Threlkeld Quarry (G.Brooks)

The building of the Lake District

Imagine thick layers of materials – mud, sand, ash, lava, and more – laid down over millions of years, new on top of old. Imagine the materials in these layers changed by heat and pressure, and then squeezed up into a dome. Imagine the top of the dome eroded by weather to expose the oldest layers in the centre, whilst remaining covered by the newer layers further out.

This picture of how the rocks that make up the Lake District got to be where they can now be found is of course very much simpler than what happened in reality. This is not the place for such complications, but the Cumberland Geological Society in their guide to the Lake District  describe a useful model that adds a little more colour to the basic picture, relating the stages of deposition of materials, and their folding and erosion over the past 500 million years. They also give a useful reminder that our region’s position has changed over time during this period, both in terms of how close it has been to the equator, but also relative to sea level – sometimes above, sometimes below. The sequence of events in the model is as follows:

  1. The oldest rocks in the region (c.500 million years ago) – were laid down as muds and sands on the bed of an ancient ocean, but have been much changed since, resulting in what we now refer to as Skiddaw Slates. These make up the slates and flagstones of the Northern Fells.

  2. After a period of folding and erosion these were overlain (450) during two periods of volcanic activity by lavas, tuffs (ash) and agglomerates (rocks), more than 4000 metres thick. The second major volcanic outburst formed rocks of the Borrowdale Volcanic Group. These make up the fells and valleys of Central Lakeland.

  3. The region was invaded by the sea to produce firstly a thin layer of lime-rich fossiliferous mudstones known as the Coniston Limestone Group (now running across Lakeland from MIllom to Shap), and later (420) by muddy and gritty sediments referred to as Silurian rocks (of Southern Lakeland)

  4. A collision of two continental masses (400) had three major effects : an arching up of the region, severe squeezing and folding of layers, and the introduction of a granite mass beneath the whole (now exposed in a number of places including Ennerdale and Threlkeld)

  5. Erosion to a rocky landscape of low relief over which tropical seas advanced and retreated (300), creating layers of limestone (from when underwater) – as in Furness, sandstone (from desert conditions), and coal measures (from swampy deltas) – as at Whitehaven.

  6. More folding and erosion, followed by deposition of sandstone (as at Penrith and St.Bees), shales and limestone during Permian (250) and Triassic (200) times.

  7. Since then gentle uplift and erosion, possibly overlain by Jurassic and Cretaceous seas, but certainly affected by glacial activity in relatively recent times.

 Cumbria sites listed in the MMP Step Three report on the quarrying industry:

315 sites throughout England and Wales are listed. 14 are graded +++, 5 of them in Cumbria

Site Grid ref Grade Components
Crowdundle Roman quarry ?
Honister slate quarry, 1643-1986 NY 215 140 ++(+) Adit (copper), adits (x32), dressing shed, bothies, office, quarries, hopper, ropeway, smithy
Gerrard House Roman quarry NY 255 462 ++ Quarry
Tilberthwaite slate quarry, C18-1930’s NY 306 007 ++ Adit, stable, dressing shed, hut, spoil heaps, tramway, working face
Hodge Close quarry, 1780’s – present NY 317 020 +++ Adit, chapel, dam, engine bed, housing, incline, railway, ropeway, spoil heap (multi-finger)
Threlkeld micro-granite quarry, 1870’s-1980’s NY 328 263 ++ Crushing mill, incline, quarry, railway, spoil heap (multi-finger), engine shed
High Quarry, Troutbeck Park, 1753 – C20 NY 430 069 +++ Adit (x4), office (x2), weigh house, dressing shed(x6), incline, leat, railway, roadway
Wetheral  Roman quarry NY 466 535 ++ Working face
Wrengill quarry NY 475 086 ++ Adit, dam, dressing shed (x2), engine house (pelton), leat, quarry, smithy (and housing), other structure, tramway
Stockdalebank, Longsleddale, 1724-80 NY 487056 ++ Dressing shed, quarry, roadway (sled), spoil heap
River Gelt Roman quarry NY 527 587 +++ Spoil heap, working face
Pigeon Crag Roman quarry NY 531 580 + Working face (?)
Coombcrag Roman quarry NY 590 650 +++ Spoil heap, working face
Whinney End slate quarry, early-middle C19 SD 250 833 R Crane (base).dressing shed (x4), quarry, roadway, spoil heap
Coniston Old Man slate quarry, C16-C20 SD 280 980 +++ Adit (many), stables, dressing shed (x9), office, pipeway, quarry, railway, ropeway, smithy, spoil heap, stone sawing mill
Underbarrow quarry, C19 SD 484 924 0 Quarry
Stainton quarry, 1866- SD 548 727 ?
Hutton Roof quarries, C19-1910s SD 571 770 R Building, quarry, roadway

The grading system:

+++ Site of exceptional national importance, for which statutory protection will almost always be appropriate, and preservation will be of high priority

++ Sites of clear national importance, for which statutory protection will normally be appropriate

+   Sites of national importance, but of lesser priority for resource allocation

R  Sites of regional rather than national importance for this industry

0  Sites which are believed to have been destroyed, or never existed at the location reported

?  Insufficient information or lack of access rendered accurate assesment impossible

The Dentdale Marble Industry (article)
A page about the Shap (pink) granite quarry

The quarries of Lakeland : David Glover, Bookcase (Carlisle), 2014
You can read more about Lake District quarries and their location by following the links to limestone and slate and brick-making
uarrying in Cumbria : David Johnson, Amberley Publishing, 2018
A building stone atlas of Cumbria and The Lake District (PDF)
Millstones of the Pennines and North West England : David Johnson, Amberley, 2023

(Page created 19/04/05. Last updated 06/01/24)