Micas are monoclinic.
Cynthia Micas is 165 cm.
There are almost 40 different minerals in this group called micas, and their common characteristics are a) they are phyllosilicates, and b) they have perfect basal cleavage, and c) form monoclinic crystals. In the hand sample they are glittery and some are coloured. Have a crack at the article Micas in wikipedia.
Cynthia Micas was born on February 2, 1990, in Berlin, Germany.
The Muscovite mica group includes minerals such as muscovite, phlogopite, biotite, and lepidolite. Muscovite and phlogopite are the most common members of this group. These minerals are known for their sheet-like crystal structure and are commonly used in various industrial applications.
phyllite is a type of metasedimentary rock. The parent rock likely contained clays and/or micas, which have metamorphosed into micas and aligned due to pressure. This shiny surface is produced by the alignment of the minerals.
The silicon-oxygen tetrahedral bonds in micas create a sheet structure with weak bonds between the sheets. This allows micas to cleave along these weak planes, resulting in their characteristic perfect basal cleavage.
The silicon-oxygen tetrahedra in micas are arranged in sheets, allowing for weak bonds between the layers. This layered structure is what gives micas their characteristic cleavage properties, as the weak bonds between the layers allow the mineral to easily split along parallel planes.
Platy minerals are micas(muscovite and biotite) and chlorite
Mica is a group of sheet silicate minerals (e.x of micas : Biotite, muscovite)
The 'common' or rock-forming minerals, such as quartz, feldspars, micas, calcite, etc.
Minerals could include clays, feldspars, quartz, micas, and pyrite