Burn O'Vat

Burn O'Vat is an example of a pothole, located close to Loch Kinord, near the village of Dinnet in Aberdeenshire, Scotland. FormationAround 16 000 years ago, the area surrounding Burn O'Vat was covered by a glacial ice sheet. As the area warmed around 14 000 years ago, the ice sheet began to melt, resulting in a torrent of meltwater that carried with it debris previously caught up in the glacial ice. This debris, consisting of rocks and boulders, is thought likely to be the most important component of the formation of Burn O'Vat. It is thought that a rock, from the meltwater stream, became lodged in a small hollow on the river bed, causing the meltwater to flow around it in a spiralling motion. This spiralling motion caused the bed underneath the rock to erode over a long period of time, creating a feature known as a pothole. Around 13 500 years ago the volume of meltwater decreased to such a level that the stream began to deposit more than it was eroding. This change resulted in the deposition of sand and gravel into the bottom of the pothole. It is believed that this sediment extends down around 5–7 metres, below the current ground level, though no-one can be certain of the true value. The pothole, known locally as 'The Vat', measures 18 metres across and 13 metres high, from present ground level.

Burn O'Vat is an example of a pothole, located close to Loch Kinord, near the village of Dinnet in Aberdeenshire, Scotland. FormationAround 16 000 years ago, the area surrounding Burn O'Vat was covered by a glacial ice sheet. As the area warmed around 14 000 years ago, the ice sheet began to melt, resulting in a torrent of meltwater that carried with it debris previously caught up in the glacial ice. This debris, consisting of rocks and boulders, is thought likely to be the most important component of the formation of Burn O'Vat. It is thought that a rock, from the meltwater stream, became lodged in a small hollow on the river bed, causing the meltwater to flow around it in a spiralling motion. This spiralling motion caused the bed underneath the rock to erode over a long period of time, creating a feature known as a pothole. Around 13 500 years ago the volume of meltwater decreased to such a level that the stream began to deposit more than it was eroding. This change resulted in the deposition of sand and gravel into the bottom of the pothole. It is believed that this sediment extends down around 5–7 metres, below the current ground level, though no-one can be certain of the true value. The pothole, known locally as 'The Vat', measures 18 metres across and 13 metres high, from present ground level.