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Glossary of Rock and Mineral Terms - X, Y, Z

A | B | C | D | E | F | G | H | I | J | K | L | M | N | O | P | Q | R | S | T | U | V | W | X | Y | Z

xenolith
A preexisting rock embedded in a newer igneous rock. Xenoliths are formed when a rising magma incorporates the preexisting rock. If the preexisting rock does not melt, it will not be assimilated into the magma and will therefore remain distinct from the new igneous rock that surrounds it.
 
xray
Electromagnetic radiation that has a very short wavelength, emitted from a substance when it is attacked by a line of electrons in a vacuum. Machines are able to produce this, and they are known as x-ray machines. They are useful in geology and mineralogy for the study of the chemical constituents of rocks and minerals.
x-ray diffraction
The scattering of X rays passed through a mineral sample so as to form a pattern peculiar to the given mineral.

yield point
The maximum stress that a given rock can withstand without becoming permanently deformed.


zeolite group
Group of around 30 minerals that are related in structure, habits, and occurrence. The zeolites are hydrous aluminum silicates that contain sodium or calcium, which can replace one another. These minerals are usually found in zeolite deposits, which are of igneous origin. Individual member is a zeolite.
zoning
The distinction of particular rock material from surrounding rock material.
zone of ablation
The part of a glacier in which there is greater overall loss than gain in volume. A zone of ablation can be identified in the summer by an expanse of bare ice. See also zone of accumulation.
zone of accumulation
The part of a glacier in which there is greater overall gain than loss in volume. A zone of accumulation can be identified by a blanket of snow that survives summer melting. See also zone of ablation.
zone of aeration
A region below the Earth's surface that is marked by the presence of both water and air in the pores of rocks and soil. Also called aeration zone.
zone of saturation
A region that lies below the zone of aeration and is marked by the presence of water and the absence of air in the pores of rocks and soil.