Had a great meal after John & Margie had stormed in on Tuesday - they'd had a cracking down-wind sail from Port Ellen in F5/6 - comfort food, stew, followed by rice pudding, with sensible amounts of whiskey, G&T and Campari (and non-alc ginger wine for Nic - 'sob'). Then they took us to the pub, which seems to close when the last customers leave ... 2330 in our case. John & Margie were off south again at 0530 the
next morning, racing to get home before the next gale arrives - sleep is for wimps when tide and wind dictates. We didn't get up to see them off!
Today is sitting tight and riding out the gale, tied firmly with double ropes to the pontoon in Glenarm Marina - trouble is, the gale is blowing straight into the harbour entrance so we are rocking and rolling even here with the warps constantly squeaking and groaning. There's still jobs on the list, and we have to go food shopping inbetween the rain storms, however we actually have time to read our books for a while - such fun.
Don't know what you must have done to upset the weather. Still, after Friday it looks like you will get a chance to make a crossing on Saturday, good luck. It is about time you had an easy run.
ReplyDeleteBasalt forms hexagonal columns because cooling lava contracts, and hexagonal cracks are the most efficient way to relieve stress, allowing the rock to split into six-sided pillars. This happens as fractures propagate inward from cooling surfaces (top/bottom) at 120° angles, creating a pattern that perfectly tiles space with minimal energy, similar to a honeycomb.
ReplyDeleteWhile the Causeway's columns step out into the sea, and Fingal's Cave is a sea cave with similar columns, they are not physically connected by an unbroken underwater pavement; erosion and tectonic shifts separated them over millions of years.
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