The Triassic succession is best known for its production of red sandstones but, significant local production of other lithologies, particularly coarse breccias and conglomerates and non-red or white sandstones were also quarried in some areas in the past. The major sandstone production came from the unit now termed the Sherwood Sandstone Group (formerly the Bunter and Keuper sandstones). In the south west of England these sandstones are generally of poor quality and were only worked for local buildings.

Production was centred on the outcrops of the lower Exe Valley (Dimes 1990). Locally the Heavitree Stone a breccia, consisting of coarse, reworked fragments of the surrounding rocks are particularly distinctive and was widely used in the Exeter area.

Further to the north in Somerset dolomitic conglomerates representing a marginal facies of the Triassic were commonly used for building stone in the Chew Valley area (West Harptree) and at Draycott where it was known as the Draycott Marble. The local red and grey sandstones also commonly appear in the village houses over much of the the outcrop (Chew Magna and Chew Stoke). No quarries are working the Triassic sandstones or breccias of the area at present.

In South Wales the red Radyr Stone is a breccia of similar origin used widely for decorative work in the Cardiff area (Llandaff Cathedral, Cardiff Docks and in the bridges of the Taff Vale Railway). Other sandstones quarried from the Triassic successions of this area include the yellow Sudbrooke Stone, a sandy limestone used by the Romans at Caerwent Fort and Caldicot Castle, and the very fine grained Quarrella (Rhaetian) and Sutton stones from the Bridgend area.

Triassic North Curry sandstone at Thorne Falcon Somerset

A number of Triassic red sandstones were quarried for building stone in the Cheshire area particularly from 1850's onwards. The main building sandstones outcrop in shallow and high ridges around the margins of the Cheshire Plain. The building stone industry was based around the quarries at Runcorn, Rainhill, Storeton and Woolton etc, many now buried beneath the suburban sprawl of Liverpool. These red sandstones were extensively used for local buildings and production was significant enough to generate an brief export trade to America.

In the Stockport and Knutsford areas the red sandstones of the Sherwood Sandst=one Group) were quarried at Lymm, Timperley, Quarrybank, Styal and near Alderley Edge. They were also quarried for building stone at Helsby, Manley, Simmond's Hill, Delamere, Kelsall and Peckforton.

Substantial quarrying of red Triassic sandstones has continued in Cumbria in the St. Bees area and the Eden Valley. The red St Bees sandstones have been quarried since earliest times but commercial production increased in the late 19th and early 20th centuries and the stone was exported to America. In the Vale of Eden the red sandstones of the Lazonby quarries have long been important and are still in production.

In south west Scotland Triassic sandstones have proved to be a particularly valuable building stone resource (Clashach, Corsehill, Locharbriggs, Corncockle, Gatelawbridge, Spynie & Cove).

Diamond pattern sandstone roof in Dumfries probably from Gatelaw Bridge quarry

In the Glasgow and Edinburgh areas of Scotland a similar picture emerges. Extensive quarrying took place near and within the present city boundaries. Much of Victorian Glasgow is built of local Triassic red sandstone while the city of Edinburgh is built largely of grey-brown Carboniferous sandstones.

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