Abstract
Matsubasemachi, Uki, Kumamoto belongs to Higo metamorphic terrane. In the metamorphic rock of this area, ultrabasic rocks called “chikuyouseki” are known to be distributed for a long time. Olivine which extended into a bamboo leaves form is included in it, and changes to serpentine including minute magnetite. There was a thing with gray or the light green around bamboo leaves parts in this area, I aim at researching mineralogical property of serpentine minerals in chikuyouseki with gray this time.