• Units
    • Unit Overview
    • Unit A: The Solid Earth
      • Get Ready
      • Unit Overview and Big Ideas
      • What Do You Already Know?
      • Literacy Link: A Walk on the Bottom of the Sea
      • Unit Lessons
      • A1: Earth as a System
          • Guiding Question: What makes up the Earth system?
          • Key Concepts
          • The Earth is a dynamic planet made up of five interrelated natural systems.
          • These natural systems consist primarily of air (atmosphere), water (hydrosphere), ice and snow (cryosphere), all living organisms (biosphere), and rocks (geosphere).
          • A1-1: Earth As A System
          • A1-2: The Atmosphere
          • A1-3: The Hydrosphere
          • A1-4: The Cryosphere
          • A1-5: The Biosphere
          • A1-6: The Geosphere
          • Lesson Summary
          • Review Questions
      • A2: Earth's Layered Structure
          • Guiding Question: What characterizes the interior of the Earth?
          • Key Concepts
          • The Earth is composed of several distinct layers, each with its own specific characteristics.
          • The interior of the Earth is heated primarily by radioactive decay.
          • A2-1: Earth's Layered Structure
          • A2-2: The Lithosphere and the Asthenosphere
          • A2-3: Where Does the Heat Come From?
          • Lesson Summary
          • Review Questions
      • A3: Oceans and Continents
          • Guiding Question: How do we distinguish between the different types of crust?
          • Key Concepts
          • Oceanic and continental crusts are primarily defined by differences in chemical composition and in density.
          • Continents and oceans each have a number of distinguishing physical features.
          • A3-1: Oceanic and Continental Crust
          • A3-2: Major Features of Continents
          • A3-3: Major Features of Oceans: Continental Margins
          • A3-4: Major Features of Oceans: Deep-Ocean Basins
          • Lesson Summary
          • Review Questions
      • Wrap Up
      • What Do You Know Now?
      • Unit Activity
    • Unit B: Plate Tectonics
      • Get Ready
      • Unit Overview and Big Ideas
      • What Do You Already Know?
      • Literacy Link: Antarctica’s Warmer, Not Gentler Past
      • Unit Lessons
      • B1: Continental Drift
          • Guiding Question: What evidence supports the idea that continents are in motion?
          • Key Concepts
          • The shape and position of today’s continents is the result of movement over time of landmasses that were originally part of a giant supercontinent.
          • The shapes of continents, as well as geologic, fossil, and climate evidence all provide clues that continents have moved over time.
          • B1-1: The Fit of the Continents
          • B1-2: The Supercontinent of Pangaea
          • B1-3: Geologic Evidence
          • B1-4: Fossil Evidence
          • B1-5: Climate Evidence
          • Lesson Summary
          • Review Questions
      • B2: Seafloor Spreading and Paleomagnetism
          • Guiding Question: Why is ocean crust so much younger than continental crust?
          • Key Concepts
          • The theory of seafloor spreading states that new ocean crust is continually being formed, and that this crust is slowly carried away from its point of origin over a period of time.
          • The study of the repeated reversal of the Earth’s magnetic poles over time has provided convincing evidence of seafloor spreading.
          • B2-1: Seafloor Spreading
          • B2-2: Magnetic Reversal and the Curie Temperature
          • B2-3: Paleomagnetism
          • B2-4: Drilling and the Age of the Seafloor
          • Lesson Summary
          • Review Questions
      • B3: The Theory of Plate Tectonics
          • Guiding Question: Why has the theory of plate tectonics been so successful as an explanation for the movement of continents?
          • Key Concepts
          • The lithosphere is broken into plates that are constantly in motion.
          • Interacting plate boundaries are distinguished by three different types of plate interactions.
          • Convection is the fundamental underlying mechanism driving plate motion.
          • B3-1: The Theory of Plate Tectonics
          • B3-2: Plate Boundaries: Divergent
          • B3-3: Plate Boundaries: Convergent
          • B3-4: Plate Boundaries: Transform Fault
          • B3-5: What Drives Plate Motion?
