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ILAKAKA
 · The plateau of Ilakaka in 1992.
Ilakaka is located on the road to Tulear,
south-west of Madagascar. The discovery of
sapphire in the current of 1998 transformed 
the area.
.
· Ilakaka in 1999.
It is in the accesses of the downwards brook 
named Ilakaka that the first sapphires
were found in 1998.  The existence of gemmiferous minerals, including
 corundum was known for a long time in the sandstones
 of Isalo. French geologists having undertaken research 
 in 1946 in particular. If their discovery did not cause 
 particular interest at that time, several reasons can be 
 advanced : the political instability which reigned after 
 the second world war in the colony, and the fact that 
 the majority of corundums coming from the area of 

 Ilakaka must be heated to be marketed, indeed,

 a blue stone, but cloudy, could not inevitably let
 suppose to its discoverers that it would become pure
 and transparent after a suitable heat treatment.
 Moreover, knowledge in this field remained
 summary at that time. In Ilakaka, the arrival of 
 merchants coming from Thailand and from Sri-Lanka 
 changed things, because this group of purchasers
        became experts in "the enhancement of corundum.
      " Tsy misy mandronono, tsy misy prix"  " Thus, the cloudy stones of better quality will often
      This sentence is none by everyone in  be sold as (untreated Sri-Lankan sapphires) 
      Ilakaka.  on the international market, this because of the
      That means that : " if the stone is not milky,   difficulties in detecting heating treatment in a stone
      its owner will generally not obtain the best price   from Ilakaka not containing other inclusion only one
      from it."  haze of tiny titanium inclusions, reabsorbed after heating.
 ( Note: that true untreated Sri-Lankan sapphires are 
 rare.)
The excavations follow the gravel deposits which the                Impressing holes bore the sandstones of
Madagascans call lalam-bato, (the way of stones.)               Ilakaka testifying to the fever of sapphire.
                             
                Alain with is team in Ilakaka.
 Ankaboka, one of the many gemmiferous places of the area.
Mahasoa
· Maromiandry is located 
The sivany (sifting of gravels) in Maromiandry. 40 kilometers north of the
Seldom practiced dry as in this place distant trunk road between
from a river. Ilakaka and Sakaraha.
    

Sifting of gemmiferous gravels in river close to Maromiandry.

· VOHIMENA VAOVAO, 25 kilometers far from
Ilakaka. One of quote headlight of the sapphires
production.
The higher edges of the rivers abound in sapphires,
chrysoberyls, etc. Here in the area of  Vohimena vaovao.
 The sandstones, fragile, have been knife cut by the river.
SANDSTONES of  ISALO
The base of the group of Isalo is entirely continental. 
Sometimes significant marine incursions and of long
duration were introduced into the medium and higher
parts. The group of Isalo begins at the top from lower
Triassic and continues until the end of the Jurassic 
means.
One separates there:
Isalo I, at the base, especially sandy, continental.
Isalo II, argilo - sandy with some marine intercalations.
Isalo III, argilo - sandy with side passage to great marine 
formations.  The essential characteristic of the Isalo formations is their
 main constitution of soft sandstones, very permeable,
 badly cemented which disaggregate easily on surfaces
 by giving thick siliceous sand coverings.
 The porous nature of the sandstones constitutes an
 excellent tank which stores the water of the rains to
 restore it during the dry season. 
 · Sakalama, 60 kilometers south from Ilakaka. MADAGASCAN CORUNDUMS
At the back, ruiniform sandstones of the Isalo range.
¦ Madagascar Safari ¦ Madagascar Safari 2 ¦ Pakistan Gem Safari ¦ Sakalama ¦
Building of our cottage in Ilakaka  in 1999,  at the beginning of the sapphire rush. GEM ADVENTURE  ( Novel )
©  All of the pictures on this website have been shot by gggems.com Text written by Alain Darbellay. 
 
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