Our first stop was Carrickfergus Castle. Even though it was early in the tour, I had already given up on listening to the tour guide, so I'm not sure why this castle is significant, but it sure is cool looking!
Our next stop was Carrick-a-Rede rope bridge. This rope bridge was originally used by fisherman to get over to the island to fish, but today it has been reinforced and used as a tourist attraction. I chose not to cross the bridge, but that left me perfectly placed to take pictures of everyone else:
| See the rain on the lens? |
"Legend has it that the Irish warrior Fionn mac Cumhaill (Finn McCool) built the causeway to walk to Scotland to fight his Scottish counterpart Benandonner. One version of the legend tells that Fionn fell asleep before he got to Scotland. When he did not arrive, the much larger Benandonner crossed the bridge looking for him. To protect Fionn, his wife Oonagh laid a blanket over him so he could pretend that he was actually their baby son. [...W]hen Benandonner saw the size of the 'infant', he assumed the alleged father, Fionn, must be gigantic indeed. Therefore, Benandonner fled home in terror, ripping up the Causeway in case he was followed by Fionn."
This makes some sort of sense, as there are similar stones on an island on the coast of Scotland. Plus, there's something about the natural beauty and wildness of Ireland and Scotland that makes you feel like the stories could be true, like this is a land where giants could have existed. Everything seems possible.
Or you could believe the slightly more scientific explanation:
"Some 50 to 60 million years ago, during the Paleogene period, Antrim was subject to intense volcanic activity, when highly fluid molten basalt intruded through chalk beds to form an extensive lava plateau. As the lava cooled rapidly, contraction occurred. Horizontal contraction fractured in a similar way to drying mud, with the cracks propagating down as the mass cooled, leaving pillarlike structures, which are also fractured horizontally into "biscuits". In many cases the horizontal fracture has resulted in a bottom face that is convex while the upper face of the lower segment is concave, producing what are called "ball and socket" joints. The size of the columns is primarily determined by the speed at which lava from a volcanic eruption cools. The extensive fracture network produced the distinctive columns seen today."
| We stopped on the side of the road to take pictures of this ruined castle. |
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