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No very satisfactory account of the mechanism that causes

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CEO
CEO
Joined: 15 Aug 2003
Posts: 3470
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Kudos [?]: 648 [0], given: 781

No very satisfactory account of the mechanism that causes [#permalink] New post 09 Apr 2004, 14:41
No very satisfactory account of the mechanism
that caused the formation of the ocean basins has
yet been given. The traditional view supposes
that the upper mantle of the earth behaves as a
(5) liquid when it is subjected to small forces for
long periods and that differences in temperature
under oceans and continents are sufficient to
produce convection in the mantle of the earth
with rising convection currents under the mid-
(10) ocean ridges and sinking currents under the con-
tinents. Theoretically, this convection would
carry the continental plates along as though they
were on a conveyor belt and would provide the
forces needed to produce the split that occurs
(15) along the ridge. This view may be correct: it has
the advantage that the currents are driven by
temperature differences that themselves depend
on the position of the continents. Such a back-
coupling, in which the position of the moving
(20) plate has an impact on the forces that move it,
could produce complicated and varying motions.
On the other hand, the theory is implausible
because convection does not normally occur
along lines. and it certainly does not occur along
(25) lines broken by frequent offsets or changes in
direction, as the ridge is. Also it is difficult to see
how the theory applies to the plate between the
Mid-Atlantic Ridge and the ridge in the Indian
Ocean. This plate is growing on both sides, and
(30) since there is no intermediate trench, the two
ridges must be moving apart. It would be odd if
the rising convection currents kept exact pace
with them. An alternative theory is that the sink-
ing part of the plate, which is denser than the
(35) hotter surrounding mantle, pulls the rest of the
plate after it. Again it is difficult to see how this
applies to the ridge in the South Atlantic, where
neither the African nor the American plate has a
sinking part.
(40) Another possibility is that the sinking plate
cools the neighboring mantle and produces con-
vection currents that move the plates. This last
theory is attractive because it gives some hope of
explaining the enclosed seas, such as the Sea of
(45) Japan. These seas have a typical oceanic floor,
except that the floor is overlaid by several kilo-
meters of sediment. Their floors have probably
been sinking for long periods. It seems possible
that a sinking current of cooled mantle material
(50) on the upper side of the plate might be the cause
of such deep basins. The enclosed seas are an
important feature of the earth's surface, and
seriously require explanation in because, addi-
tion to the enclosed seas that are developing at
present behind island arcs, there are a number of
(55) older ones of possibly similar origin, such as the
Gulf of Mexico, the Black Sea, and perhaps the
North Sea.

1. According to the traditional view of the origin of the
ocean basins, which of the following is sufficient to
move the continental plates?
(A) Increases in sedimentation on ocean floors
(B) Spreading of ocean trenches
(C) Movement of mid-ocean ridges
(D) Sinking of ocean basins
(E) Differences in temperature under oceans and
continents

2. The author refers to a "conveyor belt " in line 13 in
order to
(A) illustrate the effects of convection in the mantle
(B) show how temperature differences depend on
the positions of the continents
(C) demonstrate the linear nature of the Mid-Atlantic
Ridge
(D) describe the complicated motions made possible
by back-coupling
(E) account for the rising currents under certain mid-
ocean ridges

3. The author regards the traditional view of the origin
of the oceans with
(A) slight apprehension
(B) absolute indifference
(C) indignant anger
(D) complete disbelief
(E) guarded skepticism

4. Which of the following, if it could be demonstrated,
would most support the traditional view of ocean
formation?
(A) Convection usually occurs along lines.
(B) The upper mantle behaves as a dense solid.
(C) Sedimentation occurs at a constant rate.
(D) Sinking plates cool the mantle.
(E) Island arcs surround enclosed seas.

5. Which of the following titles would best describe the
content of the passage?
(A) A Description of the Oceans of the World
(B) Several Theories of Ocean Basin Formation
(C) The Traditional View of the Oceans
(D) Convection and Ocean Currents
(E) Temperature Differences Among the Oceans of
the World
GMAT Club Legend
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GMAT Tests User
 [#permalink] New post 09 Apr 2004, 17:19
Wow, I found this one very tough and convoluted
1-E
2-A
3-E
4-E (not too sure here)
5-C
About 14 min! Kept going back and forth to double check my answers :stupid
_________________

Best Regards,

Paul

Manager
Manager
Joined: 16 Oct 2003
Posts: 154
Location: India
Followers: 1

Kudos [?]: 1 [0], given: 0

GMAT Tests User
 [#permalink] New post 09 Apr 2004, 18:20
My answers:

1) E
2) A
3) E
4) A
5) B

Time : 8 minutes approx.
_________________

A 750 aspirant.

