What is Gneiss?
Gneiss is a foliated metamorphic rock identified by its bands and lenses of varying composition, while other bands contain granular minerals with an interlocking texture. Other bands contain platy or
elongate minerals with evidence of preferred orientation. It is this banded appearance and texture - rather than composition - that define a gneiss.
How Does Gneiss Form?
Gneiss usually forms by regional metamorphism at convergent plate boundaries. It is a high-grade
metamorphic rock in which mineral grains recrystallized under intense heat and pressure. This
alteration increased the size of the mineral grains and segregated them into bands, a transformation
which made the rock and its minerals more stable in their metamorphic environment.
Gneiss can form in several different ways. The most common path begins with shale, which is a sedimentary rock.
Regional metamorphism can transform shale into slate, then phyllite, then schist, and finally into gneiss.
During this transformation, clay particles in shale transform into micas and increase in size. Finally,
the platy micas begin to recrystallize into granular minerals. The appearance of granular minerals is what marks the transition into gneiss.
Intense heat and pressure can also metamorphose granite into a banded rock known as "granite gneiss."
This transformation is usually more of a structural change than a mineralogical transformation. Granite
gneiss can also form through the metamorphism of sedimentary rocks. The end product of their metamorphism
is a banded rock with a mineralogical composition like granite.
Composition and Texture of Gneiss
Although gneiss is not defined by its composition, most specimens have bands of feldspar and quartz grains
in an interlocking texture. These bands are usually light in color and alternate with bands of darker-colored
minerals with platy or elongate habits. The dark minerals sometimes exhibit an orientation determined by
the pressures of metamorphism.
Some specimens of gneiss contain distinctive minerals characteristic of the metamorphic environment. These
minerals might include biotite, cordierite, sillimanite, kyanite, staurolite, andalusite and garnet. Gneiss
is sometimes named for these minerals, examples of which include "garnet gneiss"and "biotite gneiss".
|Corundum Gneiss: This is a specimen of corundum gneiss from Gallatin Valley, Montana. This specimen is about four inches across and has a round blue sapphire crystal on the left side.
Uses of Gneiss
Gneiss usually does not split along planes of weakness like most other metamorphic rocks. This allows contractors to
use gneiss as a crushed stone in road construction, building site preparation, and landscaping projects.
Some gneiss is durable enough to perform well as a dimension stone. These rocks are sawn or sheared into blocks and
slabs used in a variety of building, paving, and curbing projects.
Some gneiss accepts a bright polish and is attractive enough for use as an architectural stone. Beautiful
floor tiles, facing stone, stair treads, window sills, countertops, and cemetery monuments are often made
from polished gneiss.
Don't be surprised if you see gneiss labeled as "granite" at a cabinet shop or monument company. In the
dimension stone trade, any rock with visible, interlocking grains of feldspar is considered to be "granite" in that industry. Seeing gneiss,
gabbro, labradorite, diorite, and other types of rock marketed as "granite" disturbs many
geologists. However, this long-time practice of the dimension stone trade simplifies discussions with customers since not everyone knows the technical names of unusual igneous and metamorphic rocks.
Gneiss in the Classroom
Small rock and mineral specimens about one inch in size are usually adequate for student examination and
identification. However, many rock units, identified as gneiss in the field, have bands that are thicker
than one inch. If samples of these rock units are broken into one-inch pieces, many of them will be too small
to exhibit the banding features of gneiss. This will confuse many students and cause others to incorrectly
identify the rock.
Teachers can avoid these problems by collecting specimens that clearly display a banded structure. Teachers
who purchase specimens must examine them carefully before they are presented to students.
After students have learned to identify gneiss and many other rock types, presenting specimens of gneiss that do not exhibit banding can be
a challenging way to have students: A) consider possibilities that are not obvious, and, B) realize that a
single rock specimen may not adequately represent a rock unit.
Last updated: June, 2015
Contributor: Hobart King
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|Gneiss: The specimen shown is about two inches (five centimeters) across. It is easy to see the "salt and pepper" banding of this rock.
|Gneissic Granodiorite: An outcrop of gneissic granodiorite in the Zarembo Islands area of Southeastern Alaska.
|Folded Gneiss: A photograph of polished gneiss from the stock of a countertop vendor. The view shown in the photo is about 12 inches across. Click image to enlarge.
|Garnet Gneiss: A photograph of polished garnet gneiss from the stock of a countertop vendor. The view shown in the photo is about 12 inches across. Click image to enlarge.
|Garnet Gneiss: A cabochone cut and polished from garnet gneiss. A cabochon cut from this type of material is rarely seen but it would be an interesting gem for a geologist. The stone is approximately 38 x 27 millimeters in size.