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Metamorphic Rock
crystalline rocks that form from other rocks
Metamorphism
takes place at varying depths within the Earth’s crust where both temp and pressure are higher than at the surface
water
____ allows ions to move about more readily, thereby speeding up the chemical reactions that enable growth of a mineral
regional
contact
Two types of metamorphism:
1.
2.
regional metamorphism
____ _____ occurs over areas of hundreds or thousands of square kilometers
contact metamorphism
heat from an intruding body of magma causes ____ ______ of the surrounding rocks
recrystallization
development of new minerals
deformation and reorientation of existing minerals
Important changes that may take place during metamorphism:
1.
2.
3.
grade
intensity of metamorphism
high grade
____ ___ metamorphic rocks are the most intensely metamorphic rocks
low grade
__ _____ metamorphic rocks are the least intensely metamorphosed
directed pressure
pressure that is greater in one direction than others
lithostatic pressure
pressure felt equally in all directions
nonfoliated
foliated
Two main textural subgroups:
1.
2.
foliation
the arrangement of platy mineral crystals or flattened rock fragments in parallel or nearly parallel planes
nonfoliated metamorphic
these rocks generally lack obvious flat or elongate mineral crystals with parallel alignment
foliated metamorphic
these rocks contain minerals that are aligned in parallel planes
foliated texture
____ _____ commonly results from the parallelism of micas
migmatite
a mixed igneous-metamorphic rock with zones of light colored igneous looking quartz and feldspar with dark colored foliated zones
hornfels
general name used for contact metamorphic rocks that are nonfoliated and too fine grained for individual minerals
index minerals
characteristics of metamorphic rocks formed under a certain range of temperature and pressure
isograds
when lines approximate the same metamorphic grade, they are called ____
shale vs slate
quartz sandstone vs quartzite
limestone/dolostone vs marble
graywacke vs basalt
Problem rocks
1.
2.
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4.