Erbium is typically found in natural mineral deposits such as gadolinite, euxenite, and xenotime. It almost always co-occurs in nature alongside several other heavy rare earth elements. Miners must process large amounts of heavy ore just to extract small quantities of erbium.
In the modern periodic table, erbium is situated in the f-block among the lanthanides. It displays typical lanthanide chemical behavior and exists almost entirely in the +3 oxidation state. The pure metal tarnishes slowly in air and burns to form a stable erbium(III) oxide.
It also reacts directly with various nonmetal halogens to yield brightly colored chemical compounds. A very notable characteristic of erbium is its sharp absorption spectra across multiple light wavelengths. It absorbs specific frequencies in the visible light, ultraviolet, and near-infrared optical regions.
Its positively charged ions possess optical properties that are absolutely critical for modern global telecommunications. Specifically, erbium ions have the unique ability to emit light at a wavelength of 1.55 micrometers. This exact infrared wavelength experiences the lowest possible transmission loss in standard silica-based optical fibers.
Therefore, light signals at this frequency can travel much further before they begin to fade away. Consequently, this specific physical property makes the rare element completely indispensable for transmitting high-speed long-distance internet data.

![Erbium element card: symbol Er, atomic number 68, atomic mass 167.26, electron configuration [Xe] 4f¹² 6s², oxidation states +3, Lanthanide, f-block, period 6, solid at room temperature.](https://stage.chemistry-dictionary.com/wp-content/uploads/2026/09/erbium-chemical-element.webp)