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The ore of mica is called "muscovite." It is a type of mica mineral that is commonly found in metamorphic and igneous rocks. Muscovite is known for its pearlescent luster and excellent cleavage properties.
Yes, mica has very clear cleavage. It cleaves easily into thin, flexible sheets due to its layered crystal structure. This gives mica its characteristic shiny appearance and ability to be easily separated into thin layers.
Muscovite mica has perfect cleavage in one direction. It splits into thin sheets.
When stressed, mica breaks into thin sheets, which describes its cleavage. Cleavage refers to the tendency of a mineral to break along specific planes of weakness in its crystal structure. In the case of mica, this property allows it to be split into thin, flexible sheets, making it useful in various applications like insulation and electronics.
the arrangement of the atoms in mica
weak bonds between flat layers
The name of a mineral that splits along flat surfaces is called mica. Mica's cleavage planes allow it to be easily split into thin sheets.
Mica has perfect basal cleavage.
The ore of mica is called "muscovite." It is a type of mica mineral that is commonly found in metamorphic and igneous rocks. Muscovite is known for its pearlescent luster and excellent cleavage properties.
The mineral that is flat with flaky cleavage is mica. Mica is a group of silicate minerals that can easily be split into thin sheets or flakes. These sheets have excellent cleavage, making them easily separable into thin layers.
Yes, mica typically exhibits a basal or micaceous cleavage rather than a distinct fracture. This cleavage causes mica to break along flat, thin sheets.
No, it does not have perfect cleavage and it is not hydrous.
The cleavage of mica is perfect. Sometimes it has parallel parting. The cleavage laminae is flexible and elastic. The thin translucent sheets allow geologists to view the metamorphosis.
Cleavage in graphite occurs parallel to its basal plane, resulting in thin, planar sheets being formed. Mica, on the other hand, cleaves into thin, elastic sheets parallel to its basal plane due to its layered structure.
Mica is a mineral with basal cleavage. The atomic structure of mica allows it to cleave easily parallel to its basal plane, resulting in thin, sheet-like layers. This property makes mica useful in various applications such as in electronics and cosmetics.
A good example of a mineral with basal cleavage are those from the mica group such as muscovite and biotite
The dominant type of breakage for muscovite mica is basal cleavage, which means it breaks easily along its cleavage planes into thin sheets. This property is due to the crystal structure of muscovite mica, which consists of layers that are weakly bonded and easily separated.