Chapter 4 Section 2 Igneous Rock

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What is Igneous Rock?

 Igneous rock forms when hot, liquid rock, or magma, cools and solidifies.

 The type of igneous rock that forms depends on the composition of the magma and the amount of time it takes the magma to cool.

Origins of Igneous Rock

 Igneous rock begins as magma.

 There are three ways magma can form:

 when rock is heated

 when pressure is released

 when rock changes composition.

Think about it!

 Which of the following are ways magma is formed?

 A. By compaction and cementation

 B. By melting and cooling

 C. By changes in composition

 D. By weathering and erosion

Magma can Solidify

 When magma cools enough, it solidifies to form igneous rock.

 Magma solidifies in much the same way that water freezes.

 Magma contain many different types of minerals, some minerals in the magma will freeze or become solid before other minerals do.

Composition and Texture

 Let’s look at the rocks in Figure 2.

 All of the rocks are igneous rocks even though they look different from one another.

 These rocks differ from one another in what they are made of and how fast they cooled.

Composition Continued

 The light-colored rocks are less dense than the darkcolored rocks are.

 The light-colored rocks are rich in elements such as aluminum, potassium, silicon, and sodium.

 These rocks are called felsic rocks. The dark-colored rocks, called mafic rocks, are rich in calcium, iron, and magnesium, and poor in silicon.

Figure 3 shows what happens to magma when it cools at different rates.

 The longer it takes for the magma or lava to cool, the more time mineral crystals have to grow.

 The more time the crystals have to grow, the larger the crystals are and the coarser the texture of the resulting igneous rock is

Think about it!

 What kind of texture does igneous rock have when magma cools slowly?

 A. Coarse-grained

 B. Large-grained

 C. Fine-grained

 D. Medium-grained

Figure 3 should us what?

 determines the texture of igneous rock.

 The less time magma takes to cool, the less time crystals have to grow. Therefore, the rock that is formed will be fine grained.

Think about it!

 What kind of texture does igneous rock have when magma cools rapidly?

 A. Coarse-grained

 B. Medium-grained

 C. Fine-grained

 D. Large-grained

Igneous Rock Formations

Above and Below the

 Igneous rock formations are located above and below the surface of the Earth.

 You may be familiar with igneous rock formations that were caused by lava cooling on the Earth’s surface, such as volcanoes.

 But not all magma reaches the surface. Some magma cools and solidifies deep within the Earth’s crust

Intrusive Igneous Rock

 When magma intrudes, or pushes, into surrounding rock below the Earth’s surface and cools, the rock that forms is called intrusive igneous rock.

 Intrusive igneous rock usually has a coarsegrained texture because it is well insulated by surrounding rock and cools very slowly. The minerals that form are large, visible crystals.

Extrusive Igneous Rock

 Igneous rock that forms from magma that erupts, or extrudes, onto the Earth’s surface is called extrusive igneous rock.

 Extrusive rock is common around volcanoes. It cools quickly on the surface and contains very small crystals or no crystals.

Think about it!

 What kind of rock is formed when magma intrudes into other rock?

 A. Extrusive igneous rock

 B. Sedimentary rock

 C. Intrusive igneous rock

 D. Organic sedimentary rock

Think about it!

 What kind of rock is formed from lava that cools on the Earth’s surface?

 A. Organic sedimentary rock

 B. Sedimentary rock

 C. Intrusive igneous rock

 D. Extrusive igneous rock

Section Summary

 Igneous rock forms when magma cools and hardens.

 The texture of igneous rock is determined by the rate at which the rock cools.

 Igneous rock that solidifies at Earth’s surface is extrusive. Igneous rock that solidifies within Earth’s surface is intrusive.

 Shapes of common igneous intrusive bodies include batholiths, stocks, sills, and dikes.

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