Gunung Sibayak
Singkut
Kaldera · Indonesia · 2181 m
.jpeg?width=800)
- Tipe
- Kaldera
- Negara
- Indonesia
- Wilayah
- Sunda & Banda / Sunda Volcanic Arc
- Ketinggian
- 2181 m
- Koordinat
- 3.238, 98.513
- Letusan terakhir
- 1881
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Caldera
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
The Quaternary Singkut caldera is about 7 x 4 km with the S half of the rim topographically distinct. Post-caldera cones have filled much of the crater and the N rim, including Sibayak, Pintau, and Pratektekan. The 900-m-wide Sibayak crater is partially filled on the north by Pintau. A lava flow traveled through a gap in the western crater wall from the summit lava dome of Sibayak; the active geothermal field SE of the summit has abundant solfataras and fumaroles. Area residents record legends of eruptions. Neumann van Padang (1983) cited a report by Hoekstra of ash clouds emitted from the volcano in 1881. The town of Berastagi is within the caldera immediately SE of the younger cones.
Ringkasan Wikipedia
Ringkasan InggrisMount Sibayak is a stratovolcano overlooking the town of Berastagi in northern Sumatra, Indonesia. Although its last eruption was more than a century ago, geothermal activity in the form of steam vents and hot springs remains high on and around the volcano. The vents produce crystalline sulfur, which was mined on a small scale in the past. Seepage of sulfurous gases has also caused acidic discolouration of the small crater lake.
Wikipedia · CC BY-SA · Baca artikel lengkap →
Riwayat letusan
Garis waktu rinci
- 1881VEI ?Teramati1881-07-02 – Berlangsung
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.