Sub-Area K: Eastern Deep Port Sample Clauses

Sub-Area K: Eastern Deep Port. The majority of the sediment flushed out of rivers during the summer runoff period settles in this end of the Port and has formed a large, underwater sediment shelf. Frequent seismic activity causes additional sediment disturbance along the slopes of this sediment shelf. Subsurface currents tend to be weak and nondirectional, increasing the potential for stagnation at the eastern end (City of Xxxxxx, 1992). Currents at the water surface move in a counterclockwise direction. The benthic community living on and within the soft sediments here is similar to that of the western Port. However, the increased sediment deposition results in reduced numbers of suspension feeding organisms.
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