1 / 23

Chapter 3: Rocks

Table of Contents. Chapter 3: Rocks. Section 2: Igneous Rocks. Igneous Rocks. A. Formation of Igneous Rocks. 1. When some volcanoes erupt, they eject a flow of molten rock material. 2. Molten rock material, called magma, flows when it is hot and becomes solid when it cools.

yut
Download Presentation

Chapter 3: Rocks

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Table of Contents Chapter 3: Rocks Section 2: Igneous Rocks

  2. Igneous Rocks A. Formation of Igneous Rocks 1. When some volcanoes erupt, they eject a flow of molten rock material. 2. Molten rock material, called magma, flows when it is hot and becomes solid when it cools. 3. When hot magma cools and hardens, it forms igneous(IHG nee us) rock.

  3. Igneous Rocks B. Magma 1. Most magmas come from deep below Earth’s surface. Magma is located at depths ranging from near the surface to about 150 km below the surface. 2. Temperatures of magmas range from about 650° to 1,200° C (1202° to 2192° F) depending on their chemical compositions and pressures exerted on them.

  4. Igneous Rocks B. Magma 3. The heat that melts rocks comes from sources within Earth’s interior. 4. One source is the decay of radioactive elements within Earth. 5. Some heat is left over from the formation of the planet, which originally was molten. 6. Radioactive decay of elements contained in rocks balances some heat loss as Earth continues to cool.

  5. Igneous Rocks B. Magma 7. Because magma is less dense than surrounding solid rock, it is forced upward toward the surface. 8. When magma reaches Earth’s surface and flows from volcanoes, it is called lava.

  6. Igneous Rocks C. Intrusive Rocks 1. As magma cools, atoms and compounds in the liquid rearrange themselves into new crystals called mineral grains. 2. Rocks form as these mineral grains grow together. 3. Rocks that form from magma below the surface are called intrusiveigneous rocks.

  7. Igneous Rocks D. Extrusive Rocks 1. Extrusive igneous rocks are formed as lava cools on the surface of Earth. 2. When lava flows on the surface, it is exposed to air and water, and cools quickly under these conditions.

  8. Igneous Rocks D. Extrusive Rocks 3. The quick cooling rate keeps mineral grains from growing large, because the atoms in the liquid don’t have the time to arrange into large crystals.

  9. Igneous Rocks E. Volcanic Glass 1. Pumice, obsidian, and scoria are examples of volcanic glass. 2. These rocks cooled so quickly that few or no mineral grains formed. 3. Most of the atoms in these rocks are not arranged in orderly patterns, and few crystals are present.

  10. Igneous Rocks E. Volcanic Glass 4. In the case of pumice and scoria, gases become trapped in the gooey molten material as it cools. 5. Holes are left behind where the rock formed around the pockets of gas.

  11. Igneous Rocks F. Classifying Igneous Rocks 1. Igneous rocks are intrusive or extrusive depending on how they are formed. 2. A way to further classify these rocks is by the magma from which they form. An igneous rock can form from basaltic, andesitic, or granitic magma.

  12. Igneous Rocks F. Classifying Igneous Rocks 3. The type of magma that cools to form an igneous rock determines important chemical and physical properties of that rock. 4. These include mineral composition, density, color, and melting temperature.

  13. Igneous Rocks G. Basaltic Rocks 1..Basaltic(buh SAWL tihk) igneous rocks are dense, dark-colored rocks. 2. They form from magma that is rich in iron and magnesium and poor in silica, which is the compound SiO2. 3. The presence of iron and magnesium in minerals in basalt gives basalt its dark color. 4. Basaltic lava is fluid and flows freely from volcanoes in Hawaii, such as Kilauea.

  14. Igneous Rocks H. Granitic Rocks 1. Granitic igneous rocks are light-colored rocks of lower density than basaltic rocks. 2. Granitic magma is thick and stiff and contains lots of silica but lesser amounts of iron and magnesium.

  15. Igneous Rocks I. Andesitic Rocks • Andesitic igneous rocks have mineral compositions between those of basaltic and granitic rocks. • Many volcanoes around the rim of the Pacific Ocean formed from andesitic magmas. • Like volcanoes that erupt granitic magma, these volcanoes also can erupt violently.

  16. Section Check Question 1 Igneous rock is formed by __________. A. cooling of hot magma B. change in pressure C. compression of loose materials D. pressure from watery fluids

  17. Section Check Question 2 What is the difference between intrusive and extrusive igneous rock?

  18. Section Check Question 3 Which of the following is a volcanic rock that contained trapped gases during its formation? A. marble B. pumice C. sandstone D. slate

  19. Section Check Q 1. Answer The answer is A. If igneous rock is melted, it changes to magma.

  20. Section Check Q 2. Answer Intrusive igneous rocks form from magma below Earth’s surface. Extrusive igneous rocks form from lava flowing at Earth’s surface.

  21. Section Check Q. 3 Answer The answer is B. Pumice is a low density igneous rock formed when molten material containing trapped gases cools and hardens.

  22. End of Chapter Summary File

More Related