THE MINERAL GMELINITE
- Chemistry: (Na2, Ca)Al2Si4O12 - 6H2O, Hydrated sodium calcium aluminum silicate
- Class: Silicates
- Subclass: Tektosilicates
- Group: Zeolites
- Uses: Mineral specimen and chemical filter.
Gmelinite is one of the lesser known and rarer zeolites.
Zeolites have an openness about their structure that allows large ions and molecules to reside and actually move around inside the overall framework.
The structure actually contains open channels that allow water and large ions to travel into and out of the crystal structure.
The size of these channels controls the size of the molecules or ions and therefore
a zeolite like gmelinite can act as a chemical sieve, allowing some ions to pass through while blocking others.
Crystals of gmelinite have a unique shape that could be described as being an angular version of a classic UFO flying saucer.
It is hexagonal in outline and is dominated by a dipyramid (two identical pyramids at the top and bottom).
However, the faces of the pyramids are relatively gentle in slope and are capped by a flat pedion face.
- Color is clear, white, pink, yellowish and reddish.
- Luster is vitreous.
- Transparency: Crystals are transparent to translucent.
- Crystal System is hexagonal.
- Crystal Habits include tabular to platy crystals with a clear hexagonal outline.
The crystals have a gently sloping hexagonal dipyramid
that terminates the top and bottom of the crystal that are often truncated by pinacoidal faces.
The overall effect gives the look of an angular classic UFO flying saucer.
Twinning is common with penetration twins.
- Cleavage is absent.
- Fracture is uneven.
- Hardness is 4.5.
- Specific Gravity is approximately 2.0 - 2.1 (very light)
- Streak is white.
- Other Characteristics: Vertical striations are seen on the dipyramidal faces.
- Associated Minerals are quartz,
and other zeolites.
- Notable Occurrences include Siegerland, Germany; Glenarm, Northern Ireland; New Jersey and Faroe Islands.
- Best Field Indicators are crystal habit, density, hardness and associations.