The Kelud stratovolcano located on the island of Java , has seen its alert level move from level II / Waspada ( alert ) at III / Siaga
(standby) , on 10 February .
Waiting for a change in this status, I have not commented until
now the news.
A reminder of the facts since 2007 :
After an effusive eruption on 3-4 November 2007, producing a lava dome in the crater lake, still active in December of the same year , the level of Kelud was reduced to I / Normal in June
2009, while keeping
recommendations to keep away from the dome , due to its instability , its potentially high temperature and toxic gas emanating .
Seismicity of Kelud was increasing
since January 2014 with a number of volcanic shallow earthquakes - between 2 and 8 km. under the volcano - and peaks of seismicity on 15-16 January , 28 January and 2 February.
The temperature of the crater lake had also increased by 5.5°C since September
2013. Following that, the PVMBG had passed the alert level II ( on
a scale of IV) on February 2 .
Since the elevation of the seismicity , the presence of inflation , in particular in its radial component , and the increase in water temperature of 4°C between 23 January and February 9 ,
followed by a relative decline on 10.02 , brought the
PVMBG to suspect a magmatic intrusion and change the alert level.
The evolution of the volcano is to follow!
The evolution of the seismicity between January 1 and February 10 - a decision support - doc
. VSI
Kelud - seismic swarm
between 5 and 8 February 2014 - the hypocenters (seismic foci ) are 1.5 -3.5 km below the summit . - Doc. VSI
Kelud or the tribulations of a crater lake :
The Kelud occupies a special place among Indonesian volcanoes. Despite a degree of confidentiality , 30 eruptions have been recorded since 1000 .
Eruptions from Kelud and their VEI from year 1000 - doc . GVP
The danger presented by this volcano is related to the presence of a large crater lake with a volume of up to 40 million cubic meters, which is expelled during eruptive initial stages, often
Plinian type .
In
1919, 5,160 people were killed by lahars caused by the eruption and the ejection of 38,000 m³ of water from the lake; the lahars have gone up to 37 km.
from the crater and covered 131 km², flooding 104 villages.
Solfatara in the crater of Kelud in April 1919 - doc .
Tropenmuseum
The VSI dug tunnels in the walls of Kelud
to drain the lake and maintain its volume to about 2 million m³.
The lake level has dropped by fifty meters after this action, but in 1951, a new eruption deepened the crater of 70 meters , leaving a volume of 50 million
cubic meters of water after repair of damaged tunnels . After the loss of over
200 lives following the eruption of 1966, a new tunnel was built , and the lake volume reduced to only one million cubic meters.
Kelud Crater and Lake in 1980 - photo Dan Dzurisin / USGS
The eruption of 2007 changed the situation : the lava dome that is installed in the lake did disappear almost all , minimizing the risk of interaction between
the magma , lava and water.
A detailed
analysis of Lake Kelud is available on the website of Professor Bernard / Université Libre de Bruxelles - link
Images video and thermal ( Thermacam
FLIR P25 ) of Kelud November 9, 2007, made by Solikhin & Segy / VSI - Doc ULB / Prof . Bernard / Commission of volcanic lakes.
Kelud - the lava dome collapses and 30.11.2007 - photo Tom
Pfeiffer
Kelud - the lava dome
has invaded the entire space of the former crater lake and is still smoking on 26.11.2010 ( we see one remaining bottom left) - photo Antony
Van Eeten .
Sources :
- Badan Geologi - statut éruptif du Kelud 10.02.2014
- link
- U.L.B. / Université Libre de Bruxelles - Growing lava dome observed in the lake of Kelud volcano, Indonesia - par le Prof. A.Bernard. - link
- Global Volcanism Program - Kelut
