Period of precursory earthquakes
(Nov. 1989 - 16 Nov. 1990)
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The earthquake swarm began beneath Tachibana Bay (Chijiwa Caldera)
(Nov. 1989)
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The hypocenters moved to the area of Mt. Fugen cone
and
volcanic tremors occurred. (Jul. 1990)
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Period of phreatomagmatic eruption
i17 Nov. 1990 - 19 May 1991j
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1)
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Kujukushima and Jigokuato craters were active.
(17 Nov. 1990 - 11 Feb. 1991)
Phreatic eruption began from these craters. (17 Nov. 1990)
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2)
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Byobuiwa crater was active.
(12 Feb. 1991 - 28 Mar. 1991)
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A new Byobuiwa crater began phreatic eruption. (2 Feb.)
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3)
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The above three craters were simultaneously active.
(29 Mar. 1991 - 11 May 1991): Phreatomagmatic eruption
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4)
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Period of heavy change of the crust
(12 May 1991 - 19 May 1991)
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Inflation of the edifice
of Mt. Fugen,
thermal demagnetization,
strong activation of earthquakes right under the crater,
appearance of fissures
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Period of formation of lava dome
(20 May 1991 - Mar. 1995)
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1)
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The first period (20 May 1991 - Dec. 1992):
Formation of lobes, mainly
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Start of lava extrusion (20 May),
Beginning of pyroclastic flow (24 May)
The large-scale pyroclastic flow
(3 June, 8 June and 15 Sep.,
flowed down to the Annaka areaj
Lava extrusion
sharply declined. (at the end of 1992)
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2)
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The second period (Jan. 1993 - Oct. 1993):
Formation of lobes, mainly
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Lava extrusion started again (2 Feb.)
The large-scale pyroclastic flow
(23 - 24 June: flowed down to the Senbongi area)
The large-scale pyroclastic flow
(26 Jun. and 19 Jul.: flowed down to the Annaka area)
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3)
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The third period (Nov. 1993 - Feb. 1995)
Formation of clastic lava domes, mainly
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Small and middle scale of pyroclastic flows
run down to both the south and north sides
of Mt. Fugen. (Jan. - Sep. 1994)
Cease of lava extrusion
(Feb. 1995)
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Period of succeeding variation
(Mar. 1995 - present)
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Cooling and shrinking of the lava dome and the magma conduit,
sinking down of the dome
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