yes
The temperature, pressure, and chemical composition of the magma are the main factors that determine the specific silicate minerals that form during solidification. Silicate minerals can vary in their chemical composition and crystal structure based on these conditions, leading to the formation of different minerals such as quartz, feldspar, mica, and pyroxene.
A mineral's ability to split along flat surfaces is called cleavage. Cleavage is a characteristic property of minerals related to their crystal structure and internal arrangement of atoms.
It means that the chemical bonds of the mineral aren't too strong along the lines and that when you break the mineral it'll break along those lines. please go to www.freewebs.com/mccniu (minerals aren't on it)
A cleavage is a natural division or indentation in rocks, minerals, or crystals that forms due to geological processes. It represents a tendency of certain materials to break along parallel planes, often resulting in smooth surfaces. Cleavage is related to the internal structure of the material and how its atoms are arranged.
No, quartz doesn't have distinctive cleavage, it will tend to break with a conchoidal fracture.
Cleavage is related to the minerals atomic structure because minerals are arranged in crystal lattices . It's the shape of these lattices that determine the mineral's cleavage.
Cleavage is the way a mineral breaks along planes of weakness in its atomic structure. The number and orientation of cleavage planes are determined by the arrangement of atoms in the mineral's crystal lattice. Minerals with strong atomic bonds tend to have poor or no cleavage, while those with weaker bonds exhibit good cleavage.
The temperature, pressure, and chemical composition of the magma are the main factors that determine the specific silicate minerals that form during solidification. Silicate minerals can vary in their chemical composition and crystal structure based on these conditions, leading to the formation of different minerals such as quartz, feldspar, mica, and pyroxene.
"Neon" is a noble gas and does not exhibit cleavage, as cleavage is a property related to the way minerals break along certain planes due to their internal atomic structure.
A mineral's ability to split along flat surfaces is called cleavage. Cleavage is a characteristic property of minerals related to their crystal structure and internal arrangement of atoms.
i think crystal habit is the minerals structure, while cleavage is the patter it breaks into.
Peridot (the silicate mineral) has 'poor' cleavage.See the related Wikipedia link listed below for more information:
The difference between a mineral that has cleavage and one that has fracture is that cleavage is the tendency of some minerals to brake along flat surfaces and fracture is the tendency of some minerals to brake unevenly along curved or irregular surfaces.
A mineral hasn't an atomic number.
Cleavage is a smooth and easy break in a mineral. Minerals are always solid because it is one of their classification requirements.
It means that the chemical bonds of the mineral aren't too strong along the lines and that when you break the mineral it'll break along those lines. please go to www.freewebs.com/mccniu (minerals aren't on it)
Hardness and resistance to fracture or cleavage in minerals are related but distinct properties. Hardness measures a mineral's ability to withstand scratching, while resistance to fracture or cleavage refers to how a mineral breaks under stress. A mineral can be hard but still exhibit cleavage, meaning it breaks along specific planes. Conversely, some minerals that are not very hard can still be highly resistant to fracturing.