It is a glacial-formed glen, with near vertical sides along part of the landform.

[1][2] The Little Eachaig River flows out of the glen, joining the River Eachaig and flows into the Holy Loch.

The Tarsan Dam is the other notable feature in the glen.

[3][4] There is also the buildings at risk (unlisted) ruins of a powder mill, built c. 1840, in Clachaig.

This Argyll and Bute location article is a stub.