2Chapter: Rocks and Minerals Table of ContentsChapter: Rocks and MineralsSection 1: Minerals—Earth’s JewelsSection 2: Igneous and Sedimentary RocksSection 3: Metamorphic Rocks and the Rock Cycle
3What is a mineral?— Minerals Defined Minerals—Earth’s Jewels1What is a mineral?— Minerals DefinedMinerals are inorganic, solid materials found in nature. Inorganic means they usually are not formed by plants or animals.X-ray patterns of a mineral show an orderly arrangement of atoms that looks something like a garden trellis.
4What is a mineral?— Minerals Defined Minerals—Earth’s Jewels1What is a mineral?— Minerals DefinedThe particular chemical makeup and arrangement of the atoms in the crystal is unique to each mineral.Rocks usually are made of two or more minerals.Each mineral has unique characteristics you can use to identify it.
5Minerals—Earth’s Jewels 1How do minerals form?Minerals form in several ways. One way is from melted rock material inside Earth called magma.As magma cools, atoms combine in orderly patterns to form minerals.
6How do minerals form? 1 Evaporation can form minerals. Minerals—Earth’s Jewels1How do minerals form?Evaporation can form minerals.Just as salt crystals appear when seawater evaporates, other dissolved minerals, such as gypsum, can crystallize.
7Minerals—Earth’s Jewels 1How do minerals form?A process called precipitation (prih sih puh TAY shun) can form minerals, too.Water can hold only so much dissolved material. Any extra separates and falls out as a solid.
8Minerals—Earth’s Jewels 1Formation CluesLarge mineral grains that fit together like a puzzle seem to show up in rocks formed from slow-cooling magma.
9Minerals—Earth’s Jewels 1Formation CluesIf you see large, perfectly formed crystals, it means the mineral had plenty of space in which to grow.This is a sign they may have formed in open pockets within the rock.
10Properties of Minerals Minerals—Earth’s Jewels1Properties of MineralsEach mineral has a set of physical properties that can be used to identify it.Most common minerals can be identified with items you have around the house and can carry in your pocket, such as a penny or a steel file.
11Crystals 1 All minerals have an orderly pattern of atoms. Minerals—Earth’s Jewels1CrystalsAll minerals have an orderly pattern of atoms.The atoms making up the mineral are arranged in a repeating pattern.Solid materials that have such a pattern of atoms are called crystals.
12Minerals—Earth’s Jewels 1Cleavage and FractureMinerals that split into pieces with smooth, regular planes that reflect light are said to have cleavage (KLEE vihj).Cleavage is caused by weaknesses within the arrangement of atoms that make up the mineral.
13Minerals—Earth’s Jewels 1Cleavage and FractureNot all minerals have cleavage. Some break into pieces with jagged or rough edges.Materials that break this way, such as quartz, have what is called fracture (FRAK chur).
14Minerals—Earth’s Jewels 1ColorSometimes a mineral’s color can help you figure out what it is. But color also can fool you.The common mineral pyrite (PI rite) has a shiny, gold color similar to real gold.Because of this, pyrite also is called fool’s gold.
15Minerals—Earth’s Jewels 1Streak and LusterScraping a mineral sample across an unglazed, white tile, called a streak plate, produces a streak of color.
16Minerals—Earth’s Jewels 1Streak and LusterThe streak is not necessarily the same color as the mineral itself. This streak of powdered mineral is more useful for identification than the mineral’s color.
17Minerals—Earth’s Jewels 1Streak and LusterLuster describes how light reflects from a mineral’s surface.If it shines like a metal, the mineral has metallic (muh TA lihk) luster.Nonmetallic minerals can be described as having pearly, glassy, dull, or earthy luster.
18Minerals—Earth’s Jewels 1HardnessFriedrich Mohs developed a way to classify minerals by their hardness.The Mohs scale classifies minerals from 1 (softest) to 10 (hardest).
19Minerals—Earth’s Jewels 1HardnessYou can determine hardness by trying to scratch one mineral with another to see which is harder.
