The Bonnie Banks
Loch Lomond looking west from Conic Hill on the West Highland Way above Balmaha. The string of islands on the left and the alignment of Conic Hill indicate the line of the Highland Boundary Fault the geological feature which separates the central lowlands from the highlands of Scotland. This fault runs from Stonehaven on the east coast all the way across Scotland until it is lost somewhere west of Helensburgh. It is still active and the Crieff/ Comrie section is the most seismically active area in Britain although most tremors are very low on the Richter Scale. On the right far horizon is Ben Lomond the most southerly Munro (mountain over 3000 feet) in Scotland and after Ben Nevis (the highest one in both Scotland & the UK) the most climbed.
The Bonnie Banks
Loch Lomond looking west from Conic Hill on the West Highland Way above Balmaha. The string of islands on the left and the alignment of Conic Hill indicate the line of the Highland Boundary Fault the geological feature which separates the central lowlands from the highlands of Scotland. This fault runs from Stonehaven on the east coast all the way across Scotland until it is lost somewhere west of Helensburgh. It is still active and the Crieff/ Comrie section is the most seismically active area in Britain although most tremors are very low on the Richter Scale. On the right far horizon is Ben Lomond the most southerly Munro (mountain over 3000 feet) in Scotland and after Ben Nevis (the highest one in both Scotland & the UK) the most climbed.