Buried by a 330 Foot High Wall of Water; The Greenland Megatsunami Which Just Occurred
Автор: GeologyHub
Загружено: 2023-09-25
Просмотров: 303807
Описание:
On September 16th of 2023, a landslide within a fjord generated a 328 foot or 100 meter high wall of water (a tsunami) which would go on to cause damage to several structures. This represents the second such landslide generated tsunami to have occurred within Greenland since 2016. This video will discuss this disaster and how it relates to glacial retreat.
Thumbnail Photo Credit: Tim Marshall, timmarshall, "time lapse photography of ocean waves", "Rolling wave crash", Posted on Unsplash, Unsplash License, https://unsplash.com/photos/EZSlp_sVXzM. This image was then cropped, resized, overlaid with text, and then overlaid with GeologyHub made graphics (the image border and the GeologyHub logo).
Note: This video rounds my personal estimate of a maximum 328 foot run-up tsunami height during the September 16th 2023 Greenland tsunami event to 330 feet.
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Various licenses used in sections of this video (not the entire video, this video as a whole does not completely fall under one of these licenses) and/or in this video's thumbnail image:
Public Domain: https://creativecommons.org/publicdom...
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CC BY 4.0: https://creativecommons.org/licenses/...
Sources/Citations:
[1] 2020, Strzelecki, M. C. and Jaskólski, M. W., European Geosciences Union; Arctic tsunamis threaten coastal landscapes and communities – survey of Karrat Isfjord 2017 tsunami effects in Nuugaatsiaq, western Greenland, Nat. Hazards Earth Syst. Sci., 20, 2521–2534, https://doi.org/10.5194/nhess-20-2521..., 2020. CC BY 4.0.
[2] D. Miller, “Giant Waves in Lituya Bay Alaska”, USGS, Geological Survey Professional Paper 354-C.
[3] 2018, Higman, B., Shugar, D.H., Stark, C.P. et al, Springer Nature, Scientific Reports.; The 2015 landslide and tsunami in Taan Fiord, Alaska. Sci Rep 8, 12993 (2018). https://doi.org/10.1038/s41598-018-30..., CC BY 4.0
0:00 A Greenland Megatsunami
2:49 Lituya Bay
3:18 Landslide Cause
4:22 Conclusion
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