Amarc Resources Ltd. provided details on the expansion potential of the high grade Empress Cu-Au-Ag deposit, and surrounding Greater Empress area. The Greater Empress area is a sizable subarea of Amarc's extensive 100% owned IKE Cu and Au district, and is located 6 km north of the Company's substantive IKE porphyry Cu-Mo-Ag discovery. A comprehensive review by Amarc's technical team of historical data throughout the Greater Empress area has unlocked a high potential for the discovery of substantial intrusion-related replacement and porphyry Cu-Au±Mo-Ag deposits centered on the Empress deposit. The Empress Cu-Au-Ag replacement deposit is a significant body of mineralization, characterized from historical drilling by its common high grade intersections and relatively good vertical and lateral grade continuity. These features support the strong potential for discovery of new high grade extensions to the deposit. Important potential exits for a well-planned core drilling program to expand the mineralization which remains open. In addition to the Empress deposit, the 35 km2 Greater Empress area includes seven identified compelling porphyry and replacement-style Cu-Au±Mo±Ag deposit and exploration targets. The deposit targets include, Empress East, Empress Gap, Granite and Buzzer, and the earlier-stage exploration targets include Empress West. These targets are either not fully drill delineated or have been tested only by shallow, widely-spaced historical reconnaissance percussion drilling: and can with focused exploration be brought to a drill ready status. Amarc has a permit for up to 300 drill holes for the IKE Project. Management is considering its options to advance this exciting high grade Cu-Au segment of its extensive overall IKE district mineral tenures. Amarc's IKE Cu and Au district is located in a fertile region of south-central British Columbia that hosts other large Cu±Au±Mo deposits with similar geological settings. Like many major porphyry districts, the IKE district formed in a very active environment characterised by long-lived, multi-phase magmatic-hydrothermal-structural activity, resulting in multiple centers of mineralization. The Au-bearing Empress deposit and other deposit targets within the Greater Empress area were formed at about 85-80 Ma and, as such are distinct from the hydrothermal activity that formed the approximately 46 Ma IKE porphyry Cu-Mo-Ag deposit that is hosted within the Coastal Plutonic Complex. The Greater Empress area straddles the CPC contact with volcanic rocks to the north, over a strike length of 15 km. Strong and widespread alteration with abundant sulphides is associated with a variety of deposit types including porphyry Cu±Au±Mo±Ag and high temperature Cu-Au-Ag replacement, as well as Au-Ag high sulphidation and possibly low sulphidation epithermal systems. The range of paleodepth indicated by these deposit types increases the possibility for the preservation of deposits in the IKE district, so increasing the discovery potential. Amarc's technical team diligently compiled, verified and integrated Greater Empress area historical information. This compilation of data from geochemical and geophysical surveys and drilling (including 138 core holes totaling 19,298 m averaging approximately 140 m depth, and 96 short percussion holes totaling 4,382 m averaging approximately 46 m in depth for which only Cu and Mo assay data is available), combined with the geological and geophysical survey data from the Company's programs, has permitted a rapid advancement in the understanding of the high value development potential in the Greater Empress area. Empress Cu-Au-Ag Replacement Deposit: Historical drilling at Empress has indicated a significant body of good grade Cu-Au mineralization, which remains open to expansion with a modern core drilling program. Mineralization at the Empress deposit is considered to have formed by the replacement of previously altered volcanics by a quartz-magnetite-sulphide assemblage, with higher Cu-Au-Ag grades commonly occurring within 100 m in vertical distance above the CPC's contact, within the overlying volcanics. An initial examination of historical drill core by the Amarc team recognized the nearby Granite porphyry Cu-Au-Ag-Mo deposit target, which is shallowly concealed by overburden. The Granite porphyry deposit target is considered a possible source of Empress replacement fluids. The Granite deposit target requires drill delineation. This drilling together with moderate to locally strong IP chargeability responses, magnetic geophysical features, and results from historical Cu and Au soil geochemistry (>250 ppm Cu and 50 ppb Au which closely reflect the first three historical drill samples results at the base of overburden, see Report), indicate there is significant potential with further core drilling to enlarge this body of mineralization. Notably there is a complete absence of drill holes in the southern part of this target, which is at a position that is analogous to shallower, high grade Cu- Au-Ag replacement-style mineralization at the Empress deposit to the west. Empress Gap Cu-Au-Ag Replacement Deposit Target: Results from limited historical drilling, comprising eleven shallow percussion drill holes and three deeper core holes, in the >1 km long Empress Gap zone located between the Empress and Empress East suggest a clear opportunity to discover additional Cu-Au-Ag mineralization in proximity to the volcanic-CPC contact.