IN OR OUT? IGNEOUS ROCKS

Summary:

Igneous rocks are formed by the cooling and hardening of melted rock material. Students will learn how rate of cooling affects what type of rock forms.

Instructional Method:

Game

Goal:

Students will be introduced to igneous rocks, how they form, what the different types are and how to identify them.

Objectives:

Students will be able to:

• Explain the difference between extrusive and intrusive rock.
• Classify igneous rocks based on texture.

Time:

30 minute setup
30 minute game and discussion

Materials Needed:

• String
• Scissors
• Paper punch
• Colored paper, poster board or paper and marker
• Printable rock cycle diagram

Vocabulary:

basalt	course-grained	crystal	extrusive
felsic	fine-grained	grain size	granite
igneous	intrusive	lava	mafic
magma	mineral	silica	texture
vesicles

Background:

The term igneous comes from the Latin ignis, meaning "fire". Igneous is used to describe rocks that crystallize out of hot molten material in the Earth called magma. When magma pushes up through Earth's crust to the surface, it is called lava. Both magma and lava cool and harden to form igneous rocks.

Intrusive vs. Extrusive
Igneous rocks can be classified into two main categories: intrusive and extrusive. A trick to help kids remember intrusive and extrusive is to think of intrusive -- inside and extrusive -- exit.

Intrusive rocks come from magma. They cool slowly deep in Earth's crust. When magma cools underground, the crust acts like a blanket, insulating it, keeping it warm longer. Because the magma cools slowly, crystals of different minerals have time to grow. The molecules in the magma have time to arrange themselves into crystal formations before the magma hardens. Intrusive rocks have large crystals that can be seen with the naked eye. A common example of an intrusive igneous rock is granite.

Extrusive igneous rocks come from lava. Lava, at the surface, is exposed to air and water which causes the molten rock to cool rapidly. Solidifying rocks at the surface cool too quickly for large crystals to form. Molecules in the lava do not have time to arrange themselves to form large crystals. Extrusive rocks have crystals that are too small to see without magnification. A common example of an extrusive igneous rock is basalt. Some extrusive rocks, such as obsidian and pumice, cool so rapidly that they completely lack crystal structure and are considered a volcanic glass. Pumice is just like obsidian except it is tiny shards of glass.

Texture
Within the two main categories of intrusive and extrusive, rock can be classified even further using texture and chemical composition. The word "texture" has nothing to do with how the rock feels. Texture, in geology, is used to describe how the rock looks. The most noticeable textural feature of igneous rocks is grain size. Grain size refers to the size of the individual mineral crystals. As mentioned above, intrusive igneous rocks, such as granite have large, individual crystals visible to the naked eye. The textural term used to describe a rock with large crystals is coarse-grained. In contrast, fine-grained rocks, such as basalt, are igneous rocks that have crystals too fine to see with the naked eye. Under magnification they are still very small but easily identifiable with a few optic tests. Quickly-cooled lavas can contain trapped bubbles of gas, which are called vesicles. The resulting texture is described as vesicular.

Chemical Composition
Chemical composition of igneous rock can often be estimated just from looking at the rock. Geologists look at the proportions of light-colored and dark-colored minerals in an igneous rock to estimate the chemical makeup of rock. Light-colored or felsic, minerals have more silica in them. Silica is one of the most abundant elements on Earth and is the chief component of quartz. Felsic minerals are most often colorless, white, gray or pink but can be any number of colors. The dark, or mafic, minerals are richer in iron and magnesium. Mafic minerals are chiefly black, brown, dark gray and sometimes green.

The mineral proportions of the rock are what allows geologists to classify rocks chemically. Depending on the proportion of light minerals to dark minerals, igneous rocks can be broken into four main types: felsic, intermediate, mafic and ultramafic. The following list gives more information about igneous chemical categories. This information is provided for you, the teacher, to better understand igneous rocks.

• Felsic rocks are high in silica (65% +). They are usually light-colored. Some examples are: Rhyolite (extrusive) and granite (intrusive).
• Intermediate rocks have lower silica content (55-65%). They are darker than felsic rocks but lighter than mafic rocks. Some examples are: Andesite/dacite (extrusive) and diorite/granodiorite (intrusive).
• Mafic rocks have low silica content (45-55%). They are usually dark-colored and contain iron and magnesium. Some examples are: Basalt (extrusive) and gabbro (intrusive). Basalt is the rock that is produced at spreading ridges and makes up the sea floor.
• Ultramafic rocks have extremely low silica content (less than 45%) and contain large amounts of iron and magnesium. They are usually dark-colored, but high olivine content can lend green shades to the rock. Other rare colors can be found. An example of ultramafic rock is Peridotite (intrusive).

Instructional Procedures:

• Create colored tags for the students to wear. Each color represents a certain kind of mineral in a molten material (magma or lava). Hang colored pieces by a string to make things easier.
• Split the class into at least 4-5 groups that have identical tags. There should be enough for every student to have one.
• Spread the class out randomly. Have them as far away from each other as possible.
• After the students have spread out, yell "CRYSTALLIZE!" and have students hurry to find others with their same name tag.
• After a few seconds, yell "STOP!" and have students stop where they are.
• Look around the class. How many groups have formed? Are there any groups? Use the size of each "crystal" to discuss the texture of the new rock created.
• Repeat steps 3-5 with different time intervals.
• The goal is to create 'extrusive' rocks, where either no or few crystals were formed, 'intrusive' rocks where large crystals were formed, and for more advanced students, porphyritic or vesicular rocks were formed. Consider a 'large' crystal to be three or more students of like crystal color that have found each other.
• You may want to start each round by giving the students a scenario to think about. Perhaps they are lava that has just come from a sea floor spreading ridge or has exploded from a violent volcanic eruption. Perhaps they are magma that has eased its way into the sediments of the continental crust. Then allow them the appropriate time to "crystallize".
• During the activity you may want to pull students aside and allow them to see what is happening. A video camera looking down onto the room allows students to see the game after it has been played.

Discussion:

What type of igneous rocks were formed? How did cooling rate affect the size of crystals formed? Do you think this process really happens in magma? In lava?

Extension:

For teachers interested in rock identification, the following is a suggestion of how you can set up a rock-ID activity. For information about how to identify igneous rocks, refer to the above definitions and the United States Geologic Survey's (USGS) web site for igneous rocks, http://wrgis.wr.usgs.gov/docs/parks/rxmin/rock.html.

For pictures of common rock-forming minerals, refer to http://wrgis.wr.usgs.gov/docs/parks/rxmin/mineral.html#feldspar.htm. Using this information and the rocks contained in the Rocks and Minerals Discovery Chest, pass around the rocks to small groups and have them identify the rocks based on texture, mineral content and chemical composition.

Included National Parks and other sites:

Black Canyon of the Gunnison
City of Rocks National Reserve
Crater Lake National Park
Craters of the Moon National Monument and Preserve
Devils Tower National Monument
Hawai`i Volcanoes National Park
Mount St. Helens National Volcanic Monument
Sunset Crater Volcano National Monument
Washington Monument National Monument
Yosemite National Park

Photos:

Sunset Crater Volcano
The granite Jefferson Memorial

Utah Science Core:

2nd Grade Standard 6 Objective 1, 2, 3
4th Grade Standard 3 Objective 1, 2

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