Awesome! The Buckingham property is located within the Central Metasedimentary Belt of the Grenville Geologic Province. It is underlain by paragneiss and marble, with associated pegmatite, and amphibolite. Graphite mineralization occurs in two main zones, the Case Zone and the Uncle Zone where it is disseminated in paragneiss and marble as well as in veins and masses within pegmatite and skarn.