The Highland Boundary Fault is a geological fault that crosses Scotland diagonally from Arran and Helensburgh on the west coast to Stonehaven in the east. It separates two distinctly different regions: the Highlands from the Lowlands.
The geological history of Scotland can be understood as the result of two great tectonic events. The first was the formation of the global super-continent Pangaea, the second was the break-up of Pangaea to form the continents we know today.
The fault is the middle of three great faults which run from the south-west to the north-east across Scotland. In the north there is the Great Glen Fault, and in the south the Southern Uplands Fault. Further south, just over the border with England, is the Iapetus Suture, where the palaeo-Iapetus Ocean closed. These four major geological signs mark the ancient history of Scotland.
The Highland Boundary Fault was active during the Caledonian orogeny. This was a plate tectonic collision which took place from Mid Ordovician to Mid Devonian periods (520 to 400 million years ago), during the closure of the Iapetus Ocean.
The fault allowed the Midland Valley to descend as a major rift by up to 4000 metres and there was subsequently vertical movement. This movement was later replaced by a horizontal shear. A complementary fault, the Southern Uplands Fault, forms the southern boundary for the Central Lowlands.
References[change | change source]
- "Loch Lomond–Highland Boundary Fault". Scottish geology. Hunterian Museum and others. 2006-07-20. Archived from the original on 2007-09-27. Retrieved 2006-12-13.
- Worsley, Harry Loch Lomond: the loch, the lairds and the legends ISBN 978-1-898169-34-5 Lindsay Publications (Glasgow) 1988
- "Highland Boundary Fault". Gazetteer for Scotland. University of Edinburgh and Royal Scottish Geographical Society. Retrieved 2006-12-13.