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(单词翻译:双击或拖选)
[00:00.00]在线英语听力室(www.tingroom.com)友情制作
[00:06.01]1998 Passage5
[00:08.41]Scattered around the globe are more than
[00:10.82]100 small regions of isolated1 volcanic2 activity
[00:15.23]known to geologists3 as hot spots.
[00:18.86]Unlike most of the world's volcanoes,
[00:21.38]they are not always found at the boundaries
[00:23.80]of the great drifting plates
[00:25.50]that make up the earth's surface;
[00:28.23]on the contrary, many of them lie deep
[00:30.85]in the interior of a plate.
[00:33.58]Most of the hot spots move only slowly,
[00:36.90]and in some cases the movement of the plates
[00:39.52]past them has left trails of dead volcanoes.
[00:43.76]The hot spots and their volcanic trails are milestones
[00:47.09]that mark the passage of the plates.
[00:50.07]That the plates are moving is now beyond dispute.
[00:54.12]Africa and South America, for example,
[00:57.15]are moving away from each other as new material
[01:00.18]is injected into the sea floor between them.
[01:03.61]The complementary coastlines and certain geological features
[01:07.54]that seem to span the ocean are reminders4 of
[01:10.87]where the two continents were once joined.
[01:14.49]The relative motion of the plates carrying these continents
[01:18.33]has been constructed in detail,
[01:20.96]but the motion of one plate with respect to another
[01:24.09]cannot readily be translated into motion
[01:27.31]with respect to the earth's interior.
[01:30.14]It is not possible to determine
[01:32.05]whether both continents are moving in opposite directions
[01:35.55]or whether one continent is stationary
[01:37.57]and the other is drifting away from it.
[01:40.60]Hot spots, anchored in the deeper layers of the earth,
[01:44.02]provide the measuring instruments
[01:45.73]needed to resolve the question.
[01:48.56]From an analysis of the hot-spot population it appears
[01:52.08]that the African plate is stationary
[01:55.01]and that it has not moved
[01:56.16]during the past 30 million years.
[01:58.48]在线英语听力室(www.tingroom.com)友情制作
[02:00.00]The significance of hot spots is not confined to
[02:03.01]their role as a frame of reference.
[02:05.84]It now appears that they also have an important influence
[02:09.26]on the geophysical processes
[02:11.59]that propel the plates across the globe.
[02:14.77]When a continental5 plate comes to rest over a hot spot,
[02:18.59]the material rising from deeper layers creates a broad dome6.
[02:23.63]As the dome grows, it develops deep fissures7 (cracks);
[02:28.87]in at least a few cases the continent
[02:31.80]may break entirely8 along some of these fissures,
[02:34.93]so that the hot spot initiates9 the formation of a new ocean.
[02:39.66]Thus just as earlier theories
[02:41.78]have explained the mobility10 of the continents,
[02:44.40]so hot spots may explain their mutability (inconstancy).
[00:06.01]1998 Passage5
[00:08.41]Scattered around the globe are more than
[00:10.82]100 small regions of isolated1 volcanic2 activity
[00:15.23]known to geologists3 as hot spots.
[00:18.86]Unlike most of the world's volcanoes,
[00:21.38]they are not always found at the boundaries
[00:23.80]of the great drifting plates
[00:25.50]that make up the earth's surface;
[00:28.23]on the contrary, many of them lie deep
[00:30.85]in the interior of a plate.
[00:33.58]Most of the hot spots move only slowly,
[00:36.90]and in some cases the movement of the plates
[00:39.52]past them has left trails of dead volcanoes.
[00:43.76]The hot spots and their volcanic trails are milestones
[00:47.09]that mark the passage of the plates.
[00:50.07]That the plates are moving is now beyond dispute.
[00:54.12]Africa and South America, for example,
[00:57.15]are moving away from each other as new material
[01:00.18]is injected into the sea floor between them.
[01:03.61]The complementary coastlines and certain geological features
[01:07.54]that seem to span the ocean are reminders4 of
[01:10.87]where the two continents were once joined.
[01:14.49]The relative motion of the plates carrying these continents
[01:18.33]has been constructed in detail,
[01:20.96]but the motion of one plate with respect to another
[01:24.09]cannot readily be translated into motion
[01:27.31]with respect to the earth's interior.
[01:30.14]It is not possible to determine
[01:32.05]whether both continents are moving in opposite directions
[01:35.55]or whether one continent is stationary
[01:37.57]and the other is drifting away from it.
[01:40.60]Hot spots, anchored in the deeper layers of the earth,
[01:44.02]provide the measuring instruments
[01:45.73]needed to resolve the question.
[01:48.56]From an analysis of the hot-spot population it appears
[01:52.08]that the African plate is stationary
[01:55.01]and that it has not moved
[01:56.16]during the past 30 million years.
[01:58.48]在线英语听力室(www.tingroom.com)友情制作
[02:00.00]The significance of hot spots is not confined to
[02:03.01]their role as a frame of reference.
[02:05.84]It now appears that they also have an important influence
[02:09.26]on the geophysical processes
[02:11.59]that propel the plates across the globe.
[02:14.77]When a continental5 plate comes to rest over a hot spot,
[02:18.59]the material rising from deeper layers creates a broad dome6.
[02:23.63]As the dome grows, it develops deep fissures7 (cracks);
[02:28.87]in at least a few cases the continent
[02:31.80]may break entirely8 along some of these fissures,
[02:34.93]so that the hot spot initiates9 the formation of a new ocean.
[02:39.66]Thus just as earlier theories
[02:41.78]have explained the mobility10 of the continents,
[02:44.40]so hot spots may explain their mutability (inconstancy).
点击收听单词发音
1 isolated | |
adj.与世隔绝的 | |
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2 volcanic | |
adj.火山的;象火山的;由火山引起的 | |
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3 geologists | |
地质学家,地质学者( geologist的名词复数 ) | |
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4 reminders | |
n.令人回忆起…的东西( reminder的名词复数 );提醒…的东西;(告知该做某事的)通知单;提示信 | |
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5 continental | |
adj.大陆的,大陆性的,欧洲大陆的 | |
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6 dome | |
n.圆屋顶,拱顶 | |
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7 fissures | |
n.狭长裂缝或裂隙( fissure的名词复数 );裂伤;分歧;分裂v.裂开( fissure的第三人称单数 ) | |
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8 entirely | |
ad.全部地,完整地;完全地,彻底地 | |
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9 initiates | |
v.开始( initiate的第三人称单数 );传授;发起;接纳新成员 | |
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10 mobility | |
n.可动性,变动性,情感不定 | |
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