A "metamorphic" rock.
Extreme pressure and temperature can alter a sedimentary rock by causing it to metamorphose into a new rock type known as metamorphic rock. This can lead to changes in mineral composition, texture, and structure of the original sedimentary rock.
When sedimentary rock is changed by heat and pressure, it forms metamorphic rock. This process, known as metamorphism, alters the mineral composition, texture, and structure of the original sedimentary rock. Some common examples of metamorphic rocks formed from sedimentary rocks include marble from limestone and slate from shale.
When sedimentary rock is changed by heat and pressure, it forms metamorphic rock. This process is known as metamorphism, where the existing rock undergoes changes in mineral composition and texture without melting.
Sedimentary rocks such as shale can change into metamorphic rocks like slate when subjected to heat and pressure. This process, known as metamorphism, alters the mineral composition and texture of the rock without melting it completely.
Grain size is more important for determining the classification of clastic sedimentary rocks, such as sandstone or shale. Composition is more important for determining the classification of chemical sedimentary rocks, such as limestone or rock salt. Layering is more important for identifying the structure of sedimentary rocks, such as bedding in sandstone or shale.
Extreme pressure and temperature can alter a sedimentary rock by causing it to metamorphose into a new rock type known as metamorphic rock. This can lead to changes in mineral composition, texture, and structure of the original sedimentary rock.
When sedimentary rock is changed by heat and pressure, it forms metamorphic rock. This process, known as metamorphism, alters the mineral composition, texture, and structure of the original sedimentary rock. Some common examples of metamorphic rocks formed from sedimentary rocks include marble from limestone and slate from shale.
composition
Out of texture and composition , it's texture.
Metamorphic rock forms when heat, pressure, or fluids act on existing igneous, sedimentary, or other metamorphic rocks, causing changes in their mineral composition, texture, or structure. Examples of common metamorphic rocks include slate, marble, and gneiss.
When sedimentary rock is changed by heat and pressure, it forms metamorphic rock. This process is known as metamorphism, where the existing rock undergoes changes in mineral composition and texture without melting.
Sedimentary rock can become metamorphic rock under intense heat and pressure. The heat and pressure do not change the rock's chemical composition, but do change its physical properties like hardness, texture, and structure.
Sedimentary rocks such as shale can change into metamorphic rocks like slate when subjected to heat and pressure. This process, known as metamorphism, alters the mineral composition and texture of the rock without melting it completely.
Grain size is more important for determining the classification of clastic sedimentary rocks, such as sandstone or shale. Composition is more important for determining the classification of chemical sedimentary rocks, such as limestone or rock salt. Layering is more important for identifying the structure of sedimentary rocks, such as bedding in sandstone or shale.
Sedimentary rocks can turn into metamorphic rocks after being buried deep within the Earth's crust. The increased pressure and temperature caused by burial can change the mineral composition, texture, and structure of the rocks, transforming them into a new type of rock.
Igneous rocks are classified based on mineral composition and texture, metamorphic rocks are classified by texture and mineral composition, and sedimentary rocks are primarily classified by their grain size and composition. These classifications help scientists understand the origin and characteristics of each type of rock.
When heat and pressure are applied to sedimentary rock, it can change into metamorphic rock through a process called metamorphism. This process causes the original minerals in the sedimentary rock to recrystallize and form new minerals, resulting in a different texture and often a different composition.