Mr. Alexander Stares reports

METALS CREEK CONTINUES TO SEE ENCOURAGING VISUALS IN THIRD DRILL HOLE AT THE OGDEN GOLD PROJECT, COMPLETES DRILL PROGRAM

Metals Creek Resources Corp. continues to hit visible gold (VG) in all three drill holes at the Ogden gold project in Timmins, Ont. The Ogden gold project is a 50/50 joint venture with Discovery Silver, with the company serving as the operator.

Hole TOG-26-77 was the deepest of the three holes drilled during this program targeting the lower portion of a Thomas Ogden zone (TOG) fold structure which has a shallow easterly plunge. High-grade gold mineralization has a strong preferential association with the TOG fold axis and is commonly associated with flat-lying quartz-bearing structures and zones of strong albitization, silicification and quartz flooding with associated disseminated pyrite. The company has utilized structural data generated from the last drill campaign to determine the orientations of gold-bearing quartz veins and structures. Incorporating this data has aided in optimizing drill hole orientations to better define density of gold bearing veins ensuring all mineralized veins are spatially represented.

TOG-26-77 targeted high-grade gold mineralization associated with the lower portion of the TOG fold structure. Visible gold was observed at 350.36 metres hosted within a highly silicified felsite with associated quartz veinlets and disseminated pyrite. Visible gold continues to have a strong association with strongly altered felsite hosted within strongly mineralized and albitized conglomerates with associated cross-cutting quartz veins. This alteration package is proximal to the TOG fold axis. Holes from previous drill campaigns include TOG-22-74A which returned a downhole intercept of 3.66 grams per tonne (g/t) gold (Au) over 14.66 metres (m) (see news release Nov. 15, 2022) and TOG-11-08, which returned a downhole intercept of 13.07 g/t Au over 2.88 m (see new release Nov. 16, 2011). Both of these holes also observed visible gold and mineralization hosted within altered felsite.

"We are highly encouraged to have intersected visible gold in all three holes drilled during this drill campaign. Intersecting visible gold in hole TOG-26-75 was especially encouraging in that it is located within an area of limited drilling and no documented VG," states Alexander (Sandy) Stares, president and chief executive officer.

Assay results will be released as they are received and compiled.

The presence of visible gold in drill core is considered encouraging; however, it should not be considered a definitive indicator of gold grade or continuity of mineralization. Visible gold observations are qualitative in nature and may not be representative of overall gold distribution within the drill hole or across the property. Analytical assay results are required to determine the actual gold content of the sampled intervals.

The Ogden gold project is located within the Timmins gold camp and has over eight kilometres of strike length along the prolific Porcupine-Destor Break, the key conduit for gold mineralization in the Timmins camp. This project was acquired in November, 2008, when Metals Creek signed an option joint venture agreement with Goldcorp (now Discovery Silver). Ogden is strategically located between Pan American Silvers' West Timmins mine and Galleon Golds West Cache development to the west and Discovery Silvers' Dome mine and mill complex, which is located eight km to the east. Currently there are six zones of mineralization identified; Naybob North, South and West, Porphyry Hill, Thomas Ogden (TOG) and Thomas Ogden West with Naybob South and TOG seeing the majority of the work. Highlights of drilling include 210.19 g/t gold over 12.53 metres from TOG-13-25 (see Metals Creek news release dated May 22, 2013) and 9.24 g/t gold over 6.61 m from Naybob South (see corporation's website). Additional mineralization was discovered in drilling one kilometre west of TOG returning an intercept of 5.06 g/t gold over 2.60 m (see news release dated March 4, 2016) with a follow-up hole returning a down hole intercept of 4.96 g/t gold over 3.97 m including a second zone of mineralization assaying 1.43 g/t gold over 14.00 m (see Metals Creek news release date June 5, 2017). This further highlights the exploration potential on the western portion of the property, which is contiguous with Galleon Gold and has seen minimal work.

Michael MacIsaac, PGeo, and vice-president, exploration, for the company and a qualified person as defined in National Instrument 43-101, is responsible for this release, and supervised the preparation of the information forming the basis for this release.

About Metals Creek Resources Corp.

Metals Creek Resources is a junior exploration company incorporated under the laws of the Province of Ontario, is a reporting issuer in Alberta, British Columbia and Ontario, and has its common shares listed for trading on the exchange under the symbol MEK. Metals Creek has earned a 50-per-cent interest in the Ogden gold property including the former Naybob gold mine, located six km south of Timmins, Ont., and has an eight km strike length of the prolific Porcupine-Destor Fault (P-DF).

Metals Creek has also jointly acquired through staking on a 50/50 basis with Benton Resources, potential natural white hydrogen projects in Newfoundland. The Smoking Gun prospect was selected after research uncovered highly anomalous helium with values up to 8,900 parts per billion (ppb) in water collected from an historic drill hole. These licences are located within the Deer Lake basin, which is thought to be a prospective environment for the presence helium (He) and natural (white) hydrogen (H2).

At Parson's Pond, research of historical drill logs in two holes 14.2 kilometres apart, have observed C1 methane gas levels reaching 72 per cent. The area is underlain by thrust faulted rocks of the Humber Arm supergroup. Drill logs indicate unique sedimentary units composed of shales along with sandstones containing fragments of serpentine and chrome. Of particular interest, is the presence of the mineral glauconite, which, combined with these geological indicators, suggests a highly prospective environment for the potential formation of white hydrogen (natural hydrogen) to form within the basin. The presence of such high concentrations of methane alongside hydrogen indicators suggests a potentially active gas system within the basin. In addition, surface areas have been noted to vent gas within the project boundaries.