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Company Overview

Honey Badger Exploration Inc. is a mineral exploration company whose prime focus is the exploration and development of its Gold and Base Metal Properties in Canada. Honey Badger uses the most current and innovative exploration and geological models to direct the application of leading edge exploration techniques. Notwithstanding, our experience tells us that we must also use old style prospecting and basic field work combined with the latest in technology. Our current focus is in the prolific Gold region of Northern Quebec.

Radisson, Quebec

The Radisson Project is a JV 10,698 hectare district scale property in the heart of the emerging world class Gold Camp of Northern Quebec showing promising and widespread gold, copper and silver values. A gold-bearing trend of over 8km was identified on the Radisson by Noranda in 1992-93, with historic channel samples ranging from 5.5 to 9.8 g/t Au. The Discovery Lake discovery is encompassed within the Radisson property (currently held by Amesco). This polymetallic deposit contains gold, silver, copper lead and zinc mineralization, including high-grade values of 34 gpt gold and 340 g/t Ag. The discovery zone appears to be situated near the basalt/metasediment contact (same setting as Goldcorp’s Eleonore/Roberto deposit) that extends onto the Radisson property for multiple kilometers to both the east and west. Current projects underway include Soil and Rock Sampling on the eastern portion, Ground Magnetic Survey and Geological Mapping of historical showings.

Limonite Creek, B.C.

The Limonite Creek Project is a 100% owned 1050 hectare property in the westernmost part of the Telkwa Pass about 50kms SW of Smithers, British Columbia with exploration targets of high sulfidation (HS) (Cu, Mo, Au) porphyry systems and high sulphidation epithermal (Au, Ag, Cu) systems. A large zone of hydrothermally altered rocks strikes east northeasterly across the property grid area with many occurrences of rocks displaying advanced argillic alteration mineralogy, similar to that which occurs with HS Gold - Copper deposits throughout the world. Historical Diamond Drilling has demonstrated the continuation of the hydrothermal alteration to depth, as well as continuity on strike with intermittent exposure over a length of 1100m and a width of 850m. This zone is also extensively and complexly faulted. A zone of aluminous alteration occurs adjacent to and north of the zone of argillic alteration. Typically characterized by the presence of minor to significant amounts of corundum, andalusite and, at Limonite Creek, lazulite and reflects a higher temperature environment of alteration than exists in argillic alteration. Aluminous alteration is considered to have developed deeper in the hydrothermal system than argillic alteration and may be associated with a porphyry copper environment, similar to the El Salvador deposit in Chile.