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Grain-size analyses were performed on 61 samples from the Niantic Bay vicinity in eastern Long Island Sound. The relative grain-size frequency distributions and related statistics are reported herein. Descriptions of the benthic character from video tapes and still camera photographs of the bottom at these stations, and 8 others, are also presented. Gravelly sands, gravels, and boulders dominate the surficial sediments across the southern part of the study area and in the channel between Twotree Island and White Point. These coarsegrained sediments tend to be replaced by progressively finergrained sediments toward areas that are more protected from the strong tidal currents and toward the central part of Niantic Bay where sandy silts are common. These textural distributions are a result of the late Pleistocene glaciation, the Holocene eustatic rise in sea level, and the present day tidal regime.

The texture of surficial sediments in eastern Long Island Sound near Niantic Bay, Connecticut