Geology Page reported on a new theory that Denver's mile-high elevation is a result of a flood below.
Excerpt:
No one really knows how the High Plains got so high. About 70 million years ago, eastern Colorado, southeastern Wyoming, western Kansas and western Nebraska were near sea level. Since then, the region has risen about 2 kilometers, leading to some head scratching at geology conferences.
Now researchers at the Cooperative Institute for Research in Environmental Sciences (CIRES) and the Department of Geological Sciences at the University of Colorado Boulder have proposed a new way to explain the uplift: Water trapped deep below Earth's crust may have flooded the lower crust, creating buoyancy and lift. The research appears online this week in the journal
Geology and could represent a new mechanism for elevating broad regions of continental crust.
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