✨ Discovery of the day
Year: 1949
El Kantara Gorges
The town of El Kantara is the result of Mio-Pliocene and Quaternary filling. The Ain Skhoun source is the most important in the region, the El Kantara wadi or El Haï wadi is made up of small dams which are in turn formed into four irrigation canals, to ensure the water supply of the commune. The climate is cold in winter and hot in summer. The commune is crossed by Algerian national road no. 3 and by the railway line coming from Batna and going towards Biskra.
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25 stamps
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Sericite schist
Flora
27 years
👁 50
Calco-alkaline granite
Flora
27 years
👁 49
Gneiss - Eye
Flora
27 years
👁 48
Papaver rhoeas linnaeus
Flora
29 years
👁 39
Lonicera arborea boisier
Flora
29 years
👁 38
Ficaria verna huds
Flora
29 years
👁 39
Lilac
Flora
31 years
👁 35
Zinnias
Flora
31 years
👁 30
Dahlias
Flora
31 years
👁 26
Marne in Turitella
Flora
32 years
👁 30
Cipoli
Flora
32 years
👁 32
Lite-eroded sandstone
Flora
32 years
👁 30
Ophrys apifera huds
Flora
32 years
👁 29
Ophrys lutea cavan
Flora
32 years
👁 30
Orchis simia lam
Flora
32 years
👁 31
Apricot
Flora
33 years
👁 31
Cognassier
Flora
33 years
👁 32
Medlar
Flora
33 years
👁 30
Lavandula stoechas - L (Lavender Stoechade)
Flora
34 years
👁 30
Silybum marianum - L (Milk thistle)
Flora
34 years
👁 31
Rhamnus alaternus - L (Buckthorn Alaternus)
Flora
34 years
👁 30
Ajugo iva - L (Musk Bugle)
Flora
34 years
👁 31
Cyclamen africanum - Cyclamen
Flora
35 years
👁 26
Dianthus crinitus - Carnation
Flora
35 years
👁 30