Malhmoodite

A variety of Minerals

Malhmoodite specimen - rock identification

What is Malhmoodite?

Malhmoodite is a phosphate mineral first discovered at a mine called Union Carbide in Wilson Springs, Arkansas, United States. This mine is 10 km west of Magnet Cove, an alkaline igneous complex, and Union Carbide is in a contact region of alkalic igneous rocks and surrounding sedimentary rocks. The mineral has been approved by the Commission on New Minerals and Mineral Names, IMA, to be named for the late Bertha K. Malhmood, the Administrative Assistant of the Branch of Analytical Laboratories, U.S. Geological Survey.

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North ZoneCentral RidgeSouth Basin

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Key Characteristics

Characteristics of Malhmoodite

Malhmoodite is a creamy-white mineral with a silky luster. It exhibits a 3 on the Mohs hardness scale. The spherules of Malhmoodite are made up of thin, flat, radiating, optically homogeneous crystals and seem to form in a parallel extinction and positive elongation. The cores of the spherules appear to be loose material, making up about one-third to one-half of the radius of the spherule. However, the core seems to show higher amounts of Si than the rest of the spherule by using X-ray spectra. The fibers of the mineral are soft and the density could not be directly measured. It was instead calculated using the unit-cell content of four formula units and determined to be 2.877 g/cm. In the crystal structure work of Malhmoodite, it was found that there was a common [Zr(PO4)2] layer. It is considered a pseudohexagonal with orthorhombic dimensions.

Formation of Malhmoodite

Malhmoodite occurs perched on kolbeckite plates and seems to be the last deposited in the cavities it occurs. The mineral is very rare, with the only common place to find it in Wilson Springs. However, a few other specimens have been found in Belgium and England.

Quick Facts

Physical Properties

Color
Creamy-white
Hardness (Mohs)
3
Density
2.877 g/cm³
Streak
White

Chemical Properties

Chemical Formula
FeZr(PO4)2 · 4H2O
Elements
Fe, H, O, P, Zr
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