Tranomaro in 1991 >> |
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Geographical division |
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We will distinguish: |
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1 the volcanic solid mass of |
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Androy, it is covered with |
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thorny bush and meadows. |
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2 the gneissic zone of to |
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Mandrarean Androy, fields |
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plains and hills, rare zones |
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of savanna on of red ground |
At the time |
calcareous carapace. |
of the great |
Altitude varies there from |
dryness in |
600 meters on the hills |
the south. |
to 250 meters at the bottom. |
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3 the western slope of the high Anosyans |
chains which tops are staged between |
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1500 and 2000 meters. It is a field of |
meadows. |
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Geological divisions. |
1 Crystalline schists. |
Gneiss with diopside, syenitic eysies |
gneisses, arteritic injections, gneiss at |
cordierite, etc. |
2 Old eruptive rocks. |
Pegmatites, Dissogénites, Esirians |
granites , charnockites, kalambatreans |
granites, late granites . |
3 Recent eruptive rocks. |
(Volcanic solid mass of Androy) |
a) A the base, a thick basaltic |
subhorizontale series . |
b) Basaltic dykes. On the road to Andranondambo |
c) A thick higher subhorizontale rhyolitic series. |
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d) Rhyolitic dykes . |
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4 Recent formations. |
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If russet-red sands are excluded, the recent |
formations have only a very weak development. |
It is necessary to quote the alluvial plains of |
Androtsy, Esira, Sangoria and Pisopiso. |
A notable calcareous carapace covers most of the area. |
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The anosyans granites are regarded as synorogenes, eocambrians |
formed in the androyans series to which an age higher than 2400 MY |
is allotted. |
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The esirians granites present very variable crushings of intensity which |
often give them a gneissic facies . |
Sometimes, there is passage to orthogneisses. General foliation is sub meridian. |
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The occurrences of the Andranondambo area were industrially exploited since 1993 and have been |
almost abandoned few years later. This, because of difficulties to exploit sapphire direct in the |
bedrock, usually corundum is not concentrated enough. Furthermore, the hardness of the |
rock makes its exploitation very expensive. |
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All of the pictures on this website have been shot by gggems.com |
Text written by Alain Darbellay. |
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