fundamentals of geology geologic materialsw3.salemstate.edu/~bhubeny/gls201/earthsystem.pdf ·...

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1 1 Earth System History Study of the inter- connected physical, chemical and biological changes that our planet has experienced over the course of geologic time 2 Earth Systems 3 Fundamentals of Geology Principle of Actualism (Uniformitarianism) Application of modern processes to ancient system There are inviolable laws of nature that have not changed in the course of time The Present is the Key to the Past Catastrophism 4 Geologic Materials • Minerals • Rocks The Rock Cycle Do you remember? 5 Sedimentary Rocks Stratum (Bed): – Tabular layer of sediment accumulated in discrete episodes 6 Rock Units • Formations Unit of rock formed in a particular way Formally named, often for nearby geographic feature Kaibab Limestone (Rim of the Grand Canyon) • Member Smaller rock unit • Group Groups of formations

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Page 1: Fundamentals of Geology Geologic Materialsw3.salemstate.edu/~bhubeny/GLS201/EarthSystem.pdf · Earth System History Study of the inter-connected physical, chemical and biological

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Earth System History

Study of the inter-connected physical,chemical andbiological changesthat our planet hasexperienced over thecourse of geologictime

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Earth Systems

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Fundamentals of Geology

• Principle of Actualism (Uniformitarianism)– Application of modern processes to ancient

system– There are inviolable laws of nature that have

not changed in the course of time– The Present is the Key to the Past

• Catastrophism

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Geologic Materials

• Minerals• Rocks• The Rock Cycle

– Do you remember?

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Sedimentary Rocks

• Stratum (Bed):– Tabular layer of

sedimentaccumulated indiscreteepisodes

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Rock Units

• Formations– Unit of rock formed in a particular way– Formally named, often for nearby geographic feature

• Kaibab Limestone (Rim of the Grand Canyon)

• Member– Smaller rock unit

• Group– Groups of formations

Page 2: Fundamentals of Geology Geologic Materialsw3.salemstate.edu/~bhubeny/GLS201/EarthSystem.pdf · Earth System History Study of the inter-connected physical, chemical and biological

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Geologic Time Scale

• Developed using– Relative Dating

• Principles of rock and fossilrelationships

– Absolute Dating• Radioactive Decay

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Earth’s Interior

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Outer Earth

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Plate Tectonics

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Water Cycle

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Directional vs. Cyclic Changes • Evolution

- the changing of organisms that constitute biosphere is a one-way process- Evolution and Mass Extinctions

• Cooling - the Earth’s internal temperature is slowly decreasing

• Sea Level has risen and fallen• Orogenies come and go• Surface temperatures have risen and fallen