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Aerial image 293400
Rock and mountain landscape in Val Forno in Graubuenden, Switzerland. Rock breaks during orogeny because of the enormous forces which act on the hard layers and rock masses. Cracks open deep even several hundreds and thousand meters in the undergound. Hot fluids circulate there in the hot depth of the earth, fill the cracks and cristallise when the rockformation is lifted during the orogeny and cools down. During erosion, the cracks appear as bright dykes in the dark grey and brown rock

VAL FORNO 28.08.2011

Aerial image Val Forno - Rock and mountain landscape in Val Forno in Graubuenden, Switzerland. Rock breaks during orogeny because of the enormous forces which act on the hard layers and rock masses. Cracks open deep even several hundreds and thousand meters in the undergound. Hot fluids circulate there in the hot depth of the earth, fill the cracks and cristallise when the rockformation is lifted during the orogeny and cools down. During erosion, the cracks appear as bright dykes in the dark grey and brown rock

https://www.aerialphotosearch.com/info/aerial-photos/rock-mountain-landscape-val-forno-graubuenden-switzerland-rock-breaks-during-orogeny-because-enormous-forces-which-act-hard-layers-rock-masses-cracks-open-deep-even-several-hundreds-thousand-meters-undergound-hot-fluids-circulate-there-hot-depth-earth-fill-cracks-cristallise-when-rockformation