Some minerals with a closely packed atom structure have a high density. This close packing of atoms results in a tightly packed crystal lattice, leading to a high atomic mass per unit volume. Examples of such minerals include diamond and gold.
Yes, some minerals can appear blue due to the presence of certain chemical elements or impurities in their crystal structure. For example, azurite and lapis lazuli are naturally occurring blue minerals.
There are over 4,000 known minerals in the world. Some common minerals include quartz, feldspar, mica, and calcite. Minerals are naturally occurring inorganic substances with a specific chemical composition and crystal structure.
Gypsum a+
Some minerals that are magnetic include magnetite (Fe3O4), hematite (Fe2O3), and pyrrhotite (Fe1-xS). These minerals contain iron and exhibit magnetic properties due to their crystal structure and magnetic alignment of electron spins within the material.
Some minerals with a closely packed atom structure have a high density. This close packing of atoms results in a tightly packed crystal lattice, leading to a high atomic mass per unit volume. Examples of such minerals include diamond and gold.
you know that structure . that one about the thingy. what was the question again?
A spherical bulge of closely packed stars is called a globular cluster. These clusters are typically found in the outer regions of galaxies and contain thousands to millions of stars held together by gravity. Globular clusters are some of the oldest structures in the universe.
Some minerals in silicates include quartz, feldspar, mica, amphibole, and pyroxene. These minerals are characterized by their crystalline structure composed of silicon and oxygen atoms arranged in tetrahedra.
The softness or hardness of a metal is determined by its atomic structure and how its atoms are arranged. Metals like sodium have a relatively low melting point and are more easily deformed because they have a regular, closely-packed structure with weak bonds between layers. In contrast, metals like iron have a more complex and tightly-packed structure with stronger bonds, making them harder and less malleable.
Size is a factor of habit, crystal structure, and temperature.
Most solids actually have an orderly structure. This is because the atoms of a solid are so tightly packed together.
No, not all minerals react with acids. Some minerals are resistant to acid reactions due to their chemical composition and structure. However, minerals containing carbonate or sulfide components are more likely to react with acids.
It is a box shape. Here is some more info on the subject matter pertaining to your specific circumstances:Space group: P63/mmc (Space group number: 194)Structure: hcp (hexagonal close-packed)Cell parameters: a: 266.49 pm
Solid matter has a fixed shape and volume, with particles that are closely packed together in a regular pattern. Solids are usually not compressible and have strong intermolecular forces holding the particles together. Additionally, solids maintain their shape and structure when subjected to external forces.
Yes, some minerals can appear blue due to the presence of certain chemical elements or impurities in their crystal structure. For example, azurite and lapis lazuli are naturally occurring blue minerals.
A mineral, by definition is an inorganic solid with a crystalline structure formed naturally. Wood, paper, or any other organic solids are not minerals because they have no crystalline structure and form organically. Plastic is not a mineral either because it is made synthetically out of organic materials. Some organic materials like coal and other hydrocarbons are considered minerals economically. Bones and teeth contain hydoxylapatite that is organically formed but is still considered a mineral, so there are exceptions. Whewellite is organically formed but has a crystalline structure, and is considered a mineral.