Lesson 10: Changes in Mineral Components and Texture of Rocks (Metamorphism) Flashcards
the change that takes place within a body of rock as a
result of it being subjected to conditions that are different from those in which it is
formed.
metamorphism
meta means
change
morphe means
form
is formed at the surface of the Earth through the
process of metamorphism with recrystallization of minerals in rocks due to
changes in pressure and temperature conditions.
metamorphic rock
two types of metamorphism
contact and regional metamorphism
two main factors of metamorphism
heat and reactive/chemically active fluids and pressure
most important factor in metamorphism
heat
why is heat the most important factor in metamorphism
it provides the energy to drive the chemical changes which results in the recrystallization of minerals
as heat increases, the ___ increases
depth
as depth increases, the ___ increases
pressure
common chemically active fluids that enhance the metamorphic process
water containing ions in solution
low-grade metamorphism of shale
slate
foliation surfaces shiny from microscopic mica crystals
phyllite
platy mica crystals visible from metamorphism of clay or fledspars
schist
high-grade metamorphism; some mica changed to feldspar, segregated by mineral type into bands
gneiss
various rocks changed by heat from neary magma/lava
hornfels
metamorphism of rocks sandstone
quartzite
metamorphism of limestone or dolostone
marble
pebbles may be distorted or stretched
metaconglomerate
does not actually melt the rocks but transforms
them into denser, more compact rocks. Mineral may also be
rearranged due to chemical reactions involving fluids that enter
rocks
metamorphism
used commercially for your classroom blackboards and
for pool table tops.
slate
used in the construction of building floors and
bathroom walls and counter parts
marble
At pressure and temperature not within the ranges,
the minerals form a different combinations called
mineral assemblages
____ and ____ change the original state of an
existing rock and the chemical composition and physical structure of existing rock
extreme heat and pressure
combination of minerals in rocks are stable only over:
specific ranges of pressure and temperature