Jawaban dari RDP tentang kemungkinan tsunami di Sulawesi:
 
Tulisan saya kemaren mungkin kurang tepat karena ada artikel yg baru
saja saya dapatkan bahwa tsunami di Makasar strait ternyata justru
paling banyak terjadi menurut artikel yg abstracnya aku lampirkan
dibawah. Tsunami ini akan lebih disebabkan oleh pergerakan patahan
Palu-Koro (seperti yg saya tulis sebelumnya), namun juga akan dipicu
oleh deepwater landslides (longsoran bawah laut) yg mekanismenya
sdikit berbeda dengan tsunami di Aceh.

Menurut artike tsb pantai timur Kalimantan relatif lebih "aman" dengan
2 m tsunami dan mungkin akan sedikit diredam oleh lebarnya shelf
(paparan), sedangkan pantai barat Sulawesi mungkin bisa 3 m tinggi
gelombang tsunami.

Bagi yg tertarik artikel bisa didonlod di 
http://www.geophysik.uni-muenchen.de/~wiwit/tsunami_mapaga.pdf
(thanks to Wiwit P)

RDP
=========================================

The Makassar Strait Tsunamigenic Region, Indonesia
G. S. PRASETYA,W. P. DE LANGE and T. R. HEALY
Coastal Marine Group, Department of Earth Science, University of
Waikato, Private Bag 3105, Hamilton, New Zealand
(Accepted: 31 January 2001)

Abstract. The Makassar Strait region has had the highest frequency of
historical tsunami events for Indonesia. The strait has a seismic
activity due to the convergence of four tectonic plates that produces
a complex mixture of structures. The main tsunamigenic features in the
Makassar Strait are the Palu-Koro and Pasternoster transform fault
zones, which form the boundaries of the Makassar trough.
Analysis of the seismicity, tectonics and historic tsunami events
indicates that the two fault zones have different tsunami generating
characteristics. The Palu-Koro fault zone involves shallow thrust
earthquakes that generate tsunami that have magnitudes that are
consistent with the earthquake magnitudes.
The Pasternoster fault zone involves shallower strike-slip earthquakes
that produce tsunami magnitudes larger than would normally be expected
for the earthquake magnitude. The most likely cause for the increased
tsunami energy is considered to be submarine landslides associated
with the earthquakes. Earthquakes from both fault zones appear to
cause subsidence of the west coast of Sulawesi Island.
The available data were used to construct a tsunami hazard map which
identifies the highest risk along the west coast of Sulawesi Island.
The opposite side of the Makassar Strait has a lower risk because it
is further from the historic tsunami source regions along the Sulawesi
coast, and because the continental shelf dissipates tsunami wave
energy. The greatest tsunami risk for the Makassar Strait is
attributed to locally generated tsunami due to the very short travel
times.

Key words: historical tsunami, hazard mapping, tectonics, source
mechanisms, mitigation.



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