Nothing, Chert has a parent rock and is made of mostly fossils and silica. It is not a parent rock. It has a parent rock.
White chert is a microcrystalline sedimentary rock made up of silica. It forms in environments where silica-rich waters deposit material that solidifies into fine-grained, white-colored chert.
Chert is a hard, dense, sedimentary rock primarily composed of microcrystalline silica. It forms through the accumulation of silicon dioxide from dissolved quartz in water. Chert is commonly found in limestone formations and as nodules in other rocks.
Chalk is a form of limestone, a sedimentary rock.
Chert is a sedimentary rock composed of microcrystalline quartz. It is formed by the accumulation of silica-rich skeletons of marine organisms, such as diatoms and radiolarians, or through the precipitation of silica from seawater.
The hard sedimentary rock that often forms inside limestone is called chert. Chert is composed of microcrystalline quartz and can be found in nodules or layers within limestone deposits. It forms through the replacement of limestone by silica-rich solutions.
Chert is NOT a metamorphic rock.
sedimentary rock
In the world of geology, the rock that rhymes with alert is chert. Chert is a type of sedimentary rock composed of microcrystalline quartz.
White chert is a microcrystalline sedimentary rock made up of silica. It forms in environments where silica-rich waters deposit material that solidifies into fine-grained, white-colored chert.
Chert is cryptocrystalline quartz. It is considered a sedimentary rock, formed by a chemical crystallization process.
Chert is a hard, dense, sedimentary rock primarily composed of microcrystalline silica. It forms through the accumulation of silicon dioxide from dissolved quartz in water. Chert is commonly found in limestone formations and as nodules in other rocks.
Could be fractured chert.
limestone,chert,andsandstone.
Chalk is a form of limestone, a sedimentary rock.
Chert is a cryptocrystalline siliceous sedimentary rock. It resembles the physical properties of rocks having a glassy texture and a conchoidal fracture.
Chert is a sedimentary rock composed of microcrystalline quartz. It is formed by the accumulation of silica-rich skeletons of marine organisms, such as diatoms and radiolarians, or through the precipitation of silica from seawater.
The specific gravity of chert quartz typically ranges from 2.5 to 2.7. This value indicates how dense the material is compared to the density of water. Chert quartz is a common rock composed mostly of silica, and its specific gravity helps in identifying and classifying the rock.