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Starting from August 1968, the Glomar Challenger embarked on a year-long scientific expedition, the Deep Sea Drilling Program, criss-crossing the Mid-Atlantic Ridge between South America and Africa and drilling core samples at specific locations. When the age of the samples was determined by paleontological and isotopic dating studies, this provided conclusive evidence for the seafloor spreading hypothesis, and, consequently, for continental drift.

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Q: How did research from the Glomar challenge help scientist support the theory of seaflooding spreading?
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How did research from the Glomar Challenger help scientist support the theory of seafloor spreading?

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