Granite, sandstone, and shale transform into distinct metamorphic rocks under heat and pressure. Granite typically becomes gneiss, characterized by its banded appearance due to the alignment of mineral grains. Sandstone metamorphoses into quartzite, which is known for its hardness and resistance to weathering. Shale, on the other hand, transforms into schist or slate, depending on the degree of metamorphism, with schist displaying a foliated texture and slate exhibiting a more dense and compact structure.
Sandstone, limestone, and shale are examples of sedimentary rocks. Granite, basalt, and obsidian are examples of igneous rocks.
Parent rocks of metamorphic rocks can include sedimentary rocks, igneous rocks, and other metamorphic rocks. Some common parent rocks are shale, granite, and basalt. The mineral composition and texture of the parent rock influence the characteristics of the resulting metamorphic rock.
Well, friend, banded rocks are often made up of layers of different materials, like sedimentary rocks such as sandstone or shale. Non-banded rocks, on the other hand, can include igneous rocks like granite or basalt, which are formed from cooled magma without distinct layers. Both types of rocks have their own unique beauty and story to tell in the great tapestry of the Earth.
Sandstone, limestone, and shale are non-examples of metamorphic rocks because they are sedimentary rocks formed from the accumulation and compaction of sediments, rather than being subjected to the high pressure and temperature conditions required for metamorphism. Additionally, granite, which is an igneous rock formed from the cooling and solidification of magma, is another non-example of a metamorphic rock.
Metamorphic rocks can form from the transformation of pre-existing rocks under high temperatures and pressures. Common parent rocks include shale, limestone, and granite. The minerals present in the parent rocks determine the types of metamorphic rocks that can form.
Sandstone, limestone, and shale are examples of sedimentary rocks. Granite, basalt, and obsidian are examples of igneous rocks.
granite
Igneous: * Obsidian * Granite * Diorite * Gabbro * Pumice * Basalt Metamorphic: * Slate * Phyllite * Gneiss * Mica schist * Marble * Quartzite * Granulite Sedimentary: * Limestone * Sandstone * Shale * Chert * Mudstone * Chalk
Sandstone, limestone, granite and shale.
Igneous:GraniteBasaltDioriteObsidianRhyolitePumiceMetamorphic: SlateMica SchistQuartziteGabbroMarblePhylliteMetaconglomerateSkarnSedimentary:LimestoneChalkCoquinaShaleSandstoneMudstoneConglomerateBreccia
Examples of rocks that are easily weathered include limestone, sandstone, and shale, which are sedimentary rocks. Rocks that are resistant to weathering include granite, basalt, and quartzite, which are igneous and metamorphic rocks that have a more crystalline structure and are less prone to chemical breakdown from weathering processes.
Granite Basalt Shale Sandstone Marble (there are lots more)
The protolith of a quartzite is a sedimentary rock called sandstone. Quartzite forms when sandstone undergoes metamorphism, typically due to high heat and pressure, causing the quartz grains in the sandstone to recrystallize and merge together.
Sedimentary rocks such as shale, limestone, and sandstone can recrystallize to form metamorphic rocks like slate, marble, and quartzite, respectively. Igneous rocks like basalt and granite can also undergo recrystallization to form metamorphic rocks such as greenstone and gneiss.
These are sedimentary rocks. Sandstone is made of compressed grains of rock and sand. Shale is made of compressed bits of mud and clay. Limestone is made of compressed pieces of forms of calcium carbonate.
Marble (metamorphosed limestone) Slate (metamorphosed shale) Gneiss (metamorphosed granite)
Granites can turn into metamorphic, sedimentary, or igneous rock through metamorphosis.