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Haylan, Jabal

Medan gunung api · Yemen · 1550 m

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
Yemen
Wilayah
Arabia-Central Asia Volcanic Regions / Southwest Arabia Volcanic Province
Ketinggian
1550 m
Koordinat
15.400, 45.100
Letusan terakhir
-1200
Kondisi tektonik
Intraplate / Continental crust (> 25 km)
Bentuk lahan
Cluster
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

The Jabal Haylan area contains a 75-km-long chain of tuff cones and associated olivine basaltic lava flows in eastern Yemen. The chain crosses a NW-SE-trending fault extending between the highlands and desert lowlands to the east. One of the lava flows covers alluvial terraces that accumulated behind man-made dams from about 800-1200 BCE (Catalog of Active Volcanoes of the World).

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
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1200 BCE~1200 BCE · 1 letusan · VEI maks. 01200 BCE1200 BCE1199 BCE1199 BCE1199 BCE

Garis waktu rinci

  1. 1200 SMVEI 0Perkiraan geologi
    BCE 1200 – Berlangsung
    West of Sirwan

Tautan eksternal

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