🌍 Is Africa really splitting in two?
Yes — at a few millimetres a year, unevenly, and mostly without shaking. In September 2005 a 60 km stretch of Afar opened by eight metres, and earthquakes accounted for only about 8% of it. Follow the fault blocks, the GPS arrows and the la
What you’ll learn
- A Valley Made by StretchingRecognize how extension and normal faulting build rift valleys, and why the rift branches.The visible valley is the surface expression of a broad, uneven plate-boundary process.
- Where Plates Begin to SeparateExplain why Afar, uneven volcanism and dike intrusion reveal different stages of continental breakup.Thinning crust, magma and a three-way junction make the northern rift unusually revealing — and much of the opening happens without shaking.
- Lakes, Quakes, and Living BasinsConnect rifting to lake basins, earthquake patterns, habitats and human environments.Lowered basins and active faults create archives and living landscapes, not just dramatic scenery.
- The Continent's Possible FutureWeigh multiple lines of evidence to judge what the rift's long-term future can and cannot tell us.A new ocean is a geological possibility measured in millions of years, supported by clues that are only strong together.
Questions this course answers
What makes the Great Rift Valley a rift system rather than one simple crack?
The Eastern and Western branches wrap around the Victoria basin and differ in age, speed and volcanism.
What does a normal fault do in stretching crust?
Extension makes room and gravity fills it, dropping blocks to form grabens and half-grabens.
In the 2005 Dabbahu episode, roughly how much of the measured opening did earthquakes account for?
The segment opened by up to 8 m, but seismic rupture explained only about 8% of the deformation seen from orbit.
Why are rift lakes useful geological evidence?
Lakes such as Turkana and Tanganyika sit in fault-bounded basins whose sediments record the basin's history.
What is the careful version of 'Africa is tearing in half'?
Breakup is a possible long-term outcome, and rifts can also slow, jump, branch or fail before an ocean forms.
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