In today's world, Lyonsite is a topic that has captured the attention of many people. Whether due to its relevance in modern society, its impact on popular culture or its influence on history, Lyonsite has become a topic of general interest. Over the years, it has been the subject of debates, analyzes and discussions in all areas, from politics to science. In this article, we will explore the different facets of Lyonsite and its role in today's world, offering a comprehensive view of its importance and relevance today.
| Lyonsite | |
|---|---|
| General | |
| Category | Vanadate mineral |
| Formula | Cu3Fe+34(VO4)6 |
| IMA symbol | Lyo[1] |
| Strunz classification | 8.AB.40 |
| Crystal system | Orthorhombic |
| Crystal class | Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) |
| Space group | Pmcn |
| Unit cell | a = 10.29, b = 17.2 c = 4.91 ; Z = 2 |
| Identification | |
| Color | Black; creamy white in reflected light in polished section |
| Crystal habit | As euhedral flattened lath shaped crystals |
| Cleavage | Good on {001} |
| Tenacity | Brittle |
| Luster | Metallic |
| Streak | Dark gray |
| Diaphaneity | Opaque |
| Specific gravity | 4.215 calculated |
| References | [2][3][4] |
Lyonsite (Cu3Fe+34(VO4)6) is a rare black vanadate mineral that is opaque with a metallic lustre. It crystallizes in the orthorhombic crystal system. Lyonsite often occurs as small tabular typically well formed crystals. Lyonsite has a good cleavage and a dark gray streak.
Lyonsite occurs as a sublimate in volcanic fumaroles. It is often associated with howardevansite and thenardite.[2] It was first described in 1987 for an occurrence on the Izalco volcano, El Salvador. It was named for mineralogist John Bartholomew Lyons (1916–1998) of Dartmouth College.[3] It has also been reported from a mine dump in the Lichtenberg Absetzer Mine of Thuringia, Germany.[4]