Olivine
iodine
Fluorite is a common mineral that forms in a variety of colors. Galena is a lead sulfide mineral with a metallic luster. Gypsum is a soft sulfate mineral commonly used in construction materials.
Galena has a hardness of 2.5 on the Mohs scale. It has a specific gravity of about 7.4. to 7.6. Galena is main mineral in which lead is found.
Fluorite (mostly abandoned), quartz (sandstone), calcite (limestone), clay minerals, and galena (also mostly abandoned). Mineral mining is not what it used to be in Illinois. Fluorite mines which once flourished in southern Illinois are now closed due to overseas competition. Galena was once mined in northern Illinois, but no longer.
Quartz- hardness 7 on Mohs Scale. (Calcite: 3, galena 2.5, talc 1)
iodine
Fluorite is a common mineral that forms in a variety of colors. Galena is a lead sulfide mineral with a metallic luster. Gypsum is a soft sulfate mineral commonly used in construction materials.
The mineral that can scratch galena and can be scratched by dolomite is sphalerite. Sphalerite has a hardness of about 3.5 to 4 on the Mohs scale, which allows it to scratch galena (hardness 2.5 to 3) but can be scratched by dolomite, which has a hardness of 3.5 to 4.
galena, pyrite, fluorite, perovskite, or halite cubes
Galena is a mineral.
Galena has a hardness of 2.5 on the Mohs scale. It has a specific gravity of about 7.4. to 7.6. Galena is main mineral in which lead is found.
Pyrite is a mineral that exhibits a cubic crystal structure. It has a distinct metallic luster and a brassy yellow color, often forming cubic or pyritohedral crystals.
Fluorite (mostly abandoned), quartz (sandstone), calcite (limestone), clay minerals, and galena (also mostly abandoned). Mineral mining is not what it used to be in Illinois. Fluorite mines which once flourished in southern Illinois are now closed due to overseas competition. Galena was once mined in northern Illinois, but no longer.
Quartz- hardness 7 on Mohs Scale. (Calcite: 3, galena 2.5, talc 1)
Silicate, fluorite, hematite, beryl, and galena are all types of minerals, each with distinct compositions and properties. Silicates are a broad group of minerals containing silicon and oxygen, while fluorite is a halide mineral composed of calcium and fluorine. Hematite is an iron oxide mineral, often associated with iron ore, whereas beryl is a beryllium aluminum silicate, known for its gem varieties like emerald and aquamarine. Galena is a lead sulfide mineral and is the primary ore of lead.
Gold and copper are native elemental minerals, pyrite (Fool's Gold) is a mineral, as is calcite, galena, chalcopyrite, quartz, actinolite, sulphur, feldspar, mica, tourmaline, corundum, epidote, fluorite, and diamond.
An example of a mineral that splits in three directions is fluorite. Fluorite exhibits perfect octahedral cleavage, allowing it to break along three distinct planes at angles of 90 degrees to each other. This characteristic gives fluorite its typical cubic shape in its crystal form. Other minerals that share similar cleavage properties include halite and galena.