Fracture refers to the appearance of the freshly broken mineral. Chert or flint, for instance, has a conchoidal fracture.
The fracture can be described (depending on the mineral) as:-Conchoidal fractureSubconchoidal fractureEarthy fractureHackly fractureJagged fractureSplintery fractureUneven fracture
There is no broken parts in quartz, so Quartz does not have cleavage.
A smooth break in a mineral is referred to as "conchoidal fracture." This type of fracture produces curved, shell-like surfaces that resemble the shape of a clam shell. Conchoidal fractures are characteristic of certain minerals, such as quartz and obsidian, and occur when the mineral's atomic bonds break unevenly, creating smooth, glossy surfaces. This feature can be used to identify minerals and is often seen in glassy or amorphous materials.
Cleavage
The mineral that has a pearly luster and a conchoidal fracture is talc. Talc is a soft mineral with a characteristic pearly luster due to its perfect cleavage planes and breaks with a unique conchoidal fracture pattern.
Fracture refers to the appearance of the freshly broken mineral. Chert or flint, for instance, has a conchoidal fracture.
This is known as conchoidal fracture.
The fracture can be described (depending on the mineral) as:-Conchoidal fractureSubconchoidal fractureEarthy fractureHackly fractureJagged fractureSplintery fractureUneven fracture
Dolomite typically displays a conchoidal fracture, which means it breaks along curved surfaces with sharp edges resembling broken glass. This fracture pattern is a result of the crystal structure and composition of dolomite, which is a type of carbonate mineral.
The fracture can be described (depending on the mineral) as:-Conchoidal fractureSubconchoidal fractureEarthy fractureHackly fractureJagged fractureSplintery fractureUneven fracture
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.
The Answer Is Conchoidal
The fracture of feldspar is conchoidal or brittle.
The fracture of feldspar is conchoidal or brittle.
For the uraninite: Brittle - Conchoidal - Very brittle fracture producing small, conchoidal fragments; data from http://webmineral.com/data/Uraninite.shtml. Any mineral of uranium has its specific properties - and we know now approx. 200 uranium minerals.
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.