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Scientists generally credit
violent collisions between
tectonic plates, the mobile
Line fragments of Earth’s rocky (5)outer shell, with sculpting the planet’s surface, as, for example, when what is now the Indian subcontinent col- lidedwith Asia , producing (10)the Himalayan Mountains. However, plate tectonics cannot fully explain certain massive surface features, such as the “superswell” (15)of southern Africa, a vast plateau over 1,000 miles across and nearly a mile high.Geologic evidence
shows that southern African
(20)has been slowly rising for
the past 100 million years,
yet it has not experienced
a tectonic collision for
nearly 400 million years.
(25)The explanation may be in
Earth’s mantle, the layer of
rock underlying the tectonic
plates and extending down
over 1,800 miles to the outer
(30)edge of Earth’s iron core.
Since the early twentieth
century, geophysicists have
understood that the mantle
churns and roils like a thick
(35)soup.The relative low
density of the hottest rock
makes that material buoyant,
so it slowly ascends, while
cooler, denser rock sinks
(40)until heat escaping the mol-
ten core warms it enough to
make it rise again.While
this process of convection
was known to enable the
(45)horizontal movement of tec-
tonic plates, until recently
geophysicists were skeptical
of its ability to lift or lower the
planet’s surface vertically.
(50)However, recent technolog-
ical advances have allowed
geophysicists to make three-
dimensional “snapshots”
of the mantle by measuring
(55)vibrations, or seismic waves,
set in motion by earthquakes
originating in the planet’s
outer shell and recording
the time it takes for them to
(60)travel from an earthquake’s
epicenter to a particular
recording station at the
surface.Because geo-
physicists know that seismic
(65)waves become sluggish in
hot, low-density rock, and
speed up in colder, denser
regions, they can now infer
the temperatures and den-
(70)sities in a given segment of
the interior.By compiling
a map of seismic velocities
from thousands of earth-
quakes across the globe,
(75)they can also begin to map
temperatures and densities
throughout the mantle.These
methods have revealed some
unexpectedly immense for-
(80)mations in the deepest parts
of the mantle; the largest
of these is a buoyant mass
of hot rock directly below
Africa’s southern tip.Dis-
(85)pelling researchers’ initial
doubts, computer models
have confirmed that this
formation is buoyant enough
to rise slowly within the mantle
(90)and strong enough to push
Africa upward as it rises. ---------------------------------------
Q25:
In line 10, the author mentions the Himalayan Mountains most likely in order to
A.highlight certain similarities between the southern African superswell and other massive features on Earth’s surface
B.identify a feature of Earth’s surface that predates the origins of the southern African superswell
C.provide an example of a feature of Earth’s surface that can explained by plate tectonics
D.suggest that geophysicists are correct in attributing the sculpting of Earth’s surface to violent collisions between tectonic plates
E.give an example of a feature of Earth’s surface that scientists are unable to explain fully
--------------------------- 答案是C,我觉得D和原文定位(蓝色高亮部分)更贴切。
请哪位高人指点,谢谢!
---------------------------------------
Q25:
In line 10, the author mentions the Himalayan Mountains most likely in order to
A.highlight certain similarities between the southern African superswell and other massive features on Earth’s surface
B.identify a feature of Earth’s surface that predates the origins of the southern African superswell
C.provide an example of a feature of Earth’s surface that can explained by plate tectonics
D.suggest that geophysicists are correct in attributing the sculpting of Earth’s surface to violent collisions between tectonic plates
E.give an example of a feature of Earth’s surface that scientists are unable to explain fully
--------------------------- 答案是C,我觉得D和原文定位(蓝色高亮部分)更贴切。
请哪位高人指点,谢谢! |
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