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Principal Results: Site 383 was drilled a total of 120.3 me¬ ters into the Sohm Abyssal Plain above the buried JAnomaly Ridge (Figures 1, 2). Deteriorating hole condi¬ tions and the risk of losing the bottom-hole assembly in the caving sands forced abandonment. The single core recov¬ ered (53.7-63.3 m) contains 4.9 meters of graded Pleisto¬ cene sand; the grading is undoubtedly an artifact produced by flushing of sand into the core barrel during a break in circulation. A second coring attempt (110.8-120.3 m), which yielded an empty core barrel, probably penetrated similar coarse sands. The coarse turbiditic sands are prob¬ ably derived from the Laurentian Channel.

Site 383: Drilling above the J-Anomaly Ridge in the Sohm Abyssal Plain