Kd. Young et Tj. Voight, B",subandriyo,sajiman,miswanto,"casadevall, Ground deformation at Merapi Volcano, Java, Indonesia: distance changes, June 1988-October 1995, J VOLCANOL, 100(1-4), 2000, pp. 233-259
Edifice deformations are reported here for the period 1988-1995 at Merapi v
olcano, one of the most active and dangerous volcanoes in Indonesia. The st
udy period includes a major resumption in lava effusion in January 1992 and
a major dome collapse in November 1994. The data comprise electronic dista
nce measurements (EDM) on a summit trilateration network, slope distance ch
anges measured to the upper flanks, and other data collected from 1988 to 1
995. A major consequence of this study is the documentation of a significan
t 4-year period of deformation precursory to the 1992 eruption. Cross-crate
r strain rates accelerated from less than 3 x 10(-6)/day between 1988 and 1
990 to more than 11 x 10(-6)/day just prior to the January 1992 activity, r
epresenting a general, asymmetric extension of the summit during high-level
conduit pressurization. After the vent opened and effusion of lava resumed
, strain occurred at a much-reduced rate of less than 2 x 10(-6)/day. EDM m
easurements between lower flank benchmarks and the upper edifice indicate d
isplacements as great as 1 tn per year over the four years before the 1992
eruption. The Gendol breach, a pronounced depression formed by the juxtapos
ition of old lava coulees on the southeast Rank, functioned as a major disp
lacement discontinuity. Since 1993, movements have generally not exceeded t
he 95% confidence limits of the summit network. Exceptions to this include
12 cm outward movement for the northwest crater rim in 1992-1993, probably
from loading by newly erupted dome lava, and movements as much as 7 cm on t
he south flank between November 1994 and September 1995. No short-term prec
ursors were noted before the November 1994 lava dome collapse, but long-ter
m adjustments of crater geometry accompanied lava dome growth in 1994. Shor
t-term 2-cm deflation of the edifice occurred following the November 1994 d
ome collapse. (C) 2000 Elsevier Science B.V. All rights reserved.