Cove Vein Mine

Overview

A lead vein at Whytes Cleuch in the historic Wanlockhead mining district of the Lowther Hills, opened in 1755 and developed by shafts and adits along a mile-long course, notable for its unusually wide, drusy and cavernous ground and its rare mineral specimens.

History

Cove Vein was developed by shafts and adits at approximately the middle of Whytes Cleuch, a small valley about a kilometre north-west of Wanlockhead village, part of the wider Leadhills-Wanlockhead mining district in the Lowther Hills -- a district worked since at least the mid-13th century and once nicknamed 'God's Treasure House' for its unusual mineralogical richness, with more mineral species recorded here than at any other Scottish locality. The vein itself courses north-north-west to south-south-east for about a mile. Its north end, near the head of Whytes Cleuch, was opened in 1755 by a Mr Williamson, who found the vein to vary between 12 and 20 feet in width -- drusy and cavernous, and in better condition for working than at the vein's southern end. This unusual cavity-rich character has made Cove Vein notable for its mineral specimens, including cerussite, corkite, caledonite, linarite, vanadinite and hemimorphite.

The Geological Survey's 1921 memoir on the lead and zinc ores of the district lists the Cove Vein as abandoned, the Duke of Buccleuch as proprietor and the Wanlockhead Lead Mining Co. Ltd as lessees. It says the vein takes its name from its great width, that it was first opened up by Sir James Stampfield, who worked the district's veins from 1680, and that it was worked fairly constantly until about sixty years before the memoir, which puts the end of regular working around 1860. All the workings are at the north end, before the vein's junction with the Lochnell Vein; the ore had been worked out from the surface to 60 or 70 fathoms below the adit, a total depth of 130 fathoms, and the levels appear to have been driven about 185 fathoms in ore-bearing ground. Tait's Level, driven north-eastwards from about a third of the way up Whytes Cleuch before 1800, was an important day level into the higher workings of the Cove and Belton Grain veins, and a leat once took water from it.

Geology

The Cove Vein at Whytes Cleuch in the Wanlockhead district of the Lowther Hills, coursing north-north-west to south-south-east for about a mile and worked by shafts and adits.

Workings

Developed by shafts and adits along a vein coursing NNW-SSE for about a mile, worked where it varied between 12 and 20 feet wide in drusy, cavernous ground. All the workings are at the north end, before the junction with the Lochnell Vein, and had reached a total depth of 130 fathoms, 60 or 70 fathoms below the adit. Tait's Level gave day access to the higher workings of the Cove and Belton Grain veins.

Closure

Regular working ended about 1860, sixty years before the Geological Survey's 1921 memoir describes the vein as abandoned.

What remains

Unknown.

Related mines

• New Glencrieff Mine — Both worked veins of the Wanlockhead district from Whytes Cleuch and the Wanlockhead Lead Mining Company; the Geological Survey memoir treats the Cove, New Cove and Glencrieff veins together.
• Wanlockhead — Cove Vein Mine lies in the Wanlockhead mining district and was developed by the same wider mining interests.

What's uncertain

Points where sources disagree or the record could not be settled; both accounts are kept. All open questions in the archive.

• The Geological Survey memoir says the vein was first opened up by Sir James Stampfield and takes its name from its great width. (disputed) ¹

Recorded claims

Individual factual claims, each attached to the source(s) that support it below. Where sources disagree, both are kept.

• The north end of Cove Vein, near the head of Whytes Cleuch, was opened in 1755 by a Mr Williamson, who found the vein to vary between 12 and 20 feet in width, drusy and cavernous, and in better condition for working than at the vein's southern end. ¹
• The vein courses NNW-SSE for about a mile; its unusually cavity-rich ground has yielded mineral specimens including cerussite, corkite, caledonite, linarite, vanadinite and hemimorphite. ²
• The Leadhills-Wanlockhead district, worked since at least the mid-13th century and once nicknamed 'God's Treasure House', hosts around seventy lead-zinc veins and has yielded more recorded mineral species than any other Scottish locality. ¹
• The ore had been worked out from the surface to 60 or 70 fathoms below the adit, a total depth of 130 fathoms, and levels had been driven about 185 fathoms in ore-bearing ground, all at the north end before the junction with the Lochnell Vein. ¹
• The Cove Vein was worked fairly constantly until about 1860 and was described as abandoned in 1921. ¹
• The Geological Survey memoir says the vein was first opened up by Sir James Stampfield and takes its name from its great width. (disputed) ¹
• The Duke of Buccleuch was proprietor and the Wanlockhead Lead Mining Co. Ltd the lessees in 1921. ¹
• Tait's Level was driven north-eastwards from about a third of the way up Whytes Cleuch before 1800 and gave day access to the higher workings of the Cove and Belton Grain veins. ³
• The British Geological Survey catalogues a plan of the junction of the Cove Vein and Tait's Adit, Wanlockhead. ⁴

Photographs & further reading

Sources

1. (primary) Lead and zinc ores of Scotland Area I. The Leadhills-Wanlockhead district — BGS Earthwise
2. (secondary) Cove Vein, Whytes Cleuch, Wanlockhead — Mindat.org
3. (secondary) Bay Mine (Pumping Shaft) - Scottish Cave and Mine Database site details — Scottish Cave and Mine Database (Grampian Speleological Group)
4. (primary) BGS / Mining Remediation Authority mine plans: junction of the Cove Vein and Tait's Adit, Wanlockhead (item 20848) — British Geological Survey

Record created: 31 August 2026 · Last researched: 30 September 2026