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Latest news from Merapi:
Ash plume from Merapi in Centra Java (ESA)
Thursday, Mar 27, 2014
A possibly strong eruption was reported from the volcano this afternoon (13:55 GMT). Satellite data showed an ash and SO2 plume drifting SW at estimated 32,000 ft (9 km) (VAAC Darwin). The plume is quickly dissipating, suggesting that the eruption was an isolated (possibly phreatic) explosion. ... [more]
Thursday, Dec 12, 2013
Another small phreatic explosion occurred at the summit lava dome this morning at 08:10 local time. it produced an ash plume rising 500 m. According to VSI, rainwater infiltration into the hot rocks of the dome caused the eruption. [more]
Standing on top of Merapi volcano at sunrise
Standing on top of Merapi volcano at sunrise
Pyroclastic flow from Merapi volcano
Pyroclastic flow from Merapi volcano
Merapi's steep cone seen from the east
Merapi's steep cone seen from the east

Merapi volcano

Stratovolcano 2968 m / 9,737 ft
Central Java, Indonesia, -7.54°S / 110.44°E
Current status: erupting (4 out of 5)
Merapi webcams / live data
Last update: 27 Mar 2014
Typical eruption style: Highly explosive. Large Plinian eruption every few 1000 of years (the last ones at about 1000 BP and 2000 BP), sometimes with associated flank collapse. Growth of lava domes, pyroclastic flows.
Merapi volcano eruptions: 1548, 1554, 1560, 1584, 1586(?), 1587, 1658, 1663, 1672, 1678, 1745, 1752, 1755, 1768, 1791, 1797, 1807, 1810, 1812-22, 1822-23, 1828, 1832-36, 1837-38, 1840, 1846, 1848(?), 1849, 1854(?), 1861, 1862-64, 1865-71, 1872 (large vulcanian-subplinian eruption VEI:4) , 1872-73, 1878-79, 1883-84, 1885-87, 1888, 1889, 1891-92, 1893, 1894, 1897, 1902, 1902-04, 1905, 1906-07, 1908, 1909-13, 1915, 1918, 1920-21, 1922, 1923(?), 1924, 1930-31, 1932, 1933-35, 1939-40, 1942-45, 1948, 1953-58, 1961, 1967-1970, 1971(?), 1972-85, 1986-90, 1992-2002, April-July 2006, Oct 2010-2011 Feb Glowing avalanches of hot rocks from the new lava dome (2006 eruption).
Last earthquakes nearby: No recent earthquakes
TimeMag. / DepthDistanceLocation
Merapi, a steep stratovolcano north of Central Java's capital Yogyakarta, is Indonesia's most active volcano. It erupts on average every 5-10 years and is feared for its deadly pyroclastic flows - avalanches of hot rocks and gas that are generated when parts of new lava domes constructed during eruptions in the summit crater collapse and slide down the mountain's steep flanks.
The name "Merapi" from old Javanese language means "the one making fire" is a popular name for volcanoes: another volcano with the same name Merapi is in the Ijen Massif in East Java and similarly called volcano "Marapi" lies on Sumatra Island.

Background:

Merapi dominates the landscape immediately north of the city of Yogyakarta in one of the world's most densely populated areas. Merapi is the youngest and southernmost of a volcanic chain extending NNW to Ungaran volcano. The steep-sided modern Merapi edifice, its upper part unvegetated due to frequent eruptive activity, was constructed to the SW of an arcuate scarp cutting the eroded older Batulawang volcano. Pyroclastic flows and lahars accompanying growth and collapse of the steep-sided active summit lava dome have devastated cultivated lands on the volcano's western-to-southern flanks and caused many fatalities during historical time. Since 1953, activity has been characterized by extrusion of lava into the summit crater, with periodic lava dome collapse and nuée ardente formation. Summit lava dome growth has continued since the 1969 gas explosion. It is monitored from the Merapi Volcano Observatory (MVO) in Yogyakarta.

