out of seven epochs mentioned above, what is the second one?
It is a geological epoch that lasted from about 56 to 33.9 million years ago (mya).
Eocene
is a geological epoch that lasted from about 56 to 33.9 million years ago (mya).
where was the material that was eroded by the colorado river deposited Regions in the Mesozoic and Cenozoic what is the second one? It is the current and most recent of the three geological eras of the Phanerozoic Eon. where is this era's name derive from? It means "new life," and is derived from Greek "kainós" "new," and "zōḗ" "life." what are its divisions? It is divided into three periods: the Paleogene, Neogene, and Quaternary; and seven epochs: the Paleocene, Eocene, Oligocene, Miocene, Pliocene, Pleistocene, and Holocene. what is the time period of the first division? It spans 43 million years from the end of the Cretaceous Period million years ago (Mya) to the beginning of the Neogene Period Mya. how was the climate during this period? The global climate during the Paleogene departed from the hot and humid conditions of the late Mesozoic era and began a cooling and drying trend. what type of animals were found during that time? Mammals began a rapid diversification during this period. can you mention some names? UNANSWERABLE describe something about the type of fauna at that time? Pronounced cooling in the Oligocene led to a massive floral shift and many extant modern plants arose during this time. the second division mentioned above, who coined the term? Moritz Hörnes
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Eocene [SEP] Introduction
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name "Eocene" comes from the Ancient Greek ("ēṓs", "dawn") and ("kainós", "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope C in the atmosphere was exceptionally low in comparison with the more common isotope C.