2003 Greenland Tour Geo-Adventure Report:
Experience a virtual tour through
the Ilimaussaq Complex written by one of 2003’s Geo-Adventure
participants. Lots of great scenery pics, rock pics
and a simply excellent story.
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Article (in HTML) - The Fluorescent
Minerals
of the Ilimaussaq Complex,
South Greenland or click on image for a PDF File
Iceberg Arches
Mineral
Data
Greenland Mineral Data
There are several key localities offering
the collector access to many rare and unusual minerals. Some
of these areas are small intrusions perhaps only meters wide.
Many minerals in these areas are found nowhere else in the
world. Due to the rapid weathering of the friable (brittle
and easily crumbled) syenites most of the mountains have no
vegetation (no soil), and the gray and reddish hues contrast
nicely with the deep blue fjords and gleaming white icebergs.
Ilimaussaq Complex
Perhaps the most famous is the Ilimaussaq
Complex in Southwestern Greenland - an 8x17km intrusion located
between two fjords - Kangerdluarssuk fjord and Tunulliarfik
fjord. Located near the city of Narsaq, access to certain
parts of the complex (Kvanefjeld) can be made by foot, while
other areas (Kangerdluarssuk and Tunulliarfik)
requires
travel by boat. It is without a doubt the most mineral-rich
area in Greenland. Many of these minerals are new finds
for the fluorescent collector.
New fluorescent minerals from Greenland
are being uncovered almost weekly. For the latest list
and pictures of the most significant finds download
our article “The Fluorescent Minerals of Greenland”.
(printer ready)
The complex consists
of three different intrusions. First augite syenite
formed a shell along the sides and the roof, next an
alkali granite and alkali syenite formed two thin sheets
near the top, and finally the biggest part and center
of the intrusion was formed by a layered series of under-saturated
syenites. The rocks close to the roof are the oldest.
The most common rocks in these areas are a sodalite-nepheline
syenite called naujaite, an arfvedsonite-aegrine bearing
nepheline syenite called lujavrite, and a eudialyte-bearing
nepheline syenite called kakortokite.
llimaussaq
is the area with the most minerals in Greenland -
more than 200 so far, half of them silicates. Here
the silica content is much higher than elsewhere in
the world. Numerous pegmatites and hydrothermal veins,
streaks and patches are found all over the intrusion,
but are most common in the areas of Kangerdluarssuk
and Kvanefjeld. Some of the famous minerals from this
area include: Tugtupite Sodalite Polylithionite Red Syenite (Kakortokite) Ussingite
For
more information on the formation of the Illimaussaq
complex see the Minerology Pages.
For more information on tenebrescense
visit our sodalite pages.
Fiskenaesset Complex
The Fiskenaesset area includes
a matamorphosed layered magmatic complex. It occurs
in granitic gneiss bordered by amphibolites. This
area is most known for the occurrences of:
* sapphrine
* corundum (ruby)
Godthabsfjord Area
Located in
West Greendland just east of the capital (Nuuk), this area is famous
for the oldest known rocks in the world (over 3.8 billion years
old). Several popular Greenland gemstones come form this granite
complex and associated pegmatites:
* Greenlandite (chromian muscovite
fuchsite) - considered to be the “oldest” gemstone in
the world
* Nuummite (anthophyllite-gedrite masses) - a stone with dramatic
gold and blue iridescense