Pulau Asuncion
Asuncion
Stratovolkan · United States · 857 m

- Tipe
- Stratovolkan
- Negara
- United States
- Wilayah
- Northwestern Pacific Volcanic Regions / Mariana Volcanic Arc
- Ketinggian
- 857 m
- Koordinat
- 19.671, 145.406
- Letusan terakhir
- 1906
- Kondisi tektonik
- Subduction zone / Crustal thickness unknown
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
A single large asymmetrical stratovolcano forms 3-km-wide Asuncion Island. The steeper NE flank terminates in high sea cliffs, while the gentler SW flanks have low-angle slopes bounded by sea cliffs only a few meters high. The southern flank is cut by a large landslide scar. The S and W flanks are covered by ash deposits. An explosive eruption in 1906 produced lava flows that descended about halfway down the W and SE flanks, but several other eruption reports are of uncertain validity.
Ringkasan Wikipedia
Asuncion adalah pulau paling utara ketiga di Kepulauan Mariana Utara di Samudra Pasifik. Pulau itu tidak berpenghuni dan terletak 101 kilometer (63 mi) barat laut Agrihan dan 37 km (23 mi) tenggara Kepulauan Maug.
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Riwayat letusan
Garis waktu rinci
- 1924VEI 2Perkiraan geologi1924 – Berlangsung
- 1906VEI 2Teramati1906 – BerlangsungUpper SE and W flanks
- 1775 (±10 tahun)VEI 2Perkiraan geologi1775 – Berlangsung
- 1690 (±10 tahun)VEI ?Perkiraan geologi1690 – Berlangsung
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.