The workings I'll be dealing with here are the adits to be found in Scanniclift Copse, which is to the South-West of the parish of Doddiscombsleigh. I've indicated the location on my map on the 'Mining Introduction' page, and they can be found at Ordnance Survey coordinates SX 844 863. Scanniclift Copse is managed by the Devon Wildlife Trust, and is situated on one side of a steep-sided valley adjacent to the River Teign, and paths and steps have been created within the woodland to aid access for visitors and to try to discourage people from wandering off the main route. These woods are an excellent place to see the natural flora, and occasionally the fauna, of the area, and there is a good representation of woodland plant species to be seen. Any fallen trees, and there are many in this wood, are left in situ to enhance the habitat. Bluebells are particularly prolific in this wood, and a well-timed visit will reward the visitor with a blue haze of the flowers on the woodland floor. But despite the many wonders of this place, it is the mining history I'm interested in here. At several points along the pathways which have been constructed within the woods it is possible to see depressions in the ground where exploratory excavations may have taken place as the prospectors searched for manganese ore deposits near the surface, but presumably were fairly quickly abandoned as there is rather little in the way of spoil heaps adjacent to these depressions. The geology of this particular area is especially interesting as the woods sit on a region where an intrusive plug of igneous rock meets the sedimentary, and as a result there is evidence of the effects of metamorphosis on the shales in this vicinity, although the igneous rock itself, tuff, appears at the surface within these woods in a small location at the higher Western end.
The part of this woodland of greatest interest to me, however, is a small section at the higher Eastern end which is visible in photo 1 as the section jutting out at the top left. This section of the copse was until recently privately owned, but is now in the care of the Devon Wildlife Trust, as is much of the rest of the wood. Here there is evidence of ore extraction with considerable spoil heaps adjacent to several adits, at least one at an upper level and another two occurring at lower locations, one of which appears to drain the complex as water emanates from it. Both of the two lower adits open out onto an old overgrown track passing through the upper part of Scanniclift Copse, and presumably this was how the ore was removed from the area, although it is uncertain in which direction it would have been sent. Much of the manganese ore occurred very close to the surface and as a result, the access tunnels and some stopings have collapsed, the entrances to the original adits having also fallen in although their location can be easily determined upon examination of the area.
The workings in this wood are certainly very old, although as yet I have been unable establish an age for them, as there seem to be no records associated with the area despite the fact that a good amount of ore must have come from here. A clue can perhaps be found in the large oak trees actually growing within the collapsed regions, although none of the trees growing amongst these remains were significantly larger or older than a particular oak we encountered which had been cut down further down the hill, and a growth ring count of the remaining stump suggested an age for this tree of about 120 years, so allowing for the time required for the workings to fall into ruin and become overgrown, an initial estimate based on these criteria would indicate the early part of the 19th century as a possible period of industrial activity. In support of this, there is mention that originally one of the chief producers of manganese ore in Devon was the mine in Upton Pyne which ran from 1788 until 1823, but when the ore deposits had become exhausted the focus for manganese ore production moved to the Teign Valley area. Although there are small manganese workings near Ashton, I am at the moment assuming that most of the ore was extracted at Scanniclift, and the date for the closure of the Upton Pyne mine gives us, at least, a possible date for when these mines could have been in operation.
When driving an adit into a hillside, it was usual practice for the miners to initially cut a level channel or gully into the hill, in order to expose a sufficient height of rock face to safely support a tunneling operation with minimal risk of collapse. The two lower adits can be seen to have followed this style, but they are now in a very poor state of preservation, as the sides of the cut and material from above the tunnel entrance has fallen inwards to completely block access. Photo 2 shows one of the original adit entrances at the lower level and as can be seen, is in a very poor condition. This particular adit is completely dry, with no evidence of it ever having been used for drainage, but sufficient material has fallen into the cut to completely block the entrance, assuming it is still intact, but the original rocky sides of the cut are still visible. There is a fairly large spoil heap near the mouth of this adit, and as mentioned earlier, it opens out on to an old track through the woods, which is presumably how the ore was removed from the site.
Photo 3 shows the site of the other of the two lower adits, also opening out onto the old track. I believe this adit itself to be generally intact as there is no evidence of sunken ground above it, although it is inaccessible from this side due to the rubble and earth blocking its entrance, and the uprooting of a large oak which was growing in the cut has complicated matters somewhat. There are substantial spoil heaps by this adit also suggesting much use, and a fair amount of water is running out from it indicating it also functioned as the drainage adit for the whole complex. The remains of a stone built structure can be seen next to this lower drainage adit, although it is little more now than a broken rectangle of stones which can be difficult to identify unless you happen to be standing at the correct location in the Winter, which is the only time the undergrowth has died back sufficiently to render the base of the walls visible. This building could possibly have been used as a workshop for maintaining tools and producing timber for use underground, and may have doubled up as a mine office and temporary dwelling. The remains of part of this structure, showing the top of a wall foundation, can be seen in photo 4.
A quick look over any of the spoil heaps will soon reveal pieces of manganese ore which, despite the difficulty the miners must have experienced in winning the ore from the country rock, have been discarded along with the waste although most pieces are small, impure and attached to larger pieces of waste rock. I can only assume the occasional large piece of ore wasn't of a high enough grade to sell. The manganese ore itself can easily be identified as weathered samples take on an almost purple-brown appearance under the green canopy of the trees and when a sample is broken to reveal a fresh face it displays a blue-grey colour with an almost metallic lustre, and the ore itself feels rather heavier than ordinary rock as might be expected. A good example of some of this manganese ore was discovered on one of the spoil heaps and is shown in photo No.5. Incidentally, scattered about these woods can also be found an odd rock type which appears to be a type of vesicular basalt, presumably the result of having a large body of intrusive magma so close by, although I have yet to positively identify my samples. For interest, an 80Kb picture of an example can be seen here.
