Solid oxygen has a cubic crystalline structure. Solid nitrogen has a hexagonal crystalline structure.
Mercury, at solidification temperatures, is classified in the trigonal crystal system.
That's different for each crystal. A crystal is defined by the way the atoms are arranged in it's structure, so this question is not really answerable for all crystalline structures.
The notochord is the flexible supporting structure found only in chordates. It is a rod-like structure that runs along the length of the body, providing support and allowing for some degree of movement.
Yes, each piece of a mineral typically has the same crystal structure, which is defined by the arrangement of atoms within the mineral. This uniformity in crystal structure is what characterizes a specific mineral and distinguishes it from others. However, variations can occur in different samples due to factors like impurities or environmental conditions during formation, but the fundamental crystal structure remains consistent for that mineral type.
I the crystal is shaped like a banana then it's ions of the internal structure are shaped like an apple. And vise versa.
Lentil bean
Solid oxygen has a cubic crystalline structure. Solid nitrogen has a hexagonal crystalline structure.
As a metal dubnium has a crystalline structure but this structure is not known today.
this question need more detail. first of all, a crystal's external appearance is merely a representation of its ordered internal atomic structure. to look at crystal structure in general, I recommend researching the 14 Bravais Lattices. Depending on what crystal you are talking about, its internal atomic structure will be different.
Mercury, at solidification temperatures, is classified in the trigonal crystal system.
Yes, it is. It is somewhat like cartilage.
of crystals.
Is a flexible, supporting structure
That's different for each crystal. A crystal is defined by the way the atoms are arranged in it's structure, so this question is not really answerable for all crystalline structures.
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.
An ionic crystal splits along a face that corresponds to the planes of its crystal lattice structure. These planes are determined by the repetitive arrangement of ions in the crystal lattice.