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THE EARTH ROCKS!!! Chapter 3- Section 1 Rocks Turn to page 58 Please take notes on yellow slides! What is a rock? You may be walking along and find an interesting rock. You pick it up and notice that it contains many different particles or crystals. Some of the particles may reflect light and others may be dull. The sparkles or crystals you see are actually individual minerals. For example, if you were to take a close look at the rock, granite, you would see crystals of feldspar, hornblende, mica, quartz and other minerals. Rocks – a mixture of minerals, rock fragments, volcanic glass, organic matter, or other natural materials. This is a granite rock There are many uses of granite! Carved into the Black Hills of South Dakota are the iconic faces of four former presidents of the United States--George Washington, Thomas Jefferson, Theodore Roosevelt, and Abraham Lincoln. These men were chosen to represent the first 150 years of American history and America’s cultural heritage. The idea came from Doane Robinson to promote tourism in South Dakota and his idea was wildly successful-the park attracts almost 3 million park visitors every year. This is granite! Chew on this… Many of us have rock collections OR some interesting rocks that we have found. Because we are fortunate to live by Lake Michigan, we can get cool rocks just by walking down the beach. Discuss with your partner a cool rock you may own OR perhaps a rock collection that you have. Chapter 3 – Section 1 Rocks Rock – a mixture of minerals, rock fragments, volcanic glass, organic matter, or other natural materials All rocks are made of 2 or more minerals, but minerals are not made of rocks. MINERALS A mineral is the same all the way through. That is one reason we speak of a sample or a specimen rather than a rock. There are about 4000 known minerals on earth. All rocks are made up of 2 or more of these minerals. Rocks are in a cycle… This means they continually are changing into different types of rock. The rock cycle is the process that creates and changes rock. The rock cycle shows the three types of rocks – igneous, metamorphic, and sedimentary The Rock Cycle Rock cycle – the process that creates and changes rock. Rock Cycle – the process that creates and changes rock Sedimentary Rock is . . . Rock formed when layers of small particles of shell, rock, and sand join together. Metamorphic Rock is . . . Rock that is formed when pressure and heat create changes to sedimentary or igneous rock. Igneous Rock is . . . Rock that is formed when melted rock cools and hardens. Three types of rocks Igneous Sedimentary Metamorphic Yes, over time limestone can change into gneiss which can change into granite…. See rock cycle on pg. 59 Notice that rocks change through many processes. Heat, pressure, melting, cooling, weathering/eroding, compaction and cementation On page 59 notice…. This diagram looks different than the others in this powerpoint. You must always carefully look at the rock cycle diagram being used… they are not all the same. Each type of rock can be in a different spot so you need to look carefully and read what the arrows are saying! On page 59 which type of rock is at the top? sedimentary In this diagram notice where sedimentary is..yes, at the bottom, not the top like on page 59! Here’s a short movie about the rock cycle… Why do rocks change into different types of rock? Many reasons such as Heat Pressure Melting Cooling Weathering Eroding Compaction/cementation Ex: Sedimentary rocks can change when heat and pressure are added to make a metamorphic rock Ex: Metamorphic rocks can melt and cool to form igneous rocks Ex: Igneous rocks can be broken into fragments (weathering/erosion) to form sedimentary rocks Use the chart AND get with your partner and discuss… 1. Explain how and igneous rock can change into a metamorphic rock 2. Explain how a sedimentary rock can change into an igneous 3. Explain how a metamorphic rock can change into a sedimentary rock Rocks become bigger . . . , and bigger, and bigger, and bigger By earthquakes By volcanoes By heat and pressure Rocks become smaller, and smaller, and smaller, and ... smaller By erosion By wind By earthquake By floods By rain By slides By man Some processes that change rock: Heat/pressure Weathering/eroding Compaction/cemention Cooling Melting Matter and the Rock Cycle Rocks will weather and erode and wind, water, or ice can carry away these particles. These particles are not lost or destroyed – the particles are just redistributed in other forms. Conservation of matter – the rock cycle never destroys elements of rocks but merely redistributes them. So matter is never created or destroyed. Conservation Of Matter – the rock cycle never destroys elements of rocks but merely redistributes them Matter is never created nor destroyed James Hutton is known as the father of modern geology. Geology is the study of the earths rocks and minerals. He was a Scottish physician who first noticed in 1788 that rocks undergo profound changes. He noticed that layers of rock in Siccar Point in Scotland had been altered since their formation. He noticed that some of the layers were tilted and partly eroded and not in nice layers like they once were. However, the younger rocks above them were nearly horizontal like the older rocks once were. This is a picture of Siccar Point! James Hutton, a Scottish physician, first noticed in 1788 that rocks go through changes As a general rule.. Oldest rock is at the bottom…IF IT IS AN UNDISTURBED SEQUENCE OF ROCK… Here’s a short a video about the law of conservation of matter…. Rock Words: There are many common names for rocks and the usually give you an idea of how big the rock is. Here are a few: mountain - huge, giant hunk of rock that is still attached to the earth's crust, doesn't move, tall boulder - large, taller than a person rock - large, you could get your arms around it or a bit smaller but it is usually jagged, broken off a bigger piece of rock river rock - round rocks that are along the edge & at the bottom of fast-flowing rivers stone - medium, you could hold it in two hands pebble - small, you can hold it with two fingers, could get stuck in your shoe, usually rounded