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Not much information can be found about Danan; the interior of
Krakatoa was little explored or surveyed. There were several peaks, and Verbeek surmised that it formed a "ring-shaped crater wall". In one of the photographs of Perboewatan erupting in May 1883, Danan's irregular shape can be seen in the
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Perboewatan started erupting in May 1883. In June, a black cloud hung over the islands for five days, and when it lifted on 24 June, an ash column could be seen issuing apparently from an area between
Perboewatan and Danan. By the time Captain Ferzenaar visited the island on 11 August, Danan was in
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in the flank of Danan and was stable enough to keep Danan from being destroyed in the major explosion at 10:02 am which destroyed the area to the south and the northern half of Rakata. The steep angle to the west indicates that it has moved from its original location, probably by the bulk of Danan
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full eruption and there were about a dozen steam plumes, most of which were between the two cones. The two cones continued erupting, entering the cataclysmic phase on 26 August, with four terminal events on the morning of the 27 August.
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Danan apparently joined
Perboewatan in eruption sometime after May 1680, when Perboewatan started erupting. A returning Dutch traveler saw both cones erupting in February 1681.
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background, partially obscured by the ash cloud arising from
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tilted at about a 45-degree angle to the sea surface. It probably was an
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Krakatau 1883: The
Volcanic Eruption & Its Effects
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92:(uncertain derivation) was one of the three
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205:collapsing in that direction.
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