Until the 1950s, most scientists believed that the geology of the ocean floor had remained essentially unchanged for many millions of years. But this idea became insupportable as new discoveries were made. First, scientists noticed that the ocean floor exhibited odd magnetic variations. Though unexpected, this was not entirely surprising, because it of the magnetite grains is “locked in,” recording the earth’s polarity at the time of cooling.
As more of the ocean floor was mapped, the magnetic variations revealed recognizable patterns, particularly in the area around the other great oceanic discovery of the 1950s: the global mid-ocean ridge, an immense submarine mountain range that winds its way around the earth much like the seams of a baseball. Alternating stripes oceanic crust. Over millions of years, this process, called ocean floor spreading, built the mid-ocean ridge.
This theory was supported by several lines of evidence. First, at or near the ridge crest, the rocks are very young, and they become progressively older away from the crest. Further, the youngest rocks all have normal polarity. Finally, because geophysicists had already determined the ages of continental volcanic rocks and, by is a remarkable correlation between the ages of the earth’s magnetic reversals and the striping pattern.
What this question is testing
Your task
Identify why the author included the referenced detail at that point in the passage — its function, not its content.
Common trap
Answers that merely repeat or summarize the topic of the detail instead of describing the role it plays.
Winning move
Ask what job the detail does for the paragraph, then for the passage's broader point.
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