Magma is the hot, gooey rock formed from melted minerals and gases deep inside the Earth, which creates all igneous rocks when it cools and solidifies.
Overview
Magma Chambers
Magma Vs Lava
Types Of Magma
Formation Of Magma
Composition Of Magma
Magma Differentiation
The Role Of Gases In Magma
Volcanic Eruptions And Magma
Magma Movement And Convection
Historical Impact Of Magma On Earth
Volcanic Eruption
Mount St. Helens
Hawaiian Islands
Carbon Dioxide
Mount Vesuvius
Temperature
Subduction
Convection
Pressure
Crystal
Planet
๐ Magma is formed deep inside the Earth when rocks melt from extreme heat and pressure.
๐ฒ Magma is like a soup made of molten rock, minerals, gases, and sometimes crystals.
๐งช There are four main types of magma: basaltic, andesitic, dacitic, and rhyolitic.
๐ฅ Magma can reach extremely high temperatures, often exceeding 1,200ยฐC (2,192ยฐF).
๐ค Once magma reaches the Earth's surface, it becomes lava!
๐ Volcanic eruptions happen when magma pushes through cracks in the Earth's crust.
๐ชจ Magma differentiation helps scientists understand how different rocks are formed.
๐ฌ๏ธ Gases in magma can cause it to be more explosive when it erupts.
๐ Magma moves around in a magma chamber through a process called convection.
๐ Magma has played a crucial role in shaping many of Earth's landscapes and mountains.
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