Learn on PengiAmplify Science (California) Grade 7Chapter 2: Sediment and Magma

Lesson 3: Conservation of Matter

Key Idea.

Section 1

Matter is Conserved

Key Idea

Through all geological changes—melting, weathering, or cooling—the total amount of matter remains constant. This is the Law of Conservation of Matter.

A granite mountain may break down into millions of sand grains, but the total mass of the sand equals the mass of the mountain. Rock material is never destroyed or created; it only changes its physical form and location.

Section 2

Energy Drives Change

Key Idea

Rock material changes form because energy flows through it. The rock cycle is essentially a system where matter is moved and altered by energy.

Exposure to solar energy causes rock to break into sediment, while exposure to Earth's interior energy causes rock to melt into magma. Identifying the active energy source allows scientists to explain why a rock transformed.

Book overview

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Chapter 2: Sediment and Magma

  1. Lesson 1

    Lesson 1: Sources of Sediment

  2. Lesson 2

    Lesson 2: Sources of Magma

  3. Lesson 3Current

    Lesson 3: Conservation of Matter

  4. Lesson 4

    Lesson 4: Regional Geology

Lesson overview

Expand to review the lesson summary and core properties.

Expand

Section 1

Matter is Conserved

Key Idea

Through all geological changes—melting, weathering, or cooling—the total amount of matter remains constant. This is the Law of Conservation of Matter.

A granite mountain may break down into millions of sand grains, but the total mass of the sand equals the mass of the mountain. Rock material is never destroyed or created; it only changes its physical form and location.

Section 2

Energy Drives Change

Key Idea

Rock material changes form because energy flows through it. The rock cycle is essentially a system where matter is moved and altered by energy.

Exposure to solar energy causes rock to break into sediment, while exposure to Earth's interior energy causes rock to melt into magma. Identifying the active energy source allows scientists to explain why a rock transformed.

Book overview

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

Continue this chapter

Chapter 2: Sediment and Magma

  1. Lesson 1

    Lesson 1: Sources of Sediment

  2. Lesson 2

    Lesson 2: Sources of Magma

  3. Lesson 3Current

    Lesson 3: Conservation of Matter

  4. Lesson 4

    Lesson 4: Regional Geology