fracture
Its cleavage
fracture
It tells you that that mineral is smooth and flat ,and so are the chemical bonds. Because if it didn't it would be a fracture which means it is jagged and not smooth. I am sure of this answer because cleavage means physical property of some minerals that cause them to break along smooth, flat surfaces.
You could choose just about any precious or semi-precious stone as an example - for instance, diamond which is pure carbon and crystallizes in the isometric system, meaning that it shows equal fracture lines in all three planes.
Many planes were painted as camouflage.
She used planes because she loved flying.
No, when she was younger she said that planes were just a big piece of metal.Hope that helped:D
The mineral would either cleave on planes of weakness, or fracture.
Cleavage planes occur due to a weakness or propensity to fracture in a crystalline structure.
The mineral quartz show the property of fracture. it breaks along a curved surface. this kind of fracture is called conchoidal fracture. In math the quartz is x3.
Cleavage- in geolohy, the tendency of a mineral to splitalong specific planes of weakness to format smooth flatSurface.Fracture- the manner in which a mineral breaks alongeither curved or irregular
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.
This has been answered before but there was no explanation given for the curve. Materials that do not have fracture planes such as glass and obsidian (a natural glass-like mineral) do not follow any particular structural arrangement when fracturing. The curve results from the distribution of stresses radiating from the fracture start point. The fracture pattern is called conchoidal.
Minerals that do not have weak bonds along specific planes will tend to have a higher resistance to breakage and fracturing. This is because weak bonds along specific planes create areas of weakness where the mineral is more likely to break or split. Without these weak bonds, the mineral will have a more cohesive structure and be less prone to breaking.
That is referred to as fracturing.
shear fracture.
It is a type of igneous or sedimentary rock.
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.
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.