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[历年真题] 托福阅读历年真题精选20

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发表于 2012-8-14 22:34:35 | 显示全部楼层 |阅读模式
The Moon, which has undergone a distinct and complex geological history, presents a7 ~3 Z% K# V; l; n. B
striking appearance. The moon may be divided into two major terrains: the maria (dark
; y/ t8 m% }# Q, zlowlands) and the terrace( bright highlands). The contrast in the reflectivity (the capability
6 w# O4 J  I3 _: W9 F8 g' c5 P2 b: Lof reflecting light ) of these two terrains suggested to many early observers that the two
# t5 _8 p0 N9 j/ z9 P# P) f- J(5)  terrains might have different compositions, and this supposition was confirmed by * e8 ~8 v2 M4 ~) i$ t
missions to the Moon such as Surveyor and Apollo. One of the most obvious differences1 I) J  ]& K, ^
between the terrains is the smoothness of the maria in contrast to the roughness of the
5 b0 f% o4 [% \* G0 r: Khighlands. This roughness is mostly caused by the abundance of craters; the highlands are
, \- D) f2 |2 V/ _1 r  N4 wcompletely covered by large craters( greater than 40-50 km in diameter), while the craters 6 c* N* A2 L. U; Z9 q& c
(10) of the maria tend to be much smaller. It is now known that the vast majority of the Moon’s
% c2 F) g5 {$ ?: Dcraters were formed by the impact of solid bodies with the lunar surface.9 `; N/ y9 f  @
    Most of the near side of the Moon was thoroughly mapped and studied from telescopic: P% Z7 t) Z: c2 Z
pictures years before the age of space exploration. Earth-based telescopes can resolve
" t! L% q6 M; u) w% b  c8 l* jobjects as small as a few hundred meters on the lunar surface. Close observation of 6 }& O! z) Y3 ]- t, g' }
(15) craters, combined with the way the Moon diffusely reflects sunlight, led to the
# m* D* W" @) w! {8 U$ D4 punderstanding that the Moon is covered by a surface layer, or regolith, that overlies the
0 n9 J, n  K' j, X5 ?9 nsolid rock of the Moon. Telescopic images permitted the cataloging of a bewildering array* P8 v5 p  W4 Q$ i
of land forms. Craters were studied for clues to their origin; the large circular maria were+ P  K6 x$ j, F5 c) G
(20) seen. Strange, sinuous features were observed in the maria. Although various land forms5 F/ Q! P; A4 U  P
were catalogued, the majority of astronomers’ attention was fixed on craters and their & D) s8 c! \6 M3 l8 }$ d' {5 F
origins.
, N. R) Y# ~4 U4 a/ S% I5 _    Astronomers have known for a fairly long time that the shape of craters changes as+ a; p  u3 W4 D" N1 Z  s+ ^
they increase in size. Small craters with diameters of less than 10-15 km have relatively " Y/ b( ~+ m* @
(25) simple shapes. They have rim crests that are elevated above the surrounding terrain,
7 e5 n. t1 V5 X, G# h, n- `4 O# Hsmooth, bowl-shaped interiors, and depths that are about one-fifth to one-sixth their diameters. The complexity of shape increases for larger craters.
& V0 v9 G/ l7 O& D2 M6 Z4 d: G & N$ u; J& N/ t1 d/ T* x& d
41. What does the passage mainly discuss?9 T& g# S! t. @. ^
What astronomers learned from the Surveyor and Apollo space missions# L% n" @/ M& d: u4 f! Q! w& O
Characteristics of the major terrains of the Moon( n, f& j& z6 y/ \8 A4 e
The origin of the Moon’s craters' a" d3 \" d) e4 g: R6 F
Techniques used to catalogue the Moon’s land forms
3 K+ E& v- n; E/ F( H5 c: Z   {7 F0 S# K: Q/ U* {  J8 T
42. The word ”undergone” in line1 is closest in meaning to 0 s) L) I. @6 h) O
altered1 o, \5 u# r$ s1 M$ g9 n; S
substituted
4 V/ K1 D( m6 ]experienced
' p6 t7 s" N  `preserved# R: E$ l0 B+ y) N6 z

