Learn on PengiAmplify Science (California) Grade 7Chapter 3: Movement of Rock Formations

Lesson 4: The Rock Cycle

Key Idea.

Section 1

A Web of Pathways

Key Idea

The rock cycle is not a predictable, circular loop; it acts more like a complex web of possibilities. Rocks do not follow a set itinerary.

Plate motion is the driver that determines the path. An igneous rock might remain on the surface and erode into sediment, or it could be buried immediately and melt again. The path a rock takes depends entirely on how the plates move it.

Section 2

Continuous Recycling

Key Idea

Earth operates as a dynamic, recycling system. For billions of years, the planet has been reprocessing the same crustal material.

If a rock is pushed up, it becomes sediment; if it is pushed down, it becomes magma. This continuous transformation, fueled by the interplay of sunlight and internal heat, ensures that Earth's surface is constantly changing and renewing itself.

Book overview

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Chapter 3: Movement of Rock Formations

  1. Lesson 1

    Lesson 1: Plate Motion and Vertical Movement

  2. Lesson 2

    Lesson 2: Uplift and Weathering

  3. Lesson 3

    Lesson 3: Subduction and Melting

  4. Lesson 4Current

    Lesson 4: The Rock Cycle

Lesson overview

Expand to review the lesson summary and core properties.

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Section 1

A Web of Pathways

Key Idea

The rock cycle is not a predictable, circular loop; it acts more like a complex web of possibilities. Rocks do not follow a set itinerary.

Plate motion is the driver that determines the path. An igneous rock might remain on the surface and erode into sediment, or it could be buried immediately and melt again. The path a rock takes depends entirely on how the plates move it.

Section 2

Continuous Recycling

Key Idea

Earth operates as a dynamic, recycling system. For billions of years, the planet has been reprocessing the same crustal material.

If a rock is pushed up, it becomes sediment; if it is pushed down, it becomes magma. This continuous transformation, fueled by the interplay of sunlight and internal heat, ensures that Earth's surface is constantly changing and renewing itself.

Book overview

Jump across lessons in the current chapter without opening the full course modal.

Continue this chapter

Chapter 3: Movement of Rock Formations

  1. Lesson 1

    Lesson 1: Plate Motion and Vertical Movement

  2. Lesson 2

    Lesson 2: Uplift and Weathering

  3. Lesson 3

    Lesson 3: Subduction and Melting

  4. Lesson 4Current

    Lesson 4: The Rock Cycle