You are standing near the top of the cliff (blue arrow), looking in the direction of the green arrow.
An angular unconformity is visible between the underlying folded sediments and the overlying flat-lying sediments. Fossil bivalve shells can be found as float on the surface here.
Look closer at the flat lying sediments.
Look closer at the deformed sediments.
From here you can:
Climb up to the top of the cliff.
Climb down to the entrance of the gully.
Climb down into the gully.
Cross the gully and look at deformed sediments lower down on other side
Sources: The chief reference on the stratigraphy of the Gubik is (Brigham,1985). The best reference on the fossil molluscs from the Gubik is still (MacNeil, 1957). Recent papers on the age and climate history of these deposits include (Brigham-Grette and Carter, 1992; Kaufman and Brigham-Grette, 1993 Brigham-Grette and Hopkins, 1995).
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Written by Paul J. Morris email@example.com
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Date Created: 20 April 1998
Last Updated: 22 Jan 2000