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tertiary$508171$ - перевод на голландский
![Testing telephone lines in [[London]] in 1945.](https://commons.wikimedia.org/wiki/Special:FilePath/Automatic Telephone Exchange- Communications in Wartime, London, England, UK, 1945 D23700.jpg?width=200 "Testing telephone lines in [[London]] in 1945.")
![nucleus]]. An antineutrino (not shown) is always emitted along with an electron. Insert: in the decay of a free neutron, a proton, an electron (negative beta ray), and an [[electron antineutrino]] are produced.](https://commons.wikimedia.org/wiki/Special:FilePath/Beta-minus Decay.svg?width=200 "nucleus]]. An antineutrino (not shown) is always emitted along with an electron. Insert: in the decay of a free neutron, a proton, an electron (negative beta ray), and an [[electron antineutrino]] are produced.")
![Beta radiation detected in an isopropanol [[cloud chamber]] (after insertion of an artificial source [[strontium-90]])](https://commons.wikimedia.org/wiki/Special:FilePath/Beta radiation in a cloud chamber.jpg?width=200 "Beta radiation detected in an isopropanol [[cloud chamber]] (after insertion of an artificial source [[strontium-90]])")
![Blue [[Cherenkov radiation]] light being emitted from a [[TRIGA]] reactor pool is due to high-speed beta particles traveling faster than the speed of light ([[phase velocity]]) in water (which is 75% of the speed of light in vacuum).](https://commons.wikimedia.org/wiki/Special:FilePath/TrigaReactorCore.jpeg?width=200 "Blue [[Cherenkov radiation]] light being emitted from a [[TRIGA]] reactor pool is due to high-speed beta particles traveling faster than the speed of light ([[phase velocity]]) in water (which is 75% of the speed of light in vacuum).")
Википедия
Tertiary ( TUR-shə-ree, TUR-shee-err-ee) is an obsolete term for the geologic period from 66 million to 2.6 million years ago. The period began with the demise of the non-avian dinosaurs in the Cretaceous–Paleogene extinction event, at the start of the Cenozoic Era, and extended to the beginning of the Quaternary glaciation at the end of the Pliocene Epoch. The time span covered by the Tertiary has no exact equivalent in the current geologic time system, but it is essentially the merged Paleogene and Neogene periods, which are informally called the Early Tertiary and the Late Tertiary, respectively. The Tertiary established the Antarctic as an icy island continent.
