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9 Gypsum is the most common sulfate mineral and differs from [[anhydrite>>doc:Environmental Surveys.Rock types.Salts.Anhydrite.WebHome]] in its water content. Gypsum has two water molecules attached to its sulfate molecules giving the following chemical name: CaSO,,4,,*2H,,2,,O. The mineral can be found in deposits together with halite, anhydrite, sulfur, calcite and dolomite.
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12
13 = Characteristics =
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15 Gypsum is clear colorless or clear white when pure. Impurities produce gray, yellow, red or brown. Its streak is white and gypsum has a vitreous, silky, sugary luster. Its hardness is soft, a 2 on Mohr's scale. It can be recognized by its perfect cleavage, low hardness and low specific gravity.
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17 = References =
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19 * (((
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21 [[https:~~/~~/geology.com/>>url:https://geology.com/||style="background-color: rgb(255, 255, 255); font-size: 14px;"]]
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23 * Bonewitz, Ronald Louis (2012). Rocks and Minerals. DK Publishing. p. 110. ISBN 978-0-7566-9042-7.
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30 = Gypsum =
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32 [[image:gypsum.jfif||alt="image.jpg"]]
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35 |=Type|Salt stone
36 |=Chemical formula|CaSO,,4 ,,*2 H,,2,,O
37 |=Color|clear colorless or clear white
38 |=Streak|White
39 |=Luster|Vitreous, silky and sugary
40 |=Hardness|Soft
41 |=Cleavage|Perfect
42 |=Image|(((
43 [[Gypsum>>https://upload.wikimedia.org/wikipedia/commons/thumb/7/77/Gips_-_Lubin%2C_Poland..jpg/1200px-Gips_-_Lubin%2C_Poland..jpg]]
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49 **Contents**
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51 {{toc/}}
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TerraIndex