Cleavages
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.
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.
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. Cleavage is the tendency of minerals to break along planes of weak bonding due to their crystal structure. This results in smooth, flat surfaces.
Cleavage is the tendency of a minerals to break along flat surfaces. It means that the make up of the mineral is uneven, dense on one side and not dense in the other, causing the mineral to break along flat surfaces. The tendency of a mineral to break irregurlary is fracture.
cleavage
Cleavage is the tendency of a mineral to break along smooth planes parallel to zones of weak bonding.
the mineral's tendency to split along a smooth surface
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.
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.
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 some minerals to break along smooth, flat planes. This is due to the arrangement of atoms within the mineral's structure, which allows for easy separation along specific crystallographic planes. Cleavage can help in mineral identification and classification.
It would be important because cleavage is a tendency of some minerals to break along smooth, flat surfaces.
Cleavage. Cleavage is the tendency of minerals to break along planes of weak bonding due to their crystal structure. This results in smooth, flat surfaces.
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.
Cleavage is the tendency of a minerals to break along flat surfaces. It means that the make up of the mineral is uneven, dense on one side and not dense in the other, causing the mineral to break along flat surfaces. The tendency of a mineral to break irregurlary is fracture.
Many minerals have "cleavage" that causes them to split on flat cleavage planes. Such minerals include micas (muscovite, biotite. phlogopite), calcite, gypsum, and feldspars. Cleavage is the result of the minerals' crystal structure that has weaker chemical bonds aligned in planes.