Colibri Resource Corporation announce that a permit to drill up to 56 holes at the Evelyn Gold Project, located in northern Sonora, Mexico has been received. The application was submitted to SEMERNAT (the Mexican environmental authority) on September 3rd, 2021, and permission was granted October 5, 2021. The Company continues to complete geological mapping and sampling to refine drill targets and reports an assay of 33 grams per tonne ("g/t") Au and 119 g/t Ag. The Company will begin remediation of access roads to and within the property this week. These repairs are required to support trucks carrying reverse circulation ("RC") drill equipment after what has been a particularly heavy rainy season in northern Sonora. The road work is expected to be completed within 2 weeks after which the preparation of drill access roads and drill pads will start. Contracts and arrangements for the RC drill are being finalized and the Company anticipates drilling to begin upon the completion of prioritized drill pads. The fully funded drill program of up to 10,000 metres is expected to be conducted in two phases. The Evelyn Gold Project is an Orogenic-type gold target located in the Caborca Gold Belt of northwestern Sonora. The property is located approximately 25 kilometres ("km") east of La Herradura, Mexico's largest open pit gold mine, which produced 425,288 ounces of gold in 2020 at an average grade of 0.77 grams per tonnes ("g/t") Au and is also approximately 9 km northeast of the Noche Buena mine which produced 87,988 ounces Au at an average grade of 0.52 g/t Au in 2020. The setting and style of mineralization at Evelyn is similar to that reported from La Herradura and Noche Buena. Higher grade mineralization on the Evelyn property consists of quartz veins and veinlets, ranging from 2 - 3 centimeters up to 1.5 m hosted by fault and fracture zones with minor oxidized pyrite, iron oxide, copper bearing oxide and carbonate minerals, and locally minor to trace amounts of galena, chalcopyrite, and sphalerite. Alteration of the host rocks includes iron bearing carbonate minerals, quartz, sericite, and chlorite. Lower grade mineralization is associated with altered volcanic rocks containing minor amounts of oxidized sulfide. Mineralization is hosted dominantly by Jurassic volcanic rocks consisting of andesite and rhyolite.