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We compare the morphologies and activity histories of faults in each basin using field observations and remote sensing in order to address the relative contributions of border faults and intra-rift faults to crustal strain accommodation as rifting progresses. Our study focuses on this transitional phase of continental rifting by exploring the spatial and temporal evolution of faulting in the Natron (border fault initiation at ~3 Ma) and Magadi (~7 Ma) basins of northern Tanzania and southern Kenya, respectively. The timing and nature of the transition from border fault to intra-rift-dominated strain accommodation is unclear.
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As rifting progresses, strain concentrates into the rift center, producing intra-rift faults. In the early stages of continental rifting, East African Rift (EAR) basins are conventionally depicted as asymmetric basins bounded on one side by a ~100 km-long border fault.
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“You’d literally get, say, a hundred finches washed ashore in a 50-yard stretch.The evolving contribution of border faults and intra-rift faults in early-stage East African rifts: insights from the Natron ( Tanzania) and Magadi (Kenya) basins I saw entire flocks of dead birds all washed ashore together, lemming-like,” he says. During dry season, Brandt discovered, when the water recedes, the birds’ desiccated, chemically-preserved carcasses wash up along the coastline. Brandt theorizes that the highly-reflective, chemical dense waters act like a glass door, fooling birds into thinking they’re flying through empty space (not long ago, a helicopter pilot tragically fell victim to the same illusion, and his crashed aircraft was rapidly corroded by the lake’s waters). A swallow © Nick Brandt 2013, Courtesy of Hasted Kraeutler Gallery, NYĪs you might expect, few creatures live in the harsh waters, which can reach 140 degrees Fahreinheit-they’re home to just a single fish species ( Alcolapia latilabris), some algae and a colony of flamingos that feeds on the algae and breeds on the shore.įrequently, though, migrating birds crash into the lake’s surface.
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