Orbicular rocks:
(Orbicular rock from Pengonpohja, Kuru, Finland, polished slab)
This is a short guide to help you here (www.kristallin.de).
There are three pages about orbicular rocks with the navigation at the top.
left: "Einführung in das Thema" means "introduction",
middle: "ausgewählte Kugelgesteine" means "selected rocks",
right: "Vergleich mit Rapakiwis" means "compared with Rapakivis".
The page in the middle (“ausgewählte Kugelgesteine”) presents a collection of
rocks and will lead you to each single description of an orbicular rock. These
descriptions were not translated but you will find a short summary in English at
the end.
You will see a lot of interesting photos. Please note: The red button "Großaufnahme"
(large picture) next to the pictures opens them one in a really big size. The
data volumes are between 500 and 1400 KB. You need a high speed connection
otherwise you will have to be patient for about a minute. These pictures magnify
the rocks and show a lot of details. You will find no other pictures of this
quality at the web at the moment.
(You can buy the complete website at CD.
For details click here)
The rocks are mostly from Finland, one is from Sweden (Slättemossa quartz
monzonit) and one from Norway (Romsås orbicular norit).
The first and the second presented rocks I present are boulders. These boulders
were found in northern Germany (near “Buxtehude”) and in The Netherlands (nearby
“Nieuw Schoonebeek”) in glacial drift. There is no doubt that their origin lies
somewhere in Scandinavia, but the exact places are unknown.
The northern part of Central Europe is completely covered with glacial debris
transported from the North by the ice during glaciations. The guiding line of
this website (kristallin.de) is to describe these Scandinavian rocks to
recognise them here in Germany in glacial deposits.
The section “Vergleich mit Rapakiwis”
is written to show the difference between the orbicular rocks and the Rapakivis.
Both kinds of rocks are quite different but often mixed up.
The
English summary is here:
You will find the following buttons:
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What is an
orbicular rock?
Orbicular rocks are rare textural varieties of magmatic (plutonic)
rocks.
They occur in all types of composition from granitic to mafic,
ultramafic and carbonatic rocks. Most of them are composed of the
same minerals as lots of plutonic rocks: K-feldspar and
plagioclase, quartz, dark minerals like hornblende or biotite and
some other minerals.
The typical features of orbicular rocks are round bodies, called "orbicules"
or sometimes just "orbs". These orbicules show a wide variation in
size and composition. Some of them are elongated due to
deformation.
All of them contain a core in the middle surrounded by radially
grown crystals. The outer part of an orbicule shows concentric
lines - called "shells".
Some rocks have only got one single shell, but most of the rocks
contain a lot of concentric shells.
The composition of the cores can be quite different:
- Cluster of small crystals or
- single large crystals (or pieces of them), called "nucleus" or
- Xenoliths – pieces of the host rock.
These cores are always surrounded by radially grown minerals with
a transition to the shells. These shells are composed of different
layers of crystals. Some layers are of radially grown crystals
(often plagioclase), some are tangential and others are composed
just of small grains without any orientation. The visible drawing
of the shells - concentric lines - does not always correspond with
the mineral texture, which can be seen in thin sections.
The typical texture of an orbicular rock looks like this:
(Orbicular
rock from Pengonpohja/Kuru, Finland, same occurence as above,
with reddish outer
microcline shell)
If the core consists of an
agglomeration of small mineral grains, the beginning of the radial growth is
hard to see, sometimes the transition is not visible at all. See above.
The first visible line above the core that follows the shape of the orbicule, is
often the outer rim of the inner shell.
The following scheme is from:
Hans Peter Meyer:
Zur
Petrologie von Orbiculiten, (Karlsruhe 1989).
The drawing shows the typical texture of an orbicule from Pengonpohja/Kuru. The
Orbicul is dominated by shells that show different ways of texture.
The size of the orbicules is related to the
chemistry of the rock.
The big orbicules (diameters more than 10 cm up to 40 cm) are found only in
silicatic rocks with a high amount of feldspar and quartz. Mafic rocks show
smaller orbcules and the smallest ones are found in ultramafic, peridotitic or
carbonatic rocks.
The main mineral of all silicatic orbicular rocks is plagioclase and most of the
orbicular rocks are of intermediate composition. Dioritic, gabbroic or
monzonitic to quartz-monzonitic rocks are common, true granites (more than 20%
Quartz and K-feldspar > plagioclase) are also found but they are not dominating.
Mafic rocks show also orbicular texture. The strangest rock was found in a drill
core: the
carbonatite orbicular rock from SOKLI, northern Finland.
As said above – orbicular rocks are rare. One reason for that is the tiny size
of their occurences. Nearly all orbicular rocks are located at small dykes and
lenses at the margin of magmatic intrusions. The average size of such an
occurence is about some ten meters (!) in length and 3-5 meters in width. Bigger
outcrops may be found but they are extremely rare. On the other hand a couple of
very little occurrences is known and some of them are smaller than 5 meters in
diameter.
Most of the orbicular rocks found are boulders of unknown origin. In some cases
even intensive search failed. One of the most beautiful rocks is only known from
boulders. Several attemps were made to find the outcrop – without success.
It is the orbicular rock of Kuohenmaa near Kangasala in Finland:
Kuohenmaa/Kangasala. Collection of the GTK, Espoo, Finland. Polished slab:
Nearly all occurences of orbicular rocks in Skandinavia are protected.
These rocks have to be kept from any damage. Rockhounting at these outcrops is
prohibited. In some cases it is not even allowed to enter the area where the
outcrop is located.
Only the beautiful Ruskiavuor orbicular rock is quarried and can be bought. If
you are interested, please
click here.
On this website you will see some specimen of orbicular rocks. These pieces were
collected in the years between 1890 and 1895 by Deecke and Cohen in Sweden and
in Finland.
The specimen are part of the collection “Nordische Sammlung” at the University
of Greifswald in Germany.
The last pictures show mafic rocks with a
surface, which seems to look similar to orbicular rocks.
These forms are caused by weathering and are no orbicular textures at
all.
(Tenerife, roadcut at TF-24
southwest of San Cristobal de la Laguna)
The width of the photographed area is about 1m
The same place, overview:
Literature: