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View south and west from high on Taseq slope in the Ilímaussaq complex, SW Greenland.

Ilímaussaq, SW Greenland

Known to geologists for nearly 200 years, the Ilímaussaq alkaline complex in South West Greenland has only recently become recognized as a world-class fluorescent mineral locale.

The two principal fluorescent minerals here, sodalite and tugtupite, are present in many distinctive varieties, some of which are also photochromic or tenebrescent.

Reversibly photochromic (or tenebrescent) sodalite before, during, and after illumination with shortwave ultraviolet.
Photochromic sodalite from Ilímaussaq, SW Greenland

Fluorescent colors range from pastel pinks through lavender, vibrant reds and orange. Together with associated fluorescent minerals they provide specimens in a bewildering variety of patterns and hues.

 

Specimens of sodalite (orange) and tugtupite (red) from Ilímaussaq, Greenland, showing different fluorescent responses to different UV sources.

 
Tugtupite from Kvanfjeld
Tugtupite from Kvanfjeld
Tugtupite 'treasure box'. Specimens from Kvanefjeld, Ilímaussaq, SW Greenland. Width 30 cm.
Tugtupite xls from Taseq slope.
Tugtupite crystals from Taseq slope, Ilímaussaq, SW Greenland
Tugtupite from Kangerluarsuk
Tugtupite and beryllite
Tugtupite from Kvanfjeld
Tugtupite from type locale
Tugtupite crystals from the type locale, Tugtup agtakorfia
Tugtupite and analcime
Tugtupite rimming chkalovite
Tugtupite with chkalovite and beryllite
Tugtupite slab from Kangerluarsuk, Ilímaussaq, SW Greenland
Tugtupite (pink) and sodalite (orange) from Tunulliarfik, Ilímaussaq, SW Greenland.
Complex fluorescent specimen with tugtupite (pink) and polylithionite (yellow-white) from Kangerluarsuk, Ilímaussaq, SW Greenland.
Tugtupite from Kangerluarsuk (close-up view)
Sodalite from Kangerluarsuk, Ilímaussaq, SW Greenland.
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