Ma = millions of years, Ga = billions of years
EON | ERA | PERIOD | EPOCH |
---|---|---|---|
Phanerozoic 542 Ma to present |
Cenozoic 65 Ma to present |
Quaternary 2.6 Ma to present |
Holocene 11,700 years ago to present |
Pleistocene 2.6 Ma to 11,700 years ago |
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Tertiary 65 to 2 Ma |
Pliocene 5.3 to 2.6 Ma |
||
Miocene 23.0 to 5.3 Ma |
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Oligocene 33.9 to 23.0 Ma |
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Eocene 58.7 to 33.9 Ma |
|||
Paleocene 65 to 58.7 Ma |
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Mesozoic 251 to 65 Ma |
Cretaceous 145 to 65 Ma |
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Jurassic 200 to 145 Ma |
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Triassic 251 to 200 Ma |
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Paleozoic 542 to 251 Ma |
Permian 299 to 251 Ma |
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Pennsylvanian 318 to 299 Ma |
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Mississippian 350 to 318 Ma |
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Devonian 416 to 359 Ma |
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Silurian 444 to 416 Ma |
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Ordovician 488 to 444 Ma |
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Cambrian 542 to 488 Ma |
|||
Proterozoic 2.5 Ga to 542 Ma |
Precambrian 4.54 Ga to 542 Ma |
||
Archean 4.54 Ga to 2.5 Ga |
A selection of significant events in the earth's geologic record.
Holocene epoch
- Humans develop agriculture and civilization
- Sea level rises rapidly as continental glaciers finish melting
- Mastodons and woolly mammoths and other large cold-climate mammals become extinct
Pleistocene epoch
- Large mammal species adapted to cold climates appear
- Widespread glaciation advances and retreats repeatedly in a cyclic pattern of global warming and cooling
- Homo sapiens appear
Pliocene epoch
- General global cooling trend continues
Miocene epoch
- Camels, horses and hippopotamus widespread, including in North America
Oligocene epoch
- Grasses become widespread
Eocene epoch
- Last "hot-house" global climate occurs, long-term overall cooling begins
- Indian subcontinent begins collision with Asia forming the Himalayan Mountains
- Mammals continue to diversify, ancestral horses appear
Paleocene epoch
- Mammal types begin to diversify and become widespread
Cretaceous period
- Period ends with large meteorite impact, demise of last dinosaur species
- Shallow inland ocean transgresses across entire North America except Rocky and Appalachian Mountains
- First flowering plants appear
Jurassic period
- Transgression of inland sea forms shallow marine conditions across interior North America
- Convergent plate boundary with subduction zone becomes established in western North America
- Pangaea finishes rifting into separate continents
Triassic period
- First mammals appear
- First dinosaurs appear
- Pangaea begins rifting into separate continents
- Deserts with sand dunes widespread western North America
- Several terranes that later accrete to North America exist in Tethyan area
- Single world ocean with a single large bay in Pangaea - the Tethys Sea
- Huge Pangaea landmass affects climate, causing widespread aridity
Permian period
- Greatest mass extinction in the fossil record occurs
- Relatives of mammals diverge from reptiles
- Pangaea finishes colliding and assembling
- Shallow seas cover much of western North America
Pennsylvanian period
- Widespread glaciation
Mississippian period
- First reptiles appear
- First dense forests with large primative trees appear
Devonian period
- First horsetails, clubmosses, and ferns appear
- First amphibians appear
Silurian period
- Insects appear on land
- Diverse fish types appear
Ordovician period
- Widespread glaciation for short interval
- First green plants on land appear
Cambrian period
- Several groups of animals appear, including arthropods and early ocean-dwelling vertebrates
- Ocean transgresses across much of interior and western North America, depositing sand, then mud, then lime as water gets deeper
Proterozoic eon
- Glaciation may have been widespread
- Multi-cellular organisms appear
- Single celled organisms, more complex than bacteria appear
- Mats of photosynthesizing bacteria widespread
- Atmosphere becomes oxygenated
- Continental cratons finish forming
Archean eon
- Continental cratons begin to form
- First fossil bacteria appear
- No free oxygen in the atmosphere
- Earliest crust forms
- Earth's mantle and core form
Geology 101 - Introduction to Physical Geology
Basics Table--Geologic Time Scale
Created by Ralph L. Dawes, Ph.D. and Cheryl D. Dawes, including figures unless otherwise noted
updated: 9/11/13
Basics Table--Geologic Time Scale
Created by Ralph L. Dawes, Ph.D. and Cheryl D. Dawes, including figures unless otherwise noted
updated: 9/11/13
Unless otherwise specified, this work by Washington State Colleges is licensed under a Creative Commons Attribution 3.0 United States License.
