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Davis Strait proto-microcontinent

From Wikipedia, the free encyclopedia

The Davis Strait proto-microcontinent is a failed microcontinent located in the Davis Strait between Greenland and Canada discovered in 2024.[1]

It is roughly 19 to 24 kilometres (12 to 15 mi) thick surrounded by a thinned out continental crust which is 14 to 17 kilometres (8.7 to 10.6 mi) thick on each side. It is considered a proto-microcontinent because it is incompletely rifted and submerged.[2][3] The separation of the Davis Strait proto-microcontinent coincides with a change in the orientation of tectonic spreading, which occurred between 58 and 49 million years ago.[4]

References

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  1. Pappas, Stephanie (25 July 2024). "'Failed' microcontinent found hiding beneath Greenland and Canada". Live Science.
  2. Bird, Hannah (10 July 2024). "New incompletely rifted microcontinent identified between Greenland and Canada". Phys.org.
  3. Longley, Luke; Phethean, Jordan; Schiffer, Christian (September 2024). "The Davis Strait proto-microcontinent: The role of plate tectonic reorganization in continental cleaving". Gondwana Research. 133: 14–29. Bibcode:2024GondR.133...14L. doi:10.1016/j.gr.2024.05.001.
  4. Carvajal, Guillermo (9 August 2024). "The Earth Hasn't Lost a Continent, but Has Gained a Microcontinent". LBV Magazine. Oviedo.