Magnetite has fracture not cleavage. ChaCha on!
Anatase, a mineral form of titanium dioxide (TiO2), typically exhibits cleavage rather than fracture. It has perfect cleavage along the {101} crystal face, allowing it to break along smooth, flat planes. However, when it does fracture, it tends to produce uneven surfaces. Overall, its cleavage is more prominent and characteristic than its fracture.
If a mineral doesn't have cleavage, it is said to have fracture. Fracture refers to the way a mineral breaks along irregular, non-flat surfaces. This can include minerals breaking into uneven, jagged pieces or splintering in a more random pattern.
Tuff, a type of volcanic rock composed of volcanic ash and fragments, does not exhibit true cleavage like some other minerals. Instead, it tends to break into irregular, angular fragments due to its heterogeneous composition. The texture and structure of tuff can vary significantly depending on the specific volcanic materials and processes involved in its formation. As a result, its fracture pattern is more characteristic of its volcanic origin rather than a defined cleavage.
When you strike minerals with no cleavage using a rock hammer, the minerals tend to fracture in irregular patterns rather than splitting along smooth planes. This is because they lack the internal structure that facilitates cleavage, resulting in a more chaotic breakage. The fractures can produce sharp edges and jagged surfaces, making it difficult to predict how the mineral will break. The overall outcome depends on the mineral's hardness and brittleness.
The difference between the iron in magnetite and hematite is the charge. Hematite has all 3+ iron ( the iron when make the mineral loses 3 electrons) and magnetite has some 2+ iron (it only loses 2 electrons).
Cleavage
Anatase, a mineral form of titanium dioxide (TiO2), typically exhibits cleavage rather than fracture. It has perfect cleavage along the {101} crystal face, allowing it to break along smooth, flat planes. However, when it does fracture, it tends to produce uneven surfaces. Overall, its cleavage is more prominent and characteristic than its fracture.
Silicon typically exhibits cleavage rather than fracture. Silicon has a crystal structure that allows it to cleave along specific planes with clean breaks, unlike other materials that exhibit more random fracturing patterns.
A fracture is more common than a cleavage. Fractures occur when a material breaks without any predetermined pattern, whereas cleavages occur along specific planes due to the arrangement of atoms in the material.
A fracture is a break in a material, such as a bone or rock, due to stress or force. Cleavage, on the other hand, refers to the way minerals break along flat planes determined by their crystal structure. Fracture is irregular, while cleavage is more controlled and predictable.
That is referred to as fracturing.
Cleavage fracture is more common than the formation of a new surface in minerals due to its alignment with the crystal structure's weakest plane. It produces smooth, flat surfaces, while fracture results in irregular surfaces due to breakage along the strongest planes or due to external stress.
Minerals break in the main two ways cleavage and fracture. Cleavage is breaking in flat planes but fracture is more uneven even unpredictable. The hardest mineral to break would be the diamond, which is placed at a ten on Moh's hardness scale.
Diamond stone, because of its lattice structure of carbon atoms, is identified as an 'octahedral; perfect and easy' cleavage (according to Wikipedia). Read more, below.
The cortex electrons separate as a result of broken hydrogen bonds between the subatomic particles of the atoms.
Rubies typically exhibit a conchoidal fracture, which means they break with smooth, curved surfaces similar to broken glass. Their cleavage is usually absent or very poor, meaning they do not break along distinct planes or directions.Ruby is a hard and durable stone, scoring 9 on the Mohs scale of mineral hardness, making it resistant to scratching and abrasion.
One that has only one cleavage direction will only fracture in one direction/angle to the matrix of the rock. One that only has fracture would fracture in no specific direction and is probably something like obsidian, which fractures conchoidally, like glass.