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Palinuro Seamount

Palinuro

Tipe
Gunung api majemuk
Ketinggian
70 m (bawah laut)
Letusan terakhir
-8040
Tipe
Gunung api majemuk
Negara
Italia
Wilayah
Eropa / Aeolian Volcanic Arc
Ketinggian
70 m (bawah laut)
Koordinat
39.480, 14.830
Letusan terakhir
-8040
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Komposit
Batuan utama
Fonolit
Ringkasan geologi

Palinuro seamount in the Tyrrhenian Sea north of the Eolian Islands rises nearly 3,000 m to within 70 m of the surface and has an open summit crater. A marine ash layer (PL-1) radiocarbon dated (calibrated) at 9,990 +/- 90 years ago is chemically and stratigraphically similar to two ash layers on land in southern Italy; it was tentatively correlated to Palinuro seamount activity (Siani et al., 2004).

Ringkasan Wikipedia

Ringkasan Inggris

Palinuro Seamount is a seamount in the Tyrrhenian Sea. It is an elongated 50–70 km (31–43 mi) long complex of volcanoes north of the Aeolian Islands with multiple potential calderas. The shallowest point lies at 80–70 m (260–230 ft) depth and formed an island during past episodes of low sea level. Palinuro was active during the last 800,000 years and is likely the source for a 10,000 years old tephra layer in Italy. Ongoing seismicity occurs at the seamount, which may be a tsunami hazard. The volcanic activity may somehow relate to the subduction of the Ionian Sea farther east.

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  1. 8040 SM (±100 tahun)VEI ?Perkiraan geologi
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