Wheal Fortune

Also known asGreat Wheal Fortune
LocationBreage and Sithney, Cornwall — 50.1140, -5.3198 (exact)
CommoditiesTin, Arsenic, Copper, Tungsten, Zinc
TypeMetal
Worked1855–1912

Overview

A tin, copper, zinc, tungsten and arsenic mine straddling the Breage and Sithney parish boundary near Helston, Cornwall, worked on its modern scale from 1855 to the early twentieth century. Part of the site is a Site of Special Scientific Interest and a Geological Conservation Review location, designated for a two-generation tin mineralisation sequence exposed in its opencast workings.

History

Documentary evidence suggests mining activity on the site may date back as far as 1508, under early names recorded as "Cog-an-bans" or "Goghan Bras"; tin veins from this period, known as the Conqueror branches, remain traceable on the ground. The modern mine began working in 1855, and by 1864 employed 457 people across five named lodes (Carnmeal, Blueburrow, Copper, Main and New). Copper was raised until 1884, zinc from 1860 until 1876, and arsenic and tungsten for shorter periods. Recorded tin output totalled 2,992 tons of black tin (2,569 tons 1855-1868, a further 423 tons 1873-1896), alongside 322 tons of copper ore, though the mine's own later account has tin working continuing to 1906. In 1868 the Carnmeal lode was abandoned and five engines in the mine's southern section were put up for sale, but the sett continued to be worked on a reduced scale under different companies until 1912, briefly as "New Great Wheal Fortune" in 1908-09; by 1907 only three people remained employed. A pumping engine of 45 inches was later superseded by a 70-inch engine on Harvey's Engine Shaft, and the northern Carnmeal lode was worked to a depth of 150 fathoms. Even after formal closure, a lone miner is reported to have worked the mine's burrows in the 1950s, recovering about two sacks of wolfram a day.

Geology

The deposit lies in Devonian Mylor Slate Formation metasediments ("killas") close to the roof of the Tregonning-Godolphin Granite, where a later lithium-mica granite phase (the Tregonning Granite) intruded an earlier type-C biotite granite (the Godolphin Granite). Two distinct mineralisation events are exposed here: an early ENE-trending sheeted stockwork of tin-bearing cracks bordered by greisen alteration, carrying tourmaline, topaz, mica ("gilbertite") and cassiterite; and a later phase of hydrothermal tin-vein mineralisation following structural weaknesses, in which an east-west elvan (quartz-feldspar porphyry) dyke that had displaced the earlier stockwork went on to act as a channel for the mineralising fluids. This two-generation sequence, unusually well exposed together in one opencast, is what earned the site its Geological Conservation Review status.

Geological setting: Greisen and Pegmatite Deposits (well documented example), Hydrothermal Deposits (well documented example), Veins and Lodes (well documented example)

Workings

Worked as a combination of opencast and underground workings across five lodes. The main opencast, roughly 300 m south of the engine site and considered of great antiquity, is a large openwork (a "gunnis" or "coffin") about 10 m long and up to 18 m deep, divided in two by a narrow ridge and covering some 0.55 hectares. The northern Carnmeal lode was worked underground to a depth of 150 fathoms via shafts including Harvey's Engine Shaft.

Closure

Main lode production wound down through the 1880s-90s, though the mine's own account has tin working continuing to 1906; the sett was kept going under successive companies, briefly renamed New Great Wheal Fortune in 1908-09, until 1912. Even after that, informal wolfram-scavenging from the burrows is reported into the 1950s.

What remains

A brick-and-stone engine house chimney survives above the site, its upper courses laid in a decorative diamond pattern typical of Cornish engine houses; it is heavily colonised by ivy over its lower half. A 2007 caving-forum discussion of the site describes the main opencast as "very overgrown," with old exploratory levels at its eastern end that appear to be pre-1855 workings rather than part of the main nineteenth-century sett — consistent with the site's documented earlier history.

The surviving engine house chimney and the large opencast working ("coffin"/gunnis) are the principal visible surface features; the opencast exposes the site's two-generation tin mineralisation, the basis of its SSSI/GCR designation.

Related mines

Nearby mines

Straight-line distance, within 9 miles (15 km). Show on the map.

What's uncertain

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

Recorded claims

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

Sources

  1. (secondary) Great Wheal Fortune — Wikipedia
  2. (primary) Great Wheal Fortune, Cornwall (Geological Conservation Review site GCR36) — Geological Conservation Review / Scottish Geology Trust GeoGuide
  3. (observational) Great Wheal Fortune (forum thread) — UK Caving forum
  4. (primary) Mine plan: Clifford Amalgamated Consolidated and United ... Wheal Fortune ... (abandonment plan, Copper Ore, 1870) — BGS / Mining Remediation Authority mine plans catalogue

Record created: 29 August 2026 · Last researched: 29 August 2026

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