My primary interest is in trying to better understand the formations of the phreatic systems we know to exist under Bradwell Moor/ Moss Rake and how they interplay with the mines - and where all the water went. It's still unclear (and probably unlikely) that any of the Bradwell soughs extended as far up the hill as the top of Hartle Dale/Hallam's Venture Mine/Sidebottom's quarry. Give the water-wear and phreatic passage we've seen in Raddlepits (and the probable similarities in Hugh Hill Grove/Rake Head from what I've heard), it suggests there is a quite a large-scale system, probably still active at depth, which feeds into Bagshaw. Possibly some Castleton-derived water travels SE across the moor edge to join here too.
I was always amazed how dry it was down there, and yet the walls in places indicate massive downward flow, probably through surface fissures, going straight through backfilled floors. It seems the miners were often oblivious or uninterested in speleology unless it was to their advantage (access/drainage/stacking space/ore processing), and so often may not have felt it sufficiently interesting to mention natural features. The exception being Dan Rose's 'Mosrake Head' survey of 1754, which shows a huge feature named 'Compas of the Oapnes' ('Extent of the Caverns') on the west side of the engine shaft, which would be close to the current wall. If it's as large as it appears, I would guess that there may well be a similar set of vein cavities on Moss Rake as there are on New Rake, Faucet Rake, Longcliffe, etc.
My problems is that apart from Raddlepits, I've been down very little else around there - Long Rake was closed just as I was about to go down, never seen Batham Pot, Shaft 'A', etc. So I'm wary of drawing too many conclusions from only my fragmentary evidence - my hope is that others with more experience have further or better evidence from other sites that can build up a more accurate picture.