That is cleavage.
Cleavage
It wil break & produce fragments of d same shape as d parent material bcos it broke on a flat surface
the manner in which a mineral breaks along either curved or irregular surfaces is called a FRACTURE.
Fracture. When it breaks apart cleanly, that is called Cleavage.
Begin by taking a look at the mineral's color, Examine the mineral and take note of its surface features,Get out the materials needed for the hardness test (see Things You'll need), The number is the hardness, followed by the characteristics of a mineral of that hardness and an example, Next find out your mineral's luster,Now for the streak test, You can also identify a mineral by the way it breaks. If it breaks along a smooth, flat surface (such as mica), it has cleavage. If your mineral breaks along rough, jagged surfaces, it has fracture. Thats all you need to do.
When a mineral breaks along a weakly-bonded plane, it is called cleavage. Cleavage is a property that describes how a mineral breaks along its crystal structure.
Zinc is a metal that exhibits a fracture rather than cleavage. Fracture refers to the way a mineral breaks when it is not along cleavage planes, while cleavage refers to the tendency of a mineral to break along flat planes.
Malachite exhibits a conchoidal fracture, which means it breaks with smooth, curved surfaces. It does not have cleavage, which is the tendency of a mineral to break along preferred planes.
the manner in which a mineral breaks along either curved or irregular surfaces is called a FRACTURE.
the manner in which a mineral breaks along either curved or irregular surfaces is called a FRACTURE.
the manner in which a mineral breaks along either curved or irregular surfaces is called a FRACTURE.
A mineral that breaks along a weakly bonded plane is called "cleavage". Cleavage is the tendency of a mineral to break along smooth, flat surfaces determined by its internal atomic structure.
When a mineral breaks along a weakly bonded plane, it is called cleavage. Cleavage is the tendency of a mineral to break along specific planes of weakness due to the arrangement of atoms in the crystal lattice.
It exhibits cleavage, which is the tendency of a mineral to break along certain planes of weakness determined by its atomic structure. Cleavage is a property seen in minerals with strong bonds in certain directions but weaker bonds in other directions. The resulting flat, shiny surfaces are a result of the breakage along these weakly bonded planes.
cleavage
Cleavage.
"Uneven cleavage"