by josht111 » Sun Feb 05, 2012 12:41 pm
Hello chaps,
I realise this thread has been dead for a while. I have recently been working on research to do with the glacial history of Loch Brandy. I have interpreted The Causeway as a pro-glacial recessional moraine during the LLS stillstand or later deglacation/decay period (possibly ~12.4kya). One presumes the moraine was then modified and used later when Clova was populated, most probably for brown trout fishing. Although The Causeway is extremely well-molded, it seems like a pointless and mammoth task to build it. I wondered what your opinion was and whether you had much knowledge of the glacial history of the area?