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At am, the first explosion was at Perboewatan, triggering a tsunami heading straight to Telok Betong, now known as Bandar Lampung.
At am, Krakatoa exploded again at Danan, with the resulting tsunami stretching eastward and westward.
Ash was propelled to an estimated height of 80 km (50 mi).
The eruptions diminished rapidly after that point, and by the morning of 28 August, Krakatoa was silent.
Several barographs recorded the wave seven times over the course of five days: four times with the wave travelling away from the volcano to its antipodal point, and three times travelling back to the volcano.
Hence, the wave rounded the globe three and a half times.
The combination of pyroclastic flows, volcanic ash, and tsunamis associated with the Krakatoa eruptions had disastrous regional consequences.
Some land in Banten, approximately 90 km south, was never repopulated; it reverted to jungle and is now the Ujung Kulon National Park.
The pressure wave was recorded on barographs all over the world.
Small eruptions, mostly of mud, continued into October 1883.
By then, less than 30% of the original island remained.
He noted three major ash columns (the newer from Danan), which obscured the western part of the island, and steam plumes from at least eleven other vents, mostly between Danan and Rakata. At about pm on 26 August, the volcano went into its paroxysmal phase.
When he landed, he noted an ash layer about 0.5 m (1 ft 8 in) thick, and the destruction of all vegetation, leaving only tree stumps. The next day, a ship passing to the north reported a new vent "only a few meters above sea level"; this may be the most northerly spot indicated on Ferzenaar's map. By pm, a black cloud of ash could be seen 27 kilometres high.
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Activity died down by the end of May, and there was no further recorded activity for several weeks.