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International Seminar/Workshop on Tsunmai:
“In Memoriam +,* Years of Krakatau Eruption-Tsunami
and Lesson Learned from Large Tsunami”
Yuichi NISHIMURA�
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Tsunami Information Center0I� Laura Kongj1IUGG Tsunami Commission���I ^,**-� 1"��d� Vacheslav Gusiakovj�/��J��%��J*!Kongj ��6����?9�L��s?'KL&*! Kongj � BMG�6�789��� -�s?'7�6���*W� EF�� �45���:;MN&'?*! Gusiakovj � ���=;�=��s?'<t&� �NOP�Q���R��������ST�s?'�K&*! 6�789 �����������UV�/����&�&���J'?�%� 7W�X?%U¡�/N¢£Y10�Z¤¢� N� ��UV�[�%/x�4)'?$?! 5,0� \¥x 7WB]%^&?_�`�aW5J'?�U¢l�¦b�/��2UV£���[�J§%� 6�789�0¨©IJ�ª�|1y)*!cd���«�H�� ��l�$��% ,¬ )*!�� ��U¢-. -®� Achmad Djumarma
Wirakusumah0I%6�789���-.1¯e°±fg�s?'hª*! H?'� 76b�²:=³%���� _��� ´:=� -���Uµijl�¯eQR³a�¶�A<t&*! +�� � �����¯e% ,**.�45�;=��!�*���U
�·*0*�*2+* ¸k�_¹_ +*l� 2m�_�`�l�lºjlQR»UV��QR¯e¼�;=Institute of Seismology and Volcanology, Graduate
School of Science, Hokkaido University, Kita-+*,Nishi-2, Kita-ku, Sapporo, Hokkaido *0*�*2+* Japan.
e-mail : nishi@eos.hokudai.ac.jp
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Photo +. From left to right, Vacheslav Gusiakov
(outgoing IUGG Tsunami Commission Chair),
Fauzi (Meteorological and Geophysical Agency,
Indonesia), Laura Kong (International Tsunami
Information Center Director), provided leader-
ship to construct recommendations to mitigate
future tsunami disaster in Indonesia.
Photo ,. A -** m high Anak Krakatau, which is
located at the north wall of the remaining
caldera rim and was formed at the first eruption
in +3,1.
- � 214
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��.{|}������}§��� ¨©35$�~K\w?|ª«{X@5�U~¬15�U 8��QSYA5�U3�$��Z?[gFzA�X�(Yokoyama, +32+, +321 ; Latter, +32+ : Self and Rampino,
+32+ ; Camus and Vincent, +32- ; Francis, +32/ ;
Sigurdsson et al., +33+ ; Nomambhoy and Satake, +33/ ; de
Lange et al., ,**+)� .{|}����§��� ��56,U����nA�[®�\8 ¡���A��8 (Carey, +330, ,**+)� V�9£5¯�5°±�\�²�� ¡� ���])R³,A8�X´3µ£�
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Camus, G. and Vincent, P.M. (+32-) Discussion of a new
hypothesis for the Krakatau volcanic eruption in +22-. J.
Volcanol. Geotherm. Res., +3, +01�+1-.Carey, S., Sigurdsson, H., Mandeville, C. and Bronto, S.
(+330) Pyroclastic flows and surges over water : an ex-
ample from the +22- Krakatau eruption. Bull. Volcanol.,
/1, .3-�/++.Carey, S., Morelli, D., Sigurdsson, H. and Bronto, S.
(,**+) Tsunami deposits from major explosive eruptions :
an example from the +22- eruption of Krakatau. Geolo-
gy, ,3, -.1�-/*.de Lange, W. P., Prasetya, G. S. and Healy, T.R. (,**+)
Modelling of tsunamis generated by pyroclastic flows
(ignimbrites). Natural Hazards, ,., ,/+�,00.Francis, P.W. (+32/) The origin of the +22- Krakatau
tsunamis. J. Volcanol. Geotherm. Res., ,/, -.3�-0-.Latter, J.H. (+32+) Tsunamis of volcanic origin : summary
of causes, with particular reference to Krakatoa, +22-.Bull. Volcanol., .., .01�.3*.
Nomanbhoy, N. and Satake, K. (+33/) Generation mecha-
nism of tsunamis from the +22- Krakatau eruption.
Geophys. Res. Lett., ,,, /*3�/+,.Self, S. and Rampino, M.R. (+32+) The +22- eruption of
Krakatau. Nature, ,3., 033�1*..Sigurdsson, H., Carey, S. and Mandeville (+33+) Subma-
rine pyroclastic flows of the +22- eruption of Krakatau
volcano. Nat. Geog. Res. Explor., 1, -+*�-,1.Yokoyama, I. (+32+) A geophysical interpretation of the
+22- Krakatau eruption. J. Volcanol. Geotherm. Res., 3,-/3�-12.
Yokoyama, I. (+321) A scenario of the +22- Krakatau
tsunami. J. Volcanol. Geotherm. Res., -., +,-�+-,.
Photo -. Coral boulders carried up and deposited
by the +22- Krakatau tsunami. These tsunami
evidences are commonly seen around Anyer, a
seaside town /* km east from Krakatau volcano.
.{|}�T~ +,*�� ��¶�8·Y¸�¹��º�./»¦¼ 215
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