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What is Magma?

Magma beneath Earth's surface
Magma forms deep beneath Earth's surface where temperatures are extremely high

Magma is extremely hot, molten rock found beneath Earth's surface. It forms when rocks in the Earth's mantle or crust melt due to intense heat and pressure. Magma is so hot that it can reach temperatures between 700°C and 1300°C (1300°F to 2400°F)!

Magma is made of three main components:
Liquid rock (melted minerals)
Solid crystals (minerals that haven't melted)
Dissolved gases (like water vapor, carbon dioxide, and sulfur)

This molten rock collects in areas called magma chambers beneath volcanoes. When pressure builds up, magma can erupt onto Earth's surface through volcanic vents.

Magma vs Lava: What's the Difference?

Magma vs Lava comparison
Magma becomes lava when it reaches Earth's surface

While magma and lava are both molten rock, they have one important difference based on their location:

Magma is molten rock that is still beneath Earth's surface. It's stored in magma chambers and hasn't reached the open air.

Lava is what we call magma after it erupts from a volcano and reaches Earth's surface. Once magma is exposed to air, it becomes lava.

When lava cools and hardens, it forms igneous rocks like basalt, granite, and obsidian. These rocks help scientists understand Earth's geological history.

1

Magma Formation

Rocks melt deep underground

2

Magma Chamber

Molten rock collects below surface

3

Volcanic Eruption

Pressure forces magma upward

4

Lava Flow

Magma reaches surface as lava

5

Cooling

Lava cools to form igneous rock

How Magma Forms

Magma formation process
Magma forms through melting of rocks in Earth's mantle and crust

Magma forms deep beneath Earth's surface through three main processes:

Temperature Increase

Heat from Earth's core melts rocks as they go deeper

Pressure Release

When pressure decreases, rocks melt at lower temperatures

Water Addition

Water lowers melting point of rocks, causing them to melt

Most magma forms at tectonic plate boundaries:

Divergent boundaries: Where plates pull apart, pressure decreases allowing melting
Convergent boundaries: Where plates collide, water released causes melting
Hot spots: Extra-hot areas in the mantle melt rock directly

The composition of magma depends on the type of rocks that melted to create it and how much they melted.

Magma Composition and Types

Different types of magma
Different types of magma have different compositions and properties

Scientists classify magma into three main types based on their silica content and temperature:

Type Silica Content Temperature Characteristics
Basaltic Low (45-55%) Very Hot (1000-1200°C) Thin, flows easily, forms shield volcanoes
Andesitic Medium (55-65%) Hot (800-1000°C) Medium thickness, moderately explosive
Rhyolitic High (65-75%) Cooler (700-900°C) Thick, very explosive, forms calderas

The amount of silica (a compound of silicon and oxygen) in magma affects its:

Viscosity (how thick and sticky it is)
Explosiveness (how violently it erupts)
Temperature (how hot it is)
Color when it cools into rock

Magma with high silica content is thicker and traps more gas, leading to more explosive eruptions!

Magma Quiz

Test your magma knowledge with this quiz! Answer all 5 questions to see how much you've learned.

1. What is the main difference between magma and lava?
2. Where is magma stored beneath a volcano?
3. Which type of magma has the highest silica content?
4. What is the approximate temperature range of magma?
5. What causes rocks to melt and form magma?

Frequently Asked Questions

Here are answers to some common questions about magma:

Magma Trivia

Discover some amazing facts about magma!

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