Cove Vein Mine
| Location | Whytes Cleuch, Wanlockhead, Dumfries and Galloway — 55.3990, -3.7770 (approximate) |
|---|---|
| Commodity | Lead |
| Type | Metal |
| Worked | The vein's north end was opened in 1755 by a Mr Williamson.–No reliable closure date has yet been located. |
| Maximum depth | No reliable depth figure has yet been located; developed by shafts and adits. |
| Operators | Mr Williamson (1755–?) |
| Status | Researched |
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.
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.
Abandoned workings can be dangerous — unstable ground, uncapped shafts, flooding and bad air are common even where a site looks safe from the surface. This entry describes history and general location only; it is not an access guide.
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
Photographs & further reading
This page doesn't try to reproduce everything — these are the best original sources found for this mine.
The mineral-locality record for Cove Vein, listing the specimens it has yielded.
View sourceSources
- (primary) Lead and zinc ores of Scotland Area I. The Leadhills-Wanlockhead district — BGS Earthwise
- (secondary) Cove Vein, Whytes Cleuch, Wanlockhead — Mindat.org
Record created: 31 August 2026 · Last researched: 31 August 2026