25
Lecture Outlines PowerPoint Chapter 1 Earth Science, 12e Tarbuck/Lutgens

Chapter 1_Lecture - Introduction to Earth Science

Embed Size (px)

Citation preview

Page 1: Chapter 1_Lecture - Introduction to Earth Science

Lecture Outlines PowerPoint

Chapter 1

Earth Science, 12e

Tarbuck/Lutgens

Page 2: Chapter 1_Lecture - Introduction to Earth Science

Earth Science, Earth Science, 12e12e

Introduction to Introduction to Earth ScienceEarth Science

Chapter 1Chapter 1

Page 3: Chapter 1_Lecture - Introduction to Earth Science

Earth ScienceEarth Science

Encompasses all sciences that seek to understand • Earth • Earth’s neighbors in space

Earth Science includes• Geology – literally the “study of Earth” • Oceanography – a study of the ocean

Page 4: Chapter 1_Lecture - Introduction to Earth Science

Earth ScienceEarth Science

Earth Science includes• Meteorology – the study of the atmosphere

and the processes that produce weather • Astronomy – the study of the universe

Page 5: Chapter 1_Lecture - Introduction to Earth Science

People and the environment People and the environment

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

Page 6: Chapter 1_Lecture - Introduction to Earth Science

People and the environment 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)

Page 7: Chapter 1_Lecture - Introduction to Earth Science

People and the environment 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

Page 8: Chapter 1_Lecture - Introduction to Earth Science

People and the environment People and the environment

Environmental problems• Human-induced and accentuated

• Urban air pollution• Acid rain• Ozone depletion• Global warming

• Natural hazards • Earthquakes • Landslides

Page 9: Chapter 1_Lecture - Introduction to Earth Science

People and the environment People and the environment

Environmental problems• Natural hazards continued

• Floods• Hurricanes

• World population pressures

Page 10: Chapter 1_Lecture - Introduction to Earth Science

Scientific inquiry Scientific inquiry

Science assumes the natural world is • Consistent• Predictable

Goal of science • To discover patterns in nature• To use the knowledge to predict

Page 11: Chapter 1_Lecture - Introduction to Earth Science

Scientific inquiry Scientific inquiry An idea can become a

• 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

Page 12: Chapter 1_Lecture - Introduction to Earth Science

Scientific inquiry Scientific inquiry

Scientific knowledge is gained through • Following systematic steps

• Collecting facts• Developing a hypothesis • Conduct experiments • Reexamine the hypothesis and accept, modify,

or reject• Theories that withstand examination • Totally unexpected occurrences

Page 13: Chapter 1_Lecture - Introduction to Earth Science

Early evolution of Earth 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 • Nebula was composed mostly of hydrogen and

helium

Page 14: Chapter 1_Lecture - Introduction to Earth Science

Early evolution of Earth Early evolution of Earth

Origin of Earth • Nebular hypothesis (cont’d)

• 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

Page 15: Chapter 1_Lecture - Introduction to Earth Science

The Nebular hypothesisThe Nebular hypothesis

Figure 1.8

Page 16: Chapter 1_Lecture - Introduction to Earth Science

Early evolution of Earth Early evolution of Earth Formation of Earth’s layered structure

• As Earth formed, the decay of radioactive elements and heat from high-velocity impacts caused the temperature to increase

• Iron and nickel 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

Page 17: Chapter 1_Lecture - Introduction to Earth Science

Earth’s “Spheres”Earth’s “Spheres”

Hydrosphere • Ocean – the most prominent feature of the

hydrosphere • Nearly 71% of Earth’s surface • About 97% of Earth’s water

• Also includes fresh water found in streams, lakes, and glaciers, as well as that found underground

Page 18: Chapter 1_Lecture - Introduction to Earth Science

Earth’s “Spheres”Earth’s “Spheres”

Atmosphere • Thin, tenuous blanket of air • One-half lies below 5.6 kilometers (3.5

miles) Biosphere

• Includes all life • Concentrated near the surface in a zone

that extends from the ocean floor upward for several kilometers into the atmosphere

Page 19: Chapter 1_Lecture - Introduction to Earth Science

Earth’s “Spheres”Earth’s “Spheres”

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 • Divisions of Earth’s surface – continents and

ocean basins

Page 20: Chapter 1_Lecture - Introduction to Earth Science

Earth’s layered structureEarth’s layered structure

Figure 1.13

Page 21: Chapter 1_Lecture - Introduction to Earth Science

Earth system science Earth system science 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 parts, or subsystems

System – any size group of interacting parts that form a complex whole

Page 22: Chapter 1_Lecture - Introduction to Earth Science

Earth system science Earth system science

System • Closed systems are self-contained (e.g.,

an automobile cooling system) • Open systems – both energy and matter

flow into and out of the system (e.g., a river system)

Page 23: Chapter 1_Lecture - Introduction to Earth Science

Earth system science Earth system science Feedback mechanisms

• Negative-feedback mechanisms resist change and stabilize the system

• Positive-feedback mechanisms enhance the system

Earth as a system • Consists of a nearly endless array of

subsystems (e.g., hydrologic cycle, rock cycle)

Page 24: Chapter 1_Lecture - Introduction to Earth Science

Earth system cyclesEarth system cycles

Figure 1.21

Page 25: Chapter 1_Lecture - Introduction to Earth Science

Earth system science 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 – drives internal processes including volcanoes, earthquakes, and mountain building

• Humans are part of the Earth system