GO 324A Rocks and Minerals
Dr. Susan Ward Aber

www.emporia.edu/earthsci/amber/go324/intro.htm

Emporia State University
Emporia, Kansas USA
Earth Science Department


Welcome to Rocks and Minerals!

Minerals are the main constituent of rocks and are naturally occurring, macroscopically homogeneous, and solid substances with a definite chemical composition and crystalline structure. It is usually assumed minerals are of an inorganic origin, but exceptions occur as in the case of pearl. A mineral may be simple, such as copper, which is a native element composed of... copper! A mineral may be complex, such as tourmaline, a silicate of boron and aluminum composed of Na (Mg, Fe)3Al6(BO3)3(Si6O18)(OH, F)4 with a ring-silicate or cyclosilicate crystalline structure.

Rocks are aggregates of one or many differentiated or undifferentiated minerals. For example, granite is primarily made up of differentiated quartz, mica, and feldspar, and each mineral can be clearly seen in hand specimen. In contrast, limestone consists almost entirely of undifferentiated calcite, where the calcite can be determined through testing but not clearly recognized as a crystal in hand specimen.

There are over 4,000 known minerals, but only about 20 make up some 95% of all rocks. This course will examine some of the more common minerals and rocks, with a focus on specimen identification. Minerals will be presented first because they are the foundation of rocks. Rocks are divided into one of three major classes: igneous, sedimentary, and metamorphic; rock specimen identification will comprise the remainder of the course.

Why is the study of rocks and minerals important? An understanding of Earth's 4.5 billion year history and formation is derived from discovering the differences between rock types and mineral formation. There are primarily sedimentary rocks exposed at the surface in Kansas. However, 1.2 billion year old granite and 88-90 million year old contact metamorphic rocks exposed at the surface in Kansas as well. In addition to exploring and understanding Kansas and the planet we live on, minerals and rocks are of great economic importance and humanity depends on a steady supply to live!

If you are enrolled in this course and reading this before September 8, I have a deal for you... up to 2 substitution points will be awarded on the exam of your choice, when you email me a one-page summary of the interactive online video of Spirit and Opportunity rover excursions at http://www.pbs.org/wgbh/nova/mars/upclose.html. You must launch interactive video (hearing it is best but there is a printable version as well); be sure to include rock types found and instruments used on Mars to detect the rocks and structures. These extra credit opportunities are scattered throughout the course webpages. Happy browsing and roving in this course!

Recommended References and Links

Return to the top.

Petrology Introduction
www.emporia.edu/earthsci/amber/go324/intro.htm
Minerals
www.emporia.edu/earthsci/amber/go324/mineral.htm
Rocks
www.emporia.edu/earthsci/amber/go324/rock.htm
Igneous
www.emporia.edu/earthsci/amber/go324/igneous.htm
Sedimentary Rock
www.emporia.edu/earthsci/amber/go324/sediment.htm
Metamorphic Rock
www.emporia.edu/earthsci/amber/go324/metamor.htm
Course Field Trip
www.emporia.edu/earthsci/amber/go324/field_trip.htm
Course Syllabus
www.emporia.edu/earthsci/amber/go324/syllabus.htm

This page originates from the Earth Science department for the use and benefit of students enrolled at Emporia State University. The curriculum is © by the author, 2001-2009. Last update 18 July 2009. For more information contact the course instructor, Dr. S. W. Aber, e-mail: saber@emporia.edu

To understand copyright, visit lcweb.loc.gov/copyright/. All rights reserved. Susan Ward Aber.