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Earth of the early Archean may have had a different tectonic style. It is widely believed that the early Earth was dominated by vertical tectonic processes, such as stagnant lid, [19] [20] heat-pipe, [21] or sagduction, [22] [23] [24] which eventually transitioned to plate tectonics during the planet's mid-stage evolution. However, an ...
The geologic time scale is a way of representing deep time based on events that have occurred throughout Earth's history, a time span of about 4.54 ± 0.05 Ga (4.54 billion years). [3] It chronologically organises strata, and subsequently time, by observing fundamental changes in stratigraphy that correspond to major geological or ...
Modern history – After the post-classical era Early modern period – The chronological limits of this period are open to debate. It emerges from the Late Middle Ages (c. 1500), demarcated by historians as beginning with the fall of Constantinople in 1453, in forms such as the Italian Renaissance in the West, the Ming dynasty in the East, and ...
Basin Groups Era begins on Earth. c. 4,450 Ma – 100 million years after the Moon formed, the first lunar crust, formed of lunar anorthosite, differentiates from lower magmas. The earliest Earth crust probably forms similarly out of similar material. On Earth the pluvial period starts, in which the Earth's crust cools enough to let oceans form.
Year(s) Event(s) Start End c. 2,588,000 BC c. 12,000 BC Pleistocene era c. 21,000 BC: Recent evidence indicates that humans processed (gathered) and consumed wild cereal grains as far back as 23,000 years ago. [1] c. 20,000 BC: Antarctica sees a very rapid and abrupt 6 °C increase in temperatures [2] c. 19,000 BC: Last Glacial Maximum/sea ...
See calendar and list of calendars for other groupings of years. See history, history by period, and periodization for different organizations of historical events. For earlier time periods, see Timeline of the Big Bang, Geologic time scale, Timeline of evolution, and Logarithmic timeline.
The first eon in Earth's history, the Hadean, begins with Earth's formation and is followed by the Archean eon at 3.8 Ga. [2]: 145 The oldest rocks found on Earth date to about 4.0 Ga, and the oldest detrital zircon crystals in rocks to about 4.4 Ga, [34] [35] [36] soon after the formation of Earth's crust and Earth itself.
era Archean ICS Plumb, 1991 Mesoproterozoic: 1,600 1,000 era ICS Hofmann, 1987 Mesozoic: 251.0 ± 0.7 65.5 ± 0.3 era ICS middle life: Philips, 1818 Messinian: 7.246 5.332 age Miocene ICS Messina (Italy) Mayer-Eymar, 1867 Miaogoalingian: 422 418.7 age Silurian China Miaolingian: 509 497 Epoch Cambrian ICS Migneintian: 486 478.6 ± 1.7 age ...