Leonard James Spencer

Summary

Leonard James Spencer 1911 Encyclopædia Britannica, Volume 17… (1911)

Apart from crystalline form, the external characters of marcasite are very similar to those of pyrites, and when distinct crystals are not available the two species cannot always be easily distinguished. The colour is usually pale bronze-yellow, often rather lighter than that of pyrites; on freshly fractured surfaces of pure marcasite the colour is tin-white, but this rapidly tarnishes on exposure to air. The lustre is metallic and brilliant.
Source: Wikisource

Leonard James Spencer 1911 Encyclopædia Britannica, Volume 17… (1911)

It is abundant, for example, in the plastic clay of the Brown Coal formation at Littmitz, near Carlsbad, in Bohemia, at which place it has been extensively mined for the manufacture of sulphur and ferrous sulphate. In the Chalk of the south-east of England nodules of marcasite with a fibrous radiated structure are abundant, and in the Chalk Marl between Dover and Folkestone fine twinned groups of “spear pyrites” are common. The mineral is also met with in metalliferous veins, though much less frequently than pyrites
Source: Wikisource

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