As you drive along the Uiskentuie Strand there is a steeply sloping, and in places scrub-covered, bank on the inland side. This is often (and wrongly) referred to as a raised beach. It is in fact the outwash from a glacier, a mass of stones and sand deposited by a river that flowed out of a glacier that once extended over this area. As the glacier retreated, it left all this behind. If you climb up the bank, you will see that it is up to 300 metres wide at the western end, with run-rig and old peat diggings on the top.
With the melting of the ice (once a kilometre or more thick), the sea-level rose as much as 30 metres, flowing over the bank (the trig point on it stands at 29 metres) and then gradually eroding it into the present-day steep slope as the sea-level fell. The final act of the sea, some 6,000 years ago, was to deposit a series of four gravel ridges close to the foot of the bank. There was once (1920s to 1930s and perhaps earlier) a nine-hole golf course on the ground between the bank and the road here. Even today, one occasionally sees a golfer practising his swing and knocking balls about, while passing motorists keep a very wary eye open for them!
Much of the above came from the booklet 'A Guide to the Geology of Islay' by Alex Maltman and others. Available to purchase at the INHT Centre.
Malcolm
 |
| Uiskentuie Strand with eroded bank of glacial outwash |
 |
| The top of the bank showing run-rig and, in the distance, old peat diggings |