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

Lesson 1: Plate Motion and Vertical Movement

Key Idea.

Section 1

The Global Conveyor Belt

Key Idea

Rocks possess no ability to move themselves; they are passive passengers on Earth's mobile crust. Plate motion functions as a planetary conveyor belt, slowly transporting massive rock formations across the globe.

This horizontal movement is the fundamental engine of geological change. Without moving plates, rock formed in the ocean would stay in the ocean, and rock formed deep underground would never see the light of day. The cycle depends entirely on this continuous transport system.

Section 2

Vertical Force

Key Idea

While plates drift horizontally, their collisions generate powerful vertical forces. When massive slabs of rock crash together, they cannot simply occupy the same space; the rock is forced either upward or downward.

This mechanical action creates two distinct directions for rock travel: uplift (pushing toward the surface) and subduction (pulling toward the core). Before a rock can transform, it must first be moved physically into a new position by these immense tectonic forces.

Book overview

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Chapter 3: Movement of Rock Formations

  1. Lesson 1Current

    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 4

    Lesson 4: The Rock Cycle

Lesson overview

Expand to review the lesson summary and core properties.

Expand

Section 1

The Global Conveyor Belt

Key Idea

Rocks possess no ability to move themselves; they are passive passengers on Earth's mobile crust. Plate motion functions as a planetary conveyor belt, slowly transporting massive rock formations across the globe.

This horizontal movement is the fundamental engine of geological change. Without moving plates, rock formed in the ocean would stay in the ocean, and rock formed deep underground would never see the light of day. The cycle depends entirely on this continuous transport system.

Section 2

Vertical Force

Key Idea

While plates drift horizontally, their collisions generate powerful vertical forces. When massive slabs of rock crash together, they cannot simply occupy the same space; the rock is forced either upward or downward.

This mechanical action creates two distinct directions for rock travel: uplift (pushing toward the surface) and subduction (pulling toward the core). Before a rock can transform, it must first be moved physically into a new position by these immense tectonic forces.

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 1Current

    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 4

    Lesson 4: The Rock Cycle