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

Lesson 3: Subduction and Melting

Key Idea.

Section 1

The Downward Journey

Key Idea

While uplift pushes rock into the air, subduction drags it into the abyss. This process occurs when a dense oceanic plate slides beneath another plate, carrying its cargo of rocks deep into the mantle.

This is the Earth's mechanism for burial. It effectively removes rock from the cool, low-energy surface environment and forces it down into the high-energy regime of Earth's interior.

Section 2

Transformation by Heat

Key Idea

Depth equals heat. As rock descends further during subduction, it absorbs increasing amounts of thermal energy from the surrounding mantle.

Eventually, the temperature overwhelms the rock's solid structure, causing a phase change. The solid rock melts into liquid magma. This completes the loop: material that once existed as cold sediment on the ocean floor is returned to a molten state, ready to begin the cycle again.

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 3Current

    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 Downward Journey

Key Idea

While uplift pushes rock into the air, subduction drags it into the abyss. This process occurs when a dense oceanic plate slides beneath another plate, carrying its cargo of rocks deep into the mantle.

This is the Earth's mechanism for burial. It effectively removes rock from the cool, low-energy surface environment and forces it down into the high-energy regime of Earth's interior.

Section 2

Transformation by Heat

Key Idea

Depth equals heat. As rock descends further during subduction, it absorbs increasing amounts of thermal energy from the surrounding mantle.

Eventually, the temperature overwhelms the rock's solid structure, causing a phase change. The solid rock melts into liquid magma. This completes the loop: material that once existed as cold sediment on the ocean floor is returned to a molten state, ready to begin the cycle again.

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 3Current

    Lesson 3: Subduction and Melting

  4. Lesson 4

    Lesson 4: The Rock Cycle