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Jeweller - August Issue 2018

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GEMSTONE ORIGINS<br />

MANY OF THE MINERS WERE FAMILIES WORKING<br />

IN SMALL GROUPS WITH WOMEN DOING MUCH<br />

OF THE HEAVY LABOUR<br />

PICKS, SHOVELS, BUCKETS AND HUMAN MUSCLE<br />

WERE THE ONLY MINING TECHNIQUES USED IN<br />

THE SAPPHIRE FIELDS<br />

in the country are to do with religious sites<br />

such as the Rock-Hewn Churches at Lalibela,<br />

which is a UNESCO World Heritage site. This<br />

site consists of 11 medieval monolithic cave<br />

churches from the 12th to 13th centuries<br />

and are still a place of pilgrimage and<br />

worship today.<br />

SAPPHIRE FIELDS NEAR CHILA<br />

Our expedition started with the sapphire<br />

fields near Chila. This was an area where<br />

we had the least information as to what<br />

was going on and did not know what<br />

to expect as far as the size of the mining<br />

area, the amount of miners involved or the<br />

nature of the mining. While much of what<br />

we witnessed met our preconceived ideas<br />

of the artisanal mining operations, seeing<br />

the exact nature of the mining proved<br />

very interesting, as well as learning about<br />

the reported transformation of the socioeconomic<br />

nature of the area.<br />

GEOLOGY<br />

Based on analytical results, it is clear that<br />

the sapphires are related to alkali-basalt<br />

flows. According to geological maps, there<br />

are several alkali basalt outcrops in the area,<br />

but the maps don’t indicate their presence<br />

around Chila. However, there are clearly<br />

basalt flows near the sapphire mines. Basalt<br />

flows can cover incredibly large areas<br />

with thick layers of molten rock, often in<br />

successive events.<br />

Based on our observations, the sapphirecontaining<br />

basalt flows were deposited<br />

on a flattened basement. This basement<br />

contains heterogeneous rocks of a granitic<br />

composition that belong to the Precambrian<br />

era (older than 540 Ma). The basalt flows<br />

are much younger and were deposited<br />

in the Cenozoic period (younger than 65<br />

Ma). The basalts erode much easier than<br />

the basement, creating a very wide valley<br />

flanked by flat plateaus.<br />

In the centre of the valley, we could see<br />

exposed basement. The sapphires have<br />

been released from their basalt host<br />

rock by weathering. The richest sapphire<br />

concentrations are found in the centre of<br />

the valley near the riverbed, although many<br />

miners are also working on the hill flanks.<br />

According to the locals, sapphires have also<br />

been found on top of the basalt plateaus,<br />

indicating that a lot of the basalts are<br />

sapphire bearing.<br />

MINING<br />

All of the mining we saw was classic<br />

artisanal mining on the secondary deposits.<br />

The deposits are ideal for artisanal mining<br />

techniques and family/community mining<br />

efforts. We saw no mechanisation in the<br />

mining whatsoever. All the miners in the<br />

area first dug pits with picks and shovels.<br />

Then, the gravel was taken out of the pits,<br />

often by just flinging it to the top of the pit<br />

with a shovel or by using buckets. It was<br />

then sorted through for sapphires by hand,<br />

often with just dry picking.<br />

It appeared that the dry sorting missed<br />

many of the smaller size sapphires and that<br />

most of the stones the artisanal miners were<br />

recovering were above one gram. This was<br />

also evident when we tried to buy samples<br />

for research in one-carat to half-gram sizes.<br />

It was difficult to find any sapphires in that

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