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The Ice Age refers to a period in Earth's history when global temperatures were colder than usual, causing polar ice sheets to expand and cover large portions of the planet. This resulted in significant changes to ecosystems and the distribution of plant and animal species. The most recent Ice Age occurred approximately 2.6 million years ago and ended around 11,700 years ago.

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How is the absolute age of the fossil different from the relative age?

The absolute age of a fossil provides a specific numerical age in years, usually determined through radiometric dating techniques. Relative age, on the other hand, only allows us to determine the fossil's age in relation to other fossils or rocks, based on their layering or sequence in the rock record.


The age of a rock compared with the age of other rocks?

The age of a rock can be determined through radiometric dating techniques, comparing the ratios of certain elements in the rock to known decay rates. By analyzing the age of the rock in relation to the ages of other rocks in the surrounding area or in similar geological contexts, scientists can establish the relative age of the rock within the geological timescale.


What is a non-examples for relative age?

An example of a non-example for relative age would be an absolute age. Relative age involves determining the sequence of events or objects compared to one another without assigning specific numerical ages. In contrast, absolute age provides a specific numerical age through methods like radiometric dating.


The age in years of a rock or other object is a what?

The age in years of a rock or other object is a representation of the time that has passed since its formation. This age can be determined through various methods such as radiometric dating or relative dating techniques.


Does soil age?

Yes, soil can be considered to have an age, which is determined by factors such as the length of time it has been forming and developing as well as the history of its environmental conditions. Soil age can impact its composition, fertility, and ability to support plant growth.

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