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Ciad · Stratovulcano

Ehi Mousgou

Voon, Tarso

Tipo
Stratovulcano
Altitudine
3100 m
Ultima eruzione
Sconosciuto
Ehi Mousgou
Foto: NASA · Public domain · Wikimedia Commons
Tipo
Stratovulcano
Paese
Ciad
Regione
Africa settentrionale / East Central Sahara Volcanic Province
Altitudine
3100 m
Coordinate
20.920, 17.280
Ultima eruzione
Sconosciuto
Contesto tettonico
Intraplacca / Crosta continentale (> 25 km)
Forma vulcanica
Composito
Roccia principale
Trachite / Trachidacite
Sintesi geologica

The broad summit of Tarso Voon volcano, located in the west-central part of the Tibesti Range, is truncated by a shallow 14 x 18 km wide caldera. Ignimbrite deposits surround the caldera to distances of 15-35 km. It was constructed over a basement of Precambrian schists. Youthful-looking Quaternary basaltic lava flows have been erupted from vents near the caldera rim over a 180-degree area extending counterclockwise from the NE and from Ehi Mousgau, a 3100-m-high stratovolcano located to the NW. The Soborom solfatara field, the largest in the Tibesti Range, is located in an area of volcano-tectonic uplift 5 km west of the caldera rim. Its fumaroles, active mud pots, and boiling waters are visited by Tibesti peoples for medicinal uses.

Sintesi da Wikipedia

Riassunto in inglese

The Tarso Voon is a 3,100-metre (10,200 ft) high stratovolcano in the north of the Republic of Chad. It is located in the western center of the Tibesti Mountains.

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