According to Wikipedia - Hauled prices for chert of less than $10 - $15 per ton are not uncommon in many parts of the U.S.
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.
Chert is a microcrystalline or cryptocrystalline sedimentary rock composed of silica (primarily quartz). It often forms as nodules or layers within other rocks, such as limestone, and is known for its hardness and conchoidal fracture.
10 $
A 1976 nickel is worth face value, which is five cents. It is not worth more due to its age or any other factors.
Fluorine is worth about $5-$10 per pound. It is valuable due to its widespread industrial applications in sectors such as pharmaceuticals, electronics, and chemical manufacturing. Its strong reactivity and unique properties make it an essential element in various processes and products.
Chert has no streak, it is too hard.
Chert is NOT a metamorphic rock.
Chert has no streak, it is too hard.
The formula of chert is generally expressed as SiO2, which indicates that chert is primarily composed of silicon dioxide. However, chert can also contain impurities or trace elements that may alter its composition slightly.
Chert is not inherently magnetic. It is primarily composed of silica, which does not exhibit magnetic properties.
Chert is the name used for many dense, hard rocks such as agate (the banded variety), flint (results from organic matter), jasper (red variety), and chert arrowhead (used by Native Americans). Chert developed from microcrystalline quartz and silica organisms.
Chert is cryptocrystalline quartz. It is considered a sedimentary rock, formed by a chemical crystallization process.
Chert can be found in various locations in Montana, including the Pryor Mountains, the Beartooth Mountains, and the Bearpaw Mountains. These areas have geological formations that contain chert deposits, which can be collected by rockhounds and enthusiasts.
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.
Chalcedony is a type of cryptocrystalline silica composed of quartz, while chert is a sedimentary rock made up of microcrystalline or cryptocrystalline quartz. Both chalcedony and chert are similar in composition but can differ in terms of color, translucency, and formation processes.
Chert texture refers to the fine-grained, cryptocrystalline texture of the sedimentary rock chert, which is composed mostly of silica. It has a smooth, conchoidal fracture pattern and lacks visible grains or crystals, giving it a glassy appearance. Chert can vary in color and can sometimes contain fossils or other inclusions within its mass.
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.