          • B3-6: Plate Boundaries Interactive Animation
          • Lesson Summary
          • Review Questions
      • Wrap Up
      • What Do You Know Now?
      • Unit Activity
    • Unit C: Minerals and Rocks
      • Get Ready
      • Unit Overview and Big Ideas
      • What Do You Already Know?
      • Literacy Link: The Fascination of Marble
      • Unit Lessons
      • C1: Minerals - Building Blocks of Rocks
          • Guiding Question: What is the difference between a mineral and a rock?
          • Key Concepts
          • A mineral is a solid with specific characteristics that define a unique composition and structure.
          • Rock is composed of a combination of different minerals.
          • C1-1: What Is a Mineral?
          • C1-2: Characteristics of Minerals
          • C1-3: Properties of Minerals
          • C1-4: What Is a Rock?
          • Lesson Summary
          • Review Questions
      • C2: The Rock Cycle
          • Guiding Questions: What is the rock cycle? How does the rock cycle work?
          • Key Concepts
          • The three main types of rocks, based on how they are formed, are igneous, sedimentary, and metamorphic.
          • Rocks are continuously forming, changing, and reforming through the rock cycle.
          • C2-1: The Three Types of Rocks
          • C2-2: The Rock Cycle – The Basic Cycle
          • C2-3: The Rock Cycle – Possible Pathways
          • Lesson Summary
          • Review Questions
      • C3: Igneous, Sedimentary and Metamorphic Rocks
          • Guiding Question: What are the processes that produce the different types of rock?
          • Key Concepts
          • The process by which a rock is formed influences its characteristics.
          • The environment in which the process takes place also influences a rock’s characteristics.
          • C3-1: Formation of Igneous Rock
          • C3-2: Types of Igneous Rock
          • C3-3: Formation of Sedimentary Rock
          • C3-4: Types of Sedimentary Rock
          • C3-5: Formation of Metamorphic Rock
          • C3-6: Types of Metamorphic Rock
          • Lesson Summary
          • Review Questions
      • C4: Weathering and Soil Formation
          • Guiding Question: What processes produce soil?
          • Key Concepts
          • Physical and chemical processes break down rocks over time.
          • Soil formation is influenced by the interaction of geological, biological, and meteorological processes.
          • C4-1: Mechanical Weathering
          • C4-2: Chemical Weathering
          • C4-3: Rates of Weathering
          • C4-4: Soil Formation
          • Lesson Summary
          • Review Questions
      • Wrap Up
      • What Do You Know Now?
      • Unit Activity
    • Unit D: Shaping The Earth
      • Get Ready
      • Unit Overview and Big Ideas
      • What Do You Already Know?
      • Literacy Link: Living Through the Dust Bowl
      • Unit Lessons
      • D1: Shaping Earth’s Surface
          • Guiding Question: What processes are involved in shaping Earth's many different landforms?
          • Key Concepts
          • Internal and external processes modify the Earth’s surface.
          • Erosion is one of the major processes that shape the Earth’s landforms.
          • D1-1: Internal and External Processes
          • D1-2: Erosion and Deposition
          • Lesson Summary
          • Review Questions
      • D2: Mass Movement
          • Guiding Question: What role does gravity play in shaping Earth's surface?
          • Key Concepts
          • Mass movement is the movement of rock and soil down an incline by the force of gravity.
          • Mass movement can create a variety of natural features and landforms.
          • D2-1: Mass Movement
          • D2-2: Rapid Mass Movement
          • D2-3: Slow Mass Movement
          • Lesson Summary
          • Review Questions
      • D3: Water and Ice Landforms
          • Guiding Question: What role does water and moving ice play in shaping Earth's surface?
          • Key Concepts
          • Water is the Earth’s most important agent of erosion and is responsible for shaping a variety of landforms.
