Walk down towards the treeline |
A few metres further down the hill you get your first sight
of the rock on you left, a chunky undercut of rock offers some immediate bouldering.
Right here right now, as Jesus Jones song goes, looking at
the outcrop for the first time, I’m a tad underwhelmed. It’s getting dark, it’s
muddy, and the undergrowth is all spiky trippy. I’ve got a sweat on as the
bloody manflu is still in my system. 50/50 I’m going to sod off and come
another day, and yet, there is something about this place I find strangely beguiling
and defiantly not creepy. Slightly overgrown It’s a bit of a hassle to get
further down the hill towards the stream, edging round a buttress a glorious grand
edifice of 12 to 15m high tufa reveals itself. Its mid winter and has been
raining on and off few a few days but there are still some dryish bits. This
place has certainly still has possibilities. We went to Carreg-y-Byg a while
ago, another local venue. Kind of sad in a way that these previously precious local
outdoor spots have been neglected over the last few years, regular visits and vertical
traffic used to keep the rock groomed. Like to think we do our bit by getting
out during the week, but these places are now in need of some heavy duty
cleaning… We’ll see
Not my pic but gives you some idea of scale |
…………..It’s a cliff made of
tufa, a strange looking grey rock formed by the precipitation of spring water
containing large amounts of dissolved calcium. This causes calcium carbonate to
accumulate on moss, which continues to grow, pushing through the calcium.
The new growth is then also
coated and the process continues, building an ever larger rock.Carbon dating carried out at Southstone suggests that the rock began to form about 6,700 years ago. It looks soft and spongy but in places there are smooth, hard patches – this is travertine, formed when carbon accumulates directly on existing tufa instead of on moss.
The site was apparently a medieval cell for monks from the Abbey at Evesham. No doubt the caves that form in the rock and the source of the natural spring were valuable assets to establishing a monastic presence in the locality. In Norman times the chapel of
Personally having done some climbing, I am appalled that ‘rock climbers’; should even think about this as a climbing venue given the fragility rock and the damage that would be caused.
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