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A second constraint on the timescale of canyon filling relates to the cyclic stratigraphy documented at the Umberatana syncline example.
These rocks are generally divided into two major types in view of their lithology, internal stratigraphy and contact relationships with surrounding rocks.
The up-to-date stratigraphy and earlier radiometric dates on these and other Late Precambrian rocks of this area are given in Pharaoh & Gibbons.
The late Mesozoic and Cenozoic stratigraphy of northern Chile is shown in Figure 3.
Despite his expanding interest in biological questions, Weller remained a strong proponent of stratigraphy and practical geology, both in the classroom and in research.
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