          • Glaciers produce unique landforms directly through erosion, and by the deposition of material.
          • D3-1: Water Erosion
          • D3-2: Water Landforms
          • D3-3: Glaciers
          • D3-4: Glacial Landforms: Erosion by Ice
          • D3-5: Glacial Landforms: Deposition
          • Lesson Summary
          • Review Questions
      • D4: Wind Landforms
          • Guiding Question: What role does wind play in shaping Earth's surface?
          • Key Concepts
          • Wind is an active agent of erosion.
          • Deposition of windblown sediment produces significant landforms.
          • D4-1: Shaped by the Wind
          • D4-2: Wind Erosion Processes
          • D4-3: Wind Deposition
          • Lesson Summary
          • Review Questions
      • Wrap Up
      • What Do You Know Now?
      • Unit Activity
    • Unit E: Earthquakes
      • Get Ready
      • Unit Overview and Big Ideas
      • What Do You Already Know?
      • Literacy Link: Mark Twain's First Earthquake
      • Unit Lessons
      • E1: Earthquakes and Faults
          • Guiding Question: What is an earthquake?
          • Key Concepts
          • Earthquakes are caused by the interaction of Earth's plates.
          • The sudden release of stored energy, in the form of movement along a fault, produces an earthquake.
          • E1-1: Some Great Beast!
          • E1-2: Where Are Earthquakes Located?
          • E1-3: What Causes an Earthquake?
          • Lesson Summary
          • Review Questions
      • E2: Earthquakes and Waves
          • Guiding Question: How is energy transmitted during an earthquake?
          • Key Concepts
          • Earthquake waves that travel through the Earth's interior are subdivided into primary (P) and secondary (S) waves.
          • Earthquake surface waves travel through the Earth’s outer layer.
          • E2-1: Transmitting Earthquake Energy
          • E2-2: Detecting an Earthquake
          • E2-3: Seismic Waves
          • Lesson Summary
          • Review Questions
      • E3: The Strength of Earthquakes
          • Guiding Question: How do we determine the location and strength of an earthquake?
          • Key Concepts
          • The different arrival time of earthquake waves can be used to pinpoint the location of an earthquake.
          • The strength of an earthquake can be determined either by the intensity of the earthquake or by the size of the seismic waves.
          • E3-1: The Point of Origin of an Earthquake
          • E3-2: Depth of an Earthquake
          • E3-3: Locating an Earthquake
          • E3-4: Calculating the Location of an Earthquake
          • E3-5: Measuring the Strength of an Earthquake
          • E3-6: The Largest Earthquakes
          • Lesson Summary
          • Review Questions
      • E4: Seismic Waves and the Earth's Interior
          • Guiding Question: How can seismic waves be used to help determine the composition of the Earth’s interior?
          • Key Concepts
          • The different arrival time of P waves can be used to determine the location of the crust-mantle boundary.
          • Evidence of a liquid core comes from the existence of shadow zones for P and S waves.
          • E4-1: Early Indications
          • E4-2: The Crust-Mantle Boundary
          • E4-3: The Mantle-Core Boundary
          • Lesson Summary
          • Review Questions
      • E5: Living with Earthquakes
          • Guiding Question: What is the impact of earthquakes on society?
          • Key Concept
          • Earthquakes have major social and economic consequences.
          • E5-1: Factors Affecting Earthquake Damage
          • E5-2: Related Causes of Damage - Liquefaction
          • E5-3: Related Causes of Damage - Landslides
          • E5-4: Related Causes of Damage - Tsunamis
          • E5-5: Related Causes of Damage - Fires
          • E5-6: Living in Earthquake Country
          • E5-7: Predicting Earthquakes
          • Lesson Summary
          • Review Questions
      • Wrap Up
      • What Do You Know Now?
      • Unit Activity
    • Unit F: Volcanoes
      • Get Ready
      • Unit Overview and Big Ideas
      • What Do You Already Know?
