Passage
Read the full passage. Bracketed letters like [A] mark the four positions for the insert-text question.
Two Waves, One Earthquake
¶1 An earthquake releases a burst of energy, and that energy does not travel through the Earth as a single, uniform vibration. Seismologists sort the resulting vibrations into two main types, called primary waves and secondary waves. The two types differ in how fast they move and, more importantly, in what kind of material they can pass through. That second difference might sound small. In fact, it became the key that let scientists learn what lies thousands of kilometers beneath their feet, without ever digging down to see it.
¶2 Primary waves, often called compressional waves, are the first to arrive at any measuring station after an earthquake begins. They move by squeezing and stretching the material they pass through. They push particles forward and then pull them back in the same direction the wave itself is traveling. This push-pull motion lets P-waves travel faster than any other seismic wave, often more than twice as fast as the second type. It also lets them pass through almost anything. Solid rock, liquid rock, water, and even air can all carry a P-wave. This is because the wave only needs to compress and expand the material, not bend it sideways.
¶3 Secondary waves, or S-waves, arrive at a station only after the primary waves have already passed. [A] Rather than pushing particles forward, an S-wave shakes them from side to side, at a right angle to the direction the wave is traveling. [B] That side-to-side motion makes S-waves slower than P-waves, and it also makes them far more selective about which materials they can pass through. [C] Solid rock resists being pushed sideways and springs back into its original shape, and that resistance is exactly what allows an S-wave to keep moving forward. [D] A liquid offers no such resistance. It simply flows out of the way instead of springing back, so an S-wave disappears completely once it reaches a liquid layer.
¶4 This contrast became the key to studying a place no one could ever visit. In 1906, the seismologist Richard Oldham noticed something strange. S-waves from large earthquakes never reached measuring stations on the far side of the planet, even though P-waves from the same earthquakes did. He reasoned that a wide band deep inside the Earth was blocking S-waves while still letting P-waves through, a region now called the shadow zone. Only a liquid can stop an S-wave completely. Oldham concluded that the outer core, the layer beneath Earth's rocky mantle, had to be liquid rather than solid rock. No one had dug a single meter to reach that conclusion.
- seismologist: a scientist who studies earthquakes and the seismic waves they produce
- shadow zone: an area on Earth's surface where a specific type of seismic wave cannot be detected
Questions
11 questions — every TOEFL Reading question type, in test order.
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Highlighted: "He reasoned that a wide band deep inside the Earth was blocking S-waves while still letting P-waves through, a region now called the shadow zone."
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However, that selectivity depends entirely on one property of the material the wave is passing through.
Where would the sentence best fit?
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P-waves S-waves