The Hunter (Lot 4495) and Trapper (Lot 4494) are located at the head of Pool Creek about 10 kilometres east of the village of Camborne. The Hunter-Trapper showing is located 1000 metres south of Wide West showing (082KNW129).

The Lexington Mountain region is underlain by a series of metamorphosed Cambrian to Devonian sedimentary and volcanic rocks of the Lardeau Group which overlies the Lower Cambrian Badshot Formation in the east. The predominant structural features in the area are northwest trending and plunging overturned folds and regional semiconcordant to concordant faults. The strata within these structures are steeply east dipping with a variable plunge to the northwest.

Three distinct northwest striking limestone-chlorite schist contact zones spaced at roughly 1 kilometre intervals cross the property. The Index Formation (Lardeau Group) hosts similar mineralization within these zones and may represent either folded repetitions of the same contact or stratigraphic repetitions of similar depositional environments. The mineralization occurs as both disseminated and massive zones of galena, pyrite and sphalerite associated with dolomitized limestone and silicification invariably developed with siderite-rich zones containing hematite and magnetite localized along the limestone-chlorite schist contacts.

The Hunter-Trapper showing consists of intermittent disseminated to massive galena-sphalerite in a brecciated quartz-siderite-chlorite vein at the limestone contact with phyllite. Brecciated fault splays from the main zone host irregular quartz-carbonate veins and veinlets mineralized with galena-sphalerite-tetrahedrite. Alteration consists of sericitization of phyllite, bleaching and siderite alteration of limestone. The vein has been traced for 150 metres strike length.

A chip sample across a 1 metre wide quartz-siderite pod with massive to scattered sphalerite-galena analysed greater than 102.8 grams per tonne silver, 3.08 per cent lead and 4.38 per cent zinc (Assessment Report 17978).

This area was originally explored in the late 1800s and early 1900s when prospectors discovered widespread precious and base metal mineralization. During 1985-86, Consolidated Trout Lake Mines Ltd. and Jazzman Resources Inc. acquired interests in two separately owned but interlocking claim groups (termed the Lexington Creek and Lime Dyke Claim Groups). In 1985, prospecting and reconnaissance geologic mapping was carried out on behalf of Lardeau Development Corp. and Triple M Mining Corporation. In 1987 and 1989, Consolidated Trout Lake Mines Ltd. established a grid and conducted soil sampling, ground magnetometer and VLF-EM surveys, geological mapping and rock sampling and an airborne geophysical survey. During 2006 through 2009, Mineral Mountain Resources Ltd. completed programs of prospecting, geochemical (soil, silt, talus fines and rock) sampling and an airborne geophysical survey on the area as the Kootenay Arc property.