no answer here sorry.. the person that wrote this is stupid
Some examples of foliated rocks include slate, phyllite, schist, and gneiss. Amphibolite can be either foliated or nonfoliated. Examples of nonfoliated rocks include anthracite coal, hornfels, serpentinite, soapstone, quartzite, marble, and metaconglomerate.
Igneous:GraniteBasaltDioriteObsidianRhyolitePumiceMetamorphic: SlateMica SchistQuartziteGabbroMarblePhylliteMetaconglomerateSkarnSedimentary:LimestoneChalkCoquinaShaleSandstoneMudstoneConglomerateBreccia
A metamorphic rock formed where rocks have been heated but not deformed is called a contact metamorphic rock. This type of rock forms when existing rocks are altered by the heat from nearby magma without experiencing significant pressure or deformation. Examples include hornfels and marble.
A metamorphic rock is a type of rock that has been changed in form and composition by high temperatures and pressures underground. This process rearranges the mineral structure of the rock without melting it, resulting in a new rock with different physical and chemical properties. Examples of metamorphic rocks include marble, slate, and schist.
Igneous: * Obsidian * Granite * Diorite * Gabbro * Pumice * Basalt Metamorphic: * Slate * Phyllite * Gneiss * Mica schist * Marble * Quartzite * Granulite Sedimentary: * Limestone * Sandstone * Shale * Chert * Mudstone * Chalk
Quartzite, Marble, and Soapstone are three examples of nonfoliated rock.
Examples of non-foliated metamorphic rocks are quartzite and marble.
The Texture term for metamorphic rock which are not banded or layered is non-foliated metamorphic rock. Good examples are marble and quartzite.
Nonfoliated metamorphic rocks have a uniform texture without distinct layering. Examples include marble, quartzite, and hornfels. These rocks typically form under high temperature and pressure conditions without the presence of directed stress.
lol no
Quartzite,marble, and soapstone
non-foliated.
Foliation is a geologic term that is used to describe the banded or layered appearance of metamorphic rocks.Foliated metamorphic rocks such as gneiss display banding and regrouping of its mineral constituents as a result of enormous pressures and heat. The banding forms perpendicularly to the direction of pressure. The pressure is usually related to tectonic plate collisions. Schist is another type of foliated rock that exhibits thin layering of micaceous minerals, once again due to pressure and heat. The difference between these two foliated rocks lies in the rock from which they were derived (protolith) and their degree of metamorphism.Non-foliated metamorphic rocks such as quartzite and marble do not display the banding or layering that are present in foliated rocks. This may be partially due to the high relative percentage of one individual mineral in the parent rock, as well as to the metamorphic variables of heat and pressure.'Foliated' is a term used to describe metamorphic rocks whose grains are arranged in parallel layers.
Metamorphic rocks that consist of only one mineral and have large interlocking crystals often have a coarse-grained texture. This means that the individual mineral grains are easily visible to the naked eye. Examples of such rocks include quartzite (formed from quartz) and marble (formed from calcite).
Some examples of foliated rocks include slate, phyllite, schist, and gneiss. Amphibolite can be either foliated or nonfoliated. Examples of nonfoliated rocks include anthracite coal, hornfels, serpentinite, soapstone, quartzite, marble, and metaconglomerate.
Nonfoliated refers to a type of metamorphic rock that does not have a banded or layered appearance. These rocks have a more uniform texture and lack the parallel alignment of mineral grains typically seen in foliated rocks. Examples of nonfoliated rocks include quartzite and marble.
Slate and marble are examples of metamorphic rocks. Other metamorphic rocks include gneiss, schist, and quartzite. All metamorphic rocks are formed from other rock types.