Question:easy

Passage:

The theory of plate tectonics describes the motions of the lithosphere, the comparatively rigid outer layer of the Earth that includes all the crust and part of the underlying mantle. The lithosphere is divided into a few dozen plates of various sizes and shapes; in general the plates are in motion with respect to one another. A mid-ocean ridge is a boundary between plates where new lithospheric material is injected from below. As the plates diverge from a mid-ocean ridge they slide on a more yielding layer at the base of the lithosphere.

Since the size of the Earth is essentially constant, new lithosphere can be created at the mid-ocean ridges only if an equal amount of lithospheric material is consumed elsewhere. The site of this destruction is another kind of plate boundary: a subduction zone. There one plate dives under the edge of another and is reincorporated into the mantle. Both kinds of plate boundary are associated with fault systems, earthquakes and volcanism, but the kinds of geologic activity observed at the two boundaries are quite different.

The idea of sea-floor spreading actually preceded the theory of plate tectonics. In its original version, in the early 1960s, it described the creation and destruction of the ocean floor, but it did not specify rigid lithospheric plates. The hypothesis was substantiated soon afterward by the discovery that periodic reversals of the Earth's magnetic field are recorded in the oceanic crust. As magma rises under the mid-ocean ridge, ferromagnetic minerals in the magma become magnetized in the direction of the geomagnetic field. When the magma cooks and solidifies, the direction and the polarity of the field are preserved in the magnetized volcanic rock. Reversals of the field give rise to a series of magnetic stripes running parallel to the axis of the rift. The oceanic crust thus serves as a magnetic tape recording of the history of the geomagnetic field that can be dated independently. The width of the stripes indicates the rate of the sea-floor spreading.

Question:
What is the core theme of the passage?

Show Hint

Notice that the passage starts by naming a theory and that every later paragraph, including the magnetic-stripe evidence, is used to explain or support that same theory.
Updated On: Jul 20, 2026
  • Magnetic field reversal
  • The formation of magma
  • The location of mid-ocean ridges
  • Plate tectonic theory
  • Oceanic crust sedimentation
Show Solution

The Correct Option is D

Solution and Explanation

For a "core theme" question, the trick is to separate the passage's main subject from the smaller details it uses to support that subject. A good way to do this is to summarize what each paragraph is doing rather than what it says word for word.

Paragraph one introduces and defines the theory of plate tectonics and how mid-ocean ridges add new lithosphere. Paragraph two completes the picture by explaining subduction zones, where old lithosphere is destroyed, keeping the Earth's size constant. Paragraph three shifts to history and evidence, describing how sea-floor spreading and the pattern of magnetic stripes in the oceanic crust helped confirm the theory. Notice that this third paragraph does not exist independently, it exists to strengthen the case for plate tectonics laid out in the first two paragraphs.

So if you strip away the supporting detail, what remains as the constant thread across all three paragraphs is the theory of plate tectonics itself. Magnetic reversal, magma formation, and mid-ocean ridge locations are each just one piece of evidence or mechanism mentioned along the way, and oceanic crust sedimentation is not mentioned at all. None of these narrower ideas could stand alone as a summary of the whole passage, but "plate tectonic theory" comfortably covers all three paragraphs. That confirms option (d), option 4 in this numbering, as the correct answer.
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