Peter Burgess
New member
Are there any Sub Brit members who might have information? Not all of Sub Brit devote all their time to bunkers and cold war relics.
Pitlamp said:Rob - my understanding is that brockram is a sort of limestone breccia cemented together by a sandstone matrix. It's Permian in age. (I can't remember but I think the Wookey conglomerate is lower Carboniferous and has a slightly different origin). Brockram was formed under desert conditions from angular limestone debris (originating from the proto-Pennines) accumulating on a plain. There are some small local caves formed in this rock but the tunnels in question are not natural.
There are also not so far away some very impressive aeolian sand dunes (e.g. an outcrop at Appleby in a field next to the river) which were contemporaneous with the alluvial fans. As you say, the Zechstein sea was to the east, and being normally enclosed and cut off from the Tethys Ocean, is now a major source of evaporites (e.g. Boulby Potash Mine).Pitlamp said:Thanks very much In cumbria and Simon.
Langcliffe: the clasts in the brockram are very angular suggesting they haven't been transported too far by water. The idea of occasional deluges flushing out wadis under desert conditions onto a plain makes sense. It's nice to think that lousy weather over the Pennines hasn't just been reserved for our generation eh? I have a paper on the geology of Kirkby Stephen but it's out on loan at the moment. (I think I'm right in thinking that on the far i.e. east side of the Pennines there was the Zechstien Sea in Permian times - that right?)
owd git said:Thanks guys great replies on the petrology mentioned, Les, did you have any further ref' on topic?
ta, O. G.
Pitlamp said:(I think I'm right in thinking that on the far i.e. east side of the Pennines there was the Zechstien Sea in Permian times - that right?)
Matt said:What a great idea for another film!
I can picture Steve G as the Chip Shop owner.
Watch this space.