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Museum Quality Hemimorphite Mineral Specimen -OVER 10 LBS!!! Magnificent Sample!

$ 660

Availability: 100 in stock
  • Country/Region of Manufacture: Mexico
  • All returns accepted: ReturnsNotAccepted
  • Condition: Used

    Description

    Museum Quality Hemimorphite Mineral Specimen -OVER 10 LBS!!! Magnificent Sample!
    This 4901 gram specimen is from the Santo Niño Mine, Santa Maria del Oro, Durango, Mexico.
    It measures approximately 10.5 x 8 x 4".  There are 6 crevasses in the front of the piece, 4 on the right side and 2 on the bottom, all
    engulfed and surrounded
    by Hemimorphite.
    This specimen has a flat base and stands on its own for an incredible display in many different orientations.
    Hemimorphite Background Information
    Hemimorphite most frequently occurs as the product of the
    oxidation
    of the upper parts of
    sphalerite
    bearing ore bodies, accompanied by other secondary minerals which form the so-called
    iron cap
    or
    gossan
    . Hemimorphite is an important
    ore
    of zinc and contains up to 54.2% of the metal, together with silicon, oxygen and hydrogen.
    Hemimorphite
    , is
    Zn
    4
    (
    Si
    2
    O
    7
    )(
    OH
    )
    2
    ·H
    2
    O
    , a component of
    calamine
    . It is a
    sorosilicate
    mineral
    which has been historically mined from the upper parts of
    zinc
    and
    lead
    ores
    , chiefly associated with
    smithsonite
    , ZnCO
    3
    . They were assumed to be the same mineral and both were classed under the same name of
    calamine
    . In the second half of the 18th century it was discovered that these two different minerals were both present in calamine. They closely resemble each other.
    The silicate was the rarer of the two, and was named hemimorphite, because of the hemimorph development of its
    crystals
    . This unusual form, which is typical of only a few minerals, means that the crystals are terminated by dissimilar faces. Hemimorphite most commonly forms crystalline crusts and layers, also massive, granular, rounded and reniform
    aggregates
    , concentrically striated, or finely needle-shaped, fibrous or stalactitic, and rarely fan-shaped clusters of crystals.
    Some specimens show strong green
    fluorescence
    in shortwave
    ultraviolet
    light (253.7 nm) and weak light pink fluorescence in longwave UV.
    Physical Properties
    Lustre:
    Sub-Adamantine, Vitreous, Sub-Vitreous, Greasy, Silky, Pearly
    Transparency:
    Transparent, Translucent
    Colour:
    Colorless, white, pale blue, pale green, gray, brown
    Streak:
    White
    Hardness:
    4½ - 5 on
    Mohs scale
    Tenacity:
    Brittle
    Cleavage:
    Perfect
    Perfect on {110}, poor on {101}, {001} rare
    Fracture:
    Irregular/Uneven, Sub-Conchoidal
    Density:
    3.475 g/cm
    3
    (Measured)    3.484 g/cm
    3
    (Calculated)