The Victory (East) prospect is located on an un-named tributary of the San Juan River, approximately 1.5 kilometres north of the junction of Clapp Creek and the San Juan River.

The area is underlain by Lower Jurassic Bonanza Group volcanics consisting of west-northwest striking, coarse flow rock (greenstone) which is considerably altered and rudely schistose. The showings are mainly in a massive dark grey impure limestone and marble, some of which is carbonaceous or graphitic, thought to be lenses or interbeds within the greenstone. The limestone appears to trend west and to be steeply dipping.

The showings consist of white quartz and carbonate veinlets that occur in an east striking shear zone, up to 1 metre in width. The veinlets are generally less than 3 millimetres in width, but some are as much as 8 centimetres wide. They are irregular in attitude but many strike eastward. Grains or masses of scheelite, as much as 2.5 centimetres across, are irregularly distributed in the veinlets. The veinlets also contain minor amounts of pyrite and locally, abundant stibnite.

The shear was explored in the late 1940's or early 1950's by a series of trenches and opencuts and by two adits aligned along a length of 200 metres. An upper adit has been driven west along the zone for 32 metres with at least 2 crosscuts driven off of it. One sample taken in a crosscut across 90 centimetres assayed 0.30 per cent tungstic oxide (Minister of Mines Annual Report 1952, page 216). Of several samples taken in the adit, most assayed trace or nil gold and silver. The lower adit is about 11 metres in length. Two diamond-drill holes were put down on the zone in 1969 (Philp, 1969).

In 1985, Tri-Pacific Resources completed a program of geochemical sampling, ground geophysical surveys and geological mapping. A chip sample, from a trench exposing the Pansy vein, assayed 6.6 grams per tonne over 1.7 metres (Assessment Report 14414). In 1995, a ground electromagnetic survey was completed on the area as the Dianne claim.