Logo
Unionpedia
Communication
Get it on Google Play
New! Download Unionpedia on your Android™ device!
Free
Faster access than browser!
 

Alunite and List of minerals

Shortcuts: Differences, Similarities, Jaccard Similarity Coefficient, References.

Difference between Alunite and List of minerals

Alunite vs. List of minerals

Alunite is a hydrated aluminium potassium sulfate mineral, formula KAl3(SO4)2(OH)6. This is a list of minerals for which there are articles on Wikipedia.

Similarities between Alunite and List of minerals

Alunite and List of minerals have 6 things in common (in Unionpedia): Aluminium, Anhydrite, Dolomite, Jarosite, Magnesite, Sulfur.

Aluminium

Aluminium or aluminum is a chemical element with symbol Al and atomic number 13.

Aluminium and Alunite · Aluminium and List of minerals · See more »

Anhydrite

Anhydrite is a mineral—anhydrous calcium sulfate, CaSO4.

Alunite and Anhydrite · Anhydrite and List of minerals · See more »

Dolomite

Dolomite is an anhydrous carbonate mineral composed of calcium magnesium carbonate, ideally The term is also used for a sedimentary carbonate rock composed mostly of the mineral dolomite.

Alunite and Dolomite · Dolomite and List of minerals · See more »

Jarosite

Jarosite is a basic hydrous sulfate of potassium and iron with a chemical formula of KFe3+3(OH)6(SO4)2.

Alunite and Jarosite · Jarosite and List of minerals · See more »

Magnesite

Magnesite is a mineral with the chemical formula MgCO3 (magnesium carbonate).

Alunite and Magnesite · List of minerals and Magnesite · See more »

Sulfur

Sulfur or sulphur is a chemical element with symbol S and atomic number 16.

Alunite and Sulfur · List of minerals and Sulfur · See more »

The list above answers the following questions

Alunite and List of minerals Comparison

Alunite has 40 relations, while List of minerals has 1465. As they have in common 6, the Jaccard index is 0.40% = 6 / (40 + 1465).

References

This article shows the relationship between Alunite and List of minerals. To access each article from which the information was extracted, please visit:

Hey! We are on Facebook now! »