Facts About the Geological Time Scale

The geological time scale (GTS) is a system of chronological measurement that relates stratigraphy to time, and is used by geologists, paleontologists, and other Earth scientists to describe the timing and relationships between events that have occurred throughout Earth’s history.

1-It's not a ruler, it's more like a story: Unlike a ruler with equal units, the Geological Time Scale has uneven periods. Some eras lasted hundreds of millions of years, while others were mere blips in Earth's history.

2-Evidence from radiometric dating indicates that Earth is about 4.54 billion years old. The geology or deep time of Earth’s past has been organized into various units according to events which took place in each period.

3-Different spans of time on the GTS are usually delimited by changes in the composition of strata which correspond to them, indicating major geological or paleontological events, such as mass extinctions. For example, the boundary between the Cretaceous period and the Paleogene period is defined by the Cretaceous–Paleogene extinction event, which marked the demise of the non-avian dinosaurs and many other groups of life. Older time spans which predate the reliable fossil record (before the Proterozoic Eon) are defined by the absolute age.

4-The first serious attempts to formulate a geological time scale that could be applied anywhere on Earth were made in the late 18th century. The most influential of those early attempts (championed by Abraham Werner, among others) divided the rocks of Earth’s crust into four types: Primary, Secondary, Tertiary, and Quaternary.

10 Interesting Facts About the Geological Time Scale
Ray Troll’s creative approach on displaying geologic time is not only super cool, but inspiring.

5-The first geologic time scale that included absolute dates was published in 1913 by the British geologist Arthur Holmes.

6-Geologists have divided Earth's history into a series of time intervals. These time intervals are not equal in length like the hours in a day. Instead the time intervals are variable in length. This is because geologic time is divided using significant events in the history of the Earth.

7-The largest defined unit of time is the supereon, composed of eons. Eons are divided into eras, which are in turn divided into periods, epochs and ages. The terms "eonothem", "erathem", "system", "series", and "stage" are used to refer to the layers of rock that correspond to these periods of geologic time in Earth's history.

8-Mass Extinctions: Earth has witnessed five major mass extinction events, where a significant portion of life on Earth perished in a relatively short period. The most famous is the Cretaceous-Paleogene extinction event, which wiped out the dinosaurs.

9-The term "Anthropocene" is used informally by popular culture and a growing number of scientists to describe the current epoch in which we are living. The term was coined by Paul Crutzen and Eugene Stoermer in 2000 to describe the current time, in which humans have had an enormous impact on the environment.

10-The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian.

11-The Great Unconformity: Imagine a giant gap in Earth's rock record, representing hundreds of millions of years missing. That's the Great Unconformity, a boundary between the Archean and Proterozoic eons where evidence of this lost time is absent.

12-Snowball Earth: Believe it or not, Earth might have been entirely frozen over twice during the Proterozoic eon, in events known as "Snowball Earth." These global glaciations had a profound impact on the evolution of life.

13-The Cambrian Explosion: Life on Earth took a dramatic leap forward around 541 million years ago, during the Cambrian Explosion. This period saw the rapid diversification of multicellular organisms into a vast array of forms. 

14-Continents were once one: Around 200 million years ago, all the continents were joined together in a supercontinent called Pangea. Over time, this supercontinent slowly drifted apart, forming the continents we know today.

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