      • Literacy Link: A Journey to the Center of the Earth
      • Unit Lessons
      • F1: Formation of Volcanoes
          • Guiding Question: How are volcanoes formed?
          • Key Concepts
          • Most volcanoes occur along tectonic plate boundaries.
          • Volcanoes can occur far from plate boundaries as a result of stationary plumes of molten rock called "hot spots."
          • F1-1: What Is a Volcano?
          • F1-2: Where Are Volcanoes Found?
          • F1-3: Volcanoes and Convergent Plate Boundaries
          • F1-4: Volcanoes and Divergent Plate Boundaries
          • F1-5: Volcanoes and Hot Spots
          • Lesson Summary
          • Review Questions
      • F2: Types of Volcanoes
          • Guiding Question: How do we classify volcanoes?
          • Key Concepts
          • The force of a volcanic eruption is related to its lava type.
          • The shape of a volcano is determined by the chemical composition of the magma.
          • F2-1: Mafic Lava
          • F2-2: Felsic Lava
          • F2-3: Shield Volcano
          • F2-4: Composite Volcano or Stratovolcano
          • F2-5: Cinder Cone Volcano
          • F2-6: Volcanic Features
          • F2-7: Supervolcanoes
          • F2-8: Interactive Volcano Animation
          • Lesson Summary
          • Review Questions
      • F3: Living with Volcanoes
          • Guiding Question: What are the major social and economic effects of volcanic eruptions?
          • Key Concepts
          • Volcanic eruptions have both positive and negative effects on society.
          • Scientists have had some success at predicting the general likelihood of an eruption.
          • F3-1: The Hazards of Volcanic Eruptions - I
          • F3-2: The Hazards of Volcanic Eruptions - II
          • F3-3: Benefits of Volcanoes
          • F3-4: Predicting Volcanic Eruptions
          • Lesson Summary
          • Review Questions
      • Wrap Up
      • What Do You Know Now?
      • Unit Activity
    • Unit G: Geologic Time
      • Get Ready
      • Unit Overview and Big Ideas
      • What Do You Already Know?
      • Literacy Link: There Was a Second Sun
      • Unit Lessons
      • G1: Age of the Earth
          • Guiding Question: What methods are used to learn about the long history of the Earth?
          • Key Concepts
          • Relative ages of rocks can be determined by comparing rock layers.
          • The absolute ages of rocks can be determined through radioactive decay.
          • Fossils provide evidence of the Earth’s past.
          • G1-1: Age of the Earth
          • G1-2: Relative Age
          • G1-3: Unconformities
          • G1-4: Cross-Cutting Relationships
          • G1-5: Inclusions
          • G1-6: Correlation
          • G1-7: Absolute Age: Radioactive Decay
          • G1-8: Absolute Age: Radiometric Dating
          • G1-9: Radiocarbon Dating
          • G1-10: Fossils
          • G1-11: Index Fossils
          • Lesson Summary
          • Review Questions
      • G2: The Geologic Timescale
          • Guiding Question: How have the Earth’s life-forms and landmasses changed over time?
          • Key Concepts
          • Geologic time is broken down into smaller units called eras.
          • These eras correspond to major changes in the Earth’s life-forms.
          • These eras also correspond to major changes in form and position of the Earth’s landmasses.
          • G2-1: The Geologic Timescale
          • G2-2: Precambrian Time
          • G2-3: The Paleozoic Era
          • G2-4: The Mesozoic Era
          • G2-5: The Cenozoic Era
          • Lesson Summary
          • Review Questions
      • G3: Catastrophic Events and Mass Extinction
          • Guiding Question: How have catastrophic events affected life on the Earth?
          • Key Concepts
          • A catastrophic event is a short timescale event that has long-term effects on life and the environment.
          • Catastrophic events have been responsible for a number of large mass extinctions in Earth’s history.
