Sulphur's crystal structure is orthorhombic.
Sulfur. The blue color of lazurite comes from the presence of sulfur atoms within its crystal structure.
The angles between lead and sulfur atoms in lead sulfide (PbS) are approximately 90 degrees due to the crystal structure of the compound.
Bituminous coal does not have a specific crystal structure because it is composed of amorphous carbon along with varying amounts of other elements like hydrogen, oxygen, sulfur, and nitrogen. This lack of crystalline structure is what distinguishes coal from minerals like diamond or quartz, which have well-defined crystal structures.
Sulfur can be found in a crystalline form as sulfur crystals. These crystals are typically yellow in color and may exhibit a variety of shapes and sizes depending on how they are formed.
The dominant type of breakage for sulfur is cleavage, which occurs along planes of weakness in the crystal structure, resulting in smooth, flat surfaces.
Sulfur does not exhibit cleavage because it lacks a distinct crystal structure. Instead, sulfur has a conchoidal fracture, meaning it breaks along curved, irregular surfaces similar to glass.
Sulfur has a number of allotropes, the best known is S8, commonly known as rhombic sulfur. There are some nice pictures about- google rhombic sulfur images.
Sulfur. The blue color of lazurite comes from the presence of sulfur atoms within its crystal structure.
The angles between lead and sulfur atoms in lead sulfide (PbS) are approximately 90 degrees due to the crystal structure of the compound.
Sulfur does not have cleavage because it does not have a defined crystal structure like minerals do, which is necessary for exhibiting cleavage. Instead, sulfur breaks along irregular fracture planes when subjected to external force.
According to Wikipedia: The mineral sphalerite... "crystallizes in the cubic crystal system. In the crystal structure, zinc and sulfur atoms are tetrahedrally coordinated. The structure is closely related to the structure of diamond." You can read more about Bravais lattaice by following the link, below.
Bituminous coal does not have a specific crystal structure because it is composed of amorphous carbon along with varying amounts of other elements like hydrogen, oxygen, sulfur, and nitrogen. This lack of crystalline structure is what distinguishes coal from minerals like diamond or quartz, which have well-defined crystal structures.
This element is Sulfur.
Sulfur can be found in a crystalline form as sulfur crystals. These crystals are typically yellow in color and may exhibit a variety of shapes and sizes depending on how they are formed.
There is no crystal structure.
1.you can get a sulfur crystal in any general store or 2.in any rock shop
The dominant type of breakage for sulfur is cleavage, which occurs along planes of weakness in the crystal structure, resulting in smooth, flat surfaces.