Introduction to Earth Science

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Introduction to Earth Science Overview of Earth Science Encompasses all sciences that seek to understand Earth Earth's neighbors in space Overview of Earth Science Earth science includes 1. geology, the study of Earth 2. oceanography, the study of the ocean 3. meteorology, the study of the atmosphere and the processes that produce weather 4. astronomy, the study of the universe Most researchers conclude that Earth and the other planets formed at essentially the same time. The solar system evolved from an enormous rotating cloud called the solar nebula. The nebula was composed mostly of hydrogen and helium. About 5 billion years ago, the nebula began to contract. It assumed a flat, disk shape with the protosun (pre-sun) at the center. Inner planets begin to form from metallic and rocky clumps. Larger outer planets began forming from fragments with a high percentage of ices. 1

C A E B D Layers Form on Earth As Earth formed, the decay of radioactive elements and heat from high-velocity impacts caused the temperature to increase. Lighter rocky components floated outward, toward the surface. Gaseous material escaped from Earth s interior to produce the primitive atmosphere. 1. Hydrosphere Ocean is the most prominent feature of the hydrosphere. - Is nearly 71% of Earth's surface - Holds about 97% of Earth's water Also includes fresh water found in streams, lakes, and glaciers, as well as that found underground 2. Atmosphere Thin, tenuous (not dense, slender, little substance) blanket of air One half lies below 5.6 kilometers (3.5 miles) 3. Biosphere Includes all life Concentrated near the surface in a zone that extends from the ocean floor upward for several kilometers into the atmosphere Earth s Layered Structure 4. Geosphere Based on compositional differences, it consists of the crust, mantle, and core. - Crust the thin, rocky outer layer of Earth. - Mantle the 2890-kilometer-thick layer of Earth located below the crust. - Core the innermost layer of Earth, located beneath the mantle. 2

Plate Tectonics Plate tectonics is the theory that proposes that Earth s outer shell consists of individual plates that interact in various ways and thereby produce earthquakes, volcanoes, mountains, and Earth s crust itself. Determining Location Latitude and longitude are lines on the globe that are used to determine location. Latitude is distance north or south of the equator, measured in degrees. Longitude is distance east or west of the prime meridian, measured in degrees. Maps and Mapping No matter what kind of map is made, some portion of the surface will always look either too small, too big, or out of place. Mapmakers have, however, found ways to limit the distortion of shape, size, distance and direction. Topographic Maps Topographic maps represent Earth s surface in three dimensions; they show elevation, distance directions, and slope angles. Contour lines are lines on a topographic map that indicate an elevation. Contour interval is the distance in elevation between adjacent contour lines. What Is a System? A system is any size group of interacting parts that form a complex whole. Closed systems are self contained (e.g., an automobile cooling system). Open systems allow both energy and matter to flow in and out of the system (e.g., a river system). Earth is a dynamic body with many separate but highly interacting parts or spheres. Earth system science studies Earth as a system that is composed of numerous parts, or subsystems. 3

Sources of Energy Sun drives external processes such as weather, ocean circulation and erosional processes Earth s interior drives internal processes including volcanoes, earthquakes and mountain building Consists of a nearly endless array of subsystems (e.g., hydrologic cycle) Humans are part of the Earth system. Environment Surrounds and influences organisms Physical environment encompasses water, air, soil, and rock The term environmental is usually reserved for those aspects that focus on the relationships between people and the natural environment. Resources Include water, soil, minerals, and energy Two broad categories 1. Renewable can be replenished (e.g., plants, energy from water and wind) 2. Nonrenewable cannot be replenished in the near future (e.g., metals, fuels) Growth of World Population Population Population of the planet is growing rapidly Use of minerals/energy has climbed more rapidly than the overall growth of population 4

Environmental Problems Local, regional, and global Caused by people and societies Urban air pollution Acid rain Ozone depletion Global warming Caused by natural hazards Earthquakes Landslides Science Science assumes the natural world is consistent predictable Goals of science are to discover patterns in nature to use the knowledge to predict Hypothesis and Theory An idea can become a hypothesis tentative or untested explanation theory tested, confirmed, supported hypothesis Scientific Method Gather facts through observation Formulate hypotheses Test hypotheses to formulate theories Science Methods Scientific knowledge is gained through following systematic steps 1. Collecting facts 2. Developing a hypothesis 3. Conducting experiments 4. Reexamining the hypothesis and accepting, modifying, or rejecting it theories that withstand examination totally unexpected occurrences 5