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| mintabie opal |
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OPAL IN AUSTRALIA |
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| The
Mintabie Field |
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The Mintabie opal field lies west of the
main north-south road between Adelaide and
Alice Springs, just south of the Northern
Territory border. It is about 340 km by
road from Coober Pedy. Barnes et al (R0239)
state that:
Aerial photographs of the area depict
country not unlike that around Lightning
Ridge. Aboriginals are reported to have
sold black opal from an unknown source in
Coober Pedy as early as 1919 (Keeling, R1629).
It took local miners over 10 years to discover
floaters along the Mintabie escarpment,
but mining was intermittent because of the
isolation of the field and the harder rocks
in which the opal occurred.
In 1976, heavy
equipment was moved into the area. Despite
the advent of the bulldozers and backhoes,
blasting is at times necessary because of
the hardness of the overlying rocks, before
the heavy equipment can be used. However
this has resulted in the production of much
opal, often of excellent quality. In recent
years the production has rivalled, and even
exceeded that of Coober Pedy.
By 1980, a small settlement had grown at
Mintabie, but miners still had to travel
some 400 km to Coober Pedy or 500 km to
Alice Springs for their main supplies. Now
the situation has eased because of the completion
of the standard gauge railway to Alice Springs
from the south.
The railway passes within some 50 km of
the field, and supplies brought in by train
can be obtained from the small, newly developed
town of Marla. The township of Mintabie
has also grown to the extent that there
is a restaurant and other facilities, as
well as a number of permanent homes to supplement
the temporary houses and caravans.
There is also a good airstrip so that there
is rapid access to the field by light aircraft
from the cities, as well as making available
the services of the Royal Flying Doctor
Service. |
| Geology |
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The geology
of the opal bearing horizons at Mintabie
differs from that of the other Australian
opal fields. Although Mintabie is
still at the very edge of the Great
Artesian Basin, the opal is found
in more consolidated
beds underlying the Lower Cretaceous.
The opal occurs mainly in these Paleozoic
horizons, which have yet to be dated
accurately, but may be Devonian or
as old as Ordovician. The rocks in
which the opal occurs are cross-bedded
sandstones, dipping slightly to the
southwest. The opal occurs in horizontal
bands parallel to the bedding, or
at times in vertical or steeply dipping
fissures. Opal has also been found
at deeper levels in an underlying
somewhat less consolidated sandstone.
The difference in the nature of the
opal bearing horizon at Mintabie does
not necessarily indicate a difference
in age for the formation of the gemstone,
despite its occurrence in older rocks.
The overlying physical conditions
are related, in that soluble silica,
formed from the decompositional weathering
of complex silicates, could be transported
downwards until the appropriate openings
were encountered for the entrapment
of the colloidal particles.
Somewhat similar conditions seem to
apply for the formation of precious
opal in the Brazilian fields in the
area of Pedro Secundo, where the opal
has been deposited, apparently by
weathering processes, in cavities
in broken basalt.
The Mintabie
opal itself is generally of good
quality. Keeling (R1629)
states that: |
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