People eslewhere agree on what a mountain is—or do __1__
) a4 B6 G2 _8 W9 Q* g they? The fact is that definitions vary. Everyone admits
6 W7 P4 S# c' v; v& O6 \ for example, that Everest is a mountain, the lowest of __2__
: x! V- E2 w+ n# s# C. H4 I them all, an altitude of almost 30,000 feet. But what about__3__; Y A9 U- I" m6 W1 ]
Snowdon, the loftiest peak in Wales? It raises a mere 3000__4__( Y8 ], e2 E' d- j
feet, yet it is also called a mountain. Comparison—a little$ s9 A& p4 S ?; ~+ B' y/ \
matter of relativity—is the key. To the average person
1 x# D2 j( U6 n, Z living on North America's Great Plains, Vermont's Green
" I) @& ^1 D# Y4 ?3 w: v' ^; a4 v Mountains look lofty indeed, but to anyone from the Rocky
3 b$ m# u& _# l5 ` Mountains, the Green Mountains seem something more__5__0 x; h2 j" u# j4 L. a
than hills. Geographers generally agree that, to be a mountain
5 B" ~- k$ h/ s4 p# Z topographically, a landmass might reach an altitude of 3000__6__8 a% }) k! m. t' S- D8 p. n) |
feet above the level of the sea. Mount Everest, for instance, is
) g- }- |+ V1 y g1 j' C$ x 30,000 feet above sea level, but not only 15,000 feet above the__7__
( J: v( D0 ^ n$ c4 l: } neighboring Tibetan plateau. Geologists restrict the definition
' x7 W: J! j! O even more, maintaining that a mountain is a mountain with__8__
- E+ u/ J: x6 f+ H- y; E8 b virtue of its geological structure. Some rugged highlands are7 I4 r9 i- O% B* Y
not really mountains, when some flat, low-lying rock surfaces__9__
5 N$ o) G( ]) T' t; E9 K are ture mountains. They are low now because of centuries of! `- q# k/ n! f* \0 @2 }4 u
erosion. There are even mountains under the sea—the- v* u" V1 E# ?+ z: T0 U
Mid-Atlantic Ridge, for example. Like all ture mountains,
' m/ S a9 O3 p5 Z$ L8 l: I they are originally formed by large-scale movements of the__10__
! W5 A7 Q9 ^8 H' B0 Y earth's crust.+ i0 `) h" C7 X1 o- D. H+ Q
答案:- [( \; l: t8 N4 @6 L1 h% L8 n M6 H; F
1. elsewhere—everywhere
3 p1 M" M9 N3 a& [' X6 J# _ elsewhere意为“别处”
& M. R) x& L$ A. a7 a$ C 2. lowest—highest
3 V* N5 b- \- N2 u. z 3. an前加with7 ~; Z! ]2 R3 s: R$ K7 t* t! ?
with在此处表示“具有......”相当于having% D# C7 F3 ?/ U) G5 F& l
4. raise—rises9 x" G9 Z3 g" t# n2 n4 X
raise为及物动词,其后常带宾语;rise为不及物动词a mere 3000 feet在此处不是raise的宾语,而是状语% m- v c( v4 S9 j4 B$ F9 b N
5. something—nothing5 W) a4 l5 d7 X
nothing此处为副词,修饰more。本句意义为“对生活在北美大平原地区的一般人而言,谓语Vermont州的Green Mountains看上去真的很高了,但对于任何一个来自Rocky Mountain地区的人而言,Green Mountain看上去不过是个山丘而已”。
Z; c. L) |2 u" A7 w3 D 6. might—must
4 R z, J$ e2 a7 V- ? 作为一种标准必须达到某个高度1 R2 P. [9 h/ B, r9 r
7. 删除only之前的not/ ` I9 m. M6 h6 b p1 p: R3 L
否则文理不通
8 a) q* d% I; o- e1 W0 r4 R; V0 H 8. with—in或by
$ |3 j+ A2 p' Y3 ^) x2 @ by/in virtue of:与“by reason of,because of ”同意
* s# X5 c$ Z& H" \ 9. when—while
* U( Y' a. T$ @. A# ~; n% B1 J 此处while与whereas同意,表示对照比较
6 {1 i [/ D: P+ r6 | 10. are—were7 h, H# }1 m" t2 u( g' N# B
originally formed 该动作是很早以前完成或结束的 |