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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 a) n; z! E1 F0 ^7 ^) v7 D1 R
striking appearance. The moon may be divided into two major terrains: the maria (dark 5 ^3 G9 q' |" `& x
lowlands) and the terrace( bright highlands). The contrast in the reflectivity (the capability
6 S4 i% w9 k+ Q. Xof reflecting light ) of these two terrains suggested to many early observers that the two
" f* B6 h+ ^, n- {4 n6 F5 c+ m(5)  terrains might have different compositions, and this supposition was confirmed by
9 z4 e. B, C% m" ]2 t" v$ bmissions to the Moon such as Surveyor and Apollo. One of the most obvious differences
6 `; y# ?3 S; o- R" P- kbetween the terrains is the smoothness of the maria in contrast to the roughness of the
# A5 {3 J+ x6 M3 N; M; fhighlands. This roughness is mostly caused by the abundance of craters; the highlands are ; Q3 `. e$ r% ^: m7 `$ c
completely covered by large craters( greater than 40-50 km in diameter), while the craters
, Z; o5 W/ A$ N; y(10) of the maria tend to be much smaller. It is now known that the vast majority of the Moon’s
% I" G9 ~1 t  i  Acraters were formed by the impact of solid bodies with the lunar surface.- n; d! d' V& ?$ i; ]0 q9 v% @
    Most of the near side of the Moon was thoroughly mapped and studied from telescopic
0 t$ v* a  P2 }pictures years before the age of space exploration. Earth-based telescopes can resolve
. M) {9 l7 n* v# L' J; @objects as small as a few hundred meters on the lunar surface. Close observation of
! N7 I% d  \9 K(15) craters, combined with the way the Moon diffusely reflects sunlight, led to the * v/ |/ E" c' R; G" z& l
understanding that the Moon is covered by a surface layer, or regolith, that overlies the
, s$ {& f+ M5 K" ~6 asolid rock of the Moon. Telescopic images permitted the cataloging of a bewildering array6 Y- s4 n) \4 i7 ~0 v( C
of land forms. Craters were studied for clues to their origin; the large circular maria were
1 x5 N# E5 R6 \- _(20) seen. Strange, sinuous features were observed in the maria. Although various land forms
. g' s& M; X; E& Y# ]. Hwere catalogued, the majority of astronomers’ attention was fixed on craters and their
7 c2 x$ ^2 p' Y) t! ~$ N. p, worigins.  y% B2 R& x6 h* H3 `
    Astronomers have known for a fairly long time that the shape of craters changes as
  s. ]( T$ W  R1 C$ [- d+ U# {4 Fthey increase in size. Small craters with diameters of less than 10-15 km have relatively
6 O  ]5 |7 k6 }' h9 @% o(25) simple shapes. They have rim crests that are elevated above the surrounding terrain,) ]8 T& E' L* z0 W0 F* S' o3 n: l
smooth, bowl-shaped interiors, and depths that are about one-fifth to one-sixth their diameters. The complexity of shape increases for larger craters.
' M' g) a1 y: e; F % u1 ]& ^% p& I) G4 \
41. What does the passage mainly discuss?
0 f2 @; g5 N" ~" L$ x" EWhat astronomers learned from the Surveyor and Apollo space missions4 q5 R0 I0 l! z8 y! t
Characteristics of the major terrains of the Moon
1 r4 ]; w5 ^# p! O$ {2 OThe origin of the Moon’s craters
# V0 C9 ]& y7 m) gTechniques used to catalogue the Moon’s land forms; l" l8 f" g3 m2 ^

! s1 M) p  ~: q3 s% H3 H42. The word ”undergone” in line1 is closest in meaning to 1 k& _& S2 U/ Y4 D8 _
altered1 Y* _- H, d* ~  v
substituted( X. C" B* \) N# ]
experienced& R" q/ `, _/ x8 O8 W; Z, |+ Y
preserved: ?: W1 U8 ]9 B. E& `

! Q* ~' P7 G$ a4 i0 V/ [3 C) ~43. According to the passage, the maria differ from the terrace mainly in terms of 6 M, p& e0 ?# ^4 C, l% }& u3 {
age
' q& t- N# V# I% Dmanner of creation
- F; W( a  i' h: \3 esize
! X& w) \4 c' g; o- D" G8 ?composition
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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./ w7 Q  E2 e' J( Q$ l- g
They revealed that previous ideas about the Moon’s craters were incorrect.
" n, V# |' u) k4 e& N6 e+ KThey were unable to provide detailed information about the Moon’s surface.
1 h9 U- k/ {; k' {3 [They were unable to identify how the Moon’s craters were made.
. r  u- e! ]1 u7 o4 w4 ]" [
$ G5 E- V3 u7 c" S7 w45. The word ”vast” in line 10 is closest in meaning to
% E) C  L5 F; J5 |5 E4 P7 ^) q% n(A) special9 C" L' l9 D; @9 F
(B) known
" k1 F7 T2 m, P4 @  K( D, D; E+ s3 i(C) varied
2 f$ X- }, I% f+ H9 Y. s: _3 b/ h(D) great
- H/ F; d+ \/ o* g3 o2 W* B- m
& T* g) y1 f8 R; Y2 c9 B46. All of the following are true of the maria EXCEPT:
, q! ?2 X- S6 k# v6 U$ [They have small craters.2 G; h8 O3 u- d& T% m0 B! `
They have been analyzed by astronomers.
. D, j+ r6 t9 S6 B+ ^6 o  jThey have a rough texture.2 @$ c& U2 S  k3 z
They tend to be darker than the terrace.) `3 F/ e# U5 _) Z2 @
- Y& r7 l& X+ W" i
47. All of the following terms are defined in the passage EXCEPT( ?. l5 p; r5 c- L& }# W
Moon (line1)
" q3 M% z! Z6 ?3 h$ i' {, G$ i" oreflectivity(line3)
6 C" ^( `2 `" i! ]( oregolith(line16)' o& E; k8 H; i  [7 a) ~
rays(line19). |* i) A  C9 K8 O" Z
( N3 J" P' \& ~! \' ~
48. The author mentions “wispy marks” in line 19 as an example of + e/ P; s% n$ L/ Z6 b
an aspect of the lunar surface discovered through lunar missions
7 R: E7 x# y$ |  B/ g: pa characteristic of large craters- H8 U) y5 j$ X! b( o5 I( u& W
a discovery made through the use of Earth-based telescopes' k( q) ?, L( m7 U3 M2 {& q# }
features that astronomers observed to be common to Earth and the Moon6 _; k  j4 w+ {5 M/ s: k# j. @: ^

7 p8 R5 T  p" h& C/ X49. According to the passage, lunar researchers have focused mostly on 7 \0 p1 C( R3 I$ F- Q/ C
the possibility of finding water on the Moon' M2 V2 I1 Z( Z0 h; E2 n; r8 r
the lunar regolith& o8 C; V" K1 K9 H7 w% n! N
cataloging various land formations
$ K$ l! q" d  s$ v  j8 wcraters and their origins/ ~# [1 ?1 w; B" [+ A5 J3 w9 r5 f0 a

& V5 u' f+ i6 h' f0 S# S50. The passage probably continues with a discussion of% w+ z5 D. [+ |' ]1 P+ X1 O' I
the reasons craters are difficult to study2 W( B0 q* l# X/ y$ A' l; T# v! M4 w
the different shapes small craters can have
& T, P4 w' p3 V- Z- e' Ysome features of large craters5 |) z9 v. @- C" l
some difference in the ways small and large craters were formed
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