Looking down at the top of the columns of rocks. |
Relaxing on the basalt columns |
The geological explanation of how the Causeway was formed is that 65 million years ago the landscape was covered in plants. There were gently rolling hills laying on a bed of limestone. Then about 60 million years ago the earth’s plates began to move away from each other. Molten lava from the earth’s core began to pour out through the cracks. The lava became hard and formed layers of basalt rock. Some of the lava poured into a river valley where it cooled very slowly. As it cooled, it cracked evenly, just like mud at the bottom of a puddle. It formed the regular basalt columns that make up the Causeway. Like honeycomb, nature tends toward stable structures, such as hexagonal stacks.
Part of the Giant's Causeway called the "Giant's Organ." |
The legend of the Giant’s Causeway goes something like this: There was an Irish Giant named Finn MacCool who built a Causeway all the way to Scotland to see his rival, a giant named Benandonner. When Finn got to Scotland he saw how big Benandonner was and ran all the way home afraid that he could not defeat such a huge giant. When he explained the situation to his wife, Oonagh, she promptly came up with a solution. She dressed Finn as a baby and put him in a baby carriage. When Benandonner came knocking at their door, Oonagh explained that Finn was out, but that Benandonner was welcome to come in and wait, so long as he did not wake the baby. When Benandonner got a glimpse of the huge baby he could only imagine the size of its father, Finn MacCool. He left promptly, racing back along the Causeway, tearing up the stones as he went, stopping Finn MacCool from following him. To this day the only Causeway stones that remain visible are those in the North of Ireland and on the Isle of Staffa in Scotland.
The Cobbler Do you see me on the rocks? |
Me at the Giant's Causeway |
Hope you're doing well!
Mrs. McMillan
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