The Bloss occurrence is located 5.1 kilometres east-southeast of the summit of Alberts Hump, south of Abesti Creek and 2.25 kilometres south of the BV occurrence (094E 099), approximately 300 kilometres north of Smithers. The occurrence lies within the Omineca-Cassiar Mountains in the west-central portion of the Toodoggone Gold Camp.

The Bloss prospect 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 Tertiary 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 Takla Group andesite flows and pyroclastic rocks. Takla volcanics have been intruded by the granodiorite to quartz monzonite Black Lake Suite of Early Jurassic age and are in turn unconformably overlain by or faulted against Lower Jurassic calcalkaline volcanics of the Toodoggone Formation (Hazelton Group).

The dominant structures in the area are steeply dipping faults which 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 Adoogacho and Metsantan members of the Toodoggone Formation underlie the AL property. The Adoogacho Member consists of trachyandesite ash-flow tuff with lenses of lapilli tuff, rare marlstone, and conglomerate near the base. The Metsantan Member is composed mainly of trachyandesite (latite) flows with lenses of lapilli tuff, and lahar; minor volcanic sandstone and conglomerate Bulletin 86). The Metsantan Member, in part, directly overlies the basal Adoogacho Member and is also in fault contact with it.

The Bloss prospect consists of a steeply dipping, east trending core of completely silicified rock apparently flanked by a clay alteration zone. The core has a tabular, vein-like form which outcrops as a resistant spine. The south contact or wall of the siliceous core appears to be a south-dipping fault; the north contact is not exposed. The core zone is well fractured and is locally brecciated. Fractures contain traces of pyrite with abundant limonite and minor hematite. Barite is present but not abundant. The porosity of the rock is low except where (post mineral?) fracturing and brecciation are intense. The zone is open to the east, west and north.

A series of chip samples from trenches yielded a best assay of 1.4 grams per tonne gold across 2.4 metres (sample G-174, Assessment Report 14460). Grab sample 116F, taken in 1982 from this same zone, analyzed 2.1 and 9.1 grams per tonne gold (Assessment Report 14460).

In 1985, Energex Minerals Ltd. conducted exploration work on the Bloss.

In 2007, Christopher James Gold Corp. completed a helicopter-borne magnetic gradiometer survey consisting of 2229 line-kilometres over all historic gold deposits and MINFILE occurrences on the property, including the Steve's area (Assessment Report 30132). Maps completed include coloured Total Magnetic Intensity, Measured 3-D Analytic Signal, Measured Vertical Magnetic Gradient, and colour-shaded Tilt Derivative of the Total Magnetic Intensity.

For a more detailed account of the local geology, alteration and work history refer to the Bonanza occurrence (094E 079).