Brown End Quarry
| Location | Waterhouses, Staffordshire — 53.0486, -1.8667 (approximate) |
|---|---|
| Commodity | Limestone |
| Type | Quarry |
| Worked | Mid 18th century–1960s |
| Maximum depth | An open limestone quarry; no depth applies. |
Overview
Brown End Quarry is a former limestone quarry of one hectare near Waterhouses in Staffordshire, worked from the middle of the eighteenth century until the 1960s. Further development was restricted after the Peak District National Park was created in 1951, and quarrying ended within the decade. The Staffordshire Wildlife Trust acquired the site in 1987 as its first geological nature reserve. It is a Site of Special Scientific Interest and a regionally important geological site, notified because the Milldale limestone exposed in its faces is seen in few other places in the Peak District.
History
There was quarrying at Brown End from the middle of the eighteenth century. Its working life was ended not by exhaustion but by designation: when the Peak District National Park was formed in 1951 — the first national park in Britain — further development of the quarry was restricted, and quarrying ended in the 1960s. In 1987 the Staffordshire Wildlife Trust acquired the site, its first reserve taken specifically for its geology rather than its wildlife, and laid out an interpretive trail around the workings.
Geology
The rocks exposed here were laid down about 350 million years ago in the Carboniferous, when this was a warm tropical sea and the remains of sea creatures accumulated in the North Staffordshire Basin, where the water was deeper and moved slowly. About 290 million years ago the area was uplifted above sea level. The Milldale limestone found in the quarry is not seen in many other places in the Peak District, which is the reason for the SSSI notification: its deposits formed in fairly still water about 300 metres deep and are more finely grained than limestone laid down in shallower, faster-moving water.
Geological setting: Sedimentary Beds and Seams (well documented example)
Workings
A small open limestone quarry of about a hectare. No description of its plant or working methods has been located; what the site is now valued for is the section its faces expose rather than the stone it produced. An interpretive trail runs around the quarry and it is registered as an EarthCache.
Closure
Development was restricted from 1951 with the creation of the Peak District National Park, and quarrying ended in the 1960s.
What remains
A nature reserve of the Staffordshire Wildlife Trust, acquired in 1987 as its first geological reserve, designated both a Site of Special Scientific Interest and a regionally important geological site. Cowslip, knapweed, oxeye daisy and fragrant orchid grow on the former quarry floor and spoil heaps, drawing butterflies and other insects.
The quarry faces and the spoil heaps survive, the heaps now flowering ground. The faces are the point of the designation, exposing the Milldale limestone section.
Nearby mines
- Bincliff Lead Mines — 5.7 km N
- Ecton Copper Mines — 8.2 km N
Straight-line distance, within 15 km. Show on the map.
Recorded claims
Individual factual claims, each attached to the source(s) that support it below. Where sources disagree, both are kept.
- There was quarrying at Brown End from the mid 18th century. In 1951, when the Peak District National Park was formed, further development of the quarry was restricted, and quarrying ended in the 1960s. 1
- The site was acquired by the Staffordshire Wildlife Trust in 1987, its first geological nature reserve. 1,2
- The Milldale limestone found at this quarry is not seen in many other places in the Peak District, which is the reason for the Site of Special Scientific Interest designation; its deposits accumulated in fairly still water about 300 metres deep and are more finely grained than limestone deposited in shallower, faster moving water. 1
- The rocks exposed by the quarry were laid down about 350 million years ago during the Carboniferous, when the area was a warm tropical sea and dead sea creatures were deposited in the North Staffordshire Basin; about 290 million years ago the area was uplifted above sea level. 1
Photographs & further reading
The managing trust's account of its first geological reserve — what the faces expose, why the Milldale limestone matters, and what now grows on the quarry floor and spoil heaps.
View sourceSources
- (secondary) Brown End Quarry — Wikipedia
- (secondary) Brown End Quarry nature reserve — Staffordshire Wildlife Trust
Record created: 4 September 2026 · Last researched: 4 September 2026