Limpet Burn

Limpet Mill was a railway station in Kincardineshire, Scotland from 1849 to 1850 on the Aberdeen Railway.

Bridge of Muchalls is an entirely residential hamlet in Aberdeenshire, Scotland by the North Sea. It is on the A90 dual carriageway about three miles north of Stonehaven and to the south of Muchalls Castle. This small hamlet is known for its picturesque access to the rugged North Sea coastline at Muchalls Beach. The Burn of Muchalls is a stream that flows east through the Bridge of Muchalls before passing under the A90 roadway and thence to the North Sea slightly to the north of Doonie Point. The ancient Causey Mounth trackway runs north from the now ruin Cowie Castle, past the Hill of Megray and passes over Kempstone Hill before crossing the Burn of Muchalls at the Bridge of Muchalls.

The Chapel of St. Mary and St. Nathalan is a ruined chapel overlooking the North Sea immediately north of Stonehaven, in the Mearns of Scotland, along the northern shoreline of Stonehaven Bay. (Watt, 1985) The founding of this Christian place of worship is associated with St. Nathalan. who lived circa 650 AD. The structure is alternatively known as Cowie Chapel. The chapel is at the point where the Highland Boundary Fault meets the sea and so is on the dividing line between the highlands and lowlands of Scotland.

Kempstone Hill is a landform in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains. The peak elevation of this mountain is 132 metres above mean sea level. This hill has been posited by Gabriel Jacques Surenne, Archibald Watt and C.Michael Hogan as the 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 Kempstone Hill there are fine views to the North Sea facing east and slightly to the north of Muchalls Castle. There is a UK trigpoint installation on Kempstone Hill.

Cowie Castle is a ruined fortress in Aberdeenshire, Scotland. The site lies at the northern end of Stonehaven on the North Sea coast. To the immediate south is the Cowie Bridge crossing of the Cowie Water. Evidence of prehistoric man exists in the vicinity dating to the Iron Age in the form of ring cairns.

The Mill of Muchalls is an historic water-powered mill located along the Burn of Muchalls in Aberdeenshire, Scotland. This mill is situated near to the coast of the North Sea proximate to Doonie Point. The earliest position of the village of Muchalls lay slightly to the south of the Mill of Muchalls. The Mill of Muchalls is situated slightly to the east of the ancient Causey Mounth trackway, a drovers' road established at least as early as the High Middle Ages.

Doonie Point is a rocky headland situated approximately 1.5 kilometres south of the village of Muchalls in Aberdeenshire, Scotland. The clifftop of Doonie Point yields views to the north of Grim Brigs, Brown Jewel and the coast of Newtonhill. To the south are views of the Castle Rock of Muchalls and the rugged North Sea coastline toward Stonehaven. Notable historic structures in the vicinity of Doonie Point are the Chapel of St. Mary and St. Nathalan, Muchalls Castle and the Mill of Muchalls. This site is a recognised rock climbing venue. Doonie Point is catalogued within the marine rescue activities for this part of the coast of northeast Scotland.

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.

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. Monboys Burn is a tributary to the Cowie Water.

Muchalls Castle stands overlooking the North Sea in the countryside of Kincardine and Mearns, Aberdeenshire, Scotland. The lower course is a well-preserved Romanesque, double-groined 13th-century tower house structure, built by the Frasers of Muchalls. Upon this structure, the 17th-century castle was begun by Alexander Burnett of Leys and completed by his son, Sir Thomas Burnett, 1st Baronet, in 1627. The Burnetts of Leys built the remaining four-storey present-day castle. One of the most interesting castles of North-East Scotland, according to noted architectural historian Nigel Tranter, it is designed in the classic L style with a further extension wing at the west end. Muchalls Castle entered national history in 1638 when a seminal Covenanter gathering took place there precedent to the English Civil War. The plasterwork ceilings of the principal drawing rooms are generally regarded as among the three finest examples of plasterwork ceilings in Scotland. These adornments date to 1624 and are in virtually perfect condition. They consist of heraldry of the Burnett of Leys family, along with heraldry of relations and friends intermixed with biblical iconography. The overmantel of the Great Hall fireplace features the arms of King James VI flanked by impressive egyptianesque figures.

The Burn of Muchalls is an easterly flowing stream in Aberdeenshire, Scotland that discharges to the North Sea. Its point of discharge is on a rocky beach set with scenic sea stacks. Flowing principally over agricultural lands, the Burn of Muchalls traverses through the hamlet of the Bridge of Muchalls, flows beneath the A90 road and thence to the rugged shoreline of the North Sea slightly to the south of Doonie Point. Just above the discharge to the North Sea is a scenic pool, used in the drowning scene of Ophelia in the Franco Zeffirelli film Hamlet. A northern fork of the Burn of Muchalls flows over lands of Muchalls Castle prior to the confluence with the mainstem Burn of Muchalls within the Bridge of Muchalls.

Grim Brigs (Grid reference NO9091) is a rocky headland on the North Sea at Muchalls, Scotland. Notable historic features in this vicinity include St. Ternan's Church, Muchalls Castle and Elsick House. Approximately one kilometre inland is the noted medieval drovers' road known as the Causey Mounth. The geology of Grim Brigs is associated with the harder rock formations north of the Highland Boundary Fault, which forms the boundary between the Scottish Highlands and Lowlands. This Highland Boundary Fault emerges at the North Sea approximately four kilometres south of Grim Brigs near the Chapel of St. Mary and St. Nathalan.