Ashcroftine-(Y) – [K5Na5(Y,Ca)12Si28O70(OH)2(CO3)8 · 3H2O]

Ashcroftine-(Y) had been originally described as kalithompsonite in 1924. MSH is only the second locality for this species which has the distinction of having the largest unit-cell dimensions of all known species.

PHYSICAL CHARACTERISTICS:

 

  • Color is usually very pale violet, pale pink or white.
  • Luster is vitreous to silky.
  • Diaphaneity is transparent to translucent.
  • Crystal System is tetragonal; I4/mmm.
  • Crystal Habits include very fine divergent sprays and tufts of
    randomly oriented capillary to fibrous crystals to 20mm.
  • Cleavage {100} is perfect and {001} is good.
  • Fracture is uneven.
  • Hardness is 5 – 5.5.
  • Specific Gravity is approximately 2.25 g/cm3.
  • Streak is white.
  • Associated Minerals include aegirine, albite, amphibole group,
    analcime, ancylite, bastnäsite, biotite, brookite, catapleiite,
    cordylite, donnayite, elpidite, ewaldite, fluorapatite, fluorite,
    leucophanite, leucosphenite, lorenzenite, microcline,
    molybdenite, monteregianite, narsarsukite, nepheline, raite
    and zircon.
  • Distinguishing Features: Crystal habit and color.
  • Origin: Named in 1933 for Frederik Noel Ashcroft (1878-1949),
    a proeminent mineral collector of London.

 

 

Dana class # 70.3.1.1 – Inosilicates: two-dimensionally infinite silicate units; column or tube structures
Strunz class # VIII/F.35-60 – Inosilicates (chain and band) complex chain structure; cylindric chains and others; ashcroftine-(Y) series