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Introduction
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Formation of Earth The Nebular Hypothesis
bodies in our solar system evolved from an enormous rotating cloud called the solar nebula. mostly hydrogen and helium, with some heavier elements.
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Differentiation As Earth cooled, layers formed through a process called differentiation. Denser elements (iron and nickel) sunk to Earth’s core. Lighter material migrated outward forming the mantle and crust.
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Earth’s Four Spheres Solid Earth (Lithosphere) Hydrosphere Atmosphere
Biosphere
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Solid Earth Core mostly iron and nickel densest part of Earth
inner core solid Mantle mostly iron and magnesium liquid Crust mostly silicon and oxygen rigid outer layer
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Earth’s Crust The earth’s crust is divided into: Continental crust
Oceanic crust
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Hydrosphere Ocean (the most prominent feature of the hydrosphere)
a. Nearly 71% of Earth’s surface b. About 97% of the earth’s water Fresh water a. glaciers b. rivers and lakes c. groundwater
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Atmosphere Gaseous envelope surrounding Earth a. life-giving gases
b. protects organisms from intense heat and radiation from the sun
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Biosphere Includes all life Influences the other three spheres
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Course Overview Lithosphere- Geology Water- Oceanography
Atmosphere- Meteorology Space- Astronomy
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Branches of Geology Paleontology
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Branches of Geology Volcanology
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Branches of Geology Glaciology
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Branches of Geology Seismology
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Branches of Geology Mineralogy
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Branches of Geology Sedimentology
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Branches of Geology Structural Geology
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Branches of Geology Planetary Geology
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