Ann: Company Update 12 November 2021, page-11

Thanks amigo, I'm just trying. I don't have any complaints with either team - GRL is actively exploring, which is the key to success. Interestingly there are a few more pieces in the Lewis Ponds puzzle. The description of the geology at Lewis Ponds has changed a little bit. I've copied below the Geology statements from May 2021 and November 2021. (The extra couple of sentences in the recent one are put in bold by me.) Also, in the recent announcement (on page 12) they mention: "Not commonly noted, but of great significance is the fact that much of Lewis Ponds’ early development was in lieu of the high grades of silver in its ores. It appears that silver was the major commodity mined at different points of the mines’ history. "

May 2021 - Page 11 JORC Geology
"The Lewis Ponds deposit is located in a locally highly structured zone within the western limb of a north-west plunging syncline. The deposit consists of stratabound, disseminated to massive sulphide lenses. The deposit is hosted in Silurian felsic to intermediate volcanic rocks as a thin, mostly fine-grained sedimentary unit with occasional limestone lenses that has undergone significant deformation and is now defined as a steeply east dipping body with mineralisation that occurs over a strike length of more than 2km. The southern mineralisation occurs within a limestone breccia and Tom’s mine is hosted by siltstone and consists of fine-grained tuffaceous sediments."

November 2021 - Page 12 JORC Geology
"The Lewis Ponds deposit is located in a locally highly structured zone within the western limb of a north-west plunging syncline. The deposit consists of stratabound, disseminated to massive sulphide lenses. The deposit is hosted in Silurian felsic to intermediate volcanic rocks as a thin, mostly fine-grained sedimentary unit with occasional limestone lenses that has undergone significant deformation and is now defined as a steeply east dipping body with mineralization that occurs over a strike length of more than 2km. The Southern mineralization occurs within a limestone breccia and Tom’s mine is hosted by siltstone and consists of fine-grained tuffaceous sediments. The mineralized zones unconformably overlie a sequence of strongly foliated and hydrothermally altered quartz-plagioclase dacite. Mineralization occurs in two main styles: plunging shoots of thicker, high-grade mineralization within the anticline and syncline axes; and as tabular lenses in fold limbs and shear zones."