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Latest news:jeudi, oct. 18, 2012
The MODVOLC detected thermal anomalies at Ibu on 17th September. Suggesting eruptive activity at the summit, possibly related to lava dome growth in the wide summit crater that has been documented since 2000.
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jeudi, août 13, 2009
It is reported that white and gray plumes from Ibu rose to 300-400 m altitude. There are more frequent earthquakes, that indicate an increasing activity. There were also lava flows and explosions at the summit. There was also Strombolian activity. The Alert Level was increased to 3. The lava dome is growing and is now visible from Duono village.
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Ibu volcanstratovolcan 1325 m / 4,347 ft
Halmahera, Indonesia, 1.48°N / 127.64°E Condition actuelle: Activité petite ou avertissement éruption imminente (3 sur 5) Ibu webcams / live data
Dernière mise à jour: 21 janv. 2013 (Thermal anomalies indicate continuing eruption, possible lava dome growth)
Style éruptif tipique: Explosive Eruptions du volcan Ibu: 1911, 1998, 2001, 2004 Ibu photos du volcan Derniers séismes proches:
Le volcan IBU, situé le long de l'île de la côte de Halmahera NW, est un stratovolcan avec un sommet tronqué et un certain nombre de cratères grand sommet imbriqués. Le cratère intérieur, 1 km de large et de 400 m de profondeur, contenait plusieurs lacs de petit cratère grâce à une grande partie du temps historique. Le cratère externe, 1,2 km de large, il y a violation du côté nord, créant une vallée raides. Un grand cône parasite se trouve ENE du sommet. Un plus petit qui le WSW a alimenté une coulée de lave sur le flanc ouest. Un groupe de maars est situé sous les flancs nordiques et ouest du volcan. Introduction:Ibu volcano, located along the NW coast of Halmahera Island, is a stratovolcano with a truncated summit and a number of large nested summit craters. The inner crater, 1 km wide and 400 m deep, contained several small crater lakes through much of historical time. The outer crater, 1.2 km wide, is breached on the north side, creating a steep-walled valley. A large parasitic cone is located ENE of the summit. A smaller one to the WSW has fed a lava flow down the western flank. A group of maars is located below the northern and western flanks of the volcano.Ibu Photos:
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