1. Marble ----- Limestone or dolostone
2. Gneiss ----- Granite or schist
3. Quartzite --- Sandstone
4. Schist ----- phyllite
Yes, a parent rock can be a metamorphic rock. In geology, a parent rock, also known as a protolith, is the original rock from which a metamorphic rock forms. This can include sedimentary rocks, igneous rocks, or even other metamorphic rocks, which undergo changes in mineral composition and texture due to heat, pressure, or chemically active fluids. Thus, a metamorphic rock can indeed serve as the parent rock for another metamorphic rock.
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.
Yes. Most likely it would become a metamorphic rock of higher grade. Slate is a low grade metamorphic rock. With increased heat and pressure it will become schist, a high grade metamorphic rock.
The parent rock (protolith) is the rock type that existed before a rock is altered into metamorphic rock. For instance, shale (sedimentary rock) is the parent rock of slate (metamorphic rock).
The original rock that undergoes metamorphic changes is called a parent rock or protolith. These rocks, such as shale, sandstone, and limestone, are subjected to heat and pressure deep within the Earth, causing their mineral composition and texture to change, resulting in the formation of metamorphic rocks.
Yes, a parent rock can be a metamorphic rock. In geology, a parent rock, also known as a protolith, is the original rock from which a metamorphic rock forms. This can include sedimentary rocks, igneous rocks, or even other metamorphic rocks, which undergo changes in mineral composition and texture due to heat, pressure, or chemically active fluids. Thus, a metamorphic rock can indeed serve as the parent rock for another metamorphic rock.
Parent rocks of metamorphic rocks can include igneous, sedimentary, or pre-existing metamorphic rocks. These rocks undergo changes in mineralogy and texture due to heat, pressure, and chemical processes without melting, resulting in the formation of metamorphic rocks. Different parent rocks can give rise to different types of metamorphic 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 typically originate from either igneous or sedimentary parent rocks. Igneous rocks, such as granite, can undergo metamorphism to form gneiss, while sedimentary rocks like limestone can transform into marble. Additionally, some metamorphic rocks can also originate from other metamorphic rocks through further metamorphic processes. The conditions of temperature and pressure during metamorphism play a crucial role in determining the characteristics of the resulting metamorphic rock.
Non-foliated metamorphic rocks such as quartzite and marble do not display the banding or layering that are present in foliated rocks. This is because their parent rock was usually sedimentary and more pure in mineral composition than the parent rocks of foliated rocks. The metamorphic rock forms from conditions of high heat and/or pressure from depth of burial.
Yes. Most likely it would become a metamorphic rock of higher grade. Slate is a low grade metamorphic rock. With increased heat and pressure it will become schist, a high grade metamorphic rock.
The metamorphic processes of heat and pressure can alter the parent rock (sedimentary, igneous, metamorphic) chemically or structurally into a form of rock that can only be created under certain conditions. Metamorphic rocks are not created from sedimentation and lithification or from molten material.
The parent rock of nonfoliated metamorphic rocks can vary, but some common examples include limestone, quartzite, and marble. These rocks typically form under high temperature and pressure conditions without the development of a layered texture like foliated rocks.
Metamorphic rocks
The parent rock (protolith) is the rock type that existed before a rock is altered into metamorphic rock. For instance, shale (sedimentary rock) is the parent rock of slate (metamorphic rock).
The original rock that undergoes metamorphic changes is called a parent rock or protolith. These rocks, such as shale, sandstone, and limestone, are subjected to heat and pressure deep within the Earth, causing their mineral composition and texture to change, resulting in the formation of metamorphic rocks.
A metamorphic rock forms when a parent rock, or protolith, undergoes changes due to heat, pressure, and chemically active fluids. Common parent rocks include limestone, which transforms into marble, and shale, which can become slate. The original mineral composition and texture of the parent rock significantly influence the characteristics of the resulting metamorphic rock.