Dumyat
Encyclopedia
Dumyat is a hill at the western extremity of the Ochil Hills
in central Scotland
. The name is thought to originate from Dun (hill fort) of the Maeatae
.
Although relatively small (its height is 418 metres), the characteristic shape of the hill forms an important part of the distinctive scenery of the Stirling
area, and it is often depicted (particularly in postcards and calendars) in combination with the nearby Abbey Craig
. The hill is a popular climb with tourists and visitors to the Stirling and Trossachs
area, due to the historical nature of Stirling and the proximity of the Wallace Monument
.
Dumyat has two principal summits: Castle Law on the west, and Dumyat proper on the east. On the summit of Castle Law the remains of an ancient hill fort
, originally occupied by the Maeatae, are still clearly discernible.
At one time the favourite route to the summit of either Dumyat or Castle Law was via the prominent gulley which runs almost straight up the southern scarp face, and continues down the gently sloping north face. This gulley was formed by the erosion of a fault
, resulting from the juxtaposition of soft pyroclastic rocks on one side against harder andesite
and basalt
on the other. This has resulted in an area where hard andesite
slightly overhangs, and is the darkest and least exposed part of the climb, which is not particularly difficult. Further gullies, formed by secondary tearing around the main fault (itself a product of the major disturbance which resulted from the Ochil Fault
) extend to the right into Dumyat, and form potential shortcuts to the summit. The first of these, Raeburn's Gulley, is particularly dangerous and should only be attempted by experienced and properly equipped rock climbers, however the second, Siart Gulley, is climbable by anyone of average ability, if care is taken in scrambling up the steep step at the end. The third, fourth and fifth gullies are not named, and become progressively easier.
Nowadays many people park their cars on Sheriffmuir
and take a longer but more gently sloping path to the summit, passing behind, i.e. slightly to the north of, the summit of Castle Law. The third route is via Menstrie Glen
from the east, and is a somewhat gentle ascent in the beginning, which steepens satisfactorily for those who like a decent climb, as the summit is approached.
The exposed terrain of Dumyat and the surrounding muir are suitable only for sheep farming, with several sheep folds dotting the hill's sides, along with the ruins of a shepherd's stone house. Dumyat was formerly the site of small-scale mining for copper
and barytes, although these workings are now abandoned.
The scree
on the scarp face of Castle Law is a source of agate
s, not necessarily of the finest quality, but occasionally other specimens such as smoky quartz
and citrine can be found, along with the inevitable quartz
, calcite
, barytes, and two ores of copper, malachite
, and less commonly, azurite
.
At the top is a memorial to the Argyll and Sutherland Highlanders
, a trig point
, and a characteristic cairn
with a beacon on top that is currently filled with stones.
The stones which are placed in the beacon are all wishes that have been made by others.
The beacon on the top of Dumyat was commissioned for the Queen's Silver Jubilee in 1977. It was carried up and erected by the Menstrie Scout Group and was part of the UK chain of beacons lit as part of the Jubilee celebrations.
Ochil Hills
The Ochil Hills is a range of hills in Scotland north of the Forth valley bordered by the towns of Stirling, Alloa, Kinross and Perth. The only major roads crossing the hills pass through Glen Devon/Glen Eagles and Glenfarg, the latter now largely replaced except for local traffic by the M90...
in central Scotland
Scotland
Scotland is a country that is part of the United Kingdom. Occupying the northern third of the island of Great Britain, it shares a border with England to the south and is bounded by the North Sea to the east, the Atlantic Ocean to the north and west, and the North Channel and Irish Sea to the...
. The name is thought to originate from Dun (hill fort) of the Maeatae
Maeatae
The Maeatae were a confederation of tribes who lived probably beyond the Antonine Wall in Roman Britain. The historical sources are vague as to the exact region they inhabited....
.
