«We think there were a lot of hot spring environments on Mars,» says Farmer, «and large
lake basins where evaporites may have
formed.
Lorenyang
Lake, a body of water formed during the Pleistocene (1.9 mya), was much longer - lasting than any other lake in the Turkana ba
Lake, a body of water
formed during the Pleistocene (1.9 mya), was much longer - lasting than any other
lake in the Turkana ba
lake in the Turkana
basin.
The effects of the
lake variability may have been enhanced at 1.8 Ma as key geological features that fragment the current lake Basins had yet to form; including the Barrier volcano separating Lake Turkana and the Suguta valley (∼ 1.4 Ma eastern side and ∼ 0.7 Ma western side) and the Emuruangogolak volcano (∼ 1.3 Ma), and Namarunu volcano (0.8 Ma) which separate Lake Baringo and the Suguta Valley [35]--[37], [
lake variability may have been enhanced at 1.8 Ma as key geological features that fragment the current
lake Basins had yet to form; including the Barrier volcano separating Lake Turkana and the Suguta valley (∼ 1.4 Ma eastern side and ∼ 0.7 Ma western side) and the Emuruangogolak volcano (∼ 1.3 Ma), and Namarunu volcano (0.8 Ma) which separate Lake Baringo and the Suguta Valley [35]--[37], [
lake Basins had yet to
form; including the Barrier volcano separating
Lake Turkana and the Suguta valley (∼ 1.4 Ma eastern side and ∼ 0.7 Ma western side) and the Emuruangogolak volcano (∼ 1.3 Ma), and Namarunu volcano (0.8 Ma) which separate Lake Baringo and the Suguta Valley [35]--[37], [
Lake Turkana and the Suguta valley (∼ 1.4 Ma eastern side and ∼ 0.7 Ma western side) and the Emuruangogolak volcano (∼ 1.3 Ma), and Namarunu volcano (0.8 Ma) which separate
Lake Baringo and the Suguta Valley [35]--[37], [
Lake Baringo and the Suguta Valley [35]--[37], [44].