Why this matters
Stravanan Bay features sandstone and limestone cliffs formed during the Carboniferous period, around 300 to 360 million years ago, through sedimentary deposition in shallow marine environments. The area is notable for its well-preserved fossil content and coastal erosion patterns that expose layered geological formations.
What is recorded here
Stravanan 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.