Essay on geological time scale

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Geological Time Scale Essay Sample

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(PDF) The Significance of Geological Time | Robert Frodeman and Cinzia Cervato -

The Geologic Time Scale is the history of the Earth broken down into four spans of time marked by various events, such as the emergence of certain species, their evolution, and their extinction, that help distinguish one era from another. Strictly speaking, Precambrian Time is not an actual era due to the lack of diversity of life, however, it's still considered significant because it predates the other three eras and may hold clues as to how all life on Earth eventually came to be. Precambrian Time started at the beginning of the Earth 4. For billions of years, there was no life on the planet. It wasn't until the end of Precambrian Time that single-celled organisms came into existence. The end of this time span saw the rise of a few more complex animals in the oceans, such as jellyfish.
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Geological Time Scale

Relative time - named subdivisions of the Earth's geology in a specific order for example, the "Cambrian Period", followed by the "Ordovician Period", and "Silurian Period". Most of these subdivisions are recognized globally on the basis of their relative position in the Earth's stratigraphy and their fossil content. Absolute time - numerical ages, often expressed in "millions of years before present".
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We often express time in hours or days, and 10 or 20 years certainly feels like a long time. Imagine if you needed to think about one million, million, or even several billion years. These exceptional lengths of time seem unbelievable, but they are exactly the spans of times that scientists use to describe the Earth. Have places like the Grand Canyon and the Mississippi River been around for all of those years, or were they formed more recently? When did the giant Rocky Mountains form and when did dinosaurs walk the Earth?
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