The Paget showing is located on a southern facing slope over Hauk Creek, approximately 7 kilometres south of Caycuse on Cowichan Lake. The workings are located at 808 and 758 metres elevation and consist of an upper and lower tunnel.

The area is underlain by granite, diorite and granodiorite of the Early to Middle Jurassic Island Plutonic Suite.

The upper tunnel was driven at 070 degrees for 18.3 metres on a well-defined quartz vein. The vein is about 1.8 metres wide and is mineralized with arsenopyrite, pyrite, sphalerite and minor galena. High gold values have been reported, but the values must be sporadic because a sample from the dump containing arsenopyrite assayed negative results.

The lower tunnel, almost parallel with the upper tunnel, was also reported to be 18.3 metres long. The tunnel is flooded however and therefore cannot be explored. This tunnel was apparently in gravel and no ore was encountered.

In 1980, Union Miniere completed a program of soil sampling and prospecting on the area as the Lui claim. In 2013, the area was prospected as the Annular claim.