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The Geologic Calendar is a scale in which the geological timespan of the Earth is mapped onto a calendrical year; that is to say, the day one of the Earth took place on a geologic January 1 at precisely midnight, and today's date and time is December 31 at midnight. [1]
The geologic time scale or geological time scale (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronology (a scientific branch of geology that aims to determine the age of rocks).
Geologic time shown in a diagram called a geological clock, showing the relative lengths of the eons of Earth's history and noting major events The geological history of the Earth follows the major geological events in Earth's past based on the geological time scale , a system of chronological measurement based on the study of the planet's rock ...
The geological clock: a projection of Earth's 4,5 Ga history on a clock ("Ma" = a million years (Megayear) ago; "Ga" = a billion years (Gigayear) ago) Date: 31 October 2010, 06:53: Source: This file was derived from: Geologic clock.jpg: Author: Woudloper; Derivative work: Hardwigg; Permission (Reusing this file)
The first eon in Earth's history, the Hadean, begins with the 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 the Earth's crust and the Earth itself.
For the first time in history, world timekeepers may have to consider subtracting a second from our clocks in a few years because the planet is rotating a tad faster than it used to. Clocks may ...
Date (Mya) Event Before 1,000: Faint young Sun paradox: 2,400: Great Oxidation Event probably leads to Huronian glaciation perhaps covering the whole globe : 650–600: Later Neoproterozoic Snowball Earth or Marinoan glaciation, precursor to the Cambrian explosion
The iron-rich nodules in the limestone formations act as geological clocks as they trap helium from the decay of small amounts of radioactive uranium and thorium in the soil.