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(2)
(1)
Figure 7.8. ( Continued ) (B) Observed at Crumbling Point, Pleistocene Mackenzie Delta, Canada. (1) Large sand wedge penetrates a sand and diamicton
cryofacies assemblage that overlies a layered cryofacies assemblage consisting of massive icy beds. The person in the photo is
1.8 m. (2) The generalized
cryofacies log and
O 18 profi le obtained from both cryofacies assemblages. At the contact of the two cryofacies assemblages is an isotopic (thaw?) discon-
tinuity. SMOW is standard mean ocean water. See Table 7.4 for explanation of cryofacies types indicated. From Murton and French (1994).
δ
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