Merapi Photos:



April-June 2006 eruption: new lava dome & pyroclastic flows, 2 fatalities
After a period of 5 years of relative calm, a new eruption started in April 2006. A new lava dome was built on top of the lava dome of 1998-2001, powerful pyroclastic flows descended the SW, S and SE flanks in late May and June. Tens of thousands of people were evacuated during the peak of the eruption in late May-mid June. A particularly powerful pyroclastic flow killed two workers trapped inside a shelter that was overrun by a flow on 14 June. ...more

27 May 2006 Yogyakarta earthquake
On 27 May 2006 a magnitude 6.3 tectonic earthquake near Yogyakarta caused 5750 fatalities, around 40,000 injuries and destroyed large sections of Yogyakarta and sourrounding towns, leaving more than 600,000 people homeless.
The earthquake was caused by the collission of the Australian and Sunda tectonic plates, forming a subduction zone west of the coast of Java.

Jan-Feb 2001 activity: major dome collapse on 10 February
Activity increased in January 2001, lava effusion rates were at high levels and feeding frequent pyroclastic flows. On 31 January pyroclastic flows occurred continuously, reaching up to 3.5 km from the summit, flowing mainly to the SSW, but started also to descend on the SW and W flanks of the mountain into the Senowo and Bebeng Rivers.
On 10 February 2001, a large section of the 1998 lava dome collapsed and triggered a serious of pyroclastic flows that reached 7 km distance from the crater, travelling SSW into the Sat River. Significant ash fall from the eruption occured up to 60 km E of the volcano.
After this event, activity decreased sharply, but continued at lower levels through much of 2001.

Dec 2000- Jan 2001 eruption: pyroclastic flows
Eruptive activity increased steeply during the period of 26 December 2000-22 January 2001. On 14 January, 29 pyroclastic flows traveled down the volcano's SSW and SW flanks and reached up to 4 km from their source. During the week, lava avalanches and pyroclastic flows occurred with an average interval of 0.5-1 hours.

1998-2000 activity: glowing rockfalls
Seismic activity and rockfalls from the lava dome at the summit increased again in June 1998 and peaked between 11-19 July when 128 rock avalanches and pyroclastic flows were recorded descending the Lamat, Krasak/Bebeng and Boyong rivers on the SW and SSW flanks of the volcano.
Activity decreased, but the volcano remained active through 1999 and 2000, when intense degassing, minor explosions, intermittend glow at the summit and occasional rockfalls were recorded.

1996 eruptions - contining lava dome growth and pyroclastic flows
The activity that had started in 1994 continued through 1995 and increased again starting from August 1996, when explosions and pyroclastic flows became more frequent and large. On 9 August, a pyroclastic flow traveled 3.5 km from the summit down the SSW flank and reached the upper parts of the Krasak and Boyong rivers. No casualties were reported. An explosion on 13 September created an ash cloud of ca. 4 km height above the summit.
Activity peaked on 31 October when 17 pyroclastic flows were recorded. They reached a maximum of 3 km distance and touched the upper valleys of Bebeng, Krasak, Boyong, and Kuning rivers on the SSW and SW flanks.
Pyroclastic flows decreased on 1st November and the eruption ended on 2nd November.

1994 eruption - 41 fatalities
A major collapse of the growing lava dome on November 22 1994 produced a large pyroclastic flow that ran 7.5 km on the S flank, overrunning Kaliurang village and killed at least 41 people. 6000 people were evacuated. ...more

1992-1993 eruption: new lava dome growth
A new lava dome grew in late January and early February 1992 and generated pyroclastic flows travelling up to 4 km to the SW flank. ...more

1968 eruptions
By the end of May 1968 a viscous lava flow had been extruded from the collapse scar of the Oct 1967 dome collapse and reached 875 m SW on the upper slope. Rockfalls and small pyroclastic flows from the lava flow were frequent in June through August (up to ca. 1500 per month) and died out in September. New activity began in October.

April-October 1967 eruption
A new lava dome was built in April 1967. Dome collapses in October 1967 generated pyroclastic flows into the Batang river valley on the SW side of the cone.
Merapi volcano seen from the south
Merapi volcano seen from the south
Merapi volcano seen from Yogyakarta
Merapi volcano seen from Yogyakarta
Canyons and standing blocks, remnants of the old S flank of Merapi, reshaped by landslides
Canyons and standing blocks, remnants of the old S flank of Merapi, reshaped by landslides
Merapi's lava dome
Merapi's lava dome
Spines at the lava dome of Merapi
Spines at the lava dome of Merapi

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