The Easter Fracture Zone is an oceanic fracture zone associated with the transform fault extending from the Tuamotu archipelago in the west to the Peru–Chile Trench to the east. The Easter Fracture Zone extends roughly 5900 kilometers from 20°S,131°W to 26°S,78°W. The landscape consists of several ridges and isolated volcanos with maximal peak elevation above the seafloor of 3000m. Because the local seafloor has depths around 4000m to the north of the fracture zone and 3400m to the south of the fracture zone, most of its volcanic peaks form seamounts. They do rise above sea level at the Pitcairn Islands and Easter Island.
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| - Easter Fracture Zone (en)
- Zona di frattura dell'Isola di Pasqua (it)
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| - The Easter Fracture Zone is an oceanic fracture zone associated with the transform fault extending from the Tuamotu archipelago in the west to the Peru–Chile Trench to the east. The Easter Fracture Zone extends roughly 5900 kilometers from 20°S,131°W to 26°S,78°W. The landscape consists of several ridges and isolated volcanos with maximal peak elevation above the seafloor of 3000m. Because the local seafloor has depths around 4000m to the north of the fracture zone and 3400m to the south of the fracture zone, most of its volcanic peaks form seamounts. They do rise above sea level at the Pitcairn Islands and Easter Island. (en)
- La zona di frattura dell'Isola di Pasqua è una zona di frattura oceanica nell'Oceano Pacifico associata a una faglia trasforme che si estende dalle Isole Tuamotu a ovest, fino alla fossa di Atacama a est. (it)
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| - The Easter Fracture Zone is an oceanic fracture zone associated with the transform fault extending from the Tuamotu archipelago in the west to the Peru–Chile Trench to the east. The Easter Fracture Zone extends roughly 5900 kilometers from 20°S,131°W to 26°S,78°W. The landscape consists of several ridges and isolated volcanos with maximal peak elevation above the seafloor of 3000m. Because the local seafloor has depths around 4000m to the north of the fracture zone and 3400m to the south of the fracture zone, most of its volcanic peaks form seamounts. They do rise above sea level at the Pitcairn Islands and Easter Island. (en)
- La zona di frattura dell'Isola di Pasqua è una zona di frattura oceanica nell'Oceano Pacifico associata a una faglia trasforme che si estende dalle Isole Tuamotu a ovest, fino alla fossa di Atacama a est. La zona di frattura si estende per circa 5.900 km dalle coordinate 20°S,131°W fino a 26°S,78°W. Nell'area sono presenti molte dorsali e vulcani isolati, con un'elevazione massima di circa 3.000 m al di sopra del fondale marino. Poiché il fondale ha profondità che variano tra i 4.000 m a nord della zona di frattura e i 3.400 m a sud della zona di frattura, le vette non raggiungono la superficie del mare e pertanto i rilievi appaiono come montagne sottomarine. Solo nelle Isole Pitcairn e nell'Isola di Pasqua i picchi si elevano al di sopra della superficie marina. (it)
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