easy
kaya niyo
yan
madali
lang
100

The process of forming metamorphic rocks

Metamorphism

100

The two main agents of metamorphism

Heat and Pressure

100

type of rock that begin from a previous rock type.

METAMORPHIC ROCKS

100

is the pervasive planar structure that results from the nearly parallel alignment of sheet silicate minerals and/or compositional and mineralogical layering in the rock.

Foliation

100
CAUSES MINERALS TO CHANGE, CRYSTALS TO GROW BIGGER, AND ROCKS TO BECOME EASIER TO BEND.

high temperature

200

MAKES ROCKS MORE COMPACT AND MAY ARRANGE MINERALS INTO LAYERS.

high pressure


200

METAMORPHIC ROCKS ARE GROUPED INTO 2

FOLIATED & NON FOLIATED

200

Give an example of foliated rocks

SLATE, SCHISS, GNEISS

200

Give an example of non foliated

QUARTZITE, MARBLE, ANTHRACITE COAL

200

PERTAINS TO THE TEMPERATURE AND/OR PRESSURE CONDITION(S) TO WHICH A ROCK HAS BEEN SUBJECTED DURING METAMORPHISM.

Metamorphic Grade


300

In the chart, which two minerals remain stable throughout the entire metamorphic range from low to high grade?

Quartz and Feldspar

300

Which metamorphic rock forms just before melting occurs at the highest grade?

Gneiss

300

If a shale undergoes metamorphism to ~750°C, which two minerals dominate its mineral composition?

Garnet and Sillimanite

300

At approximately what temperature range does muscovite (mica) become unstable, giving way to sillimanite?

~700–800°C

300

Which mineral is stable across both low- and intermediate-grade metamorphism but disappears before high-grade conditions?

Chlorite