 The Precambrian oval-shaped Kanichee layered intrusive complex is the largest of many sill-like mafic-ultramafic bodies in felsic and mafic metavolcanic rocks in the northern portion of the Temagami greenstone belt.It comprises five magmatic series, each of which contains one or more types of igneous rock.A succession of cumulus phases comprising every magmatic series suggests that the Kanichee layered intrusive complex is south-facing, including the surrounding metavolcanic lava flows.