The Old Ruminator
Well-known member
This week we pushed down to about 70m depth at Vurley. The current end is a boulder choke with a stream below. I noticed a very conspicuous red rock in the choke so brought it out.
Rock in situ.
It is very hard and shiny on the outside.
I tried to cut a bit off the end with an angle grinder but it was too hard. Used a flat chisel instead.
Magnified.
It looks a bit like a red brick. I was wondering about Old Red Sandstone but it is not like the ORS we had in The Silo in Reservoir Hole. This was transported into The Silo through an ancient stream sink in the gorge floor and would have been carried down from the pericline. Vurley is different. It is in a large closed depression, formerly a glacial lake, high up on the plateau. Some 15,000 years ago 7 metres of fine loess blew into the depression and sealed the cave. Possibly before that there was a lot of infill into an open cave which has now partially washed out. You can see the choke has been washed clean. Vurley lies on faults associated with The South West Overthrust and is in Clifton Down Limestone.
Rock in situ.
It is very hard and shiny on the outside.
I tried to cut a bit off the end with an angle grinder but it was too hard. Used a flat chisel instead.
Magnified.
It looks a bit like a red brick. I was wondering about Old Red Sandstone but it is not like the ORS we had in The Silo in Reservoir Hole. This was transported into The Silo through an ancient stream sink in the gorge floor and would have been carried down from the pericline. Vurley is different. It is in a large closed depression, formerly a glacial lake, high up on the plateau. Some 15,000 years ago 7 metres of fine loess blew into the depression and sealed the cave. Possibly before that there was a lot of infill into an open cave which has now partially washed out. You can see the choke has been washed clean. Vurley lies on faults associated with The South West Overthrust and is in Clifton Down Limestone.