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Sediment physical and geotechnical properties from Ocean Drilling Program Leg 146 Sites 891 and 892 on the Cascadia Margin are presented. The data are interpreted in terms of stress history, permeability, and excess pore-fluid pressures. The results show two different patterns of sediment stress history: underconsolidation and normal consolidation. Normal consolidation occurs in the upper sediment units at both sites. Underconsolidation occurs at both sites within sediment units that have been loaded by overthrusted sediment. Test results from the underconsolidated units are further interpreted in terms of excess fluid pressures.

Permeability and Stress History of Sediment from the Cascadia Margin