Crynoch Burn
Encyclopedia
Crynoch Burn is a stream
in Aberdeenshire
that is tributary
to the River Dee
. 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, and the pH
level of these greenish brown waters is approximately 8.05, or slightly alkaline
. Classified in the Strahler Stream Order
system the Crynoch Burn is a second order stream.
Stream
A stream is a body of water with a current, confined within a bed and stream banks. Depending on its locale or certain characteristics, a stream may be referred to as a branch, brook, beck, burn, creek, "crick", gill , kill, lick, rill, river, syke, bayou, rivulet, streamage, wash, run or...
in Aberdeenshire
Aberdeenshire
Aberdeenshire is one of the 32 unitary council areas in Scotland and a lieutenancy area.The present day Aberdeenshire council area does not include the City of Aberdeen, now a separate council area, from which its name derives. Together, the modern council area and the city formed historic...
that is tributary
Tributary
A tributary or affluent is a stream or river that flows into a main stem river or a lake. A tributary does not flow directly into a sea or ocean...
to the River Dee
River Dee, Aberdeenshire
The River Dee is a river in Aberdeenshire, Scotland. It rises in the Cairngorms and flows through Strathdee to reach the North Sea at Aberdeen...
. This stream rises somewhat above Netherley
Netherley, Aberdeenshire
Netherley, Scotland is a village in Aberdeenshire, situated approximately five miles northwest of Stonehaven. Netherley is located in the Mounth area of the Grampian Highlands. At the western edge of Netherley is a significant wetland bog known as Red Moss. To the southwest of Netherley lie...
and flows near Netherley House
Netherley House
Netherley House is a mansion built by Alexander Silver in the late 18th century in Netherley, Aberdeenshire, Scotland. It is situated near the northerly flowing drainage of Crynoch Burn . The home was sold to Horatio Ross by James Silver, son of George Silver in 1853 for 33,000 pounds sterling....
; and thence into the Red Moss
Red Moss, Aberdeenshire
Red Moss is a wetland bog in Aberdeenshire, Scotland, located at the northwestern edge of the village of Netherley. The moss is designated a national Site of Special Scientific Interest by Scottish Natural Heritage, due to its biodiversity and undisturbed character. The elevation of Red Moss is...
, a significant natural bog
Bog
A bog, quagmire or mire is a wetland that accumulates acidic peat, a deposit of dead plant material—often mosses or, in Arctic climates, lichens....
habitat
Habitat
* Habitat , a place where a species lives and grows*Human habitat, a place where humans live, work or play** Space habitat, a space station intended as a permanent settlement...
; thence near the historic Lairhillock Inn
Lairhillock Inn
The Lairhillock Inn is an historic coaching inn along an old carriage route approximately four miles north of Netherley, Aberdeenshire, Scotland. In 2007 a new primary school opened across the road named Lairhillock Primary School, which replaced the old Netherley School and Maryculter School and...
; and finally by the village of Maryculter
Maryculter
Maryculter or Kirkton of Maryculter is a village in the Lower Deeside area of Aberdeenshire, Scotland. The River Dee separates it from the town of Peterculter, and the B979 road runs through Maryculter. There are two hotels: The Old Mill Inn, a former coaching inn that dates back 200 years, and...
and through Oldman Wood
Oldman Wood
Oldman Wood is a publicly owned forest in Kincardineshire, Scotland.Crynoch Burn, a tributary of the River Dee, flows through the Oldman Wood.-References:...
before discharge to the Dee. Headwaters areas include the northern and western slopes of Meikle Carewe Hill
Meikle Carewe Hill
Meikle Carewe Hill is a landform in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains. The peak elevation of this mountain is 266 metres above mean sea level...
and the northern slopes of Curlethney Hill
Curlethney Hill
Curlethney Hill is a landform in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains. The peak elevation of this mountain is 246 metres above mean sea level. This landform lies slightly southwest of the village of Netherley...
.
The soils near its mouth
River delta
A delta is a landform that is formed at the mouth of a river where that river flows into an ocean, sea, estuary, lake, reservoir, flat arid area, or another river. Deltas are formed from the deposition of the sediment carried by the river as the flow leaves the mouth of the river...
at the River Dee are light and sandy, and the pH
PH
In chemistry, pH is a measure of the acidity or basicity of an aqueous solution. Pure water is said to be neutral, with a pH close to 7.0 at . Solutions with a pH less than 7 are said to be acidic and solutions with a pH greater than 7 are basic or alkaline...
level of these greenish brown waters is approximately 8.05, or slightly alkaline
Hydrology
Tributaries to the Crynoch Burn include the Cairnie BurnCairnie Burn
Cairnie Burn is a stream that rises in the Mounth, or eastern range of the Grampian Mountains, north of Netherley, Aberdeenshire, Scotland. Cairnie Burn is a generally northeast flowing watercourse that is a tributary to the Crynoch Burn...
. Classified in the Strahler Stream Order
Strahler Stream Order
In mathematics, the Strahler number or Horton–Strahler number of a mathematical tree is a numerical measure of its branching complexity....
system the Crynoch Burn is a second order stream.