Slightly higher up the hill is evidence of a lot more activity, representing what I refer to as the upper levels. I imagine there must be quite a network of tunnels and cavities under this part of the woods with large areas hollowed out as the ore, which tended to occur in large bodies rather than thin seams, was removed. Certain areas have opened up where the stoping activities of the miners have broken the surface, one such place being illustrated in photo 6. This particular site is obviously where part of the mine intentionally broke the surface in the quest for the manganese ore, and probably also served to help ventilation. The miners sensibly left a small bridge of rock in place here to help support the mass of rock to the left of the picture, which would otherwise have been liable to collapse. There is no access to the workings through this opening now, as rubble has fallen in and blocked it at the bottom.
The ground in this higher area has been so disturbed by the mining operation and later collapses that it is difficult to determine exactly how many adits were originally here, but two separate spoil heaps can easily be identified and as this mine was probably worked over a period extending to several decades, worked out parts would have been abandoned and waste rock dumped in the area leading to the apparently confused state visible now. What appear to be large excavated areas surrounded by high rock faces present themselves here, and it is probably impossible now to determine whether these areas represent collapsed underground workings or areas of essentially open cast working where the ore was accessible from the surface. I have included a photo of one positively identifiable adit entrance as photo 7, and the oak tree growing there lends weight to the considerable age of this mine. The original sides of the cut are easily visible here, although there is the inevitable build up of debris in the bottom. Further in, in the background, can be seen part of the rocky sides which presumably once formed the sides of an underground chamber, now fallen in. This can be better seen in the high resolution version of the photo.
If you walk into this old adit entrance and follow the path it would have taken when underground, you will see that it appears that the whole mine has collapsed to form a deep gorge with vertical rock faces, with the floor strewn with large boulders, fallen trees and broken branches. If you climb over these boulders which were possibly once the roof of this part of the workings, and fight your way through the jungle of undergrowth towards the remaining intact part of the adit you will be greeted with a yawning opening about fifteen feet high in the rock face, going down at about a 30° angle as a result of the build-up of fallen rocks in front of the entrance and decades of refuse dumped in over from the field just above. This opening was, I believe, once fairly deep into the mine and it is only the collapse of the area further back which has revealed it. Photo 8 was taken to show the accessible part of the workings from within this collapsed section.
The following section deals exclusively with the underground aspects of this, the only remaining accessible part of the complex. Currently the only way in is through this large opening, and to try to demonstrate the size of the cavity, I have included a picture of it here as photo 9, the large ferns on the inside giving some idea of scale. I am always cautious about entering old workings like this, and strongly recommend you don't do it unless you have at least some experience of entering such places. It is sensible to ensure you have adequate and reliable lighting, a bump hat to protect your head against possible minor rock falls, and additional company, some of whom should remain outside just in case the worst happens, as even if you have informed others of your intentions, it could still be extremely difficult for a rescue party to locate the actual part of the mine involved. In the case of this adit, I examined the entrance for evidence of instability, but the floor was green with moss and the rock of the roof was covered in lichens, indicating nothing had moved for decades, so I deemed it reasonably safe to enter. The contrast between the hot humidity of the woods and the cool of the mine was striking as I climbed down over the rubble at the entrance, and looking up, the stoping could be easily seen extending in an arc overhead as the miners had followed the path of the ore body. The chamber at this point is perhaps 10 feet wide and around 15 feet high indicating a substantial amount of ore must have been extracted here.
It is possible to continue on foot for about a hundred feet before coming to what initially appears to be the end of the workings, and from this point I took a photo to show the interior of this section of the mine which I have reproduced here as photo 10. This image was taken using the very small amount of natural light which had made it this far into the mine, and the exposure for this required a full thirty seconds to produce the result seen here. The important aspect of this is that the image shows the true daylight colours of the rocks, and in the high resolution image pieces of purple-blue manganese ore can be seen on the floor and walls. The floor is strewn with loose rocks, and my first thought was that part of the roof had collapsed, but it became apparent that this was in fact waste rock which had been piled up, mainly in order to avoid the task of removing it, but with the added benefit of raising the floor, by so doing reducing the height of the timber scaffolding required to reach the top of the stoping.
Initially, I was unable to discover any evidence of hand tool marks on the walls of this chamber, making me wonder just how the rock was broken. The ore itself is fairly soft and a pick would have succeeded in getting the job done, but the much harder surrounding rock is another matter entirely as these workings pre-date the invention of Dynamite, (invented by Alfred Nobel and patented in 1867) and only black powder explosive would have been available to the miners of the day. In order to blast the rock, deep holes would need to be drilled into the rock in order to place the explosive charge, and a further search did in fact reveal evidence of the remains of two such blast holes.
This cavity initially appears to be the limit to how far the workings progressed underground, but in fact they do continue on for some considerable distance although access is through a rather small gap at the rear left hand side of this chamber followed by a drop of about nine feet before another large chamber presents itself. Many years ago I remember shining a powerful lamp into this hole and seeing timbers lying around and considering how far into the mine this was, these timbers can only be the remains of the original scaffolding used by the miners all those years ago. Exploring this deeper section will involve climbing equipment and the assistance of people vastly more experienced than myself, and of course permission must be sought from the landowner before we attempt such a visit. If and when this happens, I'll put any additional information here.
Much about this place is guesswork as any records seem to be non-existent, so if anyone has any stories, or information on any of the manganese mines I'm studying here, whether factual or highly doubtful, third-hand or passed down from a grandfather, please contact me at the e-mail address below so we can add to the little we do know and hopefully put a few pieces of the jigsaw together, and attempt to get a better picture of Doddicombsleigh's mining history.
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