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Il rift del Golfo di Suez è una zona di ri … Il rift del Golfo di Suez è una zona di rift continentale che fu attiva tra il tardo Oligocene (circa 28 milioni di anni fa) e la fine del Miocene (circa 5 milioni di anni fa). Rappresentava una continuazione del rift del Mar Rosso fino alla separazione avvenuta a metà del Miocene, quando gran parte dello spostamento sul neo formatosi centro di divergenza del Mar Rosso andò a finire nella . Durante la breve storia successiva alla formazione del rift, la parte più profonda della topografia residua del rift è stata riempita dal mare, creando così il Golfo di Suez. A nord del Golfo di Suez, il rift diventa indistinto e la sua esatta geometria diviene incerta, collegandosi alla fine al rift di Manzala, al di sotto del delta del Nilo.i Manzala, al di sotto del delta del Nilo.
, The Gulf of Suez Rift is a continental rif … The Gulf of Suez Rift is a continental rift zone that was active between the Late Oligocene (c. 28 Ma) and the end of the Miocene (c. 5 Ma). It represented a continuation of the Red Sea Rift until break-up occurred in the middle Miocene, with most of the displacement on the newly developed Red Sea spreading centre being accommodated by the Dead Sea Transform. During its brief post-rift history, the deepest part of the remnant rift topography has been filled by the sea, creating the Gulf of Suez. North of the Gulf of Suez the rift becomes indistinct and its exact geometry uncertain, linking eventually to the beneath the Nile delta. eventually to the beneath the Nile delta.
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| rdfs:comment |
Il rift del Golfo di Suez è una zona di ri … Il rift del Golfo di Suez è una zona di rift continentale che fu attiva tra il tardo Oligocene (circa 28 milioni di anni fa) e la fine del Miocene (circa 5 milioni di anni fa). Rappresentava una continuazione del rift del Mar Rosso fino alla separazione avvenuta a metà del Miocene, quando gran parte dello spostamento sul neo formatosi centro di divergenza del Mar Rosso andò a finire nella . Durante la breve storia successiva alla formazione del rift, la parte più profonda della topografia residua del rift è stata riempita dal mare, creando così il Golfo di Suez.a dal mare, creando così il Golfo di Suez.
, The Gulf of Suez Rift is a continental rif … The Gulf of Suez Rift is a continental rift zone that was active between the Late Oligocene (c. 28 Ma) and the end of the Miocene (c. 5 Ma). It represented a continuation of the Red Sea Rift until break-up occurred in the middle Miocene, with most of the displacement on the newly developed Red Sea spreading centre being accommodated by the Dead Sea Transform. During its brief post-rift history, the deepest part of the remnant rift topography has been filled by the sea, creating the Gulf of Suez.led by the sea, creating the Gulf of Suez.
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Rift del Golfo di Suez
, Gulf of Suez Rift
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