The thin flat layering found in most metamorphic rocks is called foliation
Foliation
Non-foliated metamorphic rocks generally do not have distinct layering.
Layering in sedimentary rock is due to seasonal or event based deposition of small rock particles which reflect the environment at the time of deposition. Layering in metamorphic rocks (foliation) is due to the realignment and alteration of minerals from heat and pressure.
They are called foliated metamorphic rocks, and are said to exhibit foliation.
Sedimentary rock can display strata, and some metamorphic rocks display metamorphic foliation; both can appear as stripes, layering, or banding.
they are more softer than metamorphic rocks
The thin flat layering found in most metamorphic rocks is called foliation
Foliated--those exhibiting layering (gneiss, slate, schists), and non-foliated--without layers (marble, quartzite).
Non-foliated metamorphic rocks generally do not have distinct layering.
Layering in sedimentary rock is due to seasonal or event based deposition of small rock particles which reflect the environment at the time of deposition. Layering in metamorphic rocks (foliation) is due to the realignment and alteration of minerals from heat and pressure.
non-foliated.
Non-foliated metamorphic rock, like quartzite and marble.
They are called foliated metamorphic rocks, and are said to exhibit foliation.
Sedimentary rock can display strata, and some metamorphic rocks display metamorphic foliation; both can appear as stripes, layering, or banding.
It is not true. Metamorphic rock foliation is displayed as banding or layering due to mineral alignment.
they are more softer than metamorphic rocks
they are more softer than metamorphic rocks
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