No 171 May 1962
B
Monthly Journal Of The Bristol Exploration Club
B Vol. XVI No. 5
Taking advantage of a recent overhaul of the typewriter on which the B.B. is typed, we have had some cryptic characters added to the keyboard so that it is now possible, amongst other things, to type phrases like 'speleological manoeuvres' and similar gems of the English language. It also opens up a whole new field for original spelling mistakes, a subject for which the B.B. is noted. Once again, we have twelve pages. At one time, there was a ‘queue’ to join before stuff could be considered for publication. This has now vanished, and so the odd article would not come amiss. Whitsun Trip to Cornwall. Owing to the fantastic success of the Easter trip to this foreign land, and in spite of the damage done to vehicles, the trip is to be repeated at Whitsun. Anyone who is interested should get in touch with any of the Belfry Regulars.
DON’T FORGET THE BARBECUE IS ON JUNE 16 _______________________________________________________________________________________
CUTHBERT’S GEOLOGY (Extracted from a letter to B.M. Ellis from D.C. Ford ) When I wrote up the geology of St. Cuthbert's Swallet for Caving Report No. 7, I’d not finished work on it and so have a certain amount of revision of the ideas you've published. The controlling fault - Lake Chamber to the Duck - is not the Stock Hill Fault mentioned in the geological survey, but one sub-parallel to it to the west. It is probably in the same system. If this St. Cuthbert's fault be extended south east of the duck (bearing in mind that it might not, in fact, extend any further) it passes through Hunters Hole more or less parallel to the principal alignment of the lower cave, and about fifty feet south of it. Interesting. The controlling bedding planes in Catgut (above T-Junction) are not within the twenty foot plane of the Rabbit Warren as I wrote, but lie ten and thirty feet below (two different bedding planes). The extension then runs through higher beds to get on to the main line, so to speak, at the Sewer bedding plane. This performance is not typical of Mendip phreatic behaviour and is almost non-union activity. The main water supply during stages 1 and 2 of my sequence of development came; it emerges, from the Rocky Boulder area. This should “go” much more than it has done, back up to the surface. However, I won’t guarantee that it is not (a) solidly choked, (b) collapsed anyway. At present I am working on the south eastern parts of the cave and wondering about possible ways on, barring the sump. It doesn't look very good because every bit of passage plays a part in feeding into the Lake-Gour rift. Nothing seems to bypass it higher up and the best bets are in the rift itself. One never sees the floor of the rift. This is buried to a depth that could run into many tens of feet locally and the way on could be down it somewhere. So get digging!