Relative age dating of rocks definition
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Paleontology is the most readily recognizable subdivision of geology that applies to dinosaur studies, but other specialties, such as sedimentology, stratigraphy, and tectonics, are also essential to form a more complete, contextual view of dinosaurs (Table 4.3).
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The basic principles of geology, which were formed through many repeated observations made by field geologists through the early nineteenth century (Chapter 3), are still used by geologists and paleontologists today and are responsible for what is seen in a geologic map.
Study of the interior of the earth and how it releases energy: evaluating and predicting earthquakes.
Study of sedimentary rocks through mapping of their vertical and horizontal extents: evaluating resources such as coal, aquifers, and oil.
Study of the Earth's oceanic processes: interpreting sea-level fluctuations, earth history, and interactions of oceanic environments with other global systems.
Study of ancient climates and their changes through time: interpreting patterns in climate change and factors affecting climate in the past, including factors that might affect modern climate.
Study of the earth through principles of physics: determining presence of subsurface oil or mineral deposits.