Glencartholm
Glencartholm est un site géologique dans la région de Dumfries and Galloway en Écosse. La zone, découverte en 1879, contient des fossiles datant de l'ère Paléozoïque et particulièrement de la période du Carbonifère. On y trouve également une ferme, à proximité de la frontière avec l'Angleterre, qui est classée monument historique.
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Glencartholm
Glencartholm is a location in Dumfries and Galloway, southern Scotland, along the River Esk.
The Glencartholm Volcanic Beds contain a Palaeozoic (specifically Carboniferous) fossil fish site of international importance. Discovered in 1879, most of the fossils were removed during the 1930s, but in the 1990s a further site 50 m (160 ft) east, named Mumbie, was excavated. This led to the identification of further fish beds, where over 200 specimens of ray-finned fish were collected, including one possible new species
There is also a farmhouse known as Glencartholm, or Glencartholm Farmhouse, which is a listed building in the parish of Canonbie, not far from the border with England, and near Glencartholm Wood. The farm has an inscription celebrating the defeat of Napoleon at the Battle of Waterloo.
732 m
Gilnockie Tower
Gilnockie Tower is a 17th-century tower house, located at the hamlet of Hollows, 2.2 km north of Canonbie, in Dumfriesshire, south-west Scotland. The tower is situated on the west bank of the River Esk. It was originally known as Hollows Tower.
Gilnockie Castle is a separate, but nearby site.
1.6 km
Gilnockie railway station
Gilnockie railway station served the hamlet of Hollows, Dumfries and Galloway, Scotland from 1864 to 1967 on the Border Union Railway.
1.9 km
Fairy Loup
Fairy Loup is a waterfall located on Byre Burn, a tributary of River Esk, in Dumfries and Galloway, Scotland.
The waterfall's name originates in a local legend of "a fairy having leaped from one side to the other", and is an example of a regional tradition of associating small streams with fairies. This waterfall was one of several features near Langholm described in the poetry of Hugh MacDiarmid.
A 14.5-kilometre (9.0 mi) loop trail passing through Canonbie and Rowanburn gives access to the waterfall. Fly-tipping has been a problem in the area.
3.1 km
Canonbie Coalfield
The Canonbie Coalfield is a small and largely concealed coalfield at Canonbie in the south of Scotland. A comprehensive survey by Peach and Horne was published in 1903. Canonbie colliery was worked until 1920, and another mine at Archerbeck continued until 1942. There are some Eighteenth Century documents extant referring to coal mines at Archerbeck, Skeltonscleugh, Byerburn, Knottyholm and Fairy Loup.
Recent work has indicated potentially economically workable reserves beneath a cover of New Red Sandstone rocks.
The following coal seams occur within the Pennine Middle Coal Measures Formation in this coalfield:
Knottyholm
Archerbeck
Six Foot
Nine Foot
Five Foot
Eight Foot
Seven Foot
Further less important seams lie within the underlying Pennine Lower Coal Measures Formation and within the overlying strata of the Pennine Upper Coal Measures Formation and the Warwickshire Group including the 'High Coal' at the base of the latter.
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