I've split this off from the 'Mining subsidence' topic as it probably deserved its own:
White coal kilns (aka "Q" pits) don't need to be on the top of a scarp as they're for a relatively low-temperature process and don't want a strong draft but there do seem to few other explanations for this location
Well therein lies the problem, as there
are several more obvious 'Q-pits' scattered around the forest in various locations, and they're not all in wind-blown spots like this one is, and are usually single and relatively small - maybe 2-3m diameter and a maximum of about 0.5m deep.
Just an idea: The line of oval depressions looks like a series of catchment ponds for a waterwheel at the bottom of the scarp - similar to many in the Harz mountains of Germany - the so-called Wasserregal. Are there any signs of leats going down the hillside?
This is a very interesting idea, and may possibly be an answer - no obvious leat right there, but there are countless drainage ditches nearby in the valley floor, not all of which seem to have been done by the council. A wheel could have been be sited in the flat ground at the base of the slope and it would make a good spot for a mill - it's very close to Blackstock Road recycling centre, if anyone knows the area. There was a 'Blyth Mill' less than a mile away on the Meers Brook in the mid-16th C.
I've found at least two possible in-line dams on the main tributary of the Meers Brook nearby, both of which are far too large to have been cut out by an old meander of the stream itself - the bank has clearly been excavated. Nearby those are a series of stepped rectangular or square pits on a gentle slope, each one connected to a higher one via a small gap that could have held a small board 'sluice' to let water run down the series. Again, I have no obvious explanation for these. However, my geologist friend also dug out some soil sample data from a BGS project from many years ago and found elevated levels of lead very close to this spot. Also elevated levels of calcium - my friend suggested the large line of pits may be connected with burning Peak District limestone for soil improvement. It's very close to the Norton-Hemsworth packhorse routes from Calver, etc.
To save me posting loads of images, here's two 'general' galleries of the area, which include shots of the features discussed. The old area of 'workings' with the high lead levels and the stepped pits are in this one - also shows a persistent leakage of water' from the stream bank that never, ever dries up. It all looks backfilled to me - photos 6-11. Also some interesting metal lumps further on:
https://pwhole.com/photo_galleries/private/CarrWood2/ The two large craters and two examples from the line of escarpment pits are in this gallery, though heavily overgrown at this time of year - photos 7,8 and 9 and then 14 and 15. A 'leat' would have to run down the steep slope adjacent to (or replacing) the wooden steps in photo 16. Any potential wheel would be in photo 17. Photo 18 could conceivably be a leat back to the stream.
https://pwhole.com/photo_galleries/private/LeesHallWoods1/ And I haven't even mentioned the stone-slabbed tunnel yet...
Thanks for the interest 😉