The Mineral Gypsum

by

Jacob Bray


A Student Presentation from
Emporia State University
Earth Science Department



Image taken from:
http://www.kgs.ku.edu/
Extension/KGSrocks/gypsum_def.html

Image taken from:
http://www.kgs.ku.edu/Extension/
redhills/rocks.html
· 	Gypsum is a common mineral and is found throughout the 
	world.  There are numerous locations within the United States, 
	and North America as a whole.  New York, Utah, Colorado, 
	Oklahoma and Mexico are just a few locations where excellent 
	specimens have been found.  Gypsum is a common mineral within 
	sedimentary environments.  It is a valuable rock forming mineral 
	that is commonly found in massive beds often from precipitation 
	out of highly saline waters.  Because of its formation it can 
	and often times does have many inclusions of other minerals and 
	it may even have trapped air bubbles.  Selenite, satin spar, and 
	alabaster are a few of the variety names of gypsum.
·	Selenite is a colorless and transparent variety that can show 
	pearl-like luster, and may have a banded appearance.
·	Satin spar gypsum has a fibrous appearance, and is often times 
	a milky white or pink color.
·	Alabaster is a fine grained massive material that is carved 
	into ornaments. [Source #1]

Return to table of contents.

Physical Characteristics

·	Color:  usually white, colorless or gray, may also be shades of 
	red, brown, and yellow.
·	Luster:  vitreous to pearly especially on cleavage surfaces.
·	Transparency:  may be transparent to translucent.
·	Crystal System:  monoclinic.
·	Habits:  tabular, bladed or blocked crystals.  Pinacoid faces may 
	be present.  Long thin crystals like those found in satin spar gypsum 
	may show its flexible tenacity with curves.  Twinning is also possible.  
	Other habits can include massive, granular, earthy, and fibrous.
·	Cleavage:  good in one direction, and noticeable in two others.
·	Fracture:  rare but if seen will be uneven.
·	Hardness:  low, registers 1.5 to 2 on Moh’s Hardness Scale.
·	Specific Gravity:  2.3 to 2.4.
·	Streak:  white. [Source #1]

Other important information:

	Some crystals may be flexible.  This means that thin bands of the 
	mineral will bend and change shape but will not return to the original 
	form once the pressure is released.  This is often seen in the satin 
	spar variety. Gypsum is a poor conductor of heat, which makes it 
	useful in wall board. [Source #1]

Return to table of contents.

The Uses of Gypsum

	Gypsum is one of the most widely used minerals in the world.  
	Most is used to make wall board, also know as sheet rock.  It 
	is estimated that the average American home contains seven 
	metric tons of gypsum.  Gypsum is also added to concrete to 
	strengthen the material, so it can be used in concrete for roads, 
	bridges and sidewalks just to name a few.  Gypsum can also 
	be used as a fertilizer by adding it directly to the soil.  This 
	increases the productivity of the land. It can be added to paint 
	as a filler.  Used in these ways, gypsum must first be ground up 
	into a powder and dried.  

	It is thought that the first uses of gypsum were for sculptures.  
	Alabaster is a soft solid form of gypsum that takes carvings well 
	thus it was able to be carved into many different shaped objects.  
	5,000 years ago the Egyptians learned to turn the gypsum into what 
	we now call Plaster of Paris, and they used it to line the walls 
	of their living quarters.  They discovered that if the gypsum was 
	ground up into a fine powder and dried, that they could later add 
	water, mix and use as cement. [Source #7]  

	The transparent form of gypsum (selenite) was used for windows 
	before glass was created.  Gypsum contains a large amount of water,  
	and this gives it fire protection qualities. [Source #7]  This is important 
	because it will give some protection from house fires.  It is 
	also important because it can be used as molds, allowing melted 
	metals to be poured and formed within.  Tiles found in the 
	bathroom are more often than not attached to the wall with a 
	form of gypsum mortar.  Plates, cups and saucers from your 
	kitchen were most likely poured into a gypsum formed mold.  The 
	uses of gypsum are, as we can see nearly endless.  I have only 
	touched on a few, but we can be sure that we will encounter 
	gypsum in some form or another nearly everyday.

