The showing is located at an elevation of 152 metres on the north side of Blackwater Creek, 6.4 kilometres southwest of Juskatla.

A quarry was opened to obtain material for road construction but the material proved unsatisfactory for that purpose.

The area is underlain by a series of sub-aerial basaltic and andesitic flows with minor felsic flows and pyroclastics of the Upper Oligocene to Lower Pliocene of the Masset Formation, which form a plateau volcanic sequence up to 5 kilometres thick dipping gently to the northwest.

Bentonite occurs with rhyolite of the Tartu Facies (Bulletin 54).

The area was staked in 1986 by City Resources as the Linda claims, and prospected in 1987. No economic mineralization or significant assays were reported (Assessment Report 17083).