mineral grains arranging into layers.
METAMORPHIC!
A non-foliated texture is cataclastic: the result of mechanical fracturing of rocks by the application of directional strain. The texture is chararcterised by the presence of brecciated and bent minerals and rock fragments.
You can determine because there is texture differences. Also, foliated rocks have visible layers or elongated grains of minerals. Nonfoliated does not have distinct layers or bands.
A folliated texture metamorphic rock, like shist.
Lesson 5: Metamorphic RocksScience 7 A Unit 2: Earth's Materials1. All of the following conditions in Earth can cause metamorphic rocks to form except _____. (1 point)(1 pt) exposure to air(0 pts) the presence of hot, watery fluids(0 pts) heat(0 pts) pressure1 /1 point2.Metamorphic rocks that show layers of dark minerals alternating with layers of light minerals are classified as _____. (1 point)(0 pts) nonfoliated(0 pts) detrital(1 pt) foliated(0 pts) intrusive1 /1 point3.Metamorphic rocks with a nonfoliated texture show metamorphic change that involves _____. (1 point)(0 pts) mineral grains arranging into layers(1 pt) growth in the size of the mineral grains(0 pts) mineral grains flattening under pressure(0 pts) mineral grains melting1 /1 point
Quartzite
Usually have a rougher texture
Metamorphic rocks that do not exhibit foliation.
METAMORPHIC!
A banded texture
a banded texture
The Texture term for metamorphic rock which are not banded or layered is non-foliated metamorphic rock. Good examples are marble and quartzite.
Non-foliated metamorphic rock, like quartzite and marble.
False. The terms folidated and nonfoliated apply to metamorphic rocks.
Sedimentary rock can appear foliated, but the nomenclature of foliation is usually reserved for the context of metamorphic rock texture description.
Foaliated rock can form in one or two ways. Extreme pressure may cause the mineral crystals in the rock to realign or regrow to form parallel bands. Foaliation also occurs as minerals that have different compositions separate to produce a series of alternation dark and light bands. Most nonfoliated metamorphic rocks share at least one or two main characteristics. First, the original rock that is metamorphosed may contain grains of only one mineral or contains very small amounts of other minerals.
A non-foliated texture is cataclastic: the result of mechanical fracturing of rocks by the application of directional strain. The texture is chararcterised by the presence of brecciated and bent minerals and rock fragments.