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Geography of Loch FyneLoch Fyne is the longest and deepest of Scotlands many sea lochs. It was formed after the last glaciation in Scotland around 10000 years ago when glaciers retreated and rising sea levels flooded the lower reaches of Glen Fyne. Glen Fyne itself is a U-shaped valley which was carved out by a large glacier during the last glaciation. Since Loch Fyne was formed by sea water flooding a U-shaped valley, the loch is characteristically long, narrow and deep and penetrates many miles inland from the open sea. Marine Environment of Loch Fyne
The shorelines of sea lochs are often rocky and steep, providing ideal conditions for kelp forests to grow just below the low tide mark. Kelp forests provide habitat for vast numbers of fish, crustaceans and other marine invertebrates. In other parts the shoreline may be comprised of sediment (sand or mud). These areas are common near the heads of sea lochs or around river mouths and provide habitats for marine worms and other burrowing creatures. These in turn provide food for many shore birds such as curlews, oyster catchers and dunlins which can be seen wading in the shallows as the tide retreats. Fisheries and Aquaculture
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