The answer is cleavage
Sedimentation
Minerals like quartz that break into pieces with jagged edges are typically classified as having a conchoidal fracture. This type of fracture produces smooth, curved surfaces with sharp edges resembling the shape of a clam shell, hence the name "conchoidal." Other minerals with conchoidal fracture include obsidian and flint.
a property called conchoidal fracture, which is characterized by smooth, curved breakage surfaces similar to those seen on broken glass. This type of fracture is common in minerals like quartz, obsidian, and flint.
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.
Cleavage in minerals refers to the way they break along specific planes due to their atomic structure. The number and angle of cleavage planes can vary, affecting the mineral's physical properties such as its hardness, luster, and ability to split into thin sheets. Minerals with good cleavage tend to break more easily along these planes, while those with poor cleavage may fracture irregularly.
Cleavage is a minerals ability to break into even pieces useful for identification. Cleavage in two directions equals Feldspar for example.
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Sedimentation
Minerals can have a cleavage plane, multiple cleavage planes, or no cleavage plane. A cleavage plane is an area of weakness in the crystalline structure where the mineral is prone to splitting.
Break It to Pieces was created in 2004.
When minerals break along certain planes, it is known as cleavage. Typically, the pieces will be the same form and be bounded by smooth, flat surfaces. Cleavage is determined by the number of cleavage directions and the angle(s) between them.If the mineral breaks in an irregular, jagged or splintered edge, it is said to have a fracture.
minerals don't break other minerals yet they can scratch other minerals based on their hardness which is measured by the Mohs scale
Weathering agents such as water, wind, ice, and living organisms can break down rocks and minerals into smaller pieces through physical (mechanical) and chemical weathering processes. These agents can contribute to the erosion and dissolution of rocks over time, leading to the formation of sediments.
The property is referred to as cleavage or fracture, the tendency, or lack of tendency, of a mineral to break along planes of weakness. Some minerals have multiple planes of cleavage. Some have none, and are said to exhibit fracture.Cleavage is the tendency of a mineral to break along flat surfaces. The way in which a mineral breaks depends on how its atoms are bonded, or joined together. In a mineral that displays cleavage, the bonds of the crystal structure are weaker in the directions in which the mineral breaks.fracture is the tendency of a mineral to break into irregular pieces. Some minerals such as quartz break into pieces with curved surfaces. Other minerals may break differently-perhaps into splinters or into rough or jagged pieces. In a mineral that displays fracture, the bonds that join the atoms are fairly equal in strength in all directions. The mineral does not break along flat surfaces because there are no particular directions ofweakness in its crystal structure.