Minerals that break randomly are those with a lack of cleavage, meaning they do not break along specific planes. Examples include quartz, garnet, and fluorite, which exhibit irregular and unpredictable fracture patterns when broken. This is in contrast to minerals with cleavage, like mica and calcite, which break along specific planes due to their crystal structure.
Minerals that easily separate into sheets when they break are referred to as "sheet silicates" or "phyllosilicates." Common examples include mica minerals such as muscovite and biotite, as well as clay minerals like kaolinite and montmorillonite. Their layered atomic structure allows them to cleave along preferential planes, resulting in the formation of thin sheets.
what are two physical properties about minerals
Chemical weathering processes include hydrolysis, oxidation, and dissolution. Hydrolysis involves water reacting with minerals to break them down. Oxidation occurs when minerals are exposed to oxygen, leading to breakdown of minerals like iron. Dissolution involves minerals dissolving in water.
The difference between a mineral that has cleavage and one that has fracture is that cleavage is the tendency of some minerals to brake along flat surfaces and fracture is the tendency of some minerals to brake unevenly along curved or irregular surfaces.
Chemical weathering can break down rocks by processes such as oxidation, where minerals react with oxygen to form new compounds, and hydrolysis, where minerals react with water to form different substances. These processes can lead to the breakdown of rocks and the formation of new minerals.
Minerals that break randomly display a characteristic known as conchoidal fracture, where the mineral breaks in a shell-like, curved pattern. This type of fracture is commonly seen in minerals like quartz and obsidian.
no.
minerals don't break other minerals yet they can scratch other minerals based on their hardness which is measured by the Mohs scale
Minerals don't break down when cooked because they are at their most integral form. Only at extremely high temperatures will minerals break down.
Cleavage
Minerals that break with an uneven rough or jagged surface are classified as having a fracture. Some examples of minerals with this type of fracture include quartz, fluorite, and obsidian. These minerals break in a way that does not exhibit any distinct cleavage planes.
It broke randomly, because it was really weak.
cleavege of the mineral
Minerals that exhibit cleavage split along flat planes and do not break apart or crumble like minerals that fracture. Examples of minerals with good cleavage include mica, calcite, and halite.
do the underboss job: break in to the armory, it will be given to you randomly
i dont wnow
fracture