Gratonite is a rare mineral whose spelling is often disputed. Its correct pronunciation is /ˈɡrætənaɪt/. The word is made up of two parts, "graton" and "-ite". The first part is derived from the name of the locality where it was first discovered, Graton in California. The "-ite" suffix is a common mineral suffix. The spelling of Gratonite can be confusing, as its name is often misspelled as "Graftonite" or "Grattonite" due to its uncommon nature. However, its proper spelling remains as "Gratonite".
Gratonite is a mineral that belongs to the pyroxenoid group. It is named after the town of Graton in the California county of Sonoma, where it was first discovered. Gratonite typically has a black to dark green color, with a glassy or resinous luster. It is known for its brittle nature and subconchoidal fracture, meaning it breaks into smooth, curved surfaces.
Chemically, gratonite is a zinc aluminum sulfide mineral, with the chemical formula Zn3Al2(SO4)(OH)13·4H2O. It occurs as secondary deposits in oxidized zinc ore deposits, often associated with other minerals such as hemimorphite, hydrozincite, and smithsonite.
Gratonite is primarily sought after by mineral collectors due to its rarity and distinctive crystal habits. It usually forms as acicular or prismatic crystals, sometimes grouped into radial or fan-shaped aggregates. These crystals can have a bladed or prismatic appearance, often exhibiting a fibrous structure.
In terms of its physical properties, gratonite has a Mohs hardness of 4, which indicates its moderate resistance to scratching. Its specific gravity varies between 2.70 and 2.91, making it relatively dense. When exposed to ultraviolet (UV) light, gratonite may exhibit fluorescence, emitting a pale yellow or pale yellow-green glow.
Overall, gratonite is a unique and intriguing mineral primarily valued for its aesthetic qualities and rarity within the mineral world.
The word "gratonite" has its roots in French mineralogy. It is derived from the French word "graton", which means bits or fragments of ore. The suffix "-ite" is commonly used in mineral names to indicate that a mineral belongs to a certain group or has a specific composition. Therefore, "gratonite" refers to a mineral related to or composed of the fragments of ore, which is known for its metallic appearance and dark coloration.