Notes and points of interest
Porth yr Ogol the large Car Park
on this spot is a popular gathering point for cavers and is well
provided with toilets, a shop and picnic tables. A short walk down
steps and a rough slope takes you to the fscinating scene of a river
flowing into a large cave and disappearing into the darkness. You
may see teams of potholers and cavers gointo into the cave, but
it is not wise to follow them unless you are with a properly trained
and equipped caving team.
Pwll Du the stream that emerges from
underground at Pwll Du is such a minor tributory that the Afon Nedd
scarcely notices its arrival. But the almost circular bay that this
little stream has created is a wonderfukl tribute to the power of
water. Definitely a sight worth stopping for.
Pwll-y-rhyd the river Afon Nedd disappears
underground at this point only to re-emerge from its gravel bed
further downstream (earlier in this walk). In some conditions this
vanishing trick happens quite calmly, but at other times is becomes
an impressive torrent.
Resurgence is the name applied to
the point where an underground stream re-emerges as surface water.
Shake Holes occur often in limestone
country and simpy look like random depressions in the ground (sometimes
almost cone/funnel shaped). They are points where water seeps into
underground systems, gradually dissolving the limestone over years
and centuries. Where a stream flows into them they turn into Sink
Holes.
Sink Holes are the points where flowing
water (river or stream) suddenly disappears into underground systems.
They are common features of limestone country and may be almost
uneventful points of change or they may be dramatic waterfalls plunging
into the darkness below.
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