Investors Overview

The Illinois Creek District represents a highly prospective, district-scale carbonate replacement deposit–porphyry (“CRD–PPY”) mineral system in western Alaska. Over the past decade, Alaska Silver’s management team has consolidated a portfolio of high-quality silver, gold, copper, lead, and zinc targets originally identified through historical Anaconda exploration programs, establishing control over one of Alaska’s most compelling emerging CRD districts. 

The portfolio includes numerous high-quality gold, silver, copper, lead, and zinc exploration targets. Our flagship mineral deposit types include: carbonate replacement deposits (CRD’s)(Waterpump Creek and Illinois Creek), a porphyry copper deposit (Round Top), and a low sulfidation vein system (Honker Gold). There is current NI 43-101 compliant mineral resource for the past-producing Illinois Creek mine and the Waterpump Creek deposit. These deposits are our most advanced, however, there are numerous lower-stage exploration targets and potential for new discoveries in the district.

The portfolio includes numerous high-quality precious and base metal exploration targets. Flagship deposit styles within the district include carbonate replacement deposits (“CRDs”) at Waterpump Creek and Illinois Creek, the Round Top porphyry copper-silver-molybdenum system, and the Honker Gold low-sulfidation vein system. Current NI 43-101 compliant mineral resources have been defined for the past-producing Illinois Creek mine and the Waterpump Creek deposit. While these represent the most advanced assets in the district, Alaska Silver has also identified numerous earlier-stage targets that provide significant opportunity for new discoveries.

The Company’s evolving geological model now interprets the district as containing two distinct CRD–porphyry centers, or “hubs,” each with significant carbonate-hosted replacement potential developed within favorable reactive stratigraphy.

The first hub is the well-established Illinois Creek system, where multiple components of a large CRD system have already been identified along an approximately 8-kilometer mineralized corridor. This hub includes the existing Waterpump Creek silver-zinc-lead resource, the Illinois Creek gold-silver resource, and high-priority exploration targets including Silver Sage, Warm Springs, and several additional district prospects. While the intrusive source responsible for mineralization has not yet been directly located, geological, structural, geophysical, and geochemical evidence strongly supports the presence of a buried porphyry center at depth. 

The second hub is centered on the Round Top silver-copper-molybdenum porphyry system, located approximately 20 kilometers from Illinois Creek. In contrast to the concealed intrusive center interpreted at Illinois Creek, Round Top exposes a well-defined mineralized porphyry center at surface. This system is surrounded by extensive reactive carbonate host rocks that display strong geochemical leakage, including highly anomalous silver, lead, and zinc values extending over multi-kilometer strike lengths, highlighting substantial additional CRD discovery potential. These surrounding CRD targets include the TG and TG North prospects, which highlight substantial additional district-scale discovery potential.

All of Alaska Silver’s properties and proposed development infrastructure are located entirely on Alaska State lands, providing a favorable pathway for future exploration advancement and potential development with access to the Lower Yukon River corridor