20Minerals—Earth’s Jewels 1Specific GravitySpecific gravity compares the weight of a mineral with the weight of an equal volume of water.Pyrite—or fool’s gold—is about five times heavier than water. Pure gold is more than 19 times heavier than water.Measuring specific gravity is another way you can identify minerals.
21Other Properties 1 The mineral magnetite will attract a magnet. Minerals—Earth’s Jewels1Other PropertiesThe mineral magnetite will attract a magnet.The mineral calcite has two unusual properties. It will fizz when it comes into contact with an acid like dilute HCl.Also, if you look through a clear calcite crystal, you will see a double image.
22Minerals—Earth’s Jewels 1Common MineralsOnly a small number of the more than 4,000 minerals make up most rocks.Most of the rock-forming mineralsare silicates (SIH luh kaytz), which contain the elements silicon and oxygen.
23Minerals—Earth’s Jewels 1Common MineralsMore than half of the minerals in Earth’s crust are types of a silicate mineral called feldspar.
24Minerals—Earth’s Jewels 1Common MineralsOther important rock-forming minerals are carbonates.The carbonate mineral calcite makes up most of the common rock limestone.
25Minerals—Earth’s Jewels 1GemsGems are minerals that are rare and can be cut and polished, giving them a beautiful appearance.To be gem quality, most minerals must be clear with few or no blemishes or cracks.A gem also must have a beautiful luster or color.
26Minerals—Earth’s Jewels 1The Making of a GemOne reason why gems are so rare is that they are formed under special conditions.Diamond, for instance, is a form of the element carbon.Scientists suggest that diamond forms deep in Earth’s mantle. It takes a certain kind of volcanic eruption to bring a diamond close to Earth’s surface, where miners can find it.
27Minerals—Earth’s Jewels 1OresA mineral is called an ore if it contains enough of a useful substance that it can be sold for a profit.The iron used to make steel comes from the mineral hematite, lead for batteries is produced from galena, and the magnesium used in vitamins comes from dolomite.Ores of these useful metals must be extracted from Earth in a process called mining.
28Minerals—Earth’s Jewels 1Ore ProcessingAfter an ore has been mined, it must be processed to extract the desired mineral or element.Smelting melts the ore and thenseparates and removes most of the unwanted materials.
29Minerals—Earth’s Jewels 1Ore ProcessingAfter this smelting process, it can be refined, which means that it is purified.
30Question 1 Answer 1 What does inorganic mean? Section Check1Question 1What does inorganic mean?AnswerInorganic means not formed by plants or animals.NC: 3.04
31Section Check1Question 2List some places you might find minerals in your home.AnswerYou can find minerals in salt shakers, pencils, glasses, and ceramic dishes.NC: 3.04
32Question 3 Answer 1 Explain the difference between a rock and a gem. Section Check1Question 3Explain the difference between a rock and a gem.AnswerGems are rare minerals that can be cut and polished. They have a beautiful color and lack cracks or blemishes. Rocks are often cloudy and when they are cut, they crack.NC: 3.04
33Igneous and Sedimentary Rocks 2Igneous RockIgneous (IHG nee us) rocks form when melted rock material from inside Earth cools.When melted rock material cools on Earth’s surface, it makes an extrusive (ehk STREW sihv) igneous rock.When the melt cools below Earth’s surface, intrusive (ihn TREW sihv) igneous rock forms.
34Igneous and Sedimentary Rocks 2Chemical CompositionThe chemicals in the melted rock material determine the color of the resulting rock.If it contains a high percentageof silica and little iron, magnesium, or calcium, the rock generally will be light in color.
35Igneous and Sedimentary Rocks 2Chemical CompositionLight-colored igneous rocks are called granitic (gra NIH tihk) rocks.
36Igneous and Sedimentary Rocks 2Chemical CompositionIf the silica content is far less, but it contains more iron, magnesium, or calcium, a dark-colored or basaltic (buh SAWL tihk) rock will result.Intrusive igneous rocks often are granitic, and extrusive igneous rocks often are basaltic.
37Igneous and Sedimentary Rocks 2Rocks from LavaExtrusive igneous rocks form when melted rock material cools on Earth’s surface.
