Report on Merapi (Indonesia) — March 1976
Natural Science Event Bulletin, vol. 1, no. 6 (March 1976)
Managing Editor: David Squires.
Merapi (Indonesia) Increases in seismicity, lava dome height, and incandescent spots on dome
Please cite this report as:
Global Volcanism Program, 1976. Report on Merapi (Indonesia) (Squires, D., ed.). Natural Science Event Bulletin, 1:6. Smithsonian Institution. https://doi.org/10.5479/si.GVP.NSEB197603-263250.
7.54°S, 110.446°E; summit elev. 2910 m
All times are local (unless otherwise noted)
Activity increased in February compared to the previous month. The number of volcanic earthquakes increased, the lava dome grew higher, and red glares were observed at 2 points on the dome. The number of glowing avalanches decreased from January, however, and there was only one nuée ardente, on 4 February, that traveled about 750 m SW into the Batang River.
On 5 March at 1503, reddish white smoke emitted with strong gas pressure was observed to about 350 m above the summit. The volcano was hidden behind clouds. On 6 March, small avalanches took place continuously from 0135 until 0348, then the volcano was covered by clouds. At 1702, three avalanches were observed. From 1733 on, bigger nuées ardentes took place, interspersed with minor ones, until 13 March (table 1).
|Date||Large||Small||Maximum Distance (km)|
|06 Mar 1976||10||19||4|
|07 Mar 1976||17||16||5.5|
|08 Mar 1976||5||2||3.5|
|09 Mar 1976||5||6||6|
|10 Mar 1976||1||4||2.75|
|11 Mar 1976||1||9||5.5|
|12 Mar 1976||--||6||1.5|
|13 Mar 1976||--||3||1.5|
From the evening of 8 March until the evening of 9 March, when the volcano became visible from the Ngepos Volcano Observatory 11 km SW of the summit, it could be observed that the lower part of the lava dome, estimated to be about 400,000 m3, or almost 1/3 of its volume (1.4 x 106 m3), had slid away. During the events on 6 and 7 March nuées ardentes moved SW, entering a tributary of the Batang River and continuing much further down stream into the rivers Sat, Blongkeng, and Bebeng. The prevailing wind blew E, depositing finer volcanic products on the E and SE flanks to a maximum distance of 37.5 km. Thickest ash falls were on the ESE flank. At 6 km from the summit the deposit apparently measured 5 mm and temporarily panicked the villagers.
Nuées ardentes caused forest fires on the upper SW flank near the tributaries of the rivers Sat, Blongkeng, and Bebeng. Roughly 580,000 m3 of ash were deposited on the E flank, and around 300,000 m3 of avalanche material were deposited on the upper SW flank.
Geologic Background. Merapi, one of Indonesia's most active volcanoes, lies in one of the world's most densely populated areas and dominates the landscape immediately north of the major city of Yogyakarta. It is the youngest and southernmost of a volcanic chain extending NNW to Ungaran volcano. Growth of Old Merapi during the Pleistocene ended with major edifice collapse perhaps about 2000 years ago, leaving a large arcuate scarp cutting the eroded older Batulawang volcano. Subsequently growth of the steep-sided Young Merapi edifice, its upper part unvegetated due to frequent eruptive activity, began SW of the earlier collapse scarp. Pyroclastic flows and lahars accompanying growth and collapse of the steep-sided active summit lava dome have devastated cultivated lands on the western-to-southern flanks and caused many fatalities during historical time.
Information Contacts: D. Hadikusumo, Volcanology Division, GSI.