People eslewhere agree on what a mountain is—or do __1__
1 O1 R0 {) B. u$ ?! S they? The fact is that definitions vary. Everyone admits
0 [) {) j0 `- i for example, that Everest is a mountain, the lowest of __2__3 Z/ Q& i: {: p
them all, an altitude of almost 30,000 feet. But what about__3__# i8 m3 x( p5 y/ D
Snowdon, the loftiest peak in Wales? It raises a mere 3000__4__
0 ~( q! Z! t+ l feet, yet it is also called a mountain. Comparison—a little
- Y- S; m, H0 ? matter of relativity—is the key. To the average person
5 Y( P5 }( {# ?$ t+ z living on North America's Great Plains, Vermont's Green
2 Y, j0 R" A- z2 |. ]5 q3 Y1 V Mountains look lofty indeed, but to anyone from the Rocky5 {$ q% S+ O# }, Z7 H0 s
Mountains, the Green Mountains seem something more__5__
_( M, m, V0 V( Q& \8 i than hills. Geographers generally agree that, to be a mountain6 \7 d8 m6 n) X8 M9 d
topographically, a landmass might reach an altitude of 3000__6__
, t5 X7 M1 g) P* r. J feet above the level of the sea. Mount Everest, for instance, is w) M! z& p! |0 T
30,000 feet above sea level, but not only 15,000 feet above the__7__
% F" I7 j( O) s1 N) q neighboring Tibetan plateau. Geologists restrict the definition( M' `( `+ Q5 Q/ H) l( J0 R
even more, maintaining that a mountain is a mountain with__8__9 u$ _: O1 l Y- ~' j' q9 v0 G' Y
virtue of its geological structure. Some rugged highlands are) @& ?' T1 ~+ w/ i+ Z# o
not really mountains, when some flat, low-lying rock surfaces__9__) H, `$ d( \. ?- {5 e7 d
are ture mountains. They are low now because of centuries of* e" U# Y! m. w) r% M" a# F7 u
erosion. There are even mountains under the sea—the
7 `5 X) S6 i$ ?0 j! n- } Mid-Atlantic Ridge, for example. Like all ture mountains,( r" R8 J# } K8 A
they are originally formed by large-scale movements of the__10__
" V7 T1 i4 j9 J. X A8 H( O5 \. M earth's crust.0 |9 D1 d+ G+ C
答案:
% u1 b2 b* b _- p1 F 1. elsewhere—everywhere
" g" H+ {# o& f/ B) f! x5 z elsewhere意为“别处”' M" ^2 S/ c1 f8 B
2. lowest—highest
3 V L* G5 s/ }5 c9 ~ 3. an前加with% a$ {. D$ j; V0 G
with在此处表示“具有......”相当于having
; b Y2 I: q* b' T" q, w( G3 r3 u% b 4. raise—rises
6 g* c) Z& R; m2 Q6 T 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
, F @! J; H6 v# |/ ? 5. something—nothing
+ K" W& t5 n, Q- e3 H: R 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”。
: x: G: ~* X* I: S" k 6. might—must
4 u! ]; L% G2 w. f5 }' ^, x! ^ 作为一种标准必须达到某个高度
& e" L" _9 v; j: s9 q 7. 删除only之前的not
5 X1 ]4 C) p r: z; C 否则文理不通
0 l7 j0 u. P( P3 a4 l7 ~ 8. with—in或by
+ M3 F: u# b' k! p by/in virtue of:与“by reason of,because of ”同意
- o( }4 E" r- n: ] 9. when—while2 c5 T" T& j# |0 l/ C
此处while与whereas同意,表示对照比较
/ { `1 O( q6 ]( F: ]4 }; t; d' z 10. are—were
( M! S4 c6 H: [" K2 o- m+ P+ c originally formed 该动作是很早以前完成或结束的 |