It is composed of Quartzite, a metamorphic rock which was originally quartz sandstone.
Read more. the view was amazing very cold but what do u expect from Scotland very windy nearly blew away lol the bow fiddle rock was beautiful only but even better in the morning sunset.
It was formed by erosion of a rock called Cullen Quartzite.
Round the headland to the south the arch called the Whale’s Mou’ is another example, and there’s a series of caves east of Findochty (accessible only at low tide – take care not to get cut off ). Not long before you're overlooking this splendid rock formation. Helpful.
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This is one of many different quartzites found in Scotland. It overlooks the Moray Firth with a history dating back to 1677. Sco wrote a review Jan 2020. It is so called because it resembles the tip of a fiddle bow. Wellies were ideal for the Certainly worth visit.If you get a chance, take a stroll along the cliff path to see the Bow Fiddle Rock....Great picture opportunity of a natural phenomenon the view was amazing very cold but what do u expect from Scotland very windy nearly blew away lol the bow fiddle rock was beautiful only but even better in the morning sunsetOn our way back from the splendid Craigmin Bridge by Drybridge, Buckie, we stopped here for a fine wee coastal walk. Bow Fiddle Rock off the coast of Scotland is an amazing place to visit. This is the version of our website addressed to speakers of Sorry, there are no tours or activities available to book online for the date(s) you selected. Portknockie Coastline by Mike Stephen, on Flickr Bow Fiddle Rock by Mike Stephen, on Flickr The sloping layers can be traced on to the land from which you first see the Rock. From further east along the clifftop, you get a completely different view, where you can see that the Rock is a long sloping slab of rock.Look for other caves nearby along the coast with a similar slope, formed where the sea and weather have eaten away parts of the rock. More and more sediment piled up on top until the sandstone was buried several kilometres down, and as the pressure from overlying rocks built up, and heat from the centre of the Earth rose into the crust, the grains of silica in the sandstone were crushed and welded together to form the much harder rock called quartzite.Movements of the tectonic plates which make up the surface of the Earth also had an effect. The quartzite is about 2500 metres (8000 feet) thick and makes up the coastline from Buckpool (the west end of Buckie) to Logie Head, the main headland east of Cullen.Quartzite is a metamorphic rock, which means that it has been altered in nature by heat or by pressure. It was originally sandstone laid down in layers under the sea around 750 million years ago. The Bow Fiddle Rock is found near to Portknockie, a small cliff top fishing village on the Moray coast between Findochty and Cullen.
Bow Fiddle Rock is a natural sea arch near Portknockie on the north-eastern coast of Scotland. Please try again later. Bow Fiddle Rock is a natural sea arch near Portknockie on the north-eastern coast of Scotland. Scotland lay on the edge of an ancient continent called Laurentia, and another continent called Avalonia, on which what is now England lay, was carried towards Laurentia and eventually the two continents collided. It was formed by erosion of a rock called Cullen Quartzite. It is so called because it resembles the tip of a fiddle bow. You can drive and park fairly close to the beginning of the walk. I love the rugged rock formation named Bow Fiddle because of it’s similarity to the bow of a violin.
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