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Prentice Hall Earth Science chapter 12 Geologic Time part 1
Prentice Hall ch12 geologic time part 1 edited
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Prentice Hall Earth Science chapter 12 Geologic Time part 1
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The geologic time scale (GTS) is a system of chronological dating that relates geological strata (stratigraphy) to time. 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.
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Introduction Stratigraphy is the study of strata (sedimentary layers) in the Earth's crust, it is the relationship between rocks and time. Stratigrapher are concerned with the observation, description and interpretation of direct and tangible evidence in rocks to determine the history of the Earth. The combination of sedimentology and stratigraphy allows us to build up pictures of the Earth’s surface at different times in different places and relate them to each other through the relative ages of rocks A more modern way of stating the same principle is that the laws of nature (laws of chemistry and physics) that have operated in the same way since the beginning of time. And thus if we understand the physical and chemical principles by which nature operates, we can assume that nature operated the same way in the past. Basic principles of stratigraphy Principle of Uniformitarianism Principle of Lateral Horizontality Principle of Superposition Principle of Cross-cutting Relations Principle of Inclusions Principle of Chilled Margins Correlation
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Chapter+12+geologic+time
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