Crystal Lake Mining Corporation announced the results from Channel Sample BRCH19-01, the first ever continuous channel/trench sample at Burgundy Ridge on the Newmont Lake Project in the Golden Triangle of British Columbia. This channel sample targeted a new discovery area made late in the 2019 season called the "Green Rock Zone" as a result of rapidly receding snow/ice in the region. Channel/trench Sample BRCH19-01 cut a hydrothermal breccia exposed on surface assaying 22.00 metres of 2.00% Cu, 2.27 g/t Au, 34.26 g/t Ag, and 4.69% Zn. This hydrothermal breccia contained a high-grade centre assaying 10.00 metres of 3.29% Cu, 8.59% Zn, 3.75 g/t Au, and 63.40 g/t Ag on surface. The channel/trench sample is a 340-metre step-out from the first diamond drill hole results released at Burgundy Ridge including BRDDH19-002's 91.26 metres of 0.38% Cu, 0.30 g/t Au, 4.12 g/t Ag, starting at 36.7 metres depth. Mineralization and alteration styles outline a large copper/gold- rich alkalic porphyry system with related high-grade hydrothermal breccia and skarn mineralization seen along the entire 2.3km Burgundy Trend. 2.00% Cu, 4.69% Zn, 2.27 g/t Au, and 34.36 g/t Ag over 22.00 metres at surface. Including 3.29% Cu, 8.59% Zn, 3.75 g/t Au, and 63.40 g/t Ag over 10.00 metres at surface. 1.31% Cu, 2.97% Zn, 1.49 g/t Au, and 23.26 g/t Ag on surface over 37.00 metres on surface. Approximate 340 metre step-out from initial diamond drill hole results. Due to time and weather constraints, one diamond drill hole (BRDDH19-016) was roughly targeted towards the Green Rock Zone as the last drill hole at Burgundy Ridge in 2019. This hole was drilled from Pad C-1; a drill pad designed to target the Discovery Zone approximately 200 metres to the north of Green Rock. Diamond Drill Hold BRDDH19-016 was continued as the deepest hole of Burgundy Ridge's first-ever diamond drill campaign. Assays are pending. Channel Sample BRCH19-01's final 7.00 metres cut 0.46% Cu, 0.53 g/t Au, 10.33 g/t Ag, and 0.32% Zn on surface of strong to intense potassic altered rock mineralized with a chalcopyrite stockwork. The protolith is unknown at this time due to intensity of alteration. The alteration and mineralization styles are indicative of a copper/gold-rich alkalic porphyry systems which may be the ultimate source of mineralization seen along the entire 2.3km Burgundy Trend. Specific clasts within Green Rock's heterolithic hydrothermal breccia are potassic-altered, trachytic syenites with chalcopyrite stockwork. These clasts are highly significant as they are synonymous with the mineralization observed in the final 7.00 metres of BRCH19-01. This relationship is early evidence for a minimum of 2 mineralization events and styles at Burgundy Ridge. Earlier in the season the Company intersected the first-ever copper/gold-rich porphyry hypogene mineralization at the 72' Zone based on a blind target using hyperspectral technology which measured transitional zones of magnesium and potassium in white micas. Further lithogeochemical and geochronological analyses are underway to fingerprint the intrusion and test whether they are of the same source. BRCH19-01 represents a 37.00 metre continuous channel/trench sample taken on surface in the Green Rock Zone. The following represents a list of important steps taken to ensure the quality and reliability of results from the channel: The channel sample is perpendicular to the limestone contact as to not over-exaggerate width (true width is unknown). Surface oxides/hydroxides were avoided as to not over-exaggerate the metal grade of mineralization that was cut, and results are considered to be representative of massive to semi-massive sulphide mineralization, or stockwork sulphide mineralization. Systematic 1.00 metre whole samples were taken to eliminate sampling bias and ensure reliable assay data.