Gunung Egon
Egon
Stratovolkan · Indonesia · 1661 m

- Tipe
- Stratovolkan
- Negara
- Indonesia
- Wilayah
- Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
- Ketinggian
- 1661 m
- Koordinat
- -8.676, 122.455
- Letusan terakhir
- 2008
- Kondisi tektonik
- Subduction zone / Crustal thickness unknown
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
Gunung Egon, also known as Namang, sits within the narrow section of eastern Flores Island. The barren, sparsely vegetated summit region has a 350-m-wide, 200-m-deep crater that sometimes contains a lake. Other small crater lakes occur on the flanks. A lava dome forms the southern summit. Solfataric activity occurs on the crater wall and rim and on the upper S flank. Reports of eruptive activity prior to explosive eruptions beginning in 2004 are unconfirmed. Emissions were often observed above the summit during 1888-1892. Strong emissions in 1907 reported by Sapper (1917) was considered by the Catalog of Active Volcanoes of the World (Neumann van Padang, 1951) to be an historical eruption, but Kemmerling (1929) noted that this was likely confused with an eruption on the same date and time from Lewotobi Lakilaki.
Ringkasan Wikipedia
Gunung Egon adalah sebuah gunung berapi yang terletak di Kabupaten Sikka, Pulau Flores, provinsi Nusa Tenggara Timur, Indonesia. Gunung ini memiliki tinggi 1.703 meter dari permukaan laut. Egon kembali aktif pada 2004 setelah vakum selama 75 tahun. Egon tercatat meletus dahsyat pada 1925.
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Riwayat letusan
Garis waktu rinci
- 2008VEI 2Teramati2008-04-15 – 2008-04-28
- 2005VEI 1Teramati2005-02-06 – 2005-02-27Summit and southern flank
- 2004VEI 1Teramati2004-01-29 – 2004-02-05
- 2004VEI 2Teramati2004-07-03 – 2004-09-16
- 1888VEI 2Perkiraan geologi1888 – 1892
Tautan eksternal
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