Iron gall

Iron gallstones / Pyrite concretions These gorgeous and interesting pyrite concretions fall into that category of odd, beautiful, curious, and weird. My favorite category! A fun add to any collection, especially for pyrite collectors, or concretion lovers. Concretions are found in sedimentary rock or soil, often ovid or spherical in shape. They generally form around some type of nucleus, usually early on in the burial history of the sediment.

This makes them harder than the surrounding host sediment. Record of these geological curiosities dates back to the 18th century. They were often confused with fossils of dinosaurs, plants, humans and extraterrestrials. The name concretion is derived from Latin; con (together), crescere (grow). This specimen was collected from marine shales in Guangxi, China.

The slightly ovoidal nodule consist of layers of pyrite, or iron disulfide, and black shale material, and sits nicely without support. Origin :: Guangxi, China Measurements :: 70 x 65 x 49 mm Weight :: 10. 7 oz.

CRYSTAL HABIT:Concretionary to nodular
CRYSTAL STRUCTURE:Mineral aggregate; commonly pyrite or iron oxides in shale
MOHS:Composition-dependent
HOST ROCK:Marine shale or mudstone
ELEMENT:Earth
ZODIAC:No widely established association
PROPERTIES:Not included in the supplied summary.
MINE & LOCALITY MAPS

Locations named in this mineral summary

Guangxi, China

Maps identify the mines, districts and geographic localities named in the supplied summary. Where exact mine coordinates are unavailable, the map represents the broader named area.