List of minerals and Melanterite

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

Difference between List of minerals and Melanterite

List of minerals vs. Melanterite

This is a list of minerals for which there are articles on Wikipedia. Melanterite is a mineral form of hydrous iron(II) sulfate: FeSO4·7H2O.

Similarities between List of minerals and Melanterite

List of minerals and Melanterite have 8 things in common (in Unionpedia): Chalcanthite, Epsomite, Halotrichite, Lignite, Marcasite, Pickeringite, Pyrite, Siderotil.

Chalcanthite

Chalcanthite, whose name derives from the Greek, chalkos and anthos, meaning copper flower, is a richly colored blue/green water-soluble sulfate mineral CuSO4·5H2O.

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Epsomite

Epsomite is a hydrous magnesium sulfate mineral with formula MgSO4·7H2O.

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Halotrichite

Halotrichite, also known as feather alum, is a highly hydrated sulfate of aluminium and iron.

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Lignite

Lignite, often referred to as brown coal, is a soft, brown, combustible, sedimentary rock formed from naturally compressed peat.

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Marcasite

The mineral marcasite, sometimes called white iron pyrite, is iron sulfide (FeS2) with orthorhombic crystal structure.

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Pickeringite

Pickeringite is a magnesium aluminium sulfate mineral with formula MgAl2(SO4)4·22(H2O).

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Pyrite

The mineral pyrite, or iron pyrite, also known as fool's gold, is an iron sulfide with the chemical formula FeS2 (iron(II) disulfide).

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Siderotil

Siderotil is an iron(II) sulfate hydrate mineral with formula: FeSO4·5H2O which forms by the dehydration of melanterite.

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The list above answers the following questions

What List of minerals and Melanterite have in common
What are the similarities between List of minerals and Melanterite

List of minerals and Melanterite Comparison

List of minerals has 1465 relations, while Melanterite has 20. As they have in common 8, the Jaccard index is 0.54% = 8 / (1465 + 20).

References

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

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