Figure 1. Devil’s Tower in Wyoming is one of the most famous outcrops of igneous rock in the world. It is composed of an igneous rock type called phonolite porphyry.
All rocks found on the Earth are classified into one of three groups: igneous, sedimentary, or metamorphic. This rock classification is based on the origin of each of these rock type or the rock-forming process that formed the rock. The focus of this chapter will be on igneous rocks, which are the only rocks that form from what was once a molten or liquid state. Therefore, based on their mode of origin, igneous rocks are defined as those rock types that form by the cooling of magma or lava. You would be right in thinking that there is more to the classification of igneous rocks than stated in the previous sentence, as there are dozens of different igneous rocks that are considered commonplace, dozens of more types that are less common, and also quite a few igneous rock types that are quite scarce. Yet each igneous rock has a name that distinguishes it from all the rest. So, if they all start out as molten material (magma or lava), which must harden to form a rock, then it is logical to assume that these igneous rocks differ from one another primarily due to:
- the original composition of the molten material from which the rock is derived, and
- the cooling process of the molten material that ended up forming the rock. These two parameters— composition and texture— define the classification of igneous rocks. Igneous rock composition refers to what is in the rock (the chemical composition or the minerals that are present), and a rocks’ texture refers to the features that we see in the rock, such as the mineral sizes or the presence of glass, fragmented material, or vesicles (holes) in the igneous rock.
In this module you will be learning about intrusive and extrusive igneous rocks. Igneous rocks are very commonly encountered in nature. Well-known examples are the basalt rocks of Hawaii that formed during volcanic eruptions on the islands. However, igneous rocks have formed throughout Earth’s history and, through the process of plate tectonics, are often located at great distances from active volcanoes. For example, in the Catalina Mountains to the north of Tucson, there are many examples of igneous rocks, including three sills of granite that formed about 50 million years ago through an intrusion into an older granite unit. In this module, you will learn about the different types of igneous deposits, including sills, and how composition is related to the environment in which the rocks formed.
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Figure 2. Vesiculated tachylite (basaltic lava flow cross-section, 1969 to 1974 lava tube ceiling, Mauna Ulu Lava Field, East Rift Zone, Kilauea Volcano, Hawaii, USA)
Figure 3. Fosterite-Olivine, Suppat, Northwest Frontier Province, Pakistan
Figure 4. Obsidian (top - shiny black), Pumice (gray below), and Rhyolite (light colored rock on right)at the base of Panum Crater, Mono County, California.
Figure 5. Pumice stone in a wall in Teguise, Lanzarote, Canary Islands, Spain. Pumice is a light-colored, extremely porous igneous rock that forms during explosive volcanic eruptions. It is used as aggregate in lightweight concrete, as landscaping aggregate, and as an abrasive in a variety of industrial and consumer products. (geology.com)
Figure 6. Lava and basalt at Hawaii Volcanoes National Park (2004, Chain of Craters Road)
Figure 7. Lava and basalt at Hawaii Volcanoes National Park (2004, Chain of Craters Road)
Figure 8.The Organ Pipes near Khorixas, Namibia. They are a rock formation that comprises a group of columnar basalts which resemble organ pipes.
Figure 9. The Giant's Causeway on the Antrim Coast of Northern Ireland. A UNESCO World Heritage Site with 40,000 basalt columns from an ancient volcanic eruption.
Figure 10. Giant's Causeway, Ireland
Figure 11. Weaver's Needle seen from the Fremont Pass in the Superstition Mountains band east of Phoenix, Arizona . Weaver's Needle was created when volcanic tuff, the effect of the original volcano eruption, began to undergo rapid erosion, leaving a 1388 meter high turn. The summit was named after the famous climber Pauline Weaver.
