Why this matters
Fintray Bay features sandstone and conglomerate rock formations, primarily from the Devonian period, around 380 million years old. These rocks were deposited in a fluvial and deltaic environment and are notable for their exposure of ancient sedimentary structures and fossilised plant material.
What is recorded here
Fintray Bay is shown as a bay on the public map of Argyll and Bute. The saved point is the map point or the centre of its mapped shape.
The public map does not by itself grant access. Check current paths, opening conditions and ownership before entering.