Welcome
to GLG101C Introduction to Geology Professor James Tyburczy |
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Department of Geological Sciences | |
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Class Notes -- Chapter 3 |
Amethyst Galleries has many beautiful photos of minerals from all over the world
The US Geological Survey's Mineral Resources Program has statistics and information on the worldwide supply, demand, and flow of minerals and materials essential to the U.S. economy, the national security, and protection of the environment.
The University of Arizona has a great site showing movies of crystal models how they vary with temperature and pressure.
Here's alocation to download a pdf file from the US Geological Survey on asbestos.
Here's the Asbestos Institute site, emphasizing safe use of chrysotile asbestos.
For a map of the soil shrinking/swelling potential for the Phoenix area see: http://www.az.nrcs.usda.gov/technical/soils/shrinkswell.html
Chapter 3. MINERALS: BUILDING BLOCKS OF ROCKS
A mineral is: a naturally-occurring, crystalline solid, generally inorganic,with a specific chemical composition
Atomic Structure & Chemistry
Chemical Bonding - ionic, covalent, metallic
Chemical Composition of the Earth
Atomic and Crystal Structure of Minerals - governed by sizes of ions and the number of nearest neighbors
How do minerals form - crystallization from a melt, precipitation from water, growth in the solid state
Polymorphs - same chemical composition but different crystal structure - graphite and diamond are both made of carbon
Silicates - most common type of rock-forming mineral
Isolated silica tetrahedra - olivine, garnet
Chain silicates
Sheet silicates - micas, clay minerals
Framework silicates - quartz, feldspars (2 types of feldspar, K-rich and Ca+Na containing). Feldspars are the most abundant type of mineral in the Earth's crust
What to know about the silicate minerals:
Non-silicates
Physical properties of minerals -
Asbestos - two main types of asbestos
Swelling soils:
Certain clay minerals that occur in soils can absorb water between the silicate sheet layers (montmorillonite is the mineral name). This leads to expansion of the structure. If expansion of the soil is too great, it can cause foundations to crack and other kinds of structural damage. Areas of high potential for soil swelling can be mapped out.
For a map of the shrinking/swelling potential for the Phoenix area see: http://www.az.nrcs.usda.gov/soils/shrinkswell.html
©2004, James A. Tyburczy, Department of Geology, Arizona State University If you have any questions or concerns regarding this page, please address them to jim.tyburczy@asu.edu. Be specific in your description of the problem! Last update 8/27/04 |