Olivenite

Chambers's Encyclopaedia, Volume 7: Maltebrun to Pearson, p. 600

Olivenite, a mineral, consisting chiefly of arsenic acid and protoxide of copper, with a little phosphoric acid and a little water. It is generally of some dark shade of green, sometimes brown or yellow. It is found along with different ores of copper in Cornwall and elsewhere. It is often crystallised in oblique four-sided prisms, of which the extremities are acutely bevelled, and the obtuse lateral edges sometimes truncated, or in acute double four-sided pyramids; it is sometimes also spherical, kidney-shaped, columnar, or fibrous, which latter variety is known as wood-arseniate, and is greenish gray in colour.

Source scan(s): p. 0613