Although relatively small (its height is 418 metres), the characteristic shape of the hill forms an important part of the distinctive scenery of the Stirling
Stirling
Stirling is a city and former ancient burgh in Scotland, and is at the heart of the wider Stirling council area. The city is clustered around a large fortress and medieval old-town beside the River Forth...
area, and it is often depicted (particularly in postcards and calendars) in combination with the nearby Abbey Craig
Abbey Craig
The Abbey Craig is the hill upon which the Wallace Monument stands, at Causewayhead, just to the north of Stirling, Scotland.The Abbey Craig is part of a complex quartz-dolerite intrusion or sill within carboniferous strata, at the western edge of the Central Coal Field, known as the Stirling Sill...
. The hill is a popular climb with tourists and visitors to the Stirling and Trossachs
Trossachs
The Trossachs itself is a small woodland glen in the Stirling council area of Scotland. It lies between Ben A'an to the north and Ben Venue to the south, with Loch Katrine to the west and Loch Achray to the east. However, the name is used generally to refer to the wider area of wooded glens and...
area, due to the historical nature of Stirling and the proximity of the Wallace Monument
Wallace Monument
The National Wallace Monument is a tower standing on the summit of Abbey Craig, a hilltop near Stirling in Scotland. It commemorates Sir William Wallace, the 13th century Scottish hero....
.
Dumyat has two principal summits: Castle Law on the west, and Dumyat proper on the east. On the summit of Castle Law the remains of an ancient hill fort
Hill fort
A hill fort is a type of earthworks used as a fortified refuge or defended settlement, located to exploit a rise in elevation for defensive advantage. They are typically European and of the Bronze and Iron Ages. Some were used in the post-Roman period...
, originally occupied by the Maeatae, are still clearly discernible.
At one time the favourite route to the summit of either Dumyat or Castle Law was via the prominent gulley which runs almost straight up the southern scarp face, and continues down the gently sloping north face. This gulley was formed by the erosion of a fault
Geologic fault
In geology, a fault is a planar fracture or discontinuity in a volume of rock, across which there has been significant displacement along the fractures as a result of earth movement. Large faults within the Earth's crust result from the action of tectonic forces...
, resulting from the juxtaposition of soft pyroclastic rocks on one side against harder andesite
Andesite
Andesite is an extrusive igneous, volcanic rock, of intermediate composition, with aphanitic to porphyritic texture. In a general sense, it is the intermediate type between basalt and dacite. The mineral assemblage is typically dominated by plagioclase plus pyroxene and/or hornblende. Magnetite,...
and basalt
Basalt
Basalt is a common extrusive volcanic rock. It is usually grey to black and fine-grained due to rapid cooling of lava at the surface of a planet. It may be porphyritic containing larger crystals in a fine matrix, or vesicular, or frothy scoria. Unweathered basalt is black or grey...
on the other. This has resulted in an area where hard andesite
Andesite
Andesite is an extrusive igneous, volcanic rock, of intermediate composition, with aphanitic to porphyritic texture. In a general sense, it is the intermediate type between basalt and dacite. The mineral assemblage is typically dominated by plagioclase plus pyroxene and/or hornblende. Magnetite,...
slightly overhangs, and is the darkest and least exposed part of the climb, which is not particularly difficult. Further gullies, formed by secondary tearing around the main fault (itself a product of the major disturbance which resulted from the Ochil Fault
Ochil Fault
The Ochil Fault is the geological feature which defines the southern edge of the Ochil Hills escarpment, Scotland.North of the fault, Devonian lava flows and pyroclastic deposits slope gently down, thinning towards the north. These are in part overlain by Old Red Sandstone rocks formed later in the...
) extend to the right into Dumyat, and form potential shortcuts to the summit. The first of these, Raeburn's Gulley, is particularly dangerous and should only be attempted by experienced and properly equipped rock climbers, however the second, Siart Gulley, is climbable by anyone of average ability, if care is taken in scrambling up the steep step at the end. The third, fourth and fifth gullies are not named, and become progressively easier.
Nowadays many people park their cars on Sheriffmuir
Sheriffmuir
Sheriffmuir , the site of the inconclusive 1715 Battle of Sheriffmuir , lies on the slopes of the Ochil Hills just inside the Perthshire border in Scotland...
and take a longer but more gently sloping path to the summit, passing behind, i.e. slightly to the north of, the summit of Castle Law. The third route is via Menstrie Glen
Menstrie Glen
Menstrie Glen is the valley which separates Dumyat from Myreton Hill and the main body of the Ochil Hills in Scotland. Once farmed but no longer inhabited, it is now used for sheep pasture, a public water supply and recreation in the form of fishing and walking.-Vegetation and topography:Much of...
from the east, and is a somewhat gentle ascent in the beginning, which steepens satisfactorily for those who like a decent climb, as the summit is approached.
