Roeblingite

Roeblingite was first described in 1897 from an occurance at the Parker shaft of the Franklin Mine, Franklin, New Jersey, USA. It was named by its discoverers Samuel Lewis Penfield and Harry Ward Foote to honor of Colonel Washington A. Roebling (1837 – 1926), founder of the Mineralogical Society of America, engineer, inventor of the diving bell, builder of the Brooklyn Bridge, and avid mineral collector. Roebling donated his extensive mineral collection to the Smithsonian Institution.

Roeblingite was among the first of the lead silicate minerals found at Franklin, many of which are known only from Franklin and from Långban, Värmland, Sweden, the only other location where Roeblingite can be found. Roeblingite is valued for its rarity, its discovery at the Franklin Mine and its fluorescent properties. It fluoresces dull red to orange-red under shortwave UV light.

Chemical Formula: Pb2Ca6Mn2+Si6O18(SO4)2(OH)2 • 4(H2O)
  Hydrated Lead Calcium Manganese Silicate Sulfate Hydroxide
Molecular Weight: 1,409.57 gm
Composition: Calcium 17.06 % Ca 23.87 % CaO
  Silicon 11.95 % Si 25.58 % SiO2
  Hydrogen 0.72 % H 6.39 % H2O
  Lead 29.40 % Pb 31.67 % PbO
  Sulfur 4.55 % S 11.36 % SO3
  Oxygen 36.32 % O    
    100.00 %   98.86 % = TOTAL OXIDE

 

Crystallography: Monoclinic – Prismatic
Crystal Habit: As dense, compact, very fine grained masses of tiny lathlike crystals, which may be in parallel growth; as platy aggregates.
Twinning: None

 

Cleavage: Perfect on {001}
Fracture: Fibrous
Tenacity: Brittle
Moh’s Hardness: 3.0
Density: 3.443 (g/cm3)
Luminescence: Fluoresces dull red to dull orange-red under SW UV.
Radioactivity: Not Radioactive
Health Warning: CAUTION: Contains Lead – always wash hands after handling. Avoid inhaling dust when handling or breaking. Do not lick or ingest.
   

 

Color: White to pale pink; colorless in thin section
Transparency: Transparent, Opaque
Luster: Dull to somewhat resinous. General appearance is porcelanous.
Refractive Index: 1.640 – 1.660  Biaxial ( + ) 
Birefringence: 0.020
Dispersion: Relatively weak; r < v
Pleochroism: None