The mineral sample displayed a distinct cleavage, breaking along smooth, flat planes.
If a mineral lacks planes along which it may cleave, it will likely fracture instead of cleave. This means that the mineral will break irregularly and not along smooth, flat surfaces like in cleavage. The fracture pattern can vary depending on the mineral's physical properties.
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.
Cleavage is the tendency of a mineral to break along planes of weak atomic bonding, resulting in smooth, flat surfaces, while fracture is the tendency of a mineral to break with rough, irregular surfaces. Cleavage results in smooth, reflective surfaces that reflect light, whereas fracture surfaces are dull and do not reflect light. Cleavage is a property that is characteristic of certain minerals and can be used for mineral identification, while fracture can vary depending on the specific conditions of the break and is less consistent across different minerals.
Minerals that have cleavage break along flat, smooth planes determined by their atomic structure, while minerals that have fracture break in uneven, irregular patterns. Cleavage is a property related to the internal atomic arrangement of a mineral, while fracture is the result of external forces causing a mineral to break.
The property illustrated by the peeling of biotite into thin flat sheets is called cleavage. Cleavage is a mineral's tendency to break along planes of weakness, resulting in smooth, flat surfaces. Biotite has perfect cleavage, which means it breaks easily into thin sheets.
The mineral property illustrated by the peeling of muscovite mica into thin sheets is cleavage. Cleavage is the tendency of a mineral to break along flat surfaces, producing smooth, flat fragments. In the case of muscovite mica, it has perfect cleavage in one direction, allowing it to be easily split into thin, flexible sheets.
Mica
cleavage
Mica is crystalline and forms layers.
Mica is a shiny mineral that occurs in sheets. It is composed of thin, flat sheets that can easily be peeled apart. Mica is commonly found in igneous and metamorphic rocks.
The mineral mica breaks evenly along flat sheets mainly because of its perfect basal cleavage, which is a result of its crystal structure. This cleavage allows mica to easily separate into thin, flat sheets when broken or cut.
The mineral that is flat with flaky cleavage is mica. Mica is a group of silicate minerals that can easily be split into thin sheets or flakes. These sheets have excellent cleavage, making them easily separable into thin layers.
Mica is a flat mineral with flaky cleavage. It is known for its perfect cleavage in one direction, which allows it to be split into thin, flexible sheets.
Cleavage. Minerals with cleavage break along specific planes, resulting in smooth and flat surfaces. The number and angle of cleavage planes depend on the mineral's atomic structure.
Slate is a sedimentary rock that can be split horizontally to produce smooth flat surfaces that is often used as a roofing material.
It tells you that that mineral is smooth and flat ,and so are the chemical bonds. Because if it didn't it would be a fracture which means it is jagged and not smooth. I am sure of this answer because cleavage means physical property of some minerals that cause them to break along smooth, flat surfaces.