ISS002 Earth Sciences Results Briefing
February 14, 2002

EAST AFRICAN RIFT
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View larger image for ISS002-715-5
ISS002-715-5
Straight-shored lakes of the Ethiopian rift segment of the East African rift system reflect control of the shorelines by faults; the lake bottoms have been dropped down tens to hundreds of feet. Ziway is the large lake to the NE, Abiyatta and Shala are in the SW, and Abaiuta is to the SE in this view. Lake Shala is the southwesternmost; Abiyata and Langano are the central pair; and Ziway is the larger northeastern one.
View larger image for ISS002-723-8
ISS002-723-8
This is the first-ever, near-nadir photo of the junction of the Lake Tanganyika rift valley and the Lake Rukwa transform fault valley. Lake Tanganyika changes trend from due N to NW, where faults of the transform system begin to interact.
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ISS002-717-83
Detailed near-nadir shots such as this one of NW Lake Rukwa provide fundamental data for mapping interfering faults in remote and commonly cloud-covered regions. Colleagues at British Petroleum and at the Applied Geodynamics Laboratory (UT-Austin) are already using these data in their investigations of the Western Branch of the East African rift. Faults of several trends and senses of displacement are shown in the following view; hachures are on the downdropped sides of fault lines.
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ISS002-717-81
Another first - details of volcanic vents of the Rungwe volcanic field and faults at the SW end of Lake Rukwa can be examined in this fine telephoto view of the junction of the Lake Rukwa transform fault zone with the Lake Malawi rift valley.
View larger image for ISS002-717-84
ISS002-717-84
Volcanic fields at rift-transform intersections are places where economic deposits of minerals are commonly localized. The gold mines of the Chunya district, the regular light patches around the Mbeya Range, have yielded between 2 and 8 million ounces of gold as of March 2001.
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