Rakata

From Wikipedia, the free encyclopedia

Rakata (2667 ft; 830 m) is a stratovolcano on the Indonesian island of Krakatoa (Indonesian: Krakatau) in the Sunda Strait between the islands of Sumatra and Java. It is the largest, and southernmost, of three volcanoes that formed the island Krakatoa (the others being Danan and Perboewatan) and the only one not totally destroyed in the eruption of 1883. Rakata did lose its northern half in that eruption, leaving just its southern half. The exposed cliff is quite striking visually, partially of a large exposed dike terminating in a large lenticular extrusion at the middle of the almost vertical cliff. The feature has been called "The Eye of Krakatoa".

[edit] Name

For the origin of the name, see Krakatau.

Because the words 'Rakata' and 'Krakatau' are the same in Indonesian, both names are used interchangeably; leading to confusion in languages which distinguish between the two words. In geological usage, Krakatau is the island and Rakata is the main volcanic cone on that island. But Krakatau is also used for the volcanic edifice as a whole, including all four islands (Krakatau, Anak Krakatau, Verlaten and Lang). Before 1883 (and in many of the eruption reports) Rakata was just referred to as "The Peak" (of Krakatau).

[edit] Form

Rakata is a volcanic cone with its nothern face a vertical cliff, exposing much of it eruptive history. More than 25 extrusion dikes have been counted; the largest at the center runs from sea level 320 m and terminates in a large (abt 6 m diameter) lens-shaped feature. It is not known if the two are actually related in origin, or just coincidental.

[edit] Eruptions

There are no dated reports of eruptions from Rakata until the 1883 catastrophe, although tentative datings have been made from dating ash deposits left.

[edit] 1883

Rakata seems to have played a comparatively minor role in the eruption of 1883; there are some reports that seem to indicate it started erupting ('venting') in late July, compared to Perboewatan starting in May and Danan in June. (Furneaux mentions an unsourced report that the Peak had collapsed sometime in July.) However, it is more proper to realize that all of the eruptive centers of Krakatau have a common source and that we are talking about particular cones of the same volcano, rather than separate volcanoes. The map made by Capt. Ferzaneer from his visit on August 11 shows no eruptive "foci" from Rakata or its slopes (although there are several from the southern part of Danan), but he was not able to investigate the southern or western parts of the island due to the ash cloud blowing in that direction.

In his reconstruction of the catastrophe, R. D. M. Verbeek has Rakata's northern half destroyed along with the central part of the island in the largest explosion, at 10:02 am, August 27. Verbeek surmised that unlike Danan and Perboewatan, Rakata was not directly above the magma chamber, being connected only by a fissure which lay along the cleavage line of the caldera. However, examining the cliff from the air indicates two arcs, the second of which seems to be due to later (post-1883) landslides of unstable cliff material.

In surveys made a few months after the catastrophe, Rakata's height is given as 830 m, compared to 820 m before, however this may be due to inaccuracy of the earlier surveys. Verbeek reports that the cleavage was approximately at the old summit. The remnant of Rakata grew rather considerably in area due to falling pumice. However, most of the increased area (largely to the west and southeast) was washed away within several years by wave action.

[edit] Later Activity

Subsequent activity of Krakatoa seems to be limited to the area that had been between Danan and Perboewatan, where Anak Krakatoa has arisen, starting in 1927. Rakata cone itself would seem to be extinct since its conduit has been virtually destroyed.

[edit] References

• Furneaux, Rupert; Krakatoa (1964)
• Simkin & Fiske; Krakatau 1883: The Volcanic Eruption & Its Effects (1983)

[edit] See also

• List of volcanoes in Indonesia