May Craig is a rocky island situated along the North Sea coast of Aberdeenshire, Scotland. [1] May Craig lies about one half mile (0.8 km) south of Newtonhill and a mile (1.6 km) northeast of the village of Muchalls. A small islet of the same name lies three miles (five km) to the north-northeast.
The North Sea is a marginal sea of the Atlantic Ocean located between Great Britain, Denmark, Norway, Germany, the Netherlands, Belgium and France. An epeiric sea on the European continental shelf, it connects to the ocean through the English Channel in the south and the Norwegian Sea in the north. It is more than 970 kilometres (600 mi) long and 580 kilometres (360 mi) wide, with an area of 570,000 square kilometres (220,000 sq mi).
Aberdeenshire is one of the 32 council areas of Scotland.
Scotland is a country that is part of the United Kingdom. It covers the northern third of the island of Great Britain, with a border with England to the southeast, and is surrounded by the Atlantic Ocean to the north and west, the North Sea to the northeast, the Irish Sea to the south, and more than 790 islands, including the Northern Isles and the Hebrides.
The area to the west of May Craig was first inhabited by Pictish peoples who left prehistoric megalithic monuments along a trackway known as the Causey Mounth, a name coined in medieval times. Examples of these megaliths are Old Bourtreebush stone circle and Aquhorthies stone circle. [2] Historic structures in the general area include Elsick House, Gillybrands and Muchalls Castle. [3]
A megalith is a large stone that has been used to construct a structure or monument, either alone or together with other stones. The word megalithic describes structures made of such large stones without the use of mortar or concrete, representing periods of prehistory characterised by such constructions. For later periods, the word monolith, with an overlapping meaning, is more likely to be used.
The Causey Mounth is an ancient drovers' road over the coastal fringe of the Grampian Mountains in Aberdeenshire, Scotland. This route was developed as the main highway between Stonehaven and Aberdeen around the 12th century AD and it continued to function as the principal route connecting these two cities until the mid 20th century, when modern highway construction of the A90 road occurred in this area. There are extant paved and usable sections of this road over part of the alignment; however, many parts of the ancient route are no more than footpaths, and in some cases the road has vanished into agricultural fields. Constructed in the Middle Ages, the Causey Mounth was created as an elevated rock causeway to span many of the boggy areas such as the Portlethen Moss. A considerable portion of the alignment of the Causey Mounth is illustrated on the UK Ordnance Survey Map, although a large fraction of the route cannot be navigated by a conventional passenger vehicle.
A stone circle is a circular alignment of standing stones. They are commonly found across Northern Europe and Great Britain and typically date from the Late Neolithic and Early Bronze Age eras, with most concentrations appearing from 3000 BC. The best known examples include those at the henge monument at Avebury, the Rollright Stones and elements within the ring of standing stones at Stonehenge. Ancient stone circles appear throughout Europe with many appearing in the Pyrenees, on the Causse de Blandas in southern France in the Cevennes, in the Alps, and Bulgaria.
Coordinates: 57°1′29.56″N2°8′50.68″W / 57.0248778°N 2.1474111°W
A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.
Kincardine and Mearns is one of six area committees of the Aberdeenshire council area in Scotland. It has a population 38,506. There are significant natural features in this district including rivers, forests, mountains and bogs.
Findon or Finnan is a fishing village eight miles south of Aberdeen, famous for originating the smoked haddock known as Finnan haddie. The Findon moor has a number of paths through it, many of which run along the cliffs. Deer can often be seen there. Nearby features include the Portlethen Moss Nature Reserve.
Portlethen Village is a settlement along the North Sea coast in Aberdeenshire, Scotland. The village is also known as Old Portlethen. The skerry of Craigmaroinn is situated just off the coastline near Portlethen Village.
Downies is a cliff-top village in Aberdeenshire, Scotland situated on Cammachmore Bay. Historically Downies was a fishing village, until much of the local North Sea fishery collapsed from overfishing; presently Downies is chiefly a residential dormitory adjunct to the city of Aberdeen.
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.
The Burn of Elsick is a coastal stream in Aberdeenshire, Scotland that discharges to the North Sea. This watercourse drains primarily agricultural lands and enters the North Sea at Newtonhill.
The Burn of Pheppie is an easterly flowing coastal stream in Aberdeenshire, Scotland that discharges to the North Sea immediately north of the village of Muchalls. Draining chiefly agricultural lands, this stream has a notable lack of turbidity and a pH level of approximately 8.02. Armouring of the stream bottom consists of pebbles, many of which are quartzite in composition, leading to a golden-green effect in some locations. Other nearby watercourses discharging to the North Sea include Burn of Elsick to the north and Burn of Muchalls to the south.
Elsick House is an historic house in Kincardineshire, northeast Scotland.
Cammachmore is a hamlet in the coastal region near the North Sea in Aberdeenshire. It lies slightly west of the A90 road and the ancient Causey Mounth passes through the community. Historic Elsick House is situated due west of Cammachmore. Other nearby historic features include Gillybrands, Saint Ternan's Church, Muchalls Castle and the Lairhillock Inn.
Cookney is a hamlet in Aberdeenshire, Scotland in proximity to Netherley in the Mounth of the Grampian Highlands. The community is situated on a hilltop approximately 5 miles (8 km) northwest of Stonehaven, about 3 miles (5 km) northwest of the Bridge of Muchalls, and about 2 miles (3 km) west of Muchalls Castle. From Cookney a portion of the ancient route of the Causey Mounth is visible to the east near Whinward Farm, although the track is not truly recognizable from that distance. The Cookney Church is a prominent historic landmark of Cookney.
Banchory-Devenick is a village approximately two kilometres south of the city of Aberdeen, Scotland in the Lower Deeside area of Aberdeenshire. The village should not be confused with the historic civil parish of the same name which spanned the River Dee until 1891, its northern part lying in Aberdeenshire and its southern part in Kincardineshire. In that year the northern part became part of the neighbouring parish of Peterculter, the southern part remaining as the parish of Banchory-Devenick. The village of Banchory-Devenick lies slightly west of the A90 road, and the ancient Causey Mounth passes directly through the village. An historic graveyard dating to 1157 AD is present at the village of Banchory-Devenick. Other historic features in the vicinity include Saint Ternan's Church, Muchalls Castle and the Lairhillock Inn.
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.
Cookney Parish Church, now business premises within a converted listed building, was a Christian place of worship in the village of Cookney, Aberdeenshire, Scotland.
Cammachmore Bay is an embayment of the North Sea between Stonehaven and Aberdeen in Aberdeenshire, Scotland. The fishing village of Downies is situated on Cammachmore Bay. Cammachmore is noted for its bouldering and rock climbing opportunities.
Craigmaroinn is a skerry in the North Sea near the Aberdeenshire coastline in Scotland. Craigmaroinn is situated midway between the coastal villages of Portlethen Village and Downies. Historical points of interest in the local area are Elsick House, Gillybrands and Muchalls Castle.
Auld Bourtreebush is a prehistoric stone circle in Aberdeenshire, Scotland. This megalithic construction is situated near the Causey Mounth ancient trackway, which connects the Scottish lowlands to the highlands.
The Brown Jewel is a sea stack on the North Sea coast of Scotland, north of the village of Muchalls in Aberdeenshire.
Hare Ness is a headland landform along the North Sea coastline a few miles south of Aberdeen, Scotland.
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.
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