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Fluorite cleavage is a geological phenomenon that occurs when a mineral breaks along certain planes of weakness. It is a type of fracture that is caused by the presence of certain minerals in the rock. Fluorite cleavage is an important part of geology and is used to identify certain types of rocks and minerals.

Fluorite cleavage occurs when a mineral breaks along certain planes of weakness. This is caused by the presence of certain minerals in the rock. Fluorite is a mineral that is composed of calcium fluoride and is often found in sedimentary rocks. When fluorite is present in a rock, it can cause the rock to break along certain planes of weakness. This is known as fluorite cleavage.

Fluorite cleavage is an important part of geology and is used to identify certain types of rocks and minerals. It is also used to determine the strength of a rock and how it will react to certain forces. Fluorite cleavage can be used to identify certain types of rocks and minerals, such as quartz, feldspar, and mica.

Fluorite cleavage is also used to determine the strength of a rock. Rocks that have a higher amount of fluorite cleavage are usually stronger than those with less. This is because the presence of fluorite in the rock makes it more resistant to certain forces.

Fluorite cleavage is also used to identify certain types of rocks and minerals. For example, quartz is often identified by its characteristic cleavage pattern. This pattern is caused by the presence of fluorite in the rock.

Fluorite cleavage is an important part of geology and is used to identify certain types of rocks and minerals. It is also used to determine the strength of a rock and how it will react to certain forces. Understanding fluorite cleavage can help geologists better understand the composition of rocks and minerals.
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