granite
most abundant kind of rock in Earth’s continents
Carbonate minerals
constructed of one
or more positive ions
Dolomite
resembles calcite, but half of the calcium ions are
replaced by magnesium
Sulfate materials
formed of positive ions (such
as calcium, barium, or strontium) that are attached to
the complex ion SO4
2−
Granite
most abundant kind of rock in Earth’s continents
gabbro and basalt
two types of mafic rocks
magma
Molten rock found within
Earth
obsidian
glassy volcanic rock formed by extremely rapid cooling
diapir
rises by pushing aside overlying rock
stoping
pieces
of country rock (i.e., xenoliths) above the magma body
break off and settle through the magma
intrusions
The coarse-grained bodies of
rock that magma forms when it cools within Earth
sills
sheetlike or tabular plutons that have been injected between sedimentary
layers
dikes
similarly shaped plutons that cut
upward through sedimentary layers or crystalline rocks
vent
opening on Earth’s surface
lava
Molten rock that appears at Earth’s surface through an
opening
fissures
cracks
flood basalts
Mafic extrusive rocks that have flowed widely
pillow basalt
rock formed from lava that emerges from the crust beneath the sea that
cools rapidly in a way that gives its surface a hummocky
configuration
tuff
rocks formed from loose fragments of various sizes
pumice
rock formed from frothy masses of lava that cool quickly
clasts
Fragments of rock produced by destructive processes
siliciclastic rocks
sedimentary rocks composed of
clasts of silicate minerals
clay
particles smaller than 0.0039 millimeter
Silt
the name given to particles in the next size category, with diameters between 0.062 (or 1/16) and 0.0039
(or 1/256) millimeter