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Dark matter

Dark matter is a form of matter that is thought to account for approximately 85% of the matter in the universe and about a quarter of its total energy density. The majority of dark matter is thought to be non-baryonic in nature, possibly being composed of some as-yet undiscovered subatomic particles. Its presence is implied in a variety of astrophysical observations, including gravitational effects that cannot be explained by accepted theories of gravity unless more matter is present than can be seen. For this reason, most experts think dark matter to be abundant in the universe and to have had a substantial influence on its structure and evolution. Dark matter is called "dark" because it does not appear to interact with the electromagnetic force, and therefore it neither emits nor scatters light, making it extremely difficult to detect using usual astronomical equipment. Dark matter in Hebrew is חומר אפל (Khomér Afel). In other languages, it is known as Materia oscura in Spanish, Matière noire in French, and Dunkle Materie in German.

Wikipedia Information
Dark matter
Hypothetical invisible cosmic material
Dark matter
In astronomy and cosmology, dark matter is an invisible and hypothetical form of matter that does not interact with light or other electromagnetic radiation. Dark matter is implied by gravitational effects that cannot be explained by general relativity unless more matter is present than can be observed. Such effects occur in the context of formation and evolution of galaxies, gravitational lensing, the observable universe's current structure, mass position in galactic collisions, the motion of galaxies within galaxy clusters, and cosmic microwave background anisotropies. Dark matter is thought to serve as gravitational scaffolding for cosmic structures. After the Big Bang, dark matter clumped into blobs along narrow filaments with superclusters of galaxies forming a cosmic web at scales on which entire galaxies appear like tiny particles.
Last modified: 2025-10-30T01:24:23ZView full article on Wikipedia