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.
It wil break & produce fragments of d same shape as d parent material bcos it broke on a flat surface
Limestone, and sulfur.
Cleavage
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.
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.
Fracture. When it breaks apart cleanly, that is called Cleavage.
It wil break & produce fragments of d same shape as d parent material bcos it broke on a flat surface
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
The tendency of some minerals to break unevenly along curved or irregular surfaces is called cleavage. Cleavage is a property that describes how a mineral breaks when subjected to stress, and it is determined by the internal arrangement of atoms within the mineral's structure.
Fracture in minerals refers to the way a mineral breaks when it is not subjected to cleavage. It can result in irregular, jagged surfaces or smooth, curved surfaces. This property helps in identifying minerals based on how they break.
Limestone, and sulfur.
Cleavage
A fracture in minerals refers to the way a mineral breaks when subjected to external forces. It can be described as either conchoidal (smooth and curved) or irregular. The type of fracture can affect the mineral's physical properties, such as its hardness, cleavage, and overall durability.
Conchoidal describes a smooth, curved fracture surface similar to broken glass. Splintery texture refers to long, thin, and sharp pieces that break off a mineral. Irregular texture indicates a lack of a specific pattern or shape in the mineral's fracture.