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Holocene impact craters on Earth

Author

Listed:
  • Losiak Anna

    (Institute of Geological Sciences, Polish Academy of Sciences, Wrocław, Poland ; Universities Space Research Association, Houston, United States)

Abstract

Impact craters are formed by collisions of cosmic bodies moving with hypervelocity. The formation of these features is not restricted to the distant geological past; new structures are constantly being created and at least 13 confirmed impact craters and crater fields have formed during the Holocene alone. This short review paper: (1) introduces the basics of the impact cratering process to physical geographers and Quaternary geologists; (2) provides a short description of representative examples of such features (Morasko, Kaali, Kamil, Ilumetsa); and (3) discusses the similarities and differences among very small craters, and contrasts these with larger impact structures. This manuscript may be useful to researchers planning to test whether a small Quaternary depression in the ground may be of impact origin.

Suggested Citation

  • Losiak Anna, 2023. "Holocene impact craters on Earth," Miscellanea Geographica. Regional Studies on Development, Sciendo, vol. 27(4), pages 165-171, October.
  • Handle: RePEc:vrs:mgrsod:v:27:y:2023:i:4:p:165-171:n:2
    DOI: 10.2478/mgrsd-2023-0016
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