the word crystalline is often used to describe the internal structure of crystals
Crystal shape refers to the geometric arrangement of the atoms or molecules that make up a crystal. Crystals can exhibit a variety of shapes such as cubes, prisms, pyramids, or irregular shapes depending on the internal arrangement of their building blocks. The shape of a crystal is often determined by its atomic structure and the conditions under which it formed.
Moonstone belongs to the feldspar group and has a monoclinic crystal structure. It typically exhibits a prismatic, tabular, or blocky appearance, often with fine striations. Moonstone's crystal structure is characterized by its layers of alternating orthoclase and albite feldspar minerals, which create the mesmerizing adularescence or "moon-like" sheen when light reflects off its surface.
Flint typically forms as small, irregularly shaped nodules or masses, rather than having a distinct crystal shape. Its microcrystalline structure gives it a smooth, often waxy appearance.
Chemically the same, calcite and aragonite have different crystal latticeworks, thus their crystals have a different appearance and have different crystal classifications, making them both independently recognized minerals.
Indeed, not all crystals are perfect. Often a process called twinning occurs. On the walls of a cavity, there may be several nucleation centres, points of first formation of a crystal. As these crystals grow they will interfere in each other's space.
Crystal shape refers to the geometric arrangement of the atoms or molecules that make up a crystal. Crystals can exhibit a variety of shapes such as cubes, prisms, pyramids, or irregular shapes depending on the internal arrangement of their building blocks. The shape of a crystal is often determined by its atomic structure and the conditions under which it formed.
Moonstone belongs to the feldspar group and has a monoclinic crystal structure. It typically exhibits a prismatic, tabular, or blocky appearance, often with fine striations. Moonstone's crystal structure is characterized by its layers of alternating orthoclase and albite feldspar minerals, which create the mesmerizing adularescence or "moon-like" sheen when light reflects off its surface.
Flint typically forms as small, irregularly shaped nodules or masses, rather than having a distinct crystal shape. Its microcrystalline structure gives it a smooth, often waxy appearance.
A giant molecular crystal is a type of crystal structure where the repeating unit is a large molecule or a network of bonded atoms. These crystals often have high melting points and are characterized by strong intermolecular forces between the molecules or atoms within the structure. Examples include diamond, graphite, and quartz.
Yes, often they do. This structure is often called an anvil.
when constituent particles are present only on the corner positions of a unit cell , it is called as Primitive unit cell .
Rose quartz and smoky quartz are considered crystaline minerals due to their internal atomic arrangement, but they do not exhibit visible crystal faces because they often form in massive or granular structures rather than distinct crystal shapes. This lack of well-defined crystal faces is due to the specific conditions under which these minerals are formed in nature.
Chemically the same, calcite and aragonite have different crystal latticeworks, thus their crystals have a different appearance and have different crystal classifications, making them both independently recognized minerals.
Hydrous refers to a substance that contains water molecules within its molecular structure. This term is often used in mineralogy to describe minerals that have water molecules incorporated into their crystal structure.
The cuttlefish bone is called the "cuttlebone." It is a unique internal structure made of aragonite and serves various functions, including buoyancy regulation and providing structural support. Cuttlebones are often found in pet shops as a calcium supplement for birds and small animals.
It's most often denoted as the "outside".
Indeed, not all crystals are perfect. Often a process called twinning occurs. On the walls of a cavity, there may be several nucleation centres, points of first formation of a crystal. As these crystals grow they will interfere in each other's space.