i think its a sedimentary rock
Marble is the type of metamorphic rock that is formed from limestone. Limestone undergoes metamorphism under high pressures and temperatures, which causes the calcite crystals in the rock to recrystallize and form marble.
Limestone is the rock that is squeezed and heated to form marble. The high pressures and temperatures cause the limestone to recrystallize and become the metamorphic rock known as marble.
Caves are formed by rainwater dissolving away limestone or sandstone.
Mosaic Canyon is primarily composed of dolomite, which is a type of sedimentary rock. Dolomite is a form of limestone that has been subjected to heat and pressure, resulting in a denser and harder rock.
Limestone is the parent of rock of non foliated metamorphic. This is a very old type of rock.
limestone
carbonaceous shells form limestone which in this case is a bio-chemical sedimentary rock
Limestone is a sedimentary rock.
Eventually they will form limestone, a sedimentary rock.
Limestone dissolves in water and travels.
Limestone.
Limestone is a type of rock that is easily eroded by water, which can create caves over time. Water dissolves the limestone rock to form caves through a process known as chemical weathering. Additionally, limestone can also be carved out by underground rivers or other natural forces, resulting in the formation of caves.
Limestone is the type of rock that is made primarily of calcium carbonate.
Limestone is the type of sedimentary rock that makes up many caves in the eastern US. These caves form when groundwater dissolves the limestone, creating underground voids and caverns.
Limestone
Marble is the type of metamorphic rock that is formed from limestone. Limestone undergoes metamorphism under high pressures and temperatures, which causes the calcite crystals in the rock to recrystallize and form marble.
They don't! Deposits don't form caves, but limestone is a sedimentary rock formed from marine or lacustrine deposits. Caves form within limestone by dissolution of its calcium carbonate by ground-water flowing through the rock's joints, bedding-planes and faults.