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Southern Somalia is relatively flat while northern Somalia rises to 2,000m then drops to the Gulf of Aden. Jurassic limestone was deposited across Somalia but erosion later removed thickness locally. A Cretaceous sea then covered Somalia with transgressions and regressions. Marine Eocene rocks cover northern Somalia but are absent in southern Somalia except a narrow coastal strip. Southern Somalia uplifted in late Cretaceous while northern Somalia uplifted in middle-late Tertiary by rift faulting. The most

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yrdgcgf5664

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EN