The Deveron partakes of the character of the Dee and the character of
the Don. It is neither so sparkling and rapid as the one nor so slow
and muddy as the other. Around Huntly and in the locality of Turriff
and Eden, where it is the boundary between the counties, it has some
charmingly beautiful reaches. Along its banks is a succession of
stately manor-houses, embosomed in trees, and these highly embellished
demesnes enhance its natural charms.
[Illustration: Brig o’ Balgownie, Aberdeen]
Lakes are few in Aberdeenshire, and such as exist are not specially
remarkable. The most interesting historically are the Deeside Lochs
Kinnord and Davan which are held by antiquarians to be the seat of
an ancient city Devana—the town of the two lakes. In pre-historic
times there dwelt on the shores of these lakes as also in the valleys
that converge upon them a tribe of people who built forts, and lake
retreats, made oak canoes, and by means of palisades of the same
material created artificial islands. The canoes which have been
recovered from the bed of the loch are hollowed logs thirty feet in
length. Other relics—a bronze vessel and a bronze spearhead, together
with many beams of oak—have been fished up, all proving the existence
of an early Pictish settlement.
[Illustration: Loch Muick, near Ballater]
Besides these, there is in the same district—but south-east of
Loch-na-gar, another and larger lake called Loch Muick. From it flows
the small river Muick—a tributary of the Dee, which it joins above
Ballater. South-west of Loch-na-gar is Loch Callater, which drains
into the Clunie, another Dee tributary, which joins the main river at
Castleton of Braemar. On the lower reaches of the Dee are the Loch of
Park or Drum, and the Loch of Skene, both of which drain into the Dee.
Both are much frequented by water-fowl of various kinds.
The Loch of Strathbeg, which lies on the east coast not far from
Rattray Head, is a brackish loch of some interest. Two hundred years
ago, we are told, it was in direct communication with the sea and small
vessels were able to enter it. In a single night a furious easterly
gale blew away a sand-hill between the Castle-hill of Rattray and the
sea, with the result that the wind-driven sand formed a sand-bar where
formerly there was a clear
[Illustration: Loch Callater, Braemar]
water-way. Since that day the loch has been land-locked and though
still slightly brackish may be regarded as an inland loch.
6. Geology.
Public-domain text, read in full here on John Shaqi.
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