Reading Comprehension

PT133 · S4 · P3 · Q21 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.

21.

Which one of the following is most strongly supported by the passage?

  1. Correct

    Submarine basalt found near the

    Why this is right

    We can support this with the end of the 2nd paragraph and beginning of the 3rd paragraph. The mid-ocean ridge, which is the part of the ocean floor farthest from the continents is where the new magma comes out. That's why ... at or near the ridge crest (in the middle of the ocean), the rocks are very young, and they become progressively older away from the crest (headed towards the nearest continent). So since we know the middle of the ocean is where the newest rock on the ocean floor comes from and since we know that the rocks get progressively older as you move toward the continents, we know that the basalt rocks near the continents are way older than the ones in the middle of the ocean. We don't necessarily know that basalt rocks are older than other types of rocks, but the language of this answer choice is hedged a bit to allow for that (plus, it's only a Most Supported task). It's just saying "they're likely to be some of the oldest rocks".

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

    43% picked this

  2. The older a sample of

    Contradicted

    Once basalt cools from its liquid molten form to its rock form, the magnetite needles freeze in place. That's the only "polarity" we could speak of a sample of basalt having. So all basalt only has one polarity that's locked in when it cools. It never reverses.

    21% picked this

  3. Compass readings are more likely

    Unknown Comparison: sea vs. land

    We don't have any way to compare the magnetic disturbances of the basalt in the ocean to potential magnetic disturbances of basalt (or other magnetic stuff) on land.

    10% picked this

  4. The magnetic fields surrounding magnetite

    Out of Scope: magnetic fields weaken

    Nothing in the passage ever talked about the magnetic field of anything weakening over time, only the magnetic field of earth periodically reversing polarity.

    8% picked this

  5. Any rock that exhibits present-day

    Contradicted

    There are only two polarities, normal or inverted (positive charge on the North pole or on the South pole). The earth's magnetic field has oscillated back and forth between normal and reversed polarity many times through Earth's history. If we're currently on version 100 of earth's magnetic field, then we have same polarity as version 98, 96, 94, etc. Any rock that was formed during version 98, 96, 94, etc., would exhibit present-day magnetic polarity, even though it wasn't formed during version 100. If we think about the striping pattern on the ocean floor ... every 2nd stripe will have rocks that match present-day polarity.

    17% picked this

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