Table of Geologic Time

Eras
Periods and their Duration in Millions of Years Important Physical Events Important Organic Events
Cenozoic
Quaternary
Recent Youthful land forms having high relief formed. Dominance of man.
Pleistocene Epoch 2 M.Y. Period of glaciation; four great ice advances. Heidelberg, Neanderthal, and Crô-Magnon man; extinction of large mammals.
Tertiary
Pliocene Epoch 10 M.Y. Continuing world-wide land elevation. Intermigration of North and South American mammals. Transformation of ape to man.
Miocene Epoch 18 M.Y. Cordilleras, Alps, Himalayas formed. Widespread vulcanism-basalt flows in northwestern United States. Culmination of modern types of mammals. Apes appear in Old World.
Oligocene Epoch 10 M.Y. Land dominant; seas marginal. Carnivores and ungulates develop into importance.
Eocene Epoch 20 M.Y. Extensive sedimentation; seas marginal. Dawn of the dominance of mammals. Reptiles subordinate.
Cretaceous 65 M.Y. Widespread epicontinental seas. Laramide revolution at close of period—Rocky Mountains formed. Climax and culmination of reptiles, especially dinosaurs; first flowering plants and grasses.
Mesozoic
Jurassic 38 M.Y. Continent emergent; shallow seas on western North America. Rise of birds and flying reptiles, first modern trees.
Triassic 35 M.Y. Continent emergent; seas marginal. Rise of dinosaurs, cycads, and ammonites.
Paleozoic
Permian 35 M.Y. World-wide continental uplift and mountain building. Widespread glaciation. Extinction of most Paleozoic fauna and flora. First modern insects.
Pennsylvanian 48 M.Y. Continent alternately rising and sinking. Great coal-forming forests, of ferns and seed-ferns.
Mississippian 35 M.Y. Low lands and widespread submergence. Culmination of crinoids, numerous sharks.
Devonian 40 M.Y. Widespread submergence, local vulcanism. First known land animals, first forests.
Silurian 28 M.Y. Widespread submergence, local deserts. First lung fishes and scorpions, abundant corals.
Ordovician 65 M.Y. 60% of North America below sea. Climax of invertebrate dominance, first vertebrate.
Cambrian 105 M.Y. Widespread submergence. First abundant invertebrate fauna, trilobites dominant.
Proterozoic 700 ± M.Y. Long periods of granite intrusion, sedimentation, and mountain building. Bacteria and seaweeds present. Most invertebrates probably present, but remains are lacking.
Archeozoic 800 ± M.Y. World-wide intrusive igneous activity; some sediments. Blue-green algae present, primitive one-celled plants and animals probably present.