Burn of Monboys

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Burn of Monboys
Southwest flank of Curlethney Hill looking over Burn of Monboys watershed - geograph.org.uk - 532753.jpg
Burn of Monboys watershed looking east
Location
Country Scotland
Physical characteristics
Source 
  location Mounth (Grampian Mountains)
Mouth Cowie Water
  coordinates
57°00′44″N2°09′49″W / 57.01224°N 2.16362°W / 57.01224; -2.16362 Coordinates: 57°00′44″N2°09′49″W / 57.01224°N 2.16362°W / 57.01224; -2.16362

Burn of Monboys is a stream that rises in the Mounth, or eastern range of the Grampian Mountains, northwest of Stonehaven and south of Netherley, Aberdeenshire, Scotland. [1] Monboys Burn is a tributary to the Cowie Water.

Contents

Hydrology

The headwaters of the Burn of Monboys rise on the southern and western slopes of the Meikle Carewe Hill where the stream flows downslope at a first westerly and thence southerly as it makes its way to discharge to the Cowie Water. The southwestern flanks of Craggie Cat, a hill in the northeast part of the Burn of Monboys drainage basin, drain to the Burn of Monboys. The stream has a greenish brown appearance and generally has lush vegetation growing all the way to its margins throughout most of its course of the middle and downstream reaches. The turbidity typically measures approximately 10 JTU and the July flow rate is roughly five cubic feet per second in the headwaters reach. pH levels have been measured at 7.27, very slightly alkaline, but undoubtedly less basic than other area streams due to the drainage from the higher elevation peat moorlands of Meikle Carewe and Curlethney Hills. [2]

History

The Roman Camp Raedykes occupied the higher ground of the headwaters area of Burn of Monboys, and the east flank of Raedykes provides surface runoff to the Burn of Monboys. A number of historical analysts, including the 19th century researcher Gabriel Jaques Surenne and 20th century writers Watt and Hogan, hypothesize that the Battle of Mons Graupius was fought in the Burn of Monboys watershed. [3]

See also

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The Fetteresso Forest is a woodland that is principally coniferous situated in the Mounth range of the Grampian Mountains in Aberdeenshire, Scotland. The forest has a number of prominent mountain peaks including the Hill of Blacklodge and Craiginour peak. A good overlook for viewing the forest from the north side lies on an unnamed tarmack road which leads north from the Slug Road to the Raedykes Roman site. The Cowie Water flows through and drains much of the forest. To the north of the easternmost part of the forest is the archaeological site Raedykes Roman Camp, as well as Cowton Burn. The Slug Road runs along much of the northeast perimeter of Fetteresso Forest.

Megray Hill is a low-lying coastal mountainous landform in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains. The peak elevation of this mountain is 120 metres above mean sea level. This hill has been posited as a likely location for the noted Battle of Mons Graupius between the Romans and the indigenous Caledonians. The major Roman Camp of Raedykes is situated about three kilometres to the west. From Megray Hill there are expansive views to the North Sea facing east. The summit affords scenic views of the historic harbour of Stonehaven.

Saddle Hill (Aberdeenshire)

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Durris Forest

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Cookney Church

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Elsick Mounth

The Elsick Mounth is an ancient trackway crossing the Grampian Mountains in the vicinity of Netherley, Scotland. This trackway was one of the few means of traversing the Grampian Mounth area in prehistoric and medieval times. The highest pass of the route is attained within the Durris Forest. Notable historical structures in the vicinity are Maryculter House, Lairhillock Inn and Muchalls Castle. Most of the lands through which the Elsick Mounth passes are within the Durris Forest; while this forest would have been a mixed deciduous forest in ancient times, currently it is managed as a coniferous monoculture with extensive amounts of clearfelling and subsequent replanting.

Limpet Burn is a watercourse in Aberdeenshire, Scotland whose discharge is deemed part of the North Sea coastal drainage. Prominent geographic features in the vicinity of Limpet Burn are Megray Hill and Kempstone Hill. Notable buildings in proximity to Limpet Burn are Ury House, Muchalls Castle and Chapel of St. Mary and St. Nathalan. Part of the watershed of Limpet Burn has been suggested by some as the site of the first recorded battle in the history of Scotland, the Battle of Mons Graupius.

References

  1. United Kingdom Ordnance Survey Map Landranger 45, Stonehaven and Banchory, 1:50,000 scale, 2004
  2. C.M. Hogan, History of Muchalls Castle, Natural History Section, Lumina Press, Aberdeen (2005)
  3. Archibald Watt, Highways and Byways Round Stonehaven, Gourdas House Publishers, Aberdeen (1984)