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Sedimentary structures and grain-size spectra of drift sediments from Deep Sea Drilling Project Sites 610 and 611 are described. On the basis of structures, three facies are identified independent of lithology: homogeneous to burrowmottled sediment, partly bioturbated thin-bedded sediment, and laminated sediment. The homogeneous and bioturbated sediment facies predominate. Size spectra are controlled principally by the foraminifer and nannofossil contents of the samples. There is little evidence of current control of deposition, but more detailed analysis of vertical or lateral changes in size or compositional parameters might provide better direct evidence of current activity.

Characteristics of Sediments from Feni and Gardar Drifts, Sites 610 and 611, Deep Sea Drilling Project Leg 94