The Low View showing is underlain by a sequence of volcanic and sedimentary rocks of the Lower Jurassic Telkwa Formation of the Hazelton Group. Host rocks consist of thick-bedded purple to green lapilli tuffs and volcanic breccias dip steeply northwest and are commonly cross-cut by intermediate dikes. Black mudstone and siltstone occur in the vicinity.

Low View consists of a 0.5 to 2 metres wide quartz vein and breccia zone containing disseminated pyrite in a major shear zone. Numerous stringers are also associated with the system. The vein margins are strongly bleached and locally have a propylitic halo extending to 10 metres from the shear, which may be an extension of the main shear zone hosting the High View and South Side Showings. Previous sampling gave values to 0.24 gram per tonne gold; two further rock samples were collected from the showing in 1987, one of which returned values of 0.39 gram per tonne and 30.3 grams per tonne silver (Assessment Report 16677). Anomalous selenium, tellurium and bismuth also occur.

See Main Creek (Coles) (093E 110) for related details. The Low View showing is over 2 kilometres east of the previously defined Coles vein system, a 4 kilometres long northwest trending zone that originally included showings from Camp View, to the northeast, to the East Side and South Side showings at the southeast.