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Yaman · Medan gunung api

Haylan, Jabal

Tipe
Medan gunung api
Ketinggian
1550 m
Letusan terakhir
-1200
The Jabal Haylan volcanic field comprises scoria cones and tuff rings and associated lava flows across a 75-km-long area, with a portion of the field shown in this Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 52 km across). The chain crosses a NW-SE-trending fault that with visible offset in this image. Many of the cones and rings have experienced flank collapse, rafting, or erosion, leaving amphitheater-shaped craters. Some tuff rings appear to have lava domes that have formed within the crater.
The Jabal Haylan volcanic field comprises scoria cones and tuff rings and associated lava flows across a 75-km-long area, with a portion of the field shown in this Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 52 km across). The chain crosses a NW-SE-trending fault that with visible offset in this image. Many of the cones and rings have experienced flank collapse, rafting, or erosion, leaving amphitheater-shaped craters. Some tuff rings appear to have lava domes that have formed within the crater. · Foto: Satellite image courtesy of Planet Labs Inc., 2019 (https://www.planet.com/).
Tipe
Medan gunung api
Negara
Yaman
Wilayah
Arab & Asia Tengah / Southwest Arabia Volcanic Province
Ketinggian
1550 m
Koordinat
15.400, 45.100
Letusan terakhir
-1200
Kondisi tektonik
Intralempeng / Kerak benua (> 25 km)
Bentuk lahan
Gugusan gunung api
Batuan utama
Basal / Pikrobasal

Ringkasan geologi

Teks asli bahasa Inggris

The Jabal Haylan area contains a 75-km-long chain of tuff cones and associated olivine basaltic lava flows in eastern Yemen.

Kutipan dari Global Volcanism Program, Smithsonian Institution · Baca ringkasan lengkap di GVP →

Riwayat letusan

1 tercatatGlosarium

Ringkasan catatan

Letusan terkonfirmasi
1
Letusan tidak pasti
0
Rentang catatan terkonfirmasi
1200 SM – 1200 SM
Letusan terkonfirmasi terbesar
VEI 0 (1200 SM)
Letusan terkonfirmasi sejak 1900
0
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1200 SM~1200 SM · 1 letusan · VEI maks. 01200 SM1200 SM1199 SM1199 SM1199 SM

Garis waktu rinci

  1. 1200 SMVEI 0Perkiraan geologi
    1200 SM – akhir tidak diketahui
    West of Sirwan

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