Return to table of contents.

Mining of Gypsum

	Because gypsum is often found in large thick layers near the Earth's 
	surface, it is easily mined.  Once a large bed of gypsum is
	discovered a mining company will set up shop and begin to extract 
	the mineral from the ground.  It may take years before the site is 
	exhausted.  Large machines will be used to blast and remove the 
	gypsum, often times destruction to the environment is nearly 
	impossible to control.  The importance of gypsum has resulted in 
	a tolerance of this environmental destruction.  Once the mining 
	is no longer economically valuable the site is closed.  Then, an 
	alternate site is selected, and the mining process starts over. 
	
	This natural resource is so abundant it is not thought of as in 
	danger of being used up worldwide.  However, this may someday 
	be an issue.  Gypsum is a recyclable product, but only a small 
	amount is recycled every year because of its abundance.  Once 
	the gypsum is mined, it must then be processed.  This may consist 
	of grinding the gypsum into a powder, then heating it to remove 
	most of the moisture to allow for transport and to make the 
	transition into a final product.  In 2000, gypsum output was 
	more than 25 million tons, and was valued at $175 million. 
	[Source #6] The top producing US states were Oklahoma, California, 
	Iowa, Texas, Nevada, Michigan, and New Mexico.  These states 
	accounted for 75% of the total output.  The top three gypsum 
	producing countries in 2000 were the United States, Australia, 
	and Canada. [Source #6] 
 
Return to table of contents.

Overview
	As you can see gypsum is a valuable mineral that is needed in many 
	aspects of life.  Many may argue that gypsum is the single most 
	important mineral to our everyday life.  I will not go that far 
	but we must admit that no one could faithfully argue that gypsum 
	in its many forms is not an integral part of life as we know it.  
	Yes, if there was no such mineral as gypsum we would find alternate 
	ways to substitute for this mineral, we have even in some small 
	ways done such.  We now have a synthetic form of gypsum that will 
	assist us in the future if and when the gypsum reserves we have come 
	to rely on so heavily have been depleted.  The chances that gypsum 
	will be completely mined from the Earth within the next 100 years is 
	virtually impossible, so we should not be consumed with such a threat.  
	We should however recognize the fact that gypsum is very valuable 
	and important, and like all natural resources we should do everything 
	we can to conserve and preserve.

Return to table of contents.


Sources

Source #1
GeoKansas Gypsum, World Wide Web URL: 
http://www.kgs.ku.edu/Extension/KGSrocks/gypsum_def.html. Retrieved 
on November 19, 2002.
Source #2
Chesterman, C. 1978. The audubon society field guide to north American rocks and minerals.  
Random House.
Source #3
Pellant, C. 1992. Rocks and minerals. Dorling Kindersley, London.
Source #4
Klein, C. 2002. Mineral science (22nd ed.). John Wiley & Sons Inc., NY.

Web Page Sources

Source #5
Mineral Galleries, The Mineral Gypsum, World Wide Web URL: 
http://mineral.galleries.com/minerals/sulfates/gypsum/gypsum.htm. 
Retrieved on November 19, 2002. 

Source #6 USGS Minerals, World Wide Web URL: http://minerals.usgs.gov/minerals/. Retrieved on November 19, 2002.

Source #7 http://webmineral.com/data/Gypsum.shtml

Source #8 http://webmineral.com/cgi-bin/search/search.pl Source #9 http://archnet.org/library/downloader/document/4554/dpt0496.pdf Source #10 http://www.geo.msu.edu/geo333/gypsummining.html


Return to student webpages.

Date of creation: 19 November, 2002. Copyright 2002 Jake Bray. I can be reached at jake305@yahoo.com. All rights reserved.