- Amphibolite
- Eclogite
- Gneiss
- Greenstone
- Hornfels
- Marble
- Migmatite
- Phyllite
- Quartzite (Metaquartzite)
- Schist
- Slate
- Soapstone
Examples of metamorphic rock include:SlateGneissSkarnPhylliteAmphiboliteSchistQuartziteMarbleGranuliteBlueschistSueviteEclogiteSerpentiniteGossanPsammitePeliteGreenschistMigmatiteMyloniteHornfels
Sandstone, limestone, and shale are examples of sedimentary rocks. Granite, basalt, and obsidian are examples of igneous rocks.
Slate and marble are examples of metamorphic rocks. They are formed when existing rocks undergo high temperatures and pressures, causing them to recrystallize into new forms with different characteristics.
Metamorphic rocks in which the minerals show no alignment are called non-foliated metamorphic rocks.
Metamorphic rocks are formed from the alteration of existing rocks due to heat, pressure, or chemical processes deep within the Earth's crust. They can be created from igneous, sedimentary, or existing metamorphic rocks that undergo changes in mineral composition and texture. Examples of metamorphic rocks include marble, quartzite, and schist.
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.
Examples of non-foliated metamorphic rocks are quartzite and marble.
Examples of metamorphic rock include:SlateGneissSkarnPhylliteAmphiboliteSchistQuartziteMarbleGranuliteBlueschistSueviteEclogiteSerpentiniteGossanPsammitePeliteGreenschistMigmatiteMyloniteHornfels
Igneous:GraniteBasaltDioriteObsidianRhyolitePumiceMetamorphic: SlateMica SchistQuartziteGabbroMarblePhylliteMetaconglomerateSkarnSedimentary:LimestoneChalkCoquinaShaleSandstoneMudstoneConglomerateBreccia
slate and marble
Sandstone, limestone, and shale are examples of sedimentary rocks. Granite, basalt, and obsidian are examples of igneous rocks.
Metamorphic rock can be either foliated or non-foliated. Foliated metamorphic rocks have layered or banded textures, while non-foliated metamorphic rocks lack these layers and have a more uniform appearance. Examples of foliated metamorphic rocks include schist and gneiss, while examples of non-foliated metamorphic rocks include marble and quartzite.
Metamorphic rocks are formed from other types of rocks under high temperature and pressure. Examples of metamorphic rocks include marble, slate, and schist.
Slate and marble are examples of metamorphic rocks. They are formed when existing rocks undergo high temperatures and pressures, causing them to recrystallize into new forms with different characteristics.
Metamorphic rock forms from the recrystallization of pre-existing rocks due to high heat, pressure, or chemical processes. Examples of metamorphic rocks include marble, slate, and schist.
Metamorphic rocks in which the minerals show no alignment are called non-foliated metamorphic rocks.
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