Heat and pressure
Granite can be changed into gneiss through the process of metamorphism, where heat and pressure alter the mineral structure of the rock. This process causes the minerals in the granite to recrystallize, forming distinct banding and foliation characteristic of gneiss. The original minerals in the granite are reorganized into new minerals such as mica, quartz, and feldspar, giving gneiss its unique appearance.
Granite is an igneous rock and gneiss is a metamorphic rock.
The daughter rock of granite is gneiss. Gneiss forms from the metamorphism of granite, where the minerals in the granite recrystallize and align into distinct bands or layers, giving gneiss its characteristic appearance.
If granite were subjected to intense heat and pressure, it would likely change to gneiss, a metamorphic rock. Gneiss forms through the recrystallization of minerals in granite under high temperature and pressure conditions.
gneiss
Gneiss is a foilated metamorphic rock.
Gneiss can be formed by the metamrphism of either granite or schist.
Gneiss is a metamorphic rock and its parent rock (protolith) could be a granite or schist.
A type of metamorphic rock similar to granite is gneiss. Gneiss is a foliated metamorphic rock that has a similar composition to granite but displays a banded texture due to the alignment of mineral grains during metamorphism.
Gneiss
Granite.
Gneiss