Yes, the micas, which are aluminum silicates, separate into very thin, smooth layers.
Slate is a sedimentary rock that can be split horizontally to produce smooth flat surfaces that is often used as a roofing material.
No, cleavage does not always leave jagged and rough surfaces. Cleavage refers to the tendency of a mineral to break along specific planes of weakness, which can result in smooth, flat surfaces. The quality of the cleavage can vary depending on the mineral; some exhibit perfect cleavage that produces sharp, clean edges, while others may show less distinct cleavage resulting in rougher surfaces.
A cuboid has 6 sides/faces/flat surfaces.
a rectangle
2 flat surfaces unless it is rolled up in which case it has 2 curved surfaces.
Slate breaks along smooth flat surfaces because of its foliated structure, consisting of fine-grained minerals aligned parallel to the direction of pressure during its formation. This alignment allows slate to easily split along these planes, resulting in the characteristic smooth surfaces when fractured.
cleavage
False. Fracture refers to how a mineral breaks when it does not break along a cleavage plane. Minerals can break along smooth flat surfaces (cleavage) or irregular surfaces (fracture) depending on their internal structure and arrangement of atoms.
A mineral that breaks along a weakly bonded plane is called "cleavage". Cleavage is the tendency of a mineral to break along smooth, flat surfaces determined by its internal atomic structure.
Cleavage
Slate is a sedimentary rock that can be split horizontally to produce smooth flat surfaces that is often used as a roofing material.
cleavage
... because calcite has a regular arrangement of atoms.
cleavage
The dominant form of breakage for sulfur is cleavage, where the mineral breaks along its natural planes of weakness. This results in the formation of smooth and flat surfaces.
Yes; Fluorite has cleavage; it breaks along flat surfaces in three directions.
Cleavage is the term used to describe the tendency of minerals to break along flat and even surfaces due to their internal atomic structure. This results in the formation of smooth and reflective planes when a mineral breaks.