it probably break apart with cleavage, because the carbon atoms in graphite from sheets that could split apart easily in layers.
The cortex electrons separate as a result of broken hydrogen bonds between the subatomic particles of the atoms.
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.
That could be graphite, which is a natural allotrope of the element carbon.
Biotite Mica would fit this category as would Muscovite, native to Russia as the name implied. (Sheets) oif semi-transparent mica can be peeled right off. the mineral is useful in electrical condensers and also as a form of glass substitute that is heat-resistant, called Isinglass. it is neither Eisen-(Iron) nor Glass, but the name stuck.
Elements that are brittle and dull are likely to be nonmetals. Nonmetals tend to have brittle, dull properties compared to metals which are typically malleable and lustrous. Examples of brittle and dull elements include carbon in the form of graphite and sulfur.
The cortex electrons separate as a result of broken hydrogen bonds between the subatomic particles of the atoms.
Graphite is likely to break along its planes of weakness, resulting in cleavage fractures. These fractures occur because of the structure of graphite, which is composed of stacked layers held together by weak van der Waals forces. When a force is applied perpendicular to these layers, they are easily separated, causing the material to break cleanly along these planes.
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.
If a mineral lacks planes along which it may cleave, it will likely fracture instead of cleave. This means that the mineral will break irregularly and not along smooth, flat surfaces like in cleavage. The fracture pattern can vary depending on the mineral's physical properties.
most likely its discovery wasn't documented until 1889
Stress fracture in ArmA stress fracture within the arm will most likely result in a cast or a removable splint.Stress fracture in LegA stress fracture within the leg will usually result in a walking boot and crutches if it is extremely painful.
L4
That could be graphite, which is a natural allotrope of the element carbon.
Graphite is often mistaken for lead due to their similar appearance and use in pencils. Both graphite and lead leave behind marks when drawn on paper, but graphite is the actual material used in pencils, not lead. The misconception likely arose from historical confusion stemming from the use of the term "pencil lead" to describe graphite writing instruments.
I'm pretty sure if you have a chip fracture it means that a piece of the bone has been chipped off. A hairline fracture means the bone is broken. However the break is very minor and most likely isn't broken all the way through.
It is so hot and so pressured in the mantle that a simple stick of graphite would most likely disintegrate in the violent mantle environment.
Do it yourself!!!