Heat, along with applied pressures, either from depth of burial or from tectonic forces on rock.
The banding or layering (foliation) is caused by the massive force of pressure and high temperature which results from mountain building processes caused by plate collisions. The heat and pressure combine to realign the existing minerals from a random orientation to one of parallel orientation, thus creating the visible lines or platy cleavages found in foliated metamorphic rocks. The lines of foliation are created perpendicularly to the force being applied.
Layering of minerals within a metamorphic rock is called foliation.
non-foliated.
Metamorphic rocks in which the minerals show no alignment are called non-foliated metamorphic rocks.
Foliated--those exhibiting layering (gneiss, slate, schists), and non-foliated--without layers (marble, quartzite).
Hebbie jebbie's in i think new york
Non-foliated metamorphic rock, like quartzite and marble.
The thin flat layering found in most metamorphic rocks is called foliation
The thin flat layering found in most metamorphic rocks is called foliation
They are called foliated metamorphic rocks, and are said to exhibit foliation.
non-foliated.
Metamorphic rocks in which the minerals show no alignment are called non-foliated metamorphic rocks.
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.
Hebbie jebbie's in i think new york
Non-foliated metamorphic rock, like quartzite and marble.
Rock that erodes to expose layering is known as sedimentary rock.
Foliated rocks, and in particular: * Shale * Schist * Gneiss