People eslewhere agree on what a mountain is—or do __1__
+ `6 V# @# h7 N' J A& R- f they? The fact is that definitions vary. Everyone admits( d7 H% y2 ?# O, H9 t
for example, that Everest is a mountain, the lowest of __2__5 b$ A A9 ?, b L5 K# |& b
them all, an altitude of almost 30,000 feet. But what about__3__5 o' \& I: ~9 Y$ h2 r
Snowdon, the loftiest peak in Wales? It raises a mere 3000__4__
0 S# @- Q; {- A/ n( h* L0 e2 a feet, yet it is also called a mountain. Comparison—a little
p1 Z) u* G6 [4 {4 v matter of relativity—is the key. To the average person; }+ W! `8 s( _% }' |
living on North America's Great Plains, Vermont's Green* h) D/ V$ T n7 X1 B
Mountains look lofty indeed, but to anyone from the Rocky
9 K, K( H+ J1 R Mountains, the Green Mountains seem something more__5__
) i- c) b# G5 W& y; x$ C than hills. Geographers generally agree that, to be a mountain
7 k6 Q4 H" q1 w2 w topographically, a landmass might reach an altitude of 3000__6__; B* \# T6 a8 [; v1 v8 _* D
feet above the level of the sea. Mount Everest, for instance, is
+ V* t; w* T% Y% z% J9 `* W- j 30,000 feet above sea level, but not only 15,000 feet above the__7__
$ ]: Y1 h% y* |% m neighboring Tibetan plateau. Geologists restrict the definition5 O+ y; p# ^0 W+ g* v4 m
even more, maintaining that a mountain is a mountain with__8__
* S& j$ c' @' {+ a. I8 B& D virtue of its geological structure. Some rugged highlands are' x7 V1 A5 J# d% _
not really mountains, when some flat, low-lying rock surfaces__9__2 m; ~* c+ _- T3 L
are ture mountains. They are low now because of centuries of
8 \8 y0 h+ e& H3 @- Z6 H5 a erosion. There are even mountains under the sea—the6 E9 ^6 I" H$ H$ N6 ?- V
Mid-Atlantic Ridge, for example. Like all ture mountains,: }' c2 r: x- [, d! Q3 |9 B
they are originally formed by large-scale movements of the__10__
! h; g8 U) N" s0 V- X E earth's crust.! N4 C$ S4 z* ^ R
答案:, `! o$ B3 H" ]! t! D( n& [
1. elsewhere—everywhere
* r. z; Q& \* v# r( d elsewhere意为“别处”/ \" L5 ?! e) P( ~0 ] @
2. lowest—highest' O6 |( d) V$ ^; X1 T# I; y
3. an前加with3 W& w7 H3 D2 ^1 K1 V
with在此处表示“具有......”相当于having y, {, J9 e: w
4. raise—rises
! Z4 z$ `' Z# ?: F: b 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
& a0 L( `6 e' T8 C 5. something—nothing7 o3 W, D) ^% v1 D# }
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”。5 C$ R* y- n/ k7 N
6. might—must
: d9 l: M% \! ~* a7 p. ]- s4 j 作为一种标准必须达到某个高度% c8 O- Q4 C' g. z* @! H; z
7. 删除only之前的not
8 A7 {; i' z- h7 g 否则文理不通0 b/ n5 d1 N7 W' Z1 ^
8. with—in或by
! f; f. O6 l9 c# j$ ~ by/in virtue of:与“by reason of,because of ”同意, q3 q6 Z, ?# t3 F
9. when—while2 {, U) b t: z [) p" g5 G
此处while与whereas同意,表示对照比较
: P* Y7 s5 y- c6 J$ F5 `% F 10. are—were
* }) ]* z+ n# l: `# G originally formed 该动作是很早以前完成或结束的 |