Figure 12. Ancestral homes made of tuff, Bandolier National Monument, New Mexico. Tuff is very light and soft. Over time, wind and water gradually eroded away softer areas of tuff, creating holes in the exposed canyon faces. The Ancestral Pueblo people used these to their advantage. With hand tools, they enlarged and shaped cliff openings into useful shelters called cavates (CAVE-eights). They used tuff blocks to build apartment-like homes along the cliff faces in front of the cavates. (National Park Service)
At the completion of this module you will be able to:
- Explain the rock cycle and the processes involved.
- Name and describe the different types of intrusive and extrusive igneous deposits.
- Describe the composition of different types of igneous rocks and explain the processes involved in their formation.
- Explain which tectonic environment is associated with which kinds of igneous rock.
See the Schedule of Work for dates of availability and due dates.
Be sure to read through the directions for all of this module's activities before getting started so that you can plan your time accordingly. You are expected to work on this course throughout the week.
Physical Geology by Steven Earle
- Chapter 3 (Intrusive Igneous Rocks)
Module 5 Assignment: Igneous Rock Lab
After you complete the reading, you can start working on Module 5 Assignment - Igneous Rock Lab.
Module 5 Quiz
Module 5 Quiz has 10 multiple-choice questions and is based on the content of the Module 5 readings and Assignment 5.
The quiz is worth a total of 10 points (1 points per question). You will have only 10 minutes to complete the quiz, and you may take this quiz only once. Note
: that is not enough time to look up the answers!
Make sure that you fully understand all of the concepts presented and study for this quiz as though it were going to be proctored in a classroom, or you will likely find yourself running out of time.
Keep track of the time, and be sure to look over your full quiz results after you have submitted it for a grade.
Exam 1 is due this module. You will be asked to put your knowledge to work in the Great Outdoors or at your local rock shop! You will be assembling a mineral kit with 5 minerals of your choice, composed of samples you have collected yourself or purchased individually. As a result, your kit will be customized according to your own interests.
You can read more about this in the Exam 1 Instructions.
This is a “work-at-home” project. You will submit the results from your project in the Assignments tool.
Check the Course Schedule for due date.
Your Questions and Concerns...
Please contact me if you have any questions or concerns.
General course questions: If your question is of a general nature such that other students would benefit from the answer, then go to the discussions area and post it as a question thread in the "General course questions" discussion area.
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Licenses and Attributions
CC licensed content, Original
- Module 5: Igneous Rocks . Authored by: Anne Huth. Provided by: Pima Community College. License: CC BY: Attribution
CC licensed content, Shared previously
- Physical Geology, Adapted by Anne Huth, Pima Community College. Authored by: Steven Earle. Located at: https://opentextbc.ca/geology/. License: CC BY: Attribution
- Laboratory Manual for Introductory Geology, Adapted by Anne Huth, Pima Community College. Authored by: Bradley Deline, Randa Harris, and Karen Defend. License: CC BY: Attribution
- Figure 3. Fosterite-Olivine. Authored by: Rob Lavinsky, irocks.com. Provided by: Wikimedia Commons. License: CC BY-SA: Attribution-ShareAlike
- Figure 4. Different rocks at Panum Crater. Authored by: Daniel Mayer. Provided by: Wikimedia Commons. License: CC BY-SA: Attribution-ShareAlike
- Figure 5. Pumice Stone in a Wall. Authored by: Norbert Nagel. Provided by: Wikimedia Commons. License: CC BY-SA: Attribution-ShareAlike
- Figure 8: Basalt Structures in Namibia. Authored by: Schnobby. Provided by: Wikimedia Commons. License: CC BY: Attribution
- Figure 9: Giant's Causeway. Authored by: Tony Webster. Provided by: Wikimedia Commons. License: CC BY: Attribution
- Figure 11: Weaver's Needle seen from the Fremont Pass. Authored by: Ihelewa. Provided by: Wikimedia Commons. License: CC BY: Attribution
- Figure 12: Cliff Dwelling, Bandolier, NM. Authored by: byrdiegyrl. Provided by: Wikimedia Commons. License: CC BY: Attribution
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