6 e% D& y5 T9 z8 X
     island chains in the Pacific Ocean  
" }0 ], i/ [. F1 _2 v1 q$ z  8 p( d3 q8 k. s+ H" w* S4 I: ?
21. According to the passage, hot spots differ from  
! p. q: k2 w4 f! U, }most volcanoes in that hot spots " w+ o4 z" ^4 n: A* ^
   (A) can only be found near islands
9 K; O9 b, m5 R5 n" ]$ G+ c! c   (B) are active whereas all other volcanoes are  
3 W- f# Z4 q5 K2 d2 ^# P     extinct ) ]4 s: A  W$ O: |# e* j
   (C) are situated closer to the earth’s surface  6 N7 P9 L( n( \& K
   (D) can be found along the edges of the plates  5 _( z7 h4 Q! d
   (E) have greater amounts of alkali metals in  % I" f6 ^4 X. n
     their lavas
( k- ~1 J$ a; j  " V6 L/ H$ Q- F/ m1 _
22. It can be inferred from the passage that evidence  0 M' h3 l4 e- c$ i6 ?0 U& |! r5 q
for the apparent course of the Pacific plate has  
9 M' _6 h3 E3 ebeen provided by the  & w, h4 Q0 O6 c  |7 R9 t( M3 Y
   (A) contours of the continents. 4 j0 h* I# d" d1 e: t3 |
(B) dimensions of ocean hot spots  
( E( q- |4 M, _" v   (C) concurrent movement of two hot spots  4 o; w3 r$ G! w- L( G7 K( U
   (D) pattern of fissures in the ocean floor  
" O8 U! B/ ?4 E  R0 N) i1 ^   (E) configurations of several mid-ocean island  # X0 p% D! M, ^5 x  W8 V. `
chains
0 C; I2 b; @8 F  J! @. d5 z  Q  
: q% Y3 \" y% k1 I) S6 F& v1 m23. It can be inferred from the passage that the  
6 f3 {0 f" q2 n' f1 t+ n2 S  o  spreading out of lavas of different ages at hot  
4 X+ Z1 h3 E* A) V4 D! V8 Y  spots indicates that a  
6 k4 f* ?: x# }+ l# w5 ^, f" i   (A) hot spot is active 2 [% u1 q/ z' K# H$ |4 ~, G
   (B) continental plate has moved  
# b: Y' i% o+ G* a3 ~. P   (C) continental rupture is imminent  9 Y- I/ Y4 `7 c, A& u$ L; o) n
   (D) hot spot had been moving very rapidly  
6 \1 ]3 E0 |3 b2 d   (E) volcano contains large concentrations of  
- e5 x. i4 A' O2 C) j! i6 G     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  
. k9 v( N5 c9 r+ a   about the Hawaiian Islands, the Austral  
4 g4 K9 V0 H7 |   Ridge, and the Tuamotu Ridge?
6 D2 l) G( \) p% J* n   (A) The three chains of islands are moving east-
  x5 f# R2 X7 W1 S3 Mward.
; T8 G& ?4 V, D1 P   (B) All the islands in the three chains have  
# S0 H& {4 Z) ?/ K" c# P. n     stopped moving. $ R, |3 f0 a0 C4 Q
   (C) The three islands chains are a result of the    d* L6 [- k7 t1 Y# b
     same plate movement.
, p  r) x0 m5 H: u7 |; F( O   (D) The Hawaiian Islands are receding from  
; f' I5 b4 q3 d     the other two island chains at a relatively  
1 v! {9 w* R% p( W3 @     rapid rate. 4 q  V) q1 V' f3 Y  N( e- \
   (E) The Austral Ridge and the Tuamotu Ridge  . ?- ]6 A! y4 Z1 s7 `
     chains have moved closer together  
: J7 W' T8 V9 j8 e- V- E$ ]     whereas the Hawaiian Islands have  
8 H/ ]2 f8 T) q- @& o     remained stationary.
0 i& \4 }" ?7 F6 i8 I( X. I' d7 K1 u  ' z# f0 E! k* t; z! g
25. Which of the following, if true, would best  
4 y. ^% a7 C/ [   support the author’s statement that hot-spot  
! _1 G; n/ f. r- `8 y4 s   activity may explain the mutability of  ) A5 d: \; @! H5 s( Y; Y
   continental plates?
, ~8 j7 x+ j# B) o$ \   (A) Hot spots move more rapidly than the  
4 U. }5 \5 a& A* ~( s; b. [     continental and oceanic plates.
% d% R9 ^9 T2 T6 ~! S: j6 d8 O   (B) Hot spots are reliable indicators of the age  ; A! c% _# M& f% [+ i: I
     of continental plates.
6 z* }% V7 P: d# {8 W   (C) Hot spots are regions of volcanic activity  / \% S' e- B7 X; v/ O2 N7 g" e2 ?
     found only in the interiors of the  
3 j1 A3 r1 w: ~) u/ T' e% i" `     continental plates. 3 |8 D& H4 B9 n1 E6 C" S* E
   (D) The alignment of hot spots in the Pacific.  / I  b$ G7 Z; j$ O
     Ocean parallels the alignment of Pacific  . C* L6 ~- Z# e* T0 {
     Ocean islands.
9 w( `& q3 F2 q5 P+ N* I/ c( o   (E) The coastlines of Africa and South  4 o. l3 M% k# S% Y0 S0 U
     America suggest that they may once  . @% U. y: o+ g6 `; ^, q' S
     have constituted a single continent that  
8 I: X% ~% \3 q, c1 i, h     ruptured along a line of hot spots. + i5 t9 d9 a* h  r) T, ]( d/ h
    {6 ~% v  A0 h. B% c* X
26. The author’s argument that hot spots can be  . U8 e+ P2 h1 s5 _: j; D2 L
   used to reconstruct the movement of continental  
* B6 b8 w( B+ E9 l   plates is weakened by the fact that  6 ]9 c. w) _; f( `: f% u  y
   (A) hot spots are never found at the boundaries  
7 o; i1 n7 h9 \6 P# }     of plates / r# |, D/ x4 k: R9 C
   (B) only extinct volcanoes remain after a plate  
/ [' W2 I( f' z/ n1 g6 g6 @& v% `     moves over a hot spot
* \: @' o: }( W9 P3 X1 J: U   (C) lava flow patterns for all hot spots have not  $ z; U* \3 {: s5 ?
     been shown to be the same  0 |6 z! C( _; p9 j! `* r
   (D) the immobility or near immobility of hot  . g6 V# w4 ~7 |
     spots has not been conclusively proven  ( {! Y: ^$ ~% x6 w; l
   (E) the changing configurations of islands  
( @9 U+ h" l% B7 o$ @5 ]# K$ ]) E. r     make pinpointing the locations of hot  ( d; g6 @9 c" ^+ S* r$ M
spots difficult  9 J$ Y6 G3 ?. B
  
* r2 f5 O9 J# H/ ~  X  N- q- A27. The author’s style can best be described as  
# B6 G2 X! j" T6 U) ]# _' F) p" b   (A) dramatic  
: }: A3 U. b9 |: K   (B) archaic  
( I$ G! l" [0 M0 p5 u   (C)esoteric  
5 i5 @8 L* c! d' s$ T) Q   (D) objective  
& m3 j- Y5 i+ f: j5 H   (E) humanistic  $ h' R4 E( I& @) u; s3 H; Y
20.D 21.E 22.E 23.B 24.C 25.E 26.D 27.D
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