Secca del Capo

hydrotermální průduchy, Mediterranean, Aeolian Arc, Tyrrhenian Sea

Kde

Mediterranean, Aeolian Arc, Tyrrhenian Sea

Prostředí

arc volcano

Činnost

active, inferred

Hloubka

240 m

Objeven

1995 ROV Comex deposits only; 2007 plume only

Poloha

38,633°, 14,850°

offshore area north of Salina; Gamberi et al. (1997): "In the western high, large areas of the seafloor are extensively covered by mounds of Fe-rich, semiconsolidated crusts ... The presence of these deposits on the seafloor implies that the Secca de1 Capo region has been affected by hydrothermalism in the recent past."; Lupton et al. (2011): "found a small 3He excess at about 200 m depth"

Údaje o průduchu: InterRidge Vents Database v3.4 (CC BY-NC-SA 4.0). Další sopky a průduchy.