Hampsfell is the high point of the area and looks like limestone - in other words no catchment/any rain falling seeps in to the ground which usually equates to no enter-able caves higher up.
dunc said:I've no idea of the area, so may be wrong, but based on a quick nosey at the map...
Hampsfell is the high point of the area and looks like limestone - in other words no catchment/any rain falling seeps in to the ground which usually equates to no enter-able caves higher up. Usually in those circumstances the resurgence is the best point of entrance.
Mark said:Isn't Peak Cavern is a percolation water system with about 700ft of limestone above it
I wouldn't know, never been so have no idea where it is located. The entrance, from what I've seen in photographs appears reasonable in size, I doubt there's anything of reasonable size on Hampsfell!Fulk said:Hampsfell is the high point of the area and looks like limestone - in other words no catchment/any rain falling seeps in to the ground which usually equates to no enter-able caves higher up.
A bit like the Berger, then?
dunc said:I wouldn't know, never been so have no idea where it is located. The entrance, from what I've seen in photographs appears reasonable in size, I doubt there's anything of reasonable size on Hampsfell!Fulk said:Hampsfell is the high point of the area and looks like limestone - in other words no catchment/any rain falling seeps in to the ground which usually equates to no enter-able caves higher up.
A bit like the Berger, then?
When I said high ground I was thinking along the lines of UK (particularly the Dales of which I'm more familiar). As grahams suggested, Dowkabottom and the Sleets Gill area - large catchment, barely any known caves on the high ground (Dowka itself is more mid-ground than high and is merely a lucky collapse), Sleets Gill is lower down and a flood resurgence. So as I suggested a rising, didn't say flood rising or old rising like the Peak Cavern example mentioned by Mark, which I should have done, but forgot, would probably be best.
The problem with known old/open/dry caves, like Attermire, is that they are sometimes fairly well choked and quite often of archaeological importance.
As I said, don't know the area and was basing my answer on a quick look at a map, I won't bother next time, more hassle than it's worth!
But of course, a dig or two may yield results, caves are, as they say, where you find them...
As I said, don't know the area and was basing my answer on a quick look at a map, I won't bother next time, more hassle than it's worth!
Ignore my grumpiness, it's something that comes too naturally to me at times! I didn't make it clear what I was getting at, which is lack of entrances higher up rather than no actual cave passage.. But yes finding and gaining entry is the tricky part. There have been advances made at the risings in the wider area if my memory of Descent articles serves me right.Fulk said:Sorry, dunc, I wasn't trying to wind you up or piss you off, but to make the point that lack of obvious stream sinks down not mean lack of caves . . . though it makes them more difficult to find.As I said, don't know the area and was basing my answer on a quick look at a map, I won't bother next time, more hassle than it's worth!
Yes, outside of the main region (main Dales area) there's plenty of cave out there (like the miles of northern Dales stream passages or hidden away in the Morecambe Bay area etc), the big problem is finding a way in!I get the impression that there is more limestone outside the 'main northern caving region' than within it, some of it, as has been pointed out above, quite thick, and I feel that there is potential for (a lot) more cave to be found there.
danthecavingman said:Where is the culverted resurgence? Does it run under the railway - in which case I've probably looked at it whilst at work, unbeknowingly.
Found this as well whilst googling:
http://openplaques.org/plaques/10995
Dan.