Gunung Sumbing Jawa Tengah
Sumbing
Stratovolkan · Indonesia · 3370 m
- Tipe
- Stratovolkan
- Negara
- Indonesia
- Wilayah
- Sunda & Banda / Sunda Volcanic Arc
- Ketinggian
- 3370 m
- Koordinat
- -7.382, 110.075
- Letusan terakhir
- 1730
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
Gunung Sumbing is a stratovolcano that is the SE-most edifice of a chain of volcanoes in central Java that includes Sundoro and the Dieng Complex. Prominent cones are located on the N and SE flanks. An 800-m-wide summit crater is breached to the NE, but is partially filled by a lava dome that extended beyond the original crater rim. Emplacement of the dome followed the production of extensive pyroclastic flows down the NE flank. Activity reported in about 1730 CE may have produced the small phreatic craters found at the summit behind the dome.
Ringkasan Wikipedia
Ringkasan InggrisMount Sumbing is an active stratovolcano in Central Java, Indonesia. This volcano is symmetrical like its neighbor Mount Sindoro which lies to its northwest. Administratively, The volcano is divided between 3 regencies: Temanggung, Wonosobo, and Magelang. The only report of historical eruptions is from 1730. It has created a small phreatic crater at the summit.
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Riwayat letusan
Garis waktu rinci
- 1730VEI 1Teramati1730 – Berlangsung
Tautan eksternal
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