This is Project Copper Coast swim number nine. Yes, I know I’ve haven’t put numbers on them until this but I only foresaw one swim after this to finish.
I first visited Ballydowane as a small child with my family, and never knew the name nor location, until I visited it over 25 years later, looking for surf and recognised it instantly, the high red surrounding cliffs, the small bay and the narrow boreen down to it, that had remained present from childhood dreams. It’s another gorgeous little cove where apparently there’s something called a ripple current according to the sign. 🙂
Years later, after the surf hunting, at the start of my second year of open water swimming, Dee and I visited there on Sunday morning for my first non-wetsuit swim of the year in spring. It’s from that visit (and one other) that I still recall the physical fear that I felt before getting in the freezing water.
It was also a rough day and on trying to immerse myself, a wave washed over me, and took the decision out of my hands. I recall like it was yesterday, swimming across the cove, the burning and acid-like sensations over my whole body, until I went numb. On exiting the water, exhilarated and frozen, after 15 minutes, I discovered Dee and Luis hadn’t been able to see me due to the waves, and thought I was gone, drowned. At which point I made the situation worse by starting to hrr-hrr (laugh) through frozen jaws. Mr. Sensitivity.
I know the outside of the cove can have a current across it, but not strong enough to stop progress and from the swim from Bunmahon where I’d encountered the start of one, I assumed it flowed west, though I would be heading out across the far side anyway.
It was an hour or two after high tide. Bare northerly offshore breeze, so the water was completely clear and flat with a partly sunny sky. Out past the rocks on the right, this stretch of coast doesn’t jut outwards, instead it’s more concave, therefore I didn’t expect too many difficult currents.
The cliffs at this end of the Copper Coast are more attractive, there seems to be a slightly different range of colours and shapes but I though it might only be because it’s all new water so I’m far more conscious of it.
However on looking at a simple geological map of Waterford, it transpires that yes indeed, the rocks change east of Ballyvoyle Head from older Ordovician (volcanic, shale and sedimentary rocks) to younger Devonian (sandstones and siltstones).
I’d checked the OSI map, and it seemed from it that there are six promontories between Ballydowane and Ballyvooney, if I was to make it that far, which was by no means certain. But of course from the water, it seemed like nine of ten. It was thirty minutes before I could easily see Gull Island, the largest one of that name on the Copper Coast, (there are a few) on the far side of Ballyvooney.
Having passed what seemed many more than six promontories, I didn’t reach the outside of Ballyvooney Cove until 55 minutes, once again a cutoff time, since I also knew that I would need more time when I returned to Ballydowane.
After I turned, instead of curving back around the coast as I had on the outward trip, I swam directly across toward St. John’s Island and the thin vertical needle of the unnamed rock beside it, and I was able to hold a nice straight line by keeping the sky behind the rock spire.
I passed the turn into Ballydowane and swam across the cove, slowing down as I encountered the adverse current. I needed to overlap the finishing point of the previous day, to meet my own criteria that I’ve swam every metres of the coast.
I turned into the side of St. John’s island, where I stopped previously, then swam around the island to the east side on the other side of a reef, where, I realised, the island was virtually hollow, a huge cave being scooped out of its side. My goal was to see if I could swim around this so-called island so I swam around and behind another long reef extending outward and into the area between the island and the edge of the cove, only to discover a jumble of rocks. Only at the highest spring tide does it really become an island, and even then it’s unlikely to be navigable by a swimmer. So I swam back around the reef to have a look at the cave weaving though the reefs across the entrance.
And I realised that it wasn’t just a small cave resulting from a collapse of the sandstone but a cave and tunnel leading through the island. The combined tunnel and cave was 50 to 75 metres long and a total joy. This was no narrow tunnel, but it opened inside to a wider cavern with echoes from the pneumatic sound of water being compressed into nooks and crannies and the washing around of the water. It was bright, because the eastern-side entrance was wide enough to allow in sufficient light from the sunshine which reflected around the rocks and it was utterly magical. Only weeks ago the only caves I’d ever swam into were the few beneath Great Newtown head, but by now I’ve swum through a range of caves, arches and tunnels, leading to this stunning location.
Exiting the tunnel I realised why I hadn’t seen it. There’s a reef completely hiding the entrance for the low-level view of a swimmer, and since it faces west, it can’t be seen from the cove. It’s probable canoeists know about it, no-one beyond that. And now you know and I can’t recommend visiting it highly enough.
From there into the beach and done, another 6 k. A hike up the cliff to see if I could get a photo of the coast and by going out to the edge of the one of the promontories I was able to photograph the tunnel .
Project Copper. Almost done.