Just thought I'd provide an update for those who couldn't come.
We arrived at the DE-OV link to discover the water about 5-6 foot lower than normal and that we could pass into cwm's OV with ease and dryness.
The water was still dropping (having been dropping for about 30 hours) but was almost at the intake.
With the level dropped it was easier to see the lay of the land on the chamber floor and became obvious that the intake was not at the lowest point.
Edwin rather heroically got into the water which went up to his nose at the deepest point, and he got the strainer down to the floor at this point so now it really is at the bottom.
Right now then I would expect the chamber to virtually empty.
So what did we see?
The level progressing towards the incline was just emerging but of course it slants downwards slightly so progress that way was not possible at that time.
Particularly satisfying was the presence of the level going the other way (east), which going slightly uphill had enough airspace for Edwin to go for a swim along it. He went a reasonable way but opted to come back before finding the end. On the map this level is shown as blind, and almost certainly is but you never know.
Of interest (to me at least) in this level were some well formed stalactites on the roof. This roof level was certainly below the normal standing water surface level.
These could not have formed when the tunnel was "dry" as although the tunnel was cut about 120 years ago, it has been submerged for at least 115 of those. Therefore my conclusion is that this tunnel *must* have retained some air space under pressure. I remember having this debate a couple of years ago, as to whether this phenomena was possible over many decades.
Anyway - not much else to report at this time.
MM
Beneath my steely exterior beats the heart of a dashing hero