SiteName: Cae Coch Sulphur MineTrefriw Sub Brit site visit 16th August 2003 [Source:
Nick Catford, John Bennett
& Robert Vernon]
GEOLOGY This deposit is a major source of pyrites in Wales. Pyrites in its pure form contains 46.6% iron and 53.4% sulphur and it was for the sulphur that the Cae Coch deposit was worked, 70% iron content being found in the haematite ores worked extensively in Cumbria and Lancashire, which made them more attractive to the iron miner. The Cae Coch pyrites was not pure, typically containing 30% to 40% sulphur, with correspondingly less iron content. The Cae Coch deposit consists of two separate ore bodies. The smaller northern body outcrops to the east of Blaen-y-wern, whilst the larger and more extensively worked lies immediately to the south. The southern ore body has an average dip of thirty degrees to the south, with the superimposition of minor folding creating localised flattening or steepening of the pyrites which is clearly visible in the workings. THE WORKINGS The earliest workings are probably those of the linear quarry which
follows the outcrop of the northern ore body to the east of Blaen-y-wern.
The workings on the larger southern ore body also began as a quarrying
exercise until continued removal of the overburden became impracticable
after which the deposit was exploited by a series of adits; the most
important of these being the No.2 adit.
Photo:Timber
supports in an unstable area
Photo by Nick Catford TRIP REPORT The mine lies on Forestry Commission land and unlike many other mines in the Gwydyr Forest has not yet been gated. Access to this mine can be achieved via the forest road which leaves the B5016 Conwy to Trefriw road a short distance north of the Trefriw Spa. We decided to access the Mine from the upper road from Trefriw which eventually peters out to become a footpath at Tyddyn Wilym. In hindsight, might have been a mistake as the path down to the mine is steep, overgrown in places and badly signed. The footpath is clearly signed by a cattle grid in the road and surprisingly there was room to park our convoy of nine cars. The footpath heads in the direction of an occupied house but it isn't obvious that you have to walk up the drive of the house turning right as you pass it into a field that appears to be part of the garden. There is a gate at the eastern side of the field and this is the way on, descending steeply into a wooded area where a small open quarry is soon reached. This is the earliest upper working of the mine extracting ore from the northern ore body. At the bottom of the quarry No. 1 adit is clearly visible; this gives access to the upper underground workings but the adit was badly silted so we decided not to investigate as time was pressing. A short distance down hill there are two further adits, one is dry and extends for about 20 yards to a blind end, the other has foot deep water at the portal and runs west for some fifty yards and then turns south for a further fifteen yards where the water deepens at the blind end; both were probably exploratory drivages. From this point the footpath turns to the south and drops steeply down
hill towards a fence line which has a number of notices fixed to it
describing 'dangerous old mine workings' The footpath turns south west
along the fence line and in a gully on the left hand side of the path
the sheave wheel for the top of the 1917 aerial ropeway is still in
place. On the opposite side of the footpath are the footings of a small
building straddling the fence.
Photo:Looking
down dip towards 2 adit from the pillar and stall workings
Photo by Nick Catford No. 2 adit is obscured by bushes at this point but by climbing over the fence and into the undergrowth it quickly becomes apparent. It is not an adit in the normal sense of the term but resembles a huge cave entrance thirty feet in height and as many wide. The adit opens immediately onto the steeply upward dipping pillar and stall workings in the lower ore body. The pyrites bed was worked by leaving pillars from two to three yards
in diameter, at There are many calcite formations and some spectacular colouring in the rock and in several places there are acid pools that leave permanent stains on boots and clothing. The lower levels of the mine are flooded up to the level of No. 2 adit and are no longer accessible. At this point we had to retrace our steps but we will return to Cae Coch another day, there is plenty more to see underground and on the surface much remains including the inclines, drum house, storage bins, foundations of the processing mill, numerous other buildings and Nos. 3 & 4 blocked drainage adits. The history and geology of Cae Coch Mine is an
abridged version of Mines of the Gwyder Forest Part 7 by John Bennett
& Robert Vernon pages 12 - 39. ISBN0 9514798 6 5. It is reproduced
with permission from the author. Published by Gwydyr Mines Publications 17 Field Lane, Appleton, Warrington, WA4 5JR Mines of the Gwydyr Forest Parts 1 - 7 is available
from Moore Books
specialising in mining, caving and industrial archaeology. [Source:
Nick Catford, John Bennett
& Robert Vernon]
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