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  2. Cretaceous–Paleogene boundary - Wikipedia

    en.wikipedia.org/wiki/CretaceousPaleogene...

    The date of the impact coincides precisely with the CretaceousPaleogene boundary (K–Pg boundary), slightly more than 66 million years ago. [ 7 ] The crater is estimated to be over 150 km (93 mi) in diameter [ 10 ] and 20 km (12 mi) in depth, well into the continental crust of the region of about 10–30 km (6.2–18.6 mi) depth.

  3. Nadir crater - Wikipedia

    en.wikipedia.org/wiki/Nadir_crater

    The crater features all characteristics of an impact crater: appropriate ratio of width to depth, the height of the rims, and the height of the central uplift. [3] It was formed at or near the CretaceousPaleogene boundary about 66 mya around the same time as the Chicxulub crater. [1]

  4. Cretaceous–Paleogene extinction event - Wikipedia

    en.wikipedia.org/wiki/CretaceousPaleogene...

    Other crater-like topographic features have also been proposed as impact craters formed in connection with CretaceousPaleogene extinction. This suggests the possibility of near-simultaneous multiple impacts, perhaps from a fragmented asteroidal object similar to the Shoemaker–Levy 9 impact with Jupiter.

  5. Chicxulub crater - Wikipedia

    en.wikipedia.org/wiki/Chicxulub_crater

    Evidence for the crater's impact origin includes shocked quartz, a gravity anomaly, and tektites in surrounding areas. [3] The date of the impact coincides with the CretaceousPaleogene boundary (commonly known as the K–Pg or K–T boundary).

  6. Shiva crater - Wikipedia

    en.wikipedia.org/wiki/Shiva_crater

    The Shiva crater is the claim by paleontologist Sankar Chatterjee [2] and colleagues that the Bombay High and Surat Depression on the Indian continental shelf west of Mumbai, India represent a 500-kilometre (310 mi) impact crater, that formed around the Cretaceous-Paleogene boundary.

  7. Tanis (fossil site) - Wikipedia

    en.wikipedia.org/wiki/Tanis_(fossil_site)

    The CretaceousPaleogene ("K-Pg" or "K-T") extinction event around 66 million years ago wiped out all non-avian dinosaurs and many other species. Proposed by Luis and Walter Alvarez , it is now widely accepted that the extinction was caused by a huge asteroid or bolide that impacted Earth in the shallow seas of the Gulf of Mexico , leaving ...

  8. List of impact structures on Earth - Wikipedia

    en.wikipedia.org/wiki/List_of_impact_structures...

    The Chicxulub impact has been widely considered the most likely cause for the CretaceousPaleogene mass extinction, with some scholars linking other impacts like the Popigai impact in Russia and the Chesapeake Bay impact to later extinction events, though the causal relationship has been questioned. [16]

  9. Manson impact structure - Wikipedia

    en.wikipedia.org/wiki/Manson_impact_structure

    The Manson impact structure is an impact structure near the site of Manson, Iowa where an asteroid or comet nucleus struck the Earth during the Cretaceous Period, approximately 74 Ma. [1] It was one of the largest known impact events to have happened in North America. [ 2 ]