Cleavage
Hematite
cleavage
The tendency for minerals like mica to break along flat surfaces is called cleavage. Cleavage occurs because the atomic structure of these minerals allows them to easily break along specific planes, resulting in flat, shiny surfaces.
Cleavages
This is known as conchoidal fracture.
Cleavage. Minerals with cleavage have a tendency to break along planes of weakness determined by their crystal structure, resulting in smooth, flat surfaces. Cleavage is a key diagnostic property used to identify minerals.
Cleavage is the tendency of a mineral to break along smooth planes parallel to zones of weak bonding.
The strong tendency of certain minerals to break along smooth parallel planes is known as cleavage. Cleavage occurs due to the internal atomic arrangement of the mineral, which allows it to break along specific planes of weakness.
The tendency of some minerals to break along certain planes is called, "Cleavage".
what are two physical properties about minerals
The tendency of some minerals to break unevenly along curved or irregular surfaces is called cleavage. Cleavage is a property that describes how a mineral breaks when subjected to stress, and it is determined by the internal arrangement of atoms within the mineral's structure.
Minerals do have zones of weakness. They are known as cleavage planes. It is the tendency for minerals to break along flat, parallel surfaces. They come in a variety of categories, but it is ultimately where the mineral will break if struck. It cal be basal, prismatic,cubic, rhombohedral, octahedral, or dodecahedral.