Olaka dating

Here, the rift is expressed only in the northern part, splaying out in diverging half-graben valleys that are outside the Kenya Dome.

Large boundary faults and opposing flexural margins, producing mobile asymmetrical full and half-graben basins that are individually linked along the rift axis, mark the Western Rift Valley.

Plaka is built on top of the residential areas of the ancient town of Athens.

It is known as the "Neighborhood of the Gods" due to its proximity to the Acropolis and its many archaeological sites.

In Ethiopia, the Afar Depression, the Main Ethiopian Rift, and the broadly rifted zone of southwestern Ethiopia represent the northern segment of the EARS.

In the Kenyan sector of the EARS, uplift and doming also gave rise to the Kenya Dome.

During the years of Ottoman rule, Plaka was the known as the "Turkish quarter of Athens", and the seat of the Turkish Voevode (Governor).

During the Greek War of Independence, Plaka like the rest of Athens, was temporarily abandoned by its inhabitants because of the severe battles that took place in 1826.

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Excavations have been taking place continuously since the 19th century.Plaka is visited by hundreds of thousands of tourists around the year, and is under strict zoning and conservation regulations, as the only neighborhood in Athens where all utilities (water, power, cable television, telephone, internet, and sewage) lie underground in fully accessible, custom-made tunneling.Museums in Plaka include the new Acropolis Museum, the new Jewish Museum of Greece, the Museum of Greek Folk Art, an annex of which is the Old Public Baths building, the Frissiras Museum, the Museum of Popular Music Instruments, the Museum of Pavlos and Alexandra Kanellopoulou and the Athens University Museum.The East African Rift System (EARS) started in Late Oligocene to Early Miocene time and gradually propagated southwards from the Afar Depression, beginning in the Middle Miocene.The hot, low-density mantle material of the Afar Plume heated the overlying lithosphere, causing thinning, regional doming, and the earliest basaltic volcanism in southern Ethiopia.

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