Which evidence originally supported Hess’s idea of seafloor spreading in 1968? Younger rocks are closer to mid-ocean ridges. The destruction of crust occurs at deep-sea trenches. Oceanic rocks are pillow-shaped when formed. Rocks across the ocean floor have alternating magnetic stripes.
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By the use of sonar, Hess was able to map the ocean floor and to show that the oceans seafloor is spreading using several evidences.
- Hess Harry was a geologist and navy submarine commander during second world war.
- Part of his study was to show and identify the deepest part of ocean floor.
- In 1946 he had discovered that hundreds of flat top mountains , per harps sunken islands shape the Pacific ocean.
- This was one of the major discovery evidence that was made by this geologist of the time.
- From the discoveries , Hess established that the rocks, mountains and highlands which are come of the prominent features in the oceans are the determinants when it comes to the depth of the oceans.
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Answer:
Different types of evidence supported Hess’s theory of sea-floor spreading: eruptions of molten material, magnetic stripes in the rock of the ocean floor, and the ages of the rocks themselves.
This evidence made scientists take a second look at Wegener’s hypothesis of continental drift.
The different types of evidence were:
- Evidence from molten rocks
- Evidence from magnetic strips
- Evidence from drilling samples
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