Krakatau
Misc Stuff
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1NM = 1.852km
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Speed of sound at sea level = 1225km/hr
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Earth’s radius 6,372 km
Speed of the Tsunami
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The paroxysmal explosion and collapse of the
volcano of Krakatoa generated formidable tsunami
waves that were up to 37 m (120 feet) in height.
These waves destroyed 295 towns and villages in
the Sunda Strait in Western Java and Southern
Sumatra. A total of 36,417 people were drowned.
The tsunami, being of volcanic origin (a point
source) was only destructive locally in Indonesia.
However, small tsunami waves were recorded
Undoubtedly, the atmospheric pressure waves from the three gigantic eruptions of Krakatoa on August 26 and 27, 1883, which proceeded the fourth paroxysmal
explosion, gave rise to tsunami like waves. The first of these three proceeding violent explosions occurred at 17: 07 Greenwich time (GMT) on August 26, 1883. The second and third violent eruptions occurred at 05:30 GMT and at 06:44 GMT on August 27, 1883. Being of atmospheric origin and small in size, none of these earlier tsunami like waves were noticed or reported. At the time, the only
operating tide gauge in Batavia (Jakarta) was too far away to record these smaller sea level oscillations.
It was the fourth paroxysmal explosion of Krakatoa at 10:02 (GMT) that gave rise to the gigantic destructive tsunami waves in the Sunda Strait. This paroxysmal
explosion blew away the northern two-thirds of the island and it was almost instantaneously followed by the collapse of the unsupported volcanic chambers which formed the huge underwater caldera. It was the combined effects of the explosion and collapse of the volcano that generated the catastrophic tsunami waves that caused havoc and destruction in the Sunda Strait.