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Published on 19/10/10
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Author 'Lustgarten' (Id 129791 ) : Geological time is measured in millions of years and is divided into eras, which are themselves divided into ages. The transition from one era to another is usually marked by a sharp change in facies that we see here . On the red sandstone from the Permian age (primary age), there are conglomerates distinct Triassic (Mesozoic). The transition took place there 250 million years. This passage is very clear between the two geological layers.



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Resolution : 1600x1200 Fit for your screen resolution Wallpaper Iphone (320x480)
 
 
 
 
 
EXIF : Camera: Samsung Wb550
Aperture: f/7.5 | Exposure time: 1/750 s | ISO: 200 | Focal: 4.2 mm (eq. 24 mm)| Metering: Multi-segment (5)
Prog. expo.: Priorité ouverture (2) | Correction: 0 EV | Flash: Oui(9) | Date: 14/10/2010 15:08:32
Avenue du Pin de Galle, 83220 Le Pradet, France

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