Produced by: Mohsin Shaikh
Beneath the icy waters of the North Atlantic lies a newly discovered microcontinent, the Davis Strait.
This ancient landmass formed 33–61 million years ago, now stretching 12–15 miles long.
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Tectonic plate movements between Greenland and Canada created this thick continental crust.
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The discovery, published in Gondwana Research, sheds light on Earth’s complex past.
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Named the Davis Strait proto-microcontinent, it lies off Greenland’s western waters.
Researchers believe the mechanism behind this microcontinent applies to others worldwide.
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The study highlights how plate motion changes and transpression cause landmass formations.
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Scientists urge further research into microcontinents to refine our understanding of geology.
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The Davis Strait adds a vital fragment to Earth’s geologic history, rewriting the atlas of continents.