The Nub North occurrence is located at an elevation of approximately 1900 metres on a northeast-trending ridge, approximately 7 kilometres northwest of Budd Lake.

Regionally, the area is situated within a Mesozoic volcanic arc assemblage, which lies along the eastern margin of the Intermontane Belt, a northwest-trending belt of Paleozoic to Paleogene sediments, volcanics and intrusions bounded to the east by the Omineca Belt and to the west and southwest by the Sustut and Bowser basins.

Permian Asitka Group crystalline limestones are the oldest rocks exposed in the region. They are commonly in thrust contact with Upper Triassic Stuhini Group andesite flows and pyroclastic rocks, and marine sedimentary and volcanic rocks of the Lower to Middle Jurassic Hazelton Group. These rocks have been intruded by plutons and other bodies of the mainly granodiorite to quartz monzonite Early Jurassic Black Lake Suite and are in turn unconformably overlain by or faulted against Lower Jurassic calc-alkaline volcanics of the Toodoggone Formation (Hazelton Group).

The dominant structures in the area are steeply dipping faults that define a prominent regional northwest structural fabric trending 140 to 170 degrees. In turn, high-angle, northeast-striking faults (approximately 060 degrees) appear to truncate and displace northwest-striking faults. Collectively these faults form a boundary for variably rotated and tilted blocks underlain by monoclinal strata.

The area is underlain by undivided Lower to Middle Jurassic Hazelton Group volcanic rocks cut by feldspar porphyry dikes. Strong regional structures trend north-northwest and are accompanied by propylitic and argillic to advanced argillic alteration.

Locally, variably propylitic- to potassic-altered hostrocks described as dacites, siliceous volcanic rocks, andesitic augite porphyry and feldspar crystal tuffs host a gossanous zone with quartz-calcite and quartz-epidote-chlorite veins and breccia containing pyrite, sphalerite, galena, chalcopyrite and trace bornite mineralization. Limonite and malachite alteration are also noted. The veins, breccias and shears trend primarily north-northwest. Another zone of similar mineralization is reported approximately 200 metres to the northwest.

In 1999, a 0.60-metre chip sample (DR-39) of silicified and quartz-carbonate veined andesite assayed 325.3 grams per tonne silver, 3.63 grams per tonne gold, 0.15 per cent lead, 0.88 per cent zinc and 7.48 per cent copper, whereas a sample (DR-41) taken a short distance to the southeast from a 5-centimetre wide quartz-carbonate vein yielded 57.3 grams per tonne silver, 7.41 grams per tonne gold, 0.19 per cent copper, 1.26 per cent lead and 1.50 per cent zinc (Assessment Report 26251). Also, at this time, a sample (DB-25) from a 10-centimetre-wide quartz-carbonate vein, located approximately 200 metres to the northwest, assayed 2.33 grams per tonne gold and 5.40 grams per tonne silver (Assessment Report 26251).

In 2004, a grab sample (185428) of gossanous material with chalcopyrite, malachite and limonite assayed 120.6 grams per tonne silver, 0.135 per cent zinc and greater than 1.00 per cent copper, whereas a 1.00-metre chip sample (185875) yielded 0.35 gram per tonne gold, 100.0 grams per tonne silver, 0.345 per cent zinc and greater than 1.00 per cent copper (Assessment Report 27634).

Work History

In 1980 and 1981, Serem Ltd. completed programs of prospecting; geological mapping and rock, silt and soil sampling on the area as the Nub Mountain 1-5 claims. During 1987 through 1989, Toodoggone Gold Inc. completed programs of geological mapping, geochemical (heavy mineral, rock, silt and soil) sampling, trenching and a 248.0 line-kilometre airborne magnetic and electromagnetic survey on the area as the Fine 1-4 claims.

During 1999 through 2004, Stealth Minerals Ltd. completed programs of prospecting; geological mapping and rock, silt and soil sampling on the area as the Nub claims.

During 2016 through 2018, Amarc Resources Ltd. completed programs of soil and rock sampling, geological mapping, 115.0 line-kilometres of ground induced polarization surveying and 1940.0 line-kilometres of airborne magnetic surveying on the area as the Joy property.