Survey
* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
Download Chapter 4 Section 2 Igneous Rock
Document related concepts
Transcript
Mrs. Hutson 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. B. C. D. By compaction and cementation By melting and cooling By changes in composition 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 of Igneous Rock 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. B. C. D. Coarse-grained Large-grained Fine-grained Medium-grained Figure 3 should us what? The amount of time it takes for magma or lava to cool 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. B. C. D. Coarse-grained Medium-grained Fine-grained Large-grained Igneous Rock Formations Above and Below the Earth’s Surface 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. B. C. D. Extrusive igneous rock Sedimentary rock Intrusive igneous rock Organic sedimentary rock Think about it! What kind of rock is formed from lava that cools on the Earth’s surface? A. B. C. D. Organic sedimentary rock Sedimentary rock Intrusive igneous rock 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.
