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Crynoch Burn : ウィキペディア英語版
Crynoch Burn
Crynoch Burn is a stream in Aberdeenshire that is tributary to the River Dee.〔United Kingdom Ordnance Survey Map Landranger 45, Stonehaven and Banchory, 1:50,000 scale, 2004〕 This stream rises somewhat above Netherley and flows near Netherley House; and thence into the Red Moss, a significant natural bog habitat; thence near the historic Lairhillock Inn; and finally by the village of Maryculter and through Oldman Wood before discharge to the Dee. Headwaters areas include the northern and western slopes of Meikle Carewe Hill and the northern slopes of Curlethney Hill.
The soils near its mouth at the River Dee are light and sandy,〔(Historic profile of the village of Maryculter )〕 and the pH level of these greenish brown waters is approximately 8.05, or slightly alkaline
==References==

* John A. Henderson (1892) ''Annals of Lower Deeside: Being a Topographical, Proprietary, Ecclesiastical, and Antiquarian History of Durris, Drumoak, and Culter'', D. Wyllie and Son, 271 pages

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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