Roger Weller, geology instructor
[email protected] copyright 2010-R.Weller
massive datolite-polished
northern Michigan
Datolite is a hydrous
calcium boron silicate often associated with zeolites in basalt.
The datolite from northern Michigan occurs as cryptocrystalline fillings within gas
bubble holes in
basalt (amygdules). The most common color of the Michigan
datolites is white but they be colored
various shades of grayish pink by
inclusions
of microscopic-sized flakes of native copper.
datolite
Photo is copyright free only for
non-commercial educational uses.
Just credit photo to R.Weller/Cochise College.