The Dom occurrence is located 1.5 kilometres southeast of Kennedy Lake, approximately 3.2 kilometres southwest of the former Brynnor Mine (MINFILE 092F 001) and 12 kilometres northeast of Ucluelet, B.C.

The area is underlain by an assemblage of dioritic to quartz dioritic rocks of the pre- Westcoast Complex are the oldest rocks in the area. Volcanic and sedimentary rocks of the Upper Triassic Vancouver Group and volcanic rocks of the Lower Jurassic Bonanza Group also occur in the area. The youngest rocks are Tertiary volcanics and coeval quartz diorite to quartz monzonite of the Early to Middle Eocene Tofino Intrusive Suite (previously Catface Intrusions, Personal Communication - N. Massey, May 1990). Quartz diorite and granodiorite of the Early to Middle Jurassic Island Intrusions have also disrupted strata in the area.

Locally, a shear zone from 2 to 3 metres in width strikes 020 degrees and dips 070 degrees east through Tertiary quartz diorite. The zone is characterized by brecciation and several lenses of argillic gouge (clay). Sericitic, chloritic and limonitic alteration also occur.

In 1984, Jasmine Resources completed a program of prospecting and geochemical sampling on the area as the Lakeview claim. During 1986 through 1988, Geo. P.C. Services Inc. completed programs of prospecting, geological mapping and geochemical sampling on the area as the Dom claim. Sulphide mineralization was not observed but samples assayed as high as 1.34 grams per tonne gold (Assessment Report 17400).

During 1995 through 2009, Consolidated Logan Mines Limited and later Logan Resources Limited, completed programs of prospecting, geological mapping, geochemical sampling and an induced polarization survey on the Lucky and Redford properties.

In 2011, Logan Resources Ltd. and joint venture partner Ridgemont Iron Ore Corp. conducted ground geophysics (including Dom) and drilling over the Redford property. The 2011 Ridgemont diamond drill program, east of Draw Creek and the Brynnor Pit, consisted of 61 holes totalling 10, 234.58 metres utilizing 29 drill pads. The program coverage was categorized into three zones: the Main, East and North zones. The drill results from the East zone confirmed that magnetite mineralization was similar in strike and dip to that found in the Main zone.