Geography
This expanse was at the heart of the last significant icefield in the UK during the Loch Lomond Stadial at the end of the last ice age. Once the great mass of ice had melted, the subsequent unburdening of the Earth's crust resulted in a continuing rise in the land which is estimated to be of the order of 2–3 mm per year.
Read more about this topic: Rannoch Moor
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