Owen transform fault
hydrotermální průduchy, Indian, Carlsberg Ridge
- Kde
- Indian, Carlsberg Ridge
- Prostředí
- mid-ocean ridge
- Činnost
- inactive
- Hloubka
- 4 500 m
- Objeven
- NotProvided
- Poloha
- 9,833°, 57,950°
Mn crusts on fresh basalt; from Wikipedia: "Owen Transform Fault is used to denote the short section between the end of the Aden-Sheba ridge and the Carlsberg Ridge"; this position is southern part of Owen f.z. near Carlsberg Ridge; note: Sheba Ridge is eastern portion of Aden Ridge; Rona et al. (2005): "Further CR hydrothermal evidence includes relict sulfide chimneys at 58E"
Údaje o průduchu: InterRidge Vents Database v3.4 (CC BY-NC-SA 4.0). Další sopky a průduchy.