
Image Credit: Malcolm Southwood

Image Credit: Malcolm Southwood

Image Credit: Martin Števko; Slovak Academy of Sciences, Bratislava, Slovakia



Specimen Title
arsentsumebite after mimetite
Principal Mineral
Precursor Mineral
Size
Cabinet; 98mm
Location in the Mine
First oxidation zone
Provenance
Hancock, E.P.
Collection
MGMH; 133414
Entry Number
Specimen; TSNB775
Description
Pseudomorphs of arsentsumebite (EDS verified; Martin Števko, pers. comm. 2024) after mimetite forming a loose intergrowth of randomly orientated slender hexagonal prisms (to 25 mm) encrusting a shard of matrix also consisting largely of arsentsumebite (?) but with a core which includes relict sulphide mineralisation.
Broken pseudomorphs show arsentsumebite forming a sheath (circa 1 mm thick) around concentrically zoned mimetite crystals (Exhibit 2). Preliminary analysis (EDS) confirms arsentsumebite as the principal replacing mineral, apparently with relatively little compositional variation, but with localised inclusions of relict mimetite (Exhibit 3).
The specimen is from the E.P Hancock Collection, acquired by Harvard in 1916, which dates it to the upper part of the first oxidation zone (i.e. 6 Level or above).