In most earthquakes the Earth’s
crust cracks like porcelain, Stress
builds up until a fracture forms at a
line depth of a few kilometers and the crust
(5) slips to relieve the stress. Some
earthquakes, however, take place hun-
dreds of kilometers down in the Earth’s
mantle, where high pressure makes
rock so ductile that it flows instead of
(10) cracking, even under stress severe
enough to deform it like putty. How can
there be earthquakes at such depths?
That such deep events do occur
has been accepted only since 1927.
(15) when the seismologist Kiyoo Wadati
convincingly demonstrated their exis-
tence. Instead of comparing the arrival
times of seismic waves at different
locations, as earlier researchers had
(20) done, Wadati relied on a time differ-
ence between the arrival of primary(P)
waves and the slower secondary(S)
waves. Because P and S waves
travel at different but fairly constant
(25) speeds, the interval between their
arrivals increases in proportion to the
distance from the earthquake focus,
or initial rupture point.
For most earthquakes, wadati dis-
(30) covered, the interval was quite short
near the epicenter; the point on the sur-
face where shaking is strongest. For
a few events, however, the delay was
long even at the epicenter. Wadati saw
(35) a similar pattern when he analyzed data
on the intensity of shaking. Most earth-
quakes had a small area of intense
shaking, which weakened rapidly with
increasing distance from the epicenter.
(40) but others were characterized by a
lower peak intensity, felt over a
broader area. Both the P-S intervals
and the intensity patterns suggested
two kinds of earthquakes: the more
(45) common shallow events, in which the
focus lay just under the epicenter, and
deep events, with a focus several
hundred kilometers down.
The question remained: how can
(50) such quakes occur, given that mantle
rock at a depth of more than 50 kilo-
meters is too ductile to store enough
stress to fracture? Wadati’s work sug-
gested that deep events occur in areas
(55) (now called Wadati-Benioff zones)
where one crustal plate is forced under
another and descends into the mantle.
The descending rock is substantially
cooler than the surrounding mantle and
(60) hence is less ductile and much more
liable to fracture.
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30.
The author’s explanation of how deep events
occur would be most weakened if which of
the following were discovered to be true?
A. Deep events are far less common than
shallow events.
B. Deep events occur in places other than
where crustal plates meet.
C. Mantle rock is more ductile at a depth of
several hundred kilometers than it is
at 50 kilometers.
D. The speeds of both P and S waves are
slightly greater than previously thought.
E. Below 650 kilometers earthquakes cease
to occur.
Answer:
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31.
information presented in the passage sug-
gests that, compared with seismic activity
at the epicenter of a shallow event, seismic
activity at the epicenter of a deep event is
characterized by
A. shorter P-S intervals and higher peak
intensity
B. shorter P-S intervals and lower peak
intensity
C. longer P-S intervals and similar peak
intensity
D. longer P-S intervals and higher peak
intensity
E. longer P-S intervals and lower peak
intensity.
Answer:
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32.
The passage supports which of the following
Statements about the relationship between the
epicenter and the focus of an earthquake?
(A) P waves originate at the focus and
S waves originate at the epicenter.
(B) In deep events the epicenter and the
focus are reversed.
(C) In shallow events the epicenter and the
focus coincide
(D) In both deep and shallow events the
Focus lies beneath the epicenter
(E) The epicenter is in the crust, whereas
the focus is in the mantle.
Answer:
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33.
The passage suggests that which of the
following must take place in order for any
earthquake to occur?
1.Stress must build up.
2.Cool rock must descend
into the mantle.
3.A fracture must occur
(A) 1 only
(B) 2 only
(C) 3 only
(D) 1 and 3 only
(E) 1, 2, and 3