PROCESS
The Boticas Yellow Granite results from the solidification of magma at great depths (plutonic magmatic rock). The rocks that surround it, preventing the release of heat, do not allow a rapid cooling of the magma, delaying its solidification.
This way, the minerals that constitute it have the necessary time to develop, thus presenting the rock with a granular texture in which the constituent materials are clearly visible and identifiable: quartz, feldspars, and micas.
The Boticas Yellow Granite results from the solidification of magma at great depths (plutonic magmatic rock). The rocks that surround it, preventing the release of heat, do not allow a rapid cooling of the magma, delaying its solidification.
This way, the minerals that constitute it have the necessary time to develop, thus presenting the rock with a granular texture in which the constituent materials are clearly visible and identifiable: quartz, feldspars, and micas.