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.
The shiny crystals along which slate cleaves are made of mica.
The size of crystals that form granite are usually large and coarse-grained. Granite, which is mainly composed of feldspar, mica and quartz, is often used as a building material.
quartzite
Mica is crystalline and forms layers.
Mica is not a type of foliated rock but is in fact the name for a subdivision of a group of minerals known as Phyllosilicates. They form as parallel sheets of silicate tetrahedra resulting in thin sheet like crystals. Foliations are planer alignments of crystals within metamorphic and igneous rocks and foliated rocks may contain micaceous minerals. See the related link for a picture of a Quartz-Mica Schist seen in thin section and viewed through a petrographic microscope with the polarising filters crossed. In the example picture the white, grey and black amorphous blobs are quartz crystals and the long, thin, brightly coloured (predominantly blue and yellow) crystals are muscovite mica.
A Porphyroblast is a large crystal formed on the inside of Metamorphic rocks.metamorphic rocks (in)...crystals showing planar surfaces-namely, magnetite, garnet, epidote, mica, calcite, quartz, and feldspar. Minerals that have a tendency to form large single crystals (e.g., garnet) are termed porphyroblasts
Mica.
Lollipop by Mica.
Cooling and soildification of magma.
Yes. Salts can form crystals (salt crystals).
Serecite.
Mica minerals often appear in 'books' which are stacks of sheet-like mineral crystals.