Penylan Quarry

Also known asPen-y-lan Quarry
LocationPenylan, Cardiff — 51.5016, -3.1563 (approximate)
CommoditySandstone
TypeQuarry
WorkedBy the mid-19th century–Not worked since the 19th century
Maximum depthNo reliable working-depth figure has yet been located.

Overview

Penylan Quarry worked the outcrop of Silurian mudstone on Pen-y-lan hill in Cardiff — the oldest rocks in the city — for building stone. It has not been quarried since the nineteenth century, and it is remembered now for what the quarrymen exposed rather than for what they took away: a rich shelly fauna of brachiopods, corals, graptolites and trilobites that made it one of the most important fossil sites in Wales. It is a Site of Special Scientific Interest.

History

That Silurian rocks exist at Pen-y-lan hill and in its neighbourhood was made known as long ago as 1861, by Norman Glass, who collected a number of fossils from the quarry. The outcrop was worked for building stone, and the working itself did not outlast the nineteenth century. Its afterlife has been geological. The quarry became well known for the quality of its Silurian fossils, including complete examples of trilobites such as Encrinurus, and Calymene from Penylan is among the Silurian trilobites held by Amgueddfa Cymru. The site was described in the scientific literature — a paper on the Silurian district of Rhymney and Pen-y-lan was read to the Geological Society in 1879 — and it is now protected as a Site of Special Scientific Interest for its palaeontology. Part of it was lost when a major road was built across the ground, leaving the remainder protected.

Geology

The quarry exposes Silurian mudstone, the oldest rock in Cardiff, at an outcrop that rises through the much younger cover of the surrounding city. The rock is a marine mudstone crammed with a shelly fauna — brachiopods, corals, graptolites and trilobites — laid down in a shallow sea, and it is the fossils rather than any mineral content that give the site its standing. Complete trilobites of the genus Encrinurus have come from here, and Calymene from Penylan is among the Welsh Silurian material in the national collection. This is sedimentary rock worked as bulk building stone; there is no mineralisation and no vein.

Geological setting: Sedimentary Beds and Seams (historical documentary reference)

Workings

A surface quarry on the hill at Pen-y-lan, worked into the Silurian outcrop for building stone. Nothing consulted for this record describes its plan, its depth or how it was worked, and no figures for output or workforce have been found.

Closure

The quarry has not been worked since the nineteenth century. No source consulted here gives a closure date or a reason; the ordinary explanation for a small urban building-stone quarry of this kind is that the city grew over it and better stone came in by rail, but that is not stated anywhere read for this record and is not asserted here.

What remains

Protected as a Site of Special Scientific Interest, and partly gone: the site became partly inaccessible when a major road was built, though the remainder is now protected. It remains a notable palaeontological locality.

The quarried faces of the Silurian outcrop, so far as they survive the road that took part of the site. Nothing consulted here describes any quarry building or structure.

Nearby mines

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.

Photographs & further reading

Trilobites in Wales (reference)

Amgueddfa Cymru's account of Welsh trilobites, which places Penylan among the country's notable Silurian localities and figures a Calymene collected here.

View source

Sources

  1. (secondary) Penylan Quarry — Wikipedia
  2. (secondary) Trilobites in Wales — Amgueddfa Cymru — Museum Wales

Record created: 4 September 2026 · Last researched: 5 September 2026