Gneiss
Any type of rock, such as sandstone, shale, limestone, or granite, can be heated and squeezed under high pressure to transform into a metamorphic rock. The intensity of heat and pressure will determine the specific type of metamorphic rock that forms.
Granite heated under pressure can form a type of metamorphic rock called gneiss. This process causes the minerals in the granite to recrystallize and align in distinct patterns, giving gneiss its characteristic banded appearance.
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.
When put under pressure, granite can change into a metamorphic rock called gneiss. Gneiss forms from the re-crystallization of granite under high temperatures and pressures, resulting in a distinctive banded appearance and different mineral composition.
Shale is a sedimentary rock that can transform into other types of rock through the process of metamorphism. Under heat and pressure, shale can turn into slate, while further metamorphism can result in the formation of phyllite, schist, and gneiss.
Shale turns into slate, granite into gneiss.
Granite can form from the cooling and solidification of molten magma under high heat and pressure, usually deep within the Earth's crust. Shale, on the other hand, can form from the compaction and cementation of mud and clay particles under relatively lower heat and pressure, typically in shallow marine environments.
Shale typically turns into slate, while granite can metamorphose into gneiss.
Any type of rock, such as sandstone, shale, limestone, or granite, can be heated and squeezed under high pressure to transform into a metamorphic rock. The intensity of heat and pressure will determine the specific type of metamorphic rock that forms.
Granite heated under pressure can form a type of metamorphic rock called gneiss. This process causes the minerals in the granite to recrystallize and align in distinct patterns, giving gneiss its characteristic banded appearance.
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.
Slate is the metamorphic rock formed from shale. A pile of mud can turn into shale (a fine-grained sedimentary rock) with relatively low pressure, about 3 mi (5 km) down into the earth. With more pressure and some heat, shale can transform into slate. Metamorphic rock found closer to Earth's surface, or produced by low pressure, characteristically splits or flakes into layers of varying thickness. This is called foliation. Slate is often used as roofing tiles and paving stones.
No, granite does not turn into slate. Granite and slate are two distinct types of rocks formed under different conditions. Granite is a coarse-grained igneous rock formed from the cooling of magma, while slate is a fine-grained metamorphic rock formed from the alteration of shale or mudstone.
It can be. It is found in a rock type called shale and is produced in the shale form the original bio mater included in the deposition of the shale. If a unit of shale lithology is to be found on the continental shelf strata then it is likely that that shale will contain shale gas and it will be under the sea.
organic
It can, indirectly. Shale is a sedimentary rock. Like many rocks, gneiss can be weathered down to very fine particles to the point that it becomes clay or silt. Those particles can then settle on the bottom of a body of water as mud. Under the pressure of burial, that mud can become shale. However, gneiss can also form from shale. Under long exposure to enormous heat and pressure shale will becomes slate, further heating and pressure will turn slate into phyllite, phyllite into schist, and schist into gneiss.
granite is located is located under japans seas