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Shots taken during the 2018 edition of the Enchanted Forest event in Faskally Wood, near Pitlochry, Scotland.

Tags:   DMeadows DavidMeadows DavidAMeadows Scotland Faskally Wood Woodland Perthshire Pitlochry Night Light Lighting Lamps Lamp Event Sound Displays Path Lanterns Crowd Low Silhouette Silhouettes Forest

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Shots taken during the 2018 edition of the Enchanted Forest event in Faskally Wood, near Pitlochry, Scotland.

Tags:   DMeadows DavidMeadows DavidAMeadows Scotland Faskally Wood Woodland Perthshire Pitlochry Night Light Lighting Lamps Lamp Event Sound Displays Path Lanterns Crowd Low Silhouette Silhouettes Forest

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Shots taken during the 2018 edition of the Enchanted Forest event in Faskally Wood, near Pitlochry, Scotland.

Tags:   DMeadows DavidMeadows DavidAMeadows Scotland Faskally Wood Woodland Perthshire Pitlochry Night Light Lighting Lamps Lamp Event Sound Displays Path Lanterns Crowd Low Silhouette Silhouettes Forest

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"Bow Fiddle Rock is a natural sea arch near Portknockie on the north-eastern coast of Scotland. It is so called because it resembles the tip of a fiddle bow.

It is composed of Quartzite, a metamorphic rock which was originally quartz sandstone. This rock is part of the Cullen Quartzite formation which is seen along the coast between Buckie and Cullen. The formation is some 2,400m thick and dates from the Neoproterozoic Era, 1,000 to 541 million years ago.

These rocks were folded when the ancient continents of Laurentia and Avalonia collided during the Caledonian orogeny. They later became exposed at the surface where sea and weather eroded the structure seen today." (Source: en.wikipedia.org/wiki/Bow_Fiddle_Rock )

Tags:   DMeadows DavidMeadows DavidAMeadows Scotland Bow Fiddle Rock Portknockie North East Sea Seaside Coast Coastal Coastline Horizon Waves Water Seas Arch Archway Formation

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Bow Fiddle Rock is a natural sea arch near Portknockie on the north-eastern coast of Scotland. It is so called because it resembles the tip of a fiddle bow.

It is composed of Quartzite, a metamorphic rock which was originally quartz sandstone. This rock is part of the Cullen Quartzite formation which is seen along the coast between Buckie and Cullen. The formation is some 2,400m thick and dates from the Neoproterozoic Era, 1,000 to 541 million years ago.

These rocks were folded when the ancient continents of Laurentia and Avalonia collided during the Caledonian orogeny. They later became exposed at the surface where sea and weather eroded the structure seen today. (Source: en.wikipedia.org/wiki/Bow_Fiddle_Rock )

Tags:   DMeadows DavidMeadows DavidAMeadows Scotland Bow Fiddle Rock Portknockie North East Sea Seaside Coast Coastal Coastline Horizon Waves Water Seas Arch Archway Formation


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