The Relief occurrence is located just south of Como Lake on the south side of the road, about 3 kilometres north of the community of Atlin.

The showing is hosted within dark green, massive andesites to basalts of the upper Mississippian to Permian Nakina Formation (Cache Creek Complex). These rocks are often referred to as greenstone. The occurrence lies just south of the Jurassic Fourth of July Creek batholith which covers an area of 780 square kilometres north and northwest of Atlin. It is composed primarily of hornblende-bearing diorites to quartz diorites.

Mineralization occurs in quartz stringers up to 30 centimetres wide sparsely mineralized with pyrite. The volcanic country rock is reportedly "carbonate altered" and some references to magnesite are made; the geology and mineralization of this occurrence are poorly documented. The veins are said to strike 040 degrees, dipping 60 degrees to the southeast.

Samples taken in 1904 reportedly averaged around 9 grams per tonne gold. In 1931, a dump sample analyzed trace gold and 10 grams per tonne silver. The property was worked primarily in 1904 with a short shaft and drift but has not been worked significantly since.

In 1988, prospecting and sampling of the old workings was performed by B.T. White.

In 2005, Blind Creek Resources Ltd. collected 15 soil and 23 rock samples for analyses. In 2006, Blind Creek Resources Ltd. conducted exploration on their Como Lake property claims which covers the Relief showing. An area of about 1500 hectares was prospected and a total of 30 rock samples, of which one was float, and 32 soil samples were collected. In 2008, Blind Creek Resources Ltd. conducted geological observations and collected 45 soils, 3 silts and 11 rocks, primarily around the outside borders of the claims.