Reading Comprehension

PT133 · S4 · P3 · Q18 Ocean Floor Geologic Changes

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Until the 1950s, most scientists believed that the geology of the ocean floor had remained essentially unchanged for many millions of years.

Topic

The discovery and explanation of ocean floor spreading and the patterns of magnetic striping on the sea floor.

Framework

Old / New

Main Point

Until the 1950s, scientists believed the ocean floor was geologically unchanged for millions of years, but new discoveries—especially magnetic striping patterns and their alignment with Earth's historic magnetic reversals—revealed that the ocean floor is continually being renewed at mid-ocean ridges through a process called ocean floor spreading. ( – end of first paragraph, is the pivot sentence.)

P1: The Old Belief and the Puzzling New Discovery

Up until the 1950s, the consensus was that the ocean floor didn't really change. But when scientists started seeing weird magnetic differences in ocean floor rocks, they realized this old idea couldn't hold up. The explanation? As molten rock cools, its magnetic minerals lock in the direction of Earth's magnetic field, which has actually flipped many times in the past.

P2: Mapping the New Patterns and Formulating the New Theory

As researchers mapped more of the ocean floor, they saw clear patterns of alternating stripes with normal and reversed magnetic polarity centered on mid-ocean ridges—a network of underwater mountains. Scientists proposed the new idea of "ocean floor spreading": new crust forms at these ridges and slowly moves away, creating the striped pattern and gradually building the ridge.

P3: Evidence Supporting Ocean Floor Spreading

Several pieces of evidence supported ocean floor spreading: rocks at the ridge crest are very young and get older farther away, the youngest rocks all have normal polarity, and the ages of the stripes match documented reversals in Earth’s magnetic field—showing a striking correlation that backs up the spreading theory.

18.

According to the passage, which one of the following is true of magnetite grains?

  1. Correct

    In the youngest basalt, they

    Why this is right

    The youngest basalt means the magma that has most recently cooled. If there's a volcanic eruption in Hawaii right now, then the magma that explodes out will eventually cool into basalt, and the magnetite grain will show a snapshot of the earth's current polarity. The only way for this answer to not be true would be if the Earth's magnetic field had switched polarity since the most recent eruption of magma. But the magnetic field has reversed "at various times" over the course of Earth's 4 billion year history, suggesting that the magnetic field switches every few million years. In our lifetime, the magnetic field has never switched. Thus, any magma that has cooled in our lifetime will form basalt whose magnetite grains are pointing at the current polarity of the magnetic field.

    Skill tested: Locate Detail · how this choice captures the passage's function is the move to repeat next time.

    76% picked this

  2. In magma, most but not

    Contradicted: not all

    As far as we know, "grains of magnetite (all of them) behave like little compass needles, aligning with the earth's magnetic field".

    21% picked this

  3. They are not found in

    Too Strong: only basalt

    The only rock mentioned that has magnetite in it is basalt, but that doesn't establish that basalt is the only rock with magnetite in it.

    2% picked this

  4. They are about the size

    Unknown Comparison: size of sand

    Nothing in the two sentences we have about magnetite grains reveals the size of these grains. We couldn't compare them to typical grains of sand. This answer seems to just want people to think "a grain of this = a grain of that".

    1% picked this

  5. They are too small to

    Too Strong: too small to see

    Nothing in the two sentences we have about magnetite grains reveals the size of these grains. We have no idea whether they're visible to the naked eye or not.

    1% picked this

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