7 D: g3 l$ T+ |! \6 O* K43. According to the passage, the maria differ from the terrace mainly in terms of
+ m. \5 u. [; R/ c* w: u' mage
) c* x* m" h6 p  e9 q% I- V4 Z; cmanner of creation
- @& J# J9 d4 msize
1 X( D% U1 k: r& _! i3 Gcomposition
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 楼主| 发表于 2012-8-14 22:34:36 | 显示全部楼层

托福阅读历年真题精选20

44. The passage supports which of the following statements about the Surveyor and Apollo missions?</p>They confirmed earlier theories about the Moon’s surface.
' r3 \7 @/ _& J. pThey revealed that previous ideas about the Moon’s craters were incorrect.- I: t8 @* x" U' L9 `+ g1 O
They were unable to provide detailed information about the Moon’s surface.- U# V* |3 {; A' D
They were unable to identify how the Moon’s craters were made.
4 p: `# g9 G& q' U ! N! ?2 N6 W/ O2 Y% }
45. The word ”vast” in line 10 is closest in meaning to
1 l0 h5 Y2 x7 U: p8 n( z, u(A) special4 k  X. N6 W; d) T# r
(B) known
" S0 z( F# g3 Q: ^+ z$ D(C) varied5 `" I0 {6 o) j3 ]" P
(D) great3 B& ^: f9 ^$ r. p, u  ?

3 F) A6 {% I+ n2 C46. All of the following are true of the maria EXCEPT:4 O, }2 `. E, V6 G) n2 [+ u0 @
They have small craters.9 H6 H2 A* L: T' Z$ q
They have been analyzed by astronomers.
# A2 B" M: V+ o- ?+ I6 k- b9 nThey have a rough texture.8 r; T4 v. X' `0 Z  E. W
They tend to be darker than the terrace.
) `. A! c$ B/ o. a8 O4 ~
' y4 P6 l4 v% {) a; j4 T: ?5 y# Z47. All of the following terms are defined in the passage EXCEPT* _* @* z- E, ]- ~3 j+ u. l" ]
Moon (line1)
: q+ p" l% p8 t1 z! L  N5 b+ Yreflectivity(line3)' H- W6 u" Z; E. t; E8 f9 z
regolith(line16)$ {+ r# Y* c* f
rays(line19)$ R. l5 C1 m5 b! U- J1 t# @4 A/ J0 U5 X
9 @; r' z4 p2 @' U: O. Z& y3 J
48. The author mentions “wispy marks” in line 19 as an example of
5 ]7 r' a4 @7 }) U0 yan aspect of the lunar surface discovered through lunar missions( O4 V0 a  e' V2 j; f! K# D: c9 r
a characteristic of large craters
9 l8 ~- F- N+ C9 [( [a discovery made through the use of Earth-based telescopes
0 D: t+ P- y6 G& ^% lfeatures that astronomers observed to be common to Earth and the Moon
+ H4 }9 `/ K1 D7 Q) O7 F+ y . q) ?% C, V1 e; @$ D3 k2 ?4 A
49. According to the passage, lunar researchers have focused mostly on . ~. Q, D0 Y& u# `, m; j
the possibility of finding water on the Moon' G# @% R# |( q- |- N
the lunar regolith& O: J5 m  u4 z6 H
cataloging various land formations
+ M5 A- m8 A" f/ F! w( ^craters and their origins+ K! P) n6 b& x% y  q
  _* C$ m4 W3 E5 x
50. The passage probably continues with a discussion of
4 f$ a$ Y* g$ d8 F: h( G& S( r' }the reasons craters are difficult to study
& D  @3 c  `* L  ~  pthe different shapes small craters can have
; D0 X% `3 O% g0 Bsome features of large craters
* d) A3 o) k% S( nsome difference in the ways small and large craters were formed
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