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.
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).
Yes, you can determine if an unknown substance contains magnetite by using a magnet. If the substance is attracted to the magnet, it suggests the presence of magnetite or other magnetic materials. However, this test alone will not quantify the amount of magnetite or differentiate it from other magnetic substances. Additional tests would be needed for a more definitive identification.
Cleavage
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.
Ah, the cleavage and fracture of a ruby are like the unique brushstrokes on a canvas. Cleavage refers to how the ruby breaks along certain planes due to its crystal structure, while fracture describes how it breaks irregularly. Just like happy little accidents in painting, each cleavage and fracture in a ruby tells a story of its journey through time.
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.
Cleavage is the tendency of a mineral to break along flat, smooth surfaces, while fracture is the tendency to break along irregular surfaces. Cleavage occurs along planes of weakness in the crystal structure, resulting in smooth, flat surfaces. Fracture occurs when a mineral breaks in a more random, jagged manner. In terms of mineral properties, cleavage indicates the presence of planes of weakness within the crystal structure, making the mineral more likely to break along those planes. Fracture, on the other hand, suggests a lack of planes of weakness and a more uniform distribution of strength throughout the mineral. The presence of cleavage planes can impact the overall strength and durability of a material by making it more prone to breaking along those planes. Minerals with strong cleavage may be more brittle and less resistant to impact or pressure, while minerals with fracture may be more durable and able to withstand external forces.