1883 eruption of Krakatoa (English Wikipedia)

Analysis of information sources in references of the Wikipedia article "1883 eruption of Krakatoa" in English language version.

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  • Olson, Donald W.; Russell L. Doescher; Marilynn S. Olson (May 2005). "The Blood-Red Sky of the Scream". APS News. 13 (5). American Physical Society. Retrieved 22 December 2007.

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  • Press, Frank (November 1956). "Volcanoes, ice, and destructive waves" (PDF). Engineering and Science. 20 (2): 26–30. ISSN 0013-7812. Retrieved 5 April 2007. Fortunately, the tide gauges of 1883 were sufficiently well designed to provide fairly good records of the Krakatoa waves. Thus we have instrumental data for the Krakatoa sea waves from such widely separated places as Honolulu, San Francisco, Colon, South Georgia and English Channel ports.

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  • A documentary film showed tests made by a research team at the University of Kiel, Germany, of pyroclastic flows moving over the water. See Freundt, Armin (2002). "Entrance of hot pyroclastic flows into the sea: experimental observations". Bulletin of Volcanology. 65 (2–3): 144–164. Bibcode:2002BVol...65..144F. doi:10.1007/s00445-002-0250-1. S2CID 73620085. Retrieved 10 April 2012. The tests revealed that hot ash travelled over the water on a cloud of superheated steam, continuing to be a pyroclastic flow after crossing water; the heavy matter precipitated out of the flow shortly after initial contact with the water, creating a tsunami due to the precipitate mass.

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  • A documentary film showed tests made by a research team at the University of Kiel, Germany, of pyroclastic flows moving over the water. See Freundt, Armin (2002). "Entrance of hot pyroclastic flows into the sea: experimental observations". Bulletin of Volcanology. 65 (2–3): 144–164. Bibcode:2002BVol...65..144F. doi:10.1007/s00445-002-0250-1. S2CID 73620085. Retrieved 10 April 2012. The tests revealed that hot ash travelled over the water on a cloud of superheated steam, continuing to be a pyroclastic flow after crossing water; the heavy matter precipitated out of the flow shortly after initial contact with the water, creating a tsunami due to the precipitate mass.
  • Self, Stephen (1992). "Krakatau revisited: The course of events and interpretation of the 1883 eruption". GeoJournal. 28 (2). Springer Science+Business Media. doi:10.1007/BF00177223. S2CID 189890473. Retrieved 20 May 2022.
  • Bradley, Raymond S. (June 1988). "The explosive volcanic eruption signal in northern hemisphere continental temperature records" (PDF). Climatic Change. 12 (3): 221–243. Bibcode:1988ClCh...12..221B. doi:10.1007/bf00139431. ISSN 0165-0009. S2CID 153757349 – via Springer.
  • Self, Stephen; Rampino, Michael R. (1981). "The 1883 eruption of Krakatau". Nature. 294 (5843): 699–704. Bibcode:1981Natur.294..699S. doi:10.1038/294699a0. ISSN 1476-4687. S2CID 4340524.

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