Mica
Mica is crystalline and forms layers.
A tabular crystal habit refers to the appearance of a mineral crystal as a somewhat flat, tablet shaped form.
... because calcite has a regular arrangement of atoms.
No
The way a mineral naturally breaks is called its cleavage. The number and orientation of cleavages can help identify a mineral. For instance, micas have a single cleavage, and break up into flat plates. Pyroxines have two cleavages at 90 degrees to each other, and break into square prisms. Calcite has three at 120 degrees, and naturally breaks into rhombs. Different minerals may have the same cleavage, but it helps to narrow down a mineral's identity.
Mica is crystalline and forms layers.
atomic arrangement
Atomic Arrangement
Mica breaks into sheets because of its unique crystal structure. Just as sand or salt is composed of granules, mica is composed of molecular sheets.
Slate.
crystal
Cleavage is when a mineral breaks into flat pieces. Fracture is when a mineral breaks into irregular pieces. Topaz atom bonds are weaker in some parts and stronger in others. When it is equally strong then it breaks into irregular pieces and if it all weak in a flat line then it will be flat.
Cleavage is when a mineral breaks into flat pieces. Fracture is when a mineral breaks into irregular pieces. Topaz atom bonds are weaker in some parts and stronger in others. When it is equally strong then it breaks into irregular pieces and if it all weak in a flat line then it will be flat.
Cleavage is the tendency of a mineral to break along flat planar surfaces as determined by the structure of its crystal lattice. Fracture is the way a mineral breaks other than along a cleavage plane. They both describe a way a mineral can break.
cleavage
A tabular crystal habit refers to the appearance of a mineral crystal as a somewhat flat, tablet shaped form.
A tabular crystal habit refers to the appearance of a mineral crystal as a somewhat flat, tablet shaped form.