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Million Years Ago (song) " Million Years Ago " is a song recorded by English singer-songwriter Adele for her third studio album, 25 (2015). The song was written by Adele and Greg Kurstin, with production of the song provided by the latter. Lyrically, the track is about how fame has personally affected her and everyone around her.
The Stephanian is a stage in the regional stratigraphy of northwest Europe with an age between roughly 307.5 [1] and 299 Ma (million years ago). It is a subdivision of the Carboniferous system or period and the regional Silesian series. The uppermost units of the Coal Measures of England and Wales are probably of Stephanian age, though the ...
Late Devonian: 375 million years ago, 75% of species lost, including most trilobites. End Permian, The Great Dying: 251 million years ago, 96% of species lost, including tabulate corals, and most trees and synapsids. End Triassic: 200 million years ago, 80% of species lost, including all conodonts. End Cretaceous: 66 million years ago, 76% of ...
Carboniferous. The Carboniferous (/ ˌkɑːrbəˈnɪfərəs / KAR-bə-NIF-ər-əs) [6] is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period 358.9 Ma (million years ago) to the beginning of the Permian Period, 298.9 Ma. In North America, the Carboniferous is often treated as two ...
The Transcontinental Arch, as originally understood, was at its peak during the Pennsylvanian, around 323 to 299 million years ago. However, the arch may have been present as early as the late Proterozoic and experienced repeated rejuvenation throughout the Paleozoic (521 to 252 million years ago). [2]
Max Edward " Mark " Dinning (August 17, 1933 – March 22, 1986) [1] was an American pop music singer. In February 1960, the song "Teen Angel", written by his sister Jean (Eugenia) and her husband Red Surrey, [2] reached number one on the Billboard Hot 100 singles chart. Jean and two of her sisters, Virginia and Lucille, comprised The Dinning ...
The Eocene (IPA: / ˈ iː ə s iː n, ˈ iː oʊ-/ EE-ə-seen, EE-oh-[5] [6]) is a geological epoch that lasted from about 56 to 33.9 million years ago (Ma). It is the second epoch of the Paleogene Period in the modern Cenozoic Era.
1991. The Mesozoic Era[3] is the era of Earth's geological history, lasting from about 252 to 66 million years ago, comprising the Triassic, Jurassic and Cretaceous Periods. It is characterized by the dominance of gymnosperms and of archosaurian reptiles, such as the dinosaurs; a hot greenhouse climate; and the tectonic break-up of Pangaea.