-ite +

(Greek: a suffix; one connected with, inhabitant of [also used to indicate chemicals, minerals, etc.])


adelpholite
A Columbate of iron and manganese, found associated with Columbite in Finland.
adelphoparasite
An organism parasite on a closely related host organism.
aerolite, aerolith, aerolitic
A stony meteorite.
albite, albitic
A white part of certain granite or various igneous rocks.
amphibiolite
The remains of an amphibious animal found in the fossil state.
anthropolite, anthropolith, anthropolithic, anthropolitic
Petrified human remains or a fossil ascribed to the human species.
anthropomorphite
1. Someone who ascribes a human form or human attributes to the Deity or to a polytheistic deity.
2. Specifically, people of a sect of ancient heretics who believed that God has a human form, etc.
anthropophagite
Someone who eats human flesh; a cannibal.
anthropophysite
Someone who ascribes human nature to a deity.
aphanite
1. An igneous rock with mineral components that are too fine to be seen with the naked eye.
2. A very compact, dense, homogeneous dark-colored rock, consisting of grains which are too fine to be seen without some form of magnification.
aphrite
A variety of calcite (mineral); referring to foam because of its appearance.
aphrodite
1. A soft opaque milk-white mineral, consisting mostly of bisilicate of magnesium, allied to Sepiolite or meerschaum.
2. In the sense of foam-stone.
appetite
1. An instinctive physical desire, especially one for food or drink.
2. A strong wish or urge; such as, having an appetite for learning vocabulary.
arenicolite
A worm-hole made originally in sand and preserved in a sandstone rock.
batholite
1. A large mass of intrusive igneous rock believed to have solidified deep within the earth.
2. A large emplacement of igneous intrusive (also called plutonic) rock that forms from cooled magma deep in the earth's crust.

Batholiths are composed of multiple masses, or plutons, of magma that moved toward the surface from a zone of partial melting at the base of the earth's crust.

While moving, these plutons of relatively buoyant magma are called plutonic diapirs. Diapirs commonly intrude vertically upward along fractures or zones of structural weakness through more dense overlying rocks because of density contrast between a less dense, lower rock mass and overlying denser rocks.

Because the diapirs are liquefied and very hot, they tend to rise through the surrounding country rock, pushing it aside and partially melting it.

Most diapirs do not reach the surface to form volcanoes, but instead slow down, cool and usually solidify five to thirty kilometers underground as plutons; therefore, the use of the word pluton; in reference to the Roman god of the underworld, Pluto.


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