          • G3-1: Mass Extinctions
          • G3-2: The Death of the Dinosaurs
          • G3-3: The Great Dying
          • Lesson Summary
          • Review Questions
      • G4: Earth’s Future
          • Guiding Question: What does the future hold for the Earth?
          • Key Concepts
          • Tectonic plates will continue to move, possibly resulting in the emergence of a new supercontinent 250 million years in the future.
          • The death of the Earth is expected to occur in about 5 billion years as a result of the sun becoming a red giant.
          • G4-1: The Earth’s Future Continents
          • G4-2: The End of the Earth
          • Lesson Summary
          • Review Questions
      • Wrap Up
      • What Do You Know Now?
      • Unit Activity
    • Glossary
  • Teachable Moments
    • Lessons
    • 2011 Japan Earthquake and Tsunami
        • Guiding Question: What were the causes and effects of the March 11, 2011 earthquake in Japan?
        • Key Concepts
        • Earthquakes are caused by the interaction of Earth's tectonic plates.
        • Earthquakes can generate a tsunami.
        • Earthquakes have major social and economic consequences.
        • 1: Earthquake In Japan
        • 2: Why Did The Earthquake Occur Here?
        • 3: Calculating the Epicenter of the Earthquake
        • 4: The Tsunami
        • 5: The Fukushima Power Plants
    • 2015 Gorkha (Nepal) Earthquake
        • Guiding Question: What were the causes and effects of the massive earthquake that occurred in Nepal on April 25, 2015?
        • Key Concepts
        • Earthquakes are caused by the interaction of Earth’s tectonic plates.
        • Nepal is tectonically active because of a convergent boundary between the Indian Plate and the Eurasian Plate.
        • Earthquakes have major social and economic consequences.
        • 1: About Nepal
        • 2: The Gorkha Earthquake
        • 3: Why Did the Earthquake Occur Here?
        • 4: Damage From the Earthquake
    • 2016 Ecuador Earthquake
        • Guiding Question: What were the causes and effects of the massive earthquake that occurred in Ecuador on April 16, 2016?
        • Key Concepts
        • Earthquakes are caused by the interaction of Earth’s tectonic plates.
        • Ecuador is tectonically active because of a convergent boundary between the Nazca Plate and the South American Plate.
        • Earthquakes have major social and economic consequences.
        • 1: Earthquake In Ecuador
        • 2: Active Seismic Zone
        • 3: When Plates Collide
        • 4: Stress Over Time
    • 2018 Honduras Earthquake
        • Guiding Question: What were the causes and effects of the earthquake that occurred in Honduras on January 9, 2018?
        • Key Concepts
        • Earthquakes are caused by the interaction of Earth’s tectonic plates.
        • Honduras is tectonically active because of the four plates that form the perimeter of the Caribbean plate.
        • Earthquakes have major social and economic consequences.
        • 1: Earthquake In Honduras
        • 2: Plate Boundaries
    • 2018 Gulf Of Alaska Earthquake
        • Guiding Question: What were the causes and effects of the earthquake that occurred in the Gulf of Alaska on January 23, 2018?
        • Key Concepts
        • Earthquakes are caused by the interaction of Earth’s tectonic plates.
        • The Aleutian Arc is a tectonically active area.
        • Earthquakes have major social and economic consequences.
        • 1: Gulf Of Alaska Earthquake
        • 2: Historical Precedent
    • 2023 Turkey-Syria Earthquake
        • Guiding Question: What were the causes and effects of the massive earthquake(s) that occurred in Turkey on February 6, 2023?
        • Key Concepts
        • Earthquakes are caused by the interaction of Earth’s tectonic plates.
        • Turkey is tectonically active because of the interactions between three tectonic plates, the Anatolian Plate, the Arabian Plate, and the African Plate.
        • Earthquakes have major social and economic consequences.
        • 1: Where Did the Earthquake Occur?
        • 2: Why Did the Earthquake Occur Here?
        • 3: Damage From the Earthquake