In this article we will explore in depth the topic of Wavellite, a topic of great relevance today that affects different sectors of society. We will investigate its origin, history and evolution over time, as well as its impact on people's daily lives. In addition, we will analyze different perspectives and opinions on Wavellite, with the aim of providing a broad and complete overview of this topic. Through this research, we aim to offer our readers a deeper understanding of Wavellite, so that they can form an informed opinion and contribute to the debate around this matter.
| Wavellite | |
|---|---|
Wavellite cluster from Mauldin Mountain Quarries, Mauldin Mt., Montgomery County, Arkansas | |
| General | |
| Category | Phosphate minerals |
| Formula | Al3(PO4)2(OH,F)3·5H2O |
| IMA symbol | Wav[1] |
| Strunz classification | 8.DC.50 |
| Crystal system | Orthorhombic |
| Crystal class | Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) |
| Space group | Pcmn |
| Unit cell | a = 9.621 Å b = 17.363 Å, c = 6.994 Å; Z = 4 |
| Identification | |
| Color | Green to yellowish-green and greenish blue and blue. and yellow, brown, white and colorless |
| Crystal habit | Spherical, radial aggregates; striated prisms; crusty to stalactitic |
| Cleavage | perfect, good, distinct |
| Fracture | Uneven to subconchoidal |
| Mohs scale hardness | 3.5 - 4 |
| Luster | Vitreous to resinous, pearly |
| Streak | White |
| Diaphaneity | Translucent |
| Specific gravity | 2.36 |
| Optical properties | Biaxial (+) |
| Refractive index | nα = 1.518 - 1.535 nβ = 1.524 - 1.543 nγ = 1.544 - 1.561 |
| Birefringence | δ = 0.026 |
| Pleochroism | Weak; X = greenish; Z = yellowish |
| 2V angle | Measured: 60° to 72° |
| Fusibility | Infusable, swells and splits on heating |
| Solubility | Insoluble |
| References | [2][3][4][5] |
Wavellite is an aluminium basic phosphate mineral with formula Al3(PO4)2(OH, F)3·5H2O. Distinct crystals are rare, and it normally occurs as translucent green radial or spherical clusters.[6]

Wavellite was first described in 1805 for an occurrence at High Down, Filleigh, Devon, England and named by William Babington in 1805 in honor of Dr. William Wavell (1750–1829),[4] a Devon-based physician, botanist, historian, and naturalist, who brought the mineral to the attention of fellow mineralogists.[7][4][6][8]
It occurs in association with crandallite and variscite in fractures in aluminous metamorphic rock, in hydrothermal regions and in phosphate rock deposits.[2] It is found in a wide variety of locations, notably in the Mount Ida, Arkansas area in the Ouachita Mountains.
It is sometimes used as a gemstone.[9]