The Silver Horde occurrence is situated 0.5 kilometre east of the Kitsault River, 26 kilometres north of the town of Alice Arm. This showing was extensively prospected for its silver-lead-zinc mineralization between 1916 and 1930.

The area is underlain by a sequence of volcanics and sediments of the Upper Triassic Stuhini Group and the Lower-Upper Jurassic Hazelton Group. The sequence is folded into the doubly plunging, north-northwest trending Kitsault River syncline and has been regionally metamorphosed to greenschist facies.

The Silver Horde occurrence is comprised of a silicified zone and a quartz breccia vein developed in andesitic tuffs of the Hazelton Group. The silicified zone strikes 020 degrees and is at least 1 metre wide. It is mineralized with spherules of marcasite and galena.

The quartz breccia vein, situated 160 metres northeast of the silicified zone, strikes 040 degrees and dips 65 to 70 degrees southeast. It varies from 0.6 to 3.0 metres wide and has been traced for 30 metres. A 30 metre long adit, 9 metres below the outcrop, intersected several faults indicating the vein is terminated at shallow depths by a fault. The vein is mineralized with pyrite, marcasite, galena, sphalerite and chalcopyrite in a gangue of quartz and fragments of country rock. A 1.5 metre chip sample assayed trace gold, 209 grams per tonne silver and 0.9 per cent lead (Minister of Mines Annual Report 1951, page 97).

During 2010 through 2019, Dolly Silver Corporation explored the area as apart of the Dolly Varden property. A complete property exploration history can be found at the Dolly Varden (MINFILE 103P 188) occurrence.