Welcome to GLG101C Introduction to Geology
Fall 2004

Professor James Tyburczy

Department of Geological Sciences

  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

  1. 'white asbestos' is serpentine, a sheet silicate (specific mineral is chrysotile)
         NOT medically dangerous, except when one works with the fibers all day
         95 % of all asbestos in the US is 'white asbestos'

  2. 'blue' and 'brown' asbestos - amphibole minerals (double chain silicates)
          Very dangerous medically, but only constitutes a small fraction of the asbestos in use in the U.S. today

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


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