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Table 2.4. Sedimentary provinces and associated benthic landscapes of Georges Bank.(Provinces as defined by Valentine et al. (1993) and Valentine and Lough (1991) with additional information from Page C. Valentine (pers. comm., U.S. Geological Survey, Woods Hole, MA).Benthic assemblages as assigned by Theroux and Grosslein (1987).See text for further discussion on benthic assemblages.)

Sedimentary Province
(province no.)
Depth Range (m) Description Benthic Assemblage
Northern Edge / Northeast Peak (1) 40-200 Dominated by gravel with portions of sand, common boulder areas, and tightly packed pebbles; bryozoa, hydrozoa, anemones, and calcareous worm tubes are abundant in areas of boulders; strong tidal and storm currents Northeast Peak
Northern Slope and Northeast Channel (2) 200-240 Variable sediment type (gravel, gravel-sand, and sand) and scattered bedforms; this is a transition zone between the northern edge and southern slope; strong tidal and storm currents Northeast Peak
North /Central Shelf (3) 60-120 Highly variable sediment types (ranging from gravel to sand) with rippled sand, large bedforms, and patchy gravel lag deposits; minimal epifauna on gravel due to sand movement; epifauna in sand areas includes amphipods, sand dollars, and burrowing anemones Central Georges
Central and Southwestern Shelf - shoal ridges (4) 10-80 Dominated by sand (fine and medium grain) with large sand ridges, dunes, waves, and ripples; small bedforms in southern part; minimal epifauna on gravel due to sand movement; epifauna in sand areas includes amphipods, sand dollars, and burrowing anemones Central Georges
Central and Southwestern Shelf - shoal troughs (5) 40-60 Gravel (including gravel lag) and gravel-sand between large sand ridges; patchy large bedforms, strong currents; minimal epifauna on gravel due to sand movement; epifauna in sand areas includes amphipods, sand dollars, and burrowing anemones Central Georges
Southeastern Shelf (6) 80-200 Rippled gravel-sand (medium- and fine-grained sand) with patchy large bedforms and gravel lag; weaker currents; ripples are formed by intermittent storm currents;epifauna includes sponges attached to shell fragments and amphipods Southern Georges
Southeastern Slope (7) 400-2000 Dominated by silt and clay with portions of sand (medium and fine), with rippled sand on shallow slopes and smooth silt-sand deeper None

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(Modified Jun. 13 2008)