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Introduction 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. 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. Earth’s Four Spheres • Solid Earth (Lithosphere) • Hydrosphere • Atmosphere • Biosphere 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 Earth’s Crust • The earth’s crust is divided into: – Continental crust – Oceanic crust Hydrosphere 1. Ocean (the most prominent feature of the hydrosphere) a. Nearly 71% of Earth’s surface b. About 97% of the earth’s water 2. Fresh water a. glaciers b. rivers and lakes c. groundwater Atmosphere 1. Gaseous envelope surrounding Earth a. life-giving gases b. protects organisms from intense heat and radiation from the sun Biosphere 1. Includes all life 2. Influences the other three spheres Course Overview • Lithosphere- Geology • Water- Oceanography • Atmosphere- Meteorology • Space- Astronomy Branches of Geology • Paleontology Branches of Geology • Volcanology Branches of Geology • Glaciology Branches of Geology • Seismology Branches of Geology • Mineralogy Branches of Geology • Sedimentology Branches of Geology • Structural Geology Branches of Geology • Planetary Geology