Halogens are really the elements in group 17. Fluorine, chlorine, bromine, iodine, and astatine were indeed halogen elements. Such elements are too reactive to occur naturally, but their compounds are global. Chlorides are by far the most abundant; fluorides, bromides, and iodides are less common but still readily available.
Halides with less electronegative elements are formed by halogens. In this, metal halides range from ionic to covalent, whereas nonmetal halides are covalent. Interhalogens are being formed by combining two or more different halogens.
Minerals have been directly reacted with all of the representative halogen elements or with hydrohalic acid solutions (HF, HCl, HBr, and HI) to produce representative metal halides. In the addition of aqueous hydrohalic acids, basic anions such as hydroxides, oxides, or carbonates are involved.
There may several patterns in halogen chemistry that do not require double or triple bonds to explain the chemistry of the halogens. Fluorine chemistry has been simplified by the fact that it is the first electronegative element in the tabular array and that it has no d orbitals in its valence shell, so it cannot expand its valence shell. Chlorine, bromine, and iodine all have valence shell d orbitals that can be extended to carry up to 14 valence electrons. The chemistry of the halogens has been conquered by oxidation-reduction reactions.
alogens were indeed highly reactive nonmetal elements found in Periodic Table Group 17 of the periodic table. At room temperature, halogens seem to be solids, liquids, and gases that vary in colour.