On Scotland's northeastern coast, close to Portknockie, lies a natural sea arch known as Bow Fiddle Rock. Because it looks like the tip of a fiddle bow, it got its name.
Quartzite, a metamorphic rock that was formerly quartz sandstone, makes up its composition. This rock is a component of the Cullen Quartzite formation, which is located between Cullen and Buckie along the shore. The formation, which is around 2,400 meters thick, was formed between 1,000 and 539 million years ago during the Neoproterozoic Era.
When the ancient continents of Avalonia and Laurentia met during the Caledonian orogeny, these rocks were folded. Later, they were exposed at the surface where the current structure was eroded by the water and weather.
As the sun sets over the beach, Bow Fiddle Rock in Portknockie is a breathtaking sight to see. Explore the area's hiking paths, locate your own little piece of heaven, and watch for seabirds that nest there, including herring gulls, great black-backed gulls, and lesser black-backed gulls.
Experience luxury and adventure together as you travel some of Europe's most breathtaking rail routes, passing through well-known tourist spots and taking in stunning landscapes, tunnels, and mountains.
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