Glen Tilt
Adapted from Wikipedia · Discoverer experience
Glen Tilt (Scottish Gaelic: Gleann Teilt) is a beautiful valley located in the far north of Perth and Kinross, Scotland. It starts near the border of Aberdeenshire and stretches southwest, ending near the town of Blair Atholl. The valley is home to the river Tilt, which flows for 14 miles before joining another river called the Garry. Along its path, the Tilt meets smaller streams like the Tarf and the Fender, which create lovely small waterfalls.
One interesting part of Glen Tilt's history happened in 1847. A nobleman named George Murray, 6th Duke of Atholl tried to keep people from entering the valley, but a group called the Scottish Rights of Way Society helped make sure the public could still enjoy this beautiful place.
The eastern part of Glen Tilt is dominated by a huge mountain called Beinn a' Ghlò, which has three tall peaks known as Munros. These peaks are named Càrn nan Gabhar, Bràigh Coire Chruinn-bhalgain, and Càrn Liath.
Glen Tilt is also known for its marble, which is sometimes mined there. The unique rock formations in the area have interested scientists who study the Earth, known as geologists. Historically, the glen was part of the county of Perthshire, with Perth being the main town of that area.
Royal banquet for James V, 1532
A story from the 1570s tells of a special meal made by the Earl of Atholl for James V. This was to welcome a special guest from the Pope. It happened in 1532 in a wooden building made to look like a castle in Glen Tilt. After the meal, the building was burned down.
Later, in August 1564, Mary, Queen of Scots visited Glen Tilt and sent a letter from there to her friend Colin Campbell of Glenorchy.
History of Geology
James Hutton, a famous geologist, visited the glen in 1785. He discovered that some rocks called granite were formed from cooled molten rock, not from water, which changed how people thought about how rocks form. Another scientist, John Clerk of Eldin, made drawings of the area near an old bridge that no longer exists.
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