Metamorphic rocks - Gneiss 

Page / - last modified by Roelof Zwaan on 2021/09/30 15:18 

Gneiss 
last modified by Roelof Zwaan
on 2021/09/30 15:18

Table of Contents

Gneiss is a foliated metamorphic rock. This rock originates from shale and transformed from shale into slate, then phyllite, then schist and finally into gneiss.
Characteristics
Gneiss can't be defined on the minerals present within the rock. Gneiss can be recognized by the organization of minerals that form into bands in the rock. This happens because of the clay minerals present. Gneiss originate from regional metamorphism at convergent plate boundaries, which mean it forms under high pressure and high temperature conditions.
Gneiss can be easily mistaken for schist or granite. They can be held apart by looking at the cleavage. Breaking a gneiss generates splinters of centimeters thick and schist breaks down in splinters of only millimeters thickness. It can be held apart from granite via its origin and texture. Granite originates from solidified magma and gneiss from recrystallization of existing rock. The minerals in gneiss have a certain preferable orientation due to the fact that it contains clay minerals. Granite doesn't have this preferable orientation.
Composition
As said in the previous paragraph gneiss can be recognized by its mineral composition. However, gneiss has some minerals which are always present. These minerals are feldspar and quartz creating the interlocking band structure. These bands are usually light in color and alternate with bands of darker-colored minerals with elongate habits, like for example clay minerals.
References
•	https://geology.com/
•	NEN-EN-ISO 14688-1:2019
Gneiss

Type	Metamorphic rock	
Texture	Banded	
Clasts	Can be present	
Hardness	Very hard	
Color	Grey to dark grey	
Minerals	Quartz or feldspar and clay minerals	
Touch	Rough	
Image	Gneiss	
Contents
•	Characteristics
•	Composition
•	References
•	Gneiss