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. This record indicates that magmatic rocks of the Kanichee layered intrusive complex originally formed in a level position and most likely very shallow beneath the Earth's crust.
A sequence of cloudy phases comprising every series of molten rock indicates that the Kanichee layered intrusive complex is oriented towards the south, including surrounding volcanic lava flows. This evidence suggests that magmatic rocks of the Kanichee layered intrusive complex initially formed in a flat position and likely very near the Earth's surface.