The lagoon is connected to the Bay of Isbister via narrow channel through a shigle spit. The lagoon is 0.4 km long, has a maximum depth of 0.4 m and a tidal range about 0.5m. The salinity range was estimated to be between 5‰ and 18‰. There is substantial freshwater input from a stream which enters at the north-western corner. There is a very little disturbance from tidal currents and wave action. The lagoon is surrouned by saltmarsh and backed by pasture land.The main body of the lagoon, between 0 and 0.4 m depth, consisted of sandly gravel overlain by a layer of fine sand.
The sediment was dominated by the green alga Enteromorpha intestinalis with a few small areas of the tasselweed Ruppia sp. And the brackish-water wrak Fucus ceranoides. There were burrows of the amphipod Corophium volutator in the sediment and the mud snail Hydrobia ulvae was present on the surface of the mud.
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