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Lecture Outlines PowerPoint
Chapter 1 Earth Science 11e Tarbuck/Lutgens © 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors in teaching their courses and assessing student learning. Dissemination or sale of any part of this work (including on the World Wide Web) will destroy the integrity of the work and is not permitted. The work and materials from it should never be made available to students except by instructors using the accompanying text in their classes. All recipients of this work are expected to abide by these restrictions and to honor the intended pedagogical purposes and the needs of other instructors who rely on these materials.
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Introduction to Earth Science Chapter 1
Earth Science, 11e Introduction to Earth Science Chapter 1
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What is Earth Science? Encompasses all sciences that seek to understand Earth Earth's neighbors in space Seeks to answer questions such as... What forces produce mountains? Why is our daily weather so variable? Is climate really changing? How old is the Earth?
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Earth Science Earth Science includes
Geology - literally the “study of Earth” Oceanography – a study of the ocean Meteorology - the study of the atmosphere and the processes that produce weather Astronomy - the study of the universe
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People and the environment
Surrounds and influences organisms Physical environment encompasses water, air, soil, and rock Term “environmental” is usually reserved for those aspects that focus on the relationships between people and the natural environment
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People and the environment
Resources An important focus of the Earth sciences Includes water, soil, minerals, and energy Two broad categories Renewable – can be replenished (examples include plants and energy from water and wind) Nonrenewable – metals (examples include metals and fuels)
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People and the environment
Population Population of the planet is growing rapidly Rate of mineral and energy usage has climbed more rapidly than the overall growth of population Environmental problems Local, regional, and global
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People and the environment
Environmental problems Human-induced and accentuated Urban air pollution Acid rain Ozone depletion Global warming Natural hazards Earthquakes Landslides
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People and the environment
Environmental problems Natural hazards continued Floods Hurricanes World population pressures
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Scientific inquiry Science assumes the natural world is
Consistent Predictable Goal of science To discover patterns, trends in nature To use the knowledge to make predictions
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Scientific inquiry An idea can become a Scientific method
Hypothesis (tentative or untested explanation) Theory (tested and confirmed hypothesis) Paradigm (a theory that explains a large number of interrelated aspects of the natural world) Scientific method Gather facts through observation Formulate hypotheses and theories
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Scientific inquiry Scientific knowledge is gained through
Following systematic steps Collecting facts Developing a hypothesis Conduct experiments Re-examine the hypothesis and accept, modify, or reject Theories that withstand examination Totally unexpected occurrences
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Notes Check (in your notebooks)
Name the specific earth science: a. ocean dynamics b. “study of the Earth” c. understanding of atmosphere d. understanding of Earth’s place in the universe. 2. Contrast renewable and non renewable resources. Give 2 examples of each. 3. Compare the world population in 2010 to beginning of the 1900. List 5 natural hazards.
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Earth’s Time and Scale The study of Earth involves vast space and times. Compare….. - the flash of lightning to building of a mountain. - The size of an atom in minerals or the distances in our galaxy.
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Early evolution of Earth
Origin of Earth Most researchers believe that Earth and the other planets formed at essentially the same time Nebular hypothesis Solar system evolved from an enormous rotating cloud called the solar nebula
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The Nebular hypothesis
Figure 1.7
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Early evolution of Earth
Origin of Earth Nebula was composed mostly of hydrogen and helium gas About 5 billion years ago the nebula began to contract Assumes 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
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Early evolution of Earth
Formation of Earth’s layered structure HEAT from the decay of radioactive elements and heat from high-velocity impacts caused the temperature to increase Iron and nickel metals began to melt and sink toward the center Lighter rocky components floated outward, toward the surface Gaseous material escaped from Earth’s interior to produce the primitive atmosphere
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Earth’s layered structure
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Earth's “Spheres" Earth’s physical environment is divided into three major spheres: The water portion: __________________ The gaseous envelope: _______________ The solid earth: _____________________ Do you see all 3 ‘spheres in the photo of the Earth from space?
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Hydrosphere All the water Lakes, rivers Oceans Glaciers Aquifers
In your note book, Rank them in order from most to least amount.
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Atmosphere Atmosphere layered Thin, tenuous blanket of air
One half lies below 5.6 kilometers (3.5 miles) What layer do we live in?
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Biosphere Biosphere Includes all life
Concentrated near the surface in a zone that extends from the ocean floor upward for several kilometers into the atmosphere. From ________ to ________ (smallest) (largest)
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Geosphere Solid Earth Based on compositional differences, it consists of the crust, mantle, and core Divisions of the outer portion are based on how materials behave Lithosphere - rigid outer layer Continents and Ocean basins (land) (sea-floor)
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Earth system science page 20
Earth is a dynamic body with many separate but highly interacting parts or spheres Earth system science studies Earth as a system composed of numerous complex, continuously interacting parts, or subsystems System - any size group of interacting parts that form a complex whole
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Earth system science System
Closed systems: matter is contained, but energy can freely flow in and out. Open systems - both energy and matter flow into and out of the system (e.g. a river system) B C D A
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Planet Earth: Open or Closed System?
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Earth system science Feedback mechanisms
Negative-feedback mechanisms resist change and stabilize the system Positive-feedback mechanisms enhance the system and changes the system for the better or worse. Earth consists of a nearly endless array of subsystems (rock cycle, water cycle) Ex: perspiration works to maintain an even body temperature Ex: deforestation: cutting down large areas of trees - reduces photosynthesis – increases CO2 - increases greenhouse gases – increases global temperatures
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Earth system CYCLES Also: Carbon cycle Recycling cycles Interface:
A common boundary where different parts of a system com in contact and interact Figure 1.17
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Earth system science Earth as a system Sources of ENERGY
Sun – drives external processes such as weather, ocean circulation and erosional processes Earth’s interior heat– drives internal processes including volcanoes, earthquakes and mountain building
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End of Chapter 1
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