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Shandchem
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Syneresis cracks, formed underwater due to changes in salinity in Lake Orcadie, which covered Caithness, the Orkney Isle, part of the Shetland Isles and the Southern Moray Firth during the Devonian period, approximately 390 million years ago.



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Taken on: January 18, 2015
Sets appears in:   Scotland - Caithness, North-east Scotland    Geology   
Camera: Canon EOS 700D, f/22.0, 8 sec, 51mm, ISO 100 (more info) (hide info)
Camera: Canon EOS 700D
Aperture: f/22.0
Exposure Time: 8
Focal Length: 51mm
ISO: 100
Exposure Bias: 0 EV
Flash: Off, Did not fire
Exposure Mode: Manual
White Balance: Auto
Color Space: sRGB
Software: Adobe Photoshop Elements 8.0 Windows
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