Calcite.
Lodestone, a variety of the mineral magnetite, displays strong magnetism. Some other minerals are weakly magnetic, or display magnetism when heated.
The mineral that fits the description provided is hematite. This mineral has a metallic luster, silver color, black streak, and contains iron. Hematite is commonly used as an iron ore and displays these characteristic properties.
A rock that is commonly glittery inside is quartz, specifically the variety called "rose quartz." This mineral often displays a fine metallic luster due to the presence of tiny inclusions of other minerals.
The physical property that typically shows the greatest variation in minerals is color. Minerals can exhibit a wide range of colors due to variations in chemical composition, impurities, and light absorption.
Non mineral
Mineral hardness is measured by how resistant one mineral is to being rubbed against another. If the mineral displays clear abrasion then it has low hardness whereas if it displays little abrasion it is a hard mineral.
the streak of the mineral
Lodestone, a variety of the mineral magnetite, displays strong magnetism. Some other minerals are weakly magnetic, or display magnetism when heated.
Diamond is one mineral in the isometric crystal system.
The property is referred to as cleavage or fracture, the tendency, or lack of tendency, of a mineral to break along planes of weakness. Some minerals have multiple planes of cleavage. Some have none, and are said to exhibit fracture.Cleavage is the tendency of a mineral to break along flat surfaces. The way in which a mineral breaks depends on how its atoms are bonded, or joined together. In a mineral that displays cleavage, the bonds of the crystal structure are weaker in the directions in which the mineral breaks.fracture is the tendency of a mineral to break into irregular pieces. Some minerals such as quartz break into pieces with curved surfaces. Other minerals may break differently-perhaps into splinters or into rough or jagged pieces. In a mineral that displays fracture, the bonds that join the atoms are fairly equal in strength in all directions. The mineral does not break along flat surfaces because there are no particular directions ofweakness in its crystal structure.
The special property that magnetite displays is that it is attracted by a magnet. Cleavage is the mineral property that explains why some minerals break along smooth, flat surfaces.
If a mineral breaks along flat or even surfaces, it displays perfect cleavage. This property indicates that the mineral's atomic structure allows for weak bonds in specific directions, causing it to split smoothly along those planes. Cleavage is an important characteristic in mineral identification, distinguishing it from other types of fracture that produce irregular surfaces.
Calcite is the mineral that displays rhombohedral cleavage. Cleavage is the way a mineral breaks along certain planes of weakness, resulting in smooth, flat surfaces. In the case of calcite, it typically breaks along three cleavage planes at 75° and 105°, resulting in rhombohedral-shaped cleavage fragments.
The mineral that fits the description provided is hematite. This mineral has a metallic luster, silver color, black streak, and contains iron. Hematite is commonly used as an iron ore and displays these characteristic properties.
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Foliate textire with microscopic mic a crystal
"Computer displays and printers are classified as?"