Start Of The Linn Of Dee.

At Linn of Dee the river passes through a 300 metre natural rock gorge. Between there and Braemar, Lui Water (formed by Luibeg and Derry Burns) and Quoich Water join the growing River Dee. Clunie Water and Callater Burn join together and flow into the Dee at Braemar.
The River Dee rises at approximately 4,000 feet in elevation on the plateau of Braeriach, the highest source of any major river in the British Isles. Water emerges in a number of pools and flows across the plateau to the cliff edge, then plunges into An Garbh Choire. The young Dee joins a tributary from the Pools of Dee in the Lairig Ghru and passes between Ben Macdui and Cairn Toul. It flows over falls in the Chest of Dee on its way to White Bridge, the confluence of the Geldie Burn.
In Scotland and northern England a Linn is a geographical water feature.
In Scotland it describes where a watercourse has cut through a shelf of hard rock creating a narrow (usually), steep-sided cut though which the watercourse runs.
A linn may also refer to a waterfall or a pool at the foot of a waterfall, with the derivation a confusion of Scots Gaelic linne (pool) and Old English hlynn (torrent).

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