A faint, extended region of diffuse emission surrounding a bright central source.A halo is a faint, extended region of diffuse emission that surrounds a bright central source. In astrophysics, halos are observed around galaxies, where they consist of hot gas, dark matter, and globular clusters; around X-ray binaries and active galactic nuclei, where they are made of scattered light or ejected material; and around gamma-ray bursts, where they arise from dust scattering. Halos provide crucial information about the environment and history of the central object, as their size, shape, and spectrum reveal the density and composition of the surrounding medium.
The concept of a galactic halo dates back to the 1950s, when astronomers like Jan Oort and Lyman Spitzer studied the distribution of stars and gas around the Milky Way. The term 'halo' became standard in the 1970s with the discovery of dark matter halos in cosmological simulations.
Halos form through various mechanisms. For example, in a gamma-ray burst, the prompt X-rays and gamma-rays scatter off dust grains in the host galaxy, producing a faint, expanding 'echo' halo around the burst position. In galaxies, the halo is a reservoir of hot gas that accretes onto the disk, fueling star formation. The emission from a halo is typically much fainter than the central source, so detecting it requires long exposures and careful subtraction of the bright core. The study of halos often uses surface brightness profiles to map their radial structure.
In observational astronomy, halos are used to probe the interstellar and intergalactic medium, and to measure distances to gamma-ray bursts via the time delay of the scattered light. In cosmology, dark matter halos are the scaffolding for galaxy formation.
The halo of the Milky Way contains some of the oldest stars in the universe, with ages exceeding 13 billion years — nearly as old as the Big Bang itself.