Senior Manager
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Posts: 291
Location: USA
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GMAT Tests User
 [#permalink] New post 10 Apr 2004, 13:32
Took 7 minutes!!
1. E
2. A
3. E
4. D
5. B
SVP
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Location: NewJersey USA
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GMAT Tests User
 [#permalink] New post 11 Apr 2004, 10:14
7 Minutes

1.E
2.A
3.E (Could be A )
4.A
5.B
CEO
CEO
Joined: 15 Aug 2003
Posts: 3470
Followers: 57

Kudos [?]: 648 [0], given: 781

Re: [#3] RC Challenge: Oceans [#permalink] New post 11 Apr 2004, 20:59
Good work guys. cbfr3 and paul were really close. but Aspire and anand got this one. Would you like to explain this please?

Quote:
No very satisfactory account of the mechanism
that caused the formation of the ocean basins has
yet been given. The traditional view supposes
that the upper mantle of the earth behaves as a
(5) liquid when it is subjected to small forces for
long periods and that differences in temperature
under oceans and continents are sufficient to
produce convection in the mantle of the earth
with rising convection currents under the mid-
(10) ocean ridges and sinking currents under the con-
tinents. Theoretically, this convection would
carry the continental plates along as though they
were on a conveyor belt and would provide the
forces needed to produce the split that occurs
(15) along the ridge. This view may be correct: it has
the advantage that the currents are driven by
temperature differences that themselves depend
on the position of the continents. Such a back-
coupling, in which the position of the moving
(20) plate has an impact on the forces that move it,
could produce complicated and varying motions.
On the other hand, the theory is implausible
because convection does not normally occur
along lines. and it certainly does not occur along
(25) lines broken by frequent offsets or changes in
direction, as the ridge is. Also it is difficult to see
how the theory applies to the plate between the
Mid-Atlantic Ridge and the ridge in the Indian
Ocean. This plate is growing on both sides, and
(30) since there is no intermediate trench, the two
ridges must be moving apart. It would be odd if
the rising convection currents kept exact pace
with them. An alternative theory is that the sink-
ing part of the plate, which is denser than the
(35) hotter surrounding mantle, pulls the rest of the
plate after it. Again it is difficult to see how this
applies to the ridge in the South Atlantic, where
neither the African nor the American plate has a
sinking part.
(40) Another possibility is that the sinking plate
cools the neighboring mantle and produces con-
vection currents that move the plates. This last
theory is attractive because it gives some hope of
explaining the enclosed seas, such as the Sea of
(45) Japan. These seas have a typical oceanic floor,
except that the floor is overlaid by several kilo-
meters of sediment. Their floors have probably
been sinking for long periods. It seems possible
that a sinking current of cooled mantle material
(50) on the upper side of the plate might be the cause
of such deep basins. The enclosed seas are an
important feature of the earth's surface, and
seriously require explanation in because, addi-
tion to the enclosed seas that are developing at
present behind island arcs, there are a number of
(55) older ones of possibly similar origin, such as the
Gulf of Mexico, the Black Sea, and perhaps the
North Sea.


Quote:
1. According to the traditional view of the origin of the
ocean basins, which of the following is sufficient to
move the continental plates?
(A) Increases in sedimentation on ocean floors
(B) Spreading of ocean trenches
(C) Movement of mid-ocean ridges
(D) Sinking of ocean basins
(E) Differences in temperature under oceans and
continents


Answer: E

Quote:
2. The author refers to a "conveyor belt " in line 13 in
order to
(A) illustrate the effects of convection in the mantle
(B) show how temperature differences depend on
the positions of the continents
(C) demonstrate the linear nature of the Mid-Atlantic
Ridge
(D) describe the complicated motions made possible
by back-coupling
(E) account for the rising currents under certain mid-
ocean ridges


Answer: A

Quote:
3. The author regards the traditional view of the origin
of the oceans with
(A) slight apprehension
(B) absolute indifference
(C) indignant anger
(D) complete disbelief
(E) guarded skepticism


Answer: E

Quote:
4. Which of the following, if it could be demonstrated,
would most support the traditional view of ocean
formation?
(A) Convection usually occurs along lines.
(B) The upper mantle behaves as a dense solid.
(C) Sedimentation occurs at a constant rate.
(D) Sinking plates cool the mantle.
(E) Island arcs surround enclosed seas.


Answer: A

Quote:
5. Which of the following titles would best describe the
content of the passage?
(A) A Description of the Oceans of the World
(B) Several Theories of Ocean Basin Formation
(C) The Traditional View of the Oceans
(D) Convection and Ocean Currents
(E) Temperature Differences Among the Oceans of
the World


Answer: B
Senior Manager
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Posts: 295
Location: US
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GMAT Tests User
 [#permalink] New post 12 Apr 2004, 06:46
Have also done this in the past.
  [#permalink] 12 Apr 2004, 06:46
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