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Historical geology

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that are at work today, the product of slow and continuous geological changes. The theory can be summarized by the phrase "the present is the key to the past." Hutton also described the concept of deep time. The prevailing conceptualization of Earth history in 18th-century Europe, grounded in a
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Historical geology covers much of the same subject matter as physical geology, the study of geological processes and the ways in which they shape the Earth's structure and composition. Historical geology extends physical geology into the past.
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are organic traces of Earth's history. In a historical geology context, paleontological methods can be used to study fossils and their environments, including surrounding rocks, and place them within the geologic time scale.
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further developed the theory of uniformitarianism in the 19th century. Modern geologists have generally acknowledged that Earth's geological history is a product of both sudden, cataclysmic events (such as
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Historical geology makes use of relative dating in order to establish the sequence of geological events in relation to each another, without determining their specific numerical ages or ranges.
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Absolute dating allows geologists to determine a more precise chronology of geological events, based on numerical ages or ranges. Absolute dating includes the use of
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was the first to observe and propose a number of basic principles of historical geology, including three key stratigraphic principles: the
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Theory of the Earth; or an Investigation of the Laws Observable in the Composition, Dissolution, and Restoration of Land upon the Globe
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are examples of gradual geological processes, taking place over large sections of the geologic time scale. In the
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Geology is considered a historical science; accordingly, historical geology plays a prominent role in the field.
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of Earth's history. Stratigraphy is the study of strata: their order, position, and age.
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events. Hutton, however, depicted a very old Earth, shaped by slow, continuous change.
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Sedimentology is the study of the formation, transport, deposition, and diagenesis of
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plates has structured the Earth throughout its geological history.
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to tell the sequence of these events. It also focuses on the
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techniques in the 20th century provided a means of deriving
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10.1130/0016-7606(1995)107<0960:GRGAAI>2.3.CO;2
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is the study of past climates recorded in geological time.
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The theory of plate tectonics explains how the movement of
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is a discipline that uses the principles and methods of
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(2017). 939: 103: 1120: 36: 27:Study of the geological history of Earth 184:ages of events in geological history. 14: 1747: 361:are other methods of absolute dating. 152:, was that of a young Earth shaped by 1269: 256: 187: 96:during different time periods in the 935: 933: 1727: 411: 377:Weathering, erosion, and deposition 202:, the search for and extraction of 118:principle of original horizontality 24: 364: 322: 308: 25: 1766: 1238: 930: 1726: 1715: 1714: 1702: 1334: 292: 214:, which examines the impacts of 64:, gradual and sudden, over this 1213: 1188: 1163: 1121:Frodeman, Robert (1995-08-01). 274: 234: 122:principle of lateral continuity 1114: 1094: 1066: 1045: 1025: 1000: 979: 958: 13: 1: 7: 1359:Geological history of Earth 1295: 1260:GEOL 102 Historical Geology 135:by proposing the theory of 58:geological history of Earth 10: 1771: 1332: 1085:Royal Society of Edinburgh 752: 737: 452: 426: 326: 312: 278: 260: 238: 229: 148:literal interpretation of 29: 1696: 1670: 1599: 1561: 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Index

Paleohydrogeology
History of geology

geology
geological history of Earth
Earth
deep time
plate tectonics
stratigraphy
structural geology
paleontology
sedimentology
evolution
life
geologic time scale
Nicolas Steno
law of superposition
principle of original horizontality
principle of lateral continuity
James Hutton
Earth's history
uniformitarianism
Earth
natural phenomena
Christian scripture
catastrophic
Charles Lyell
meteorite impacts
volcanic eruptions
radioactive decay

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