The exposed terrain of Dumyat and the surrounding muir are suitable only for sheep farming, with several sheep folds dotting the hill's sides, along with the ruins of a shepherd's stone house. Dumyat was formerly the site of small-scale mining for copper
Copper
Copper is a chemical element with the symbol Cu and atomic number 29. It is a ductile metal with very high thermal and electrical conductivity. Pure copper is soft and malleable; an exposed surface has a reddish-orange tarnish...
and barytes, although these workings are now abandoned.
The scree
Scree
Scree, also called talus, is a term given to an accumulation of broken rock fragments at the base of crags, mountain cliffs, or valley shoulders. Landforms associated with these materials are sometimes called scree slopes or talus piles...
on the scarp face of Castle Law is a source of agate
Agate
Agate is a microcrystalline variety of silica, chiefly chalcedony, characterised by its fineness of grain and brightness of color. Although agates may be found in various kinds of rock, they are classically associated with volcanic rocks and can be common in certain metamorphic rocks.-Etymology...
s, not necessarily of the finest quality, but occasionally other specimens such as smoky quartz
Smoky quartz
Smoky or smokey quartz is a brown to black variety of quartz. Like other quartz gems, it is a silicon dioxide crystal. The smoky colour results from free silicon, formed from the silicon dioxide by natural irradiation.-Morion:...
and citrine can be found, along with the inevitable quartz
Quartz
Quartz is the second-most-abundant mineral in the Earth's continental crust, after feldspar. It is made up of a continuous framework of SiO4 silicon–oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall formula SiO2. There are many different varieties of quartz,...
, calcite
Calcite
Calcite is a carbonate mineral and the most stable polymorph of calcium carbonate . The other polymorphs are the minerals aragonite and vaterite. Aragonite will change to calcite at 380-470°C, and vaterite is even less stable.-Properties:...
, barytes, and two ores of copper, malachite
Malachite
Malachite is a copper carbonate mineral, with the formula Cu2CO32. This green-colored mineral crystallizes in the monoclinic crystal system, and most often forms botryoidal, fibrous, or stalagmitic masses. Individual crystals are rare but do occur as slender to acicular prisms...
, and less commonly, azurite
Azurite
Azurite is a soft, deep blue copper mineral produced by weathering of copper ore deposits. It is also known as Chessylite after the type locality at Chessy-les-Mines near Lyon, France...
.
At the top is a memorial to the Argyll and Sutherland Highlanders
Argyll and Sutherland Highlanders
The Argyll and Sutherland Highlanders, 5th Battalion The Royal Regiment of Scotland is an infantry battalion of the Royal Regiment of Scotland....
, a trig point
Trig point
A triangulation station, also known as a triangulation pillar, trigonometrical station, trigonometrical point, trig station, trig beacon or trig point, and sometimes informally as a trig, is a fixed surveying station, used in geodetic surveying and other surveying projects in its vicinity...
, and a characteristic cairn
Cairn
Cairn is a term used mainly in the English-speaking world for a man-made pile of stones. It comes from the or . Cairns are found all over the world in uplands, on moorland, on mountaintops, near waterways and on sea cliffs, and also in barren desert and tundra areas...
with a beacon on top that is currently filled with stones.
The stones which are placed in the beacon are all wishes that have been made by others.
The beacon on the top of Dumyat was commissioned for the Queen's Silver Jubilee in 1977. It was carried up and erected by the Menstrie Scout Group and was part of the UK chain of beacons lit as part of the Jubilee celebrations.
External links
- Undiscovered Scotland's page on Dumyat
- Information about the hill fort
- Aerial photo of Dumyat: Web page and image P000728 (01-Jan-1976) from British Geological Survey
- Photographs of Dumyat and the surrounding area