38Igneous and Sedimentary Rocks 2Rocks from LavaWhen the melt reaches Earth’s surface, it is called lava.
39Igneous and Sedimentary Rocks 2Rocks from LavaLava cools quickly before large mineral crystals have time to form.
40Rocks from Lava 2 Extrusive igneous rocks can form in two ways. Igneous and Sedimentary Rocks2Rocks from LavaExtrusive igneous rocks can form in two ways.
41Igneous and Sedimentary Rocks 2Rocks from LavaIn one way, volcanoes erupt and shoot out lava and ash.
42Igneous and Sedimentary Rocks 2Rocks from LavaAlso, large cracks in Earth’s crust, called fissures (FIH shurz), can open up.
43Igneous and Sedimentary Rocks 2Rocks from LavaOozing lava from a fissure or a volcano is called a lava flow.The fastest cooling lava forms no grains at all. This is how obsidian, a type of volcanic glass, forms.
44Igneous and Sedimentary Rocks 2Rocks from MagmaIntrusive igneous rocks are produced when magma cools below the surface of Earth.
45Igneous and Sedimentary Rocks 2Rocks from MagmaIntrusive igneous rocks form when a huge glob of magma from inside Earth is forced upward toward the surface but never reaches it.
46Igneous and Sedimentary Rocks 2Rocks from MagmaIntrusive igneous rocks generally have large crystals that are easy to see.Some extrusive igneous rocks do not have large crystals that you can see easily.Others are a mixture of small crystals and larger, visible crystals.
47Igneous and Sedimentary Rocks 2Sedimentary RocksPieces of broken rock, shells, mineral grains, and other materials make up what is called sediment (SE duh munt).Sediment can collect in layers to form rocks. These are called sedimentary (sed uh MEN tuh ree) rocks.
48Igneous and Sedimentary Rocks 2Sedimentary RocksWhen sediment is dropped, or deposited, by wind, ice, gravity, or water, it collects in layers.After sediment is deposited, it begins the long process of becoming rock.Most sedimentary rocks take thousands to millions of years to form.
49Igneous and Sedimentary Rocks 2Detrital RocksDetrital rocks are made of grains of minerals or other rocks that have moved and been deposited in layers by water, ice, gravity, or wind.Other minerals dissolved in water act to cement these particles together.
50Identifying Detrital Rocks Igneous and Sedimentary Rocks2Identifying Detrital RocksTo identify a detrital sedimentary rock, you use the size of the grains that make up the rock.
51Identifying Detrital Rocks Igneous and Sedimentary Rocks2Identifying Detrital RocksThe smallest, clay-sized grains feel slippery when wet and make up a rock called shale.Silt-sized grains make up the rougher-feeling siltstone.
52Identifying Detrital Rocks Igneous and Sedimentary Rocks2Identifying Detrital RocksSandstone is made of yet larger, sand-sized grains.Pebbles mixed and cemented together with other sedimentup rocks calledmakeconglomerates (kun GLAHM ruts).sandstone
53Igneous and Sedimentary Rocks 2Chemical RocksChemical sedimentary rock forms when mineral-rich water from geysers, hot springs, or salty lakes evaporates.As the water evaporates, layers of the minerals are left behind.Chemical rocks form from evaporation or other chemical processes.
54Igneous and Sedimentary Rocks 2Organic RocksChalk and coal are examples of the group of sedimentary rocks called organic rocks.Living matterdies, piles up, and then is compressed into rock.
55Igneous and Sedimentary Rocks 2Organic RocksIf the rock is produced from layers of plants piled on top of one another, it is called coal.
56Igneous and Sedimentary Rocks 2FossilsChalk and other types of fossiliferous limestone are made from the fossils of millions of tiny organisms.A fossil is the remains or trace of a once-living plant or animal.
57Section Check2Question 1What type of rock forms when melted rock material from inside Earth cools?A. igneousB. lavaC. oreD. sedimentaryNC: 3.04
58Section Check2AnswerThe correct answer is A. Igneous rock forms when melted rock, called magma, cools.NC: 3.04
59Question 2 Answer 2 What determines the color of igneous rock? Section Check2Question 2What determines the color of igneous rock?AnswerThe chemicals in the melted rock determine the color of igneous rock.NC: 3.04
60Question 3 2 The photo shows _______ rock. A. igneous B. metamorphic Section Check2Question 3The photo shows _______ rock.A. igneousB. metamorphicC. sedimentaryD. volcanicNC: 3.04
61Section Check2AnswerThe answer is C. Sedimentary rocks are formed by layers of different sediments over time.NC: 3.04
62Metamorphic Rocks and the Rock Cycle 3New Rock from Old RockMany physical changes on and within Earth are at work, constantly changing rocks.It can take millions of years for rock to change.Sometimes existing rocks are cooked when magma is forced upward into Earth’s crust, changing their mineral crystals.All these events can make new rocks out of old rocks.
63Metamorphic Rocks and the Rock Cycle 3Metamorphic RocksNew rocks that form when existing rocks are heated or squeezed but are not melted are called metamorphic (me tuh MOR fihk) rocks.
64Metamorphic Rocks 3 Granite can change to gneiss. Metamorphic Rocks and the Rock Cycle3Metamorphic RocksGranite can change to gneiss.The sedimentary rock sandstone can become quartzite, and limestone can change to marble.
65Metamorphic Rocks and the Rock Cycle 3Types of Changed RocksA physical characteristic helpful for classifying all rocks is the texture of the rocks.Texture differences in metamorphic rocks divide them into two main groups— foliated (FOH lee ay tud) and nonfoliated.
66Metamorphic Rocks and the Rock Cycle 3Types of Changed RocksFoliated rocks have visible layers or elongated grains of minerals.These minerals have been heated and squeezed into parallel layers, or leaves.Many foliated rocks have bands of different-colored minerals.
67Metamorphic Rocks and the Rock Cycle 3Types of Changed RocksNonfoliated rocks do not have distinct layers or bands.These rocks, such as quartzite, marble, and soapstone, often are more even in color than foliated rocks.
68Metamorphic Rocks and the Rock Cycle 3The Rock CycleScientists have created a model called the rock cycle to describe how different kinds of rock are related to one another and how rocks change from one type to another.Click image to view movie.
69Metamorphic Rocks and the Rock Cycle 3The Journey of a RockA blob of lava that oozes to the surface and cools forms an igneous rock.Wind, rain, and ice wear away at the rock, breaking off small pieces. These pieces are called sediment.
70Metamorphic Rocks and the Rock Cycle 3The Journey of a RockMineral-rich water seeps through the sediment and glues, or cements, it together. It becomes a sedimentary rock.Pressure and heat inside Earth can change it into a metamorphic rock.Metamorphic rock deep inside Earth can melt and begin the cycle again.
71Section Check3Question 1What type of rock results when an existing rock changes form?A. igneous rockB. metamorphic rockC. a mineralD. sedimentary rockNC: 3.04
72Section Check3AnswerThe answer is B. A metamorphic rock is formed when an existing rock is heated by Earth’s temperature or squeezed by intense pressure.NC: 3.04
73Section Check3Question 2Compare and contrast the two groups of metamorphic rocks.AnswerFoliated rocks have many layers. Nonfoliated rocks do not have layers and the individual mineral grains can be difficult to see.NC: 3.04
74Section Check3Question 3Would you expect to find a well-preserved artifact in a metamorphic rock such as quartzite? Explain.NC: 3.04
75Section Check3AnswerNo; quartzite is an example of a nonfoliated metamorphic rock. These rocks do not have distinct layers. Quartzite forms when quartz sand grains recrystallize during intense heating and pressure. An artifact would get destroyed during this process.NC: 3.04
76HelpTo advance to the next item or next page click on any of the following keys: mouse, space bar, enter, down or forward arrow.Click on this icon to return to the table of contentsClick on this icon to return to the previous slideClick on this icon to move to the next slideClick on this icon to open the resources file.Click on this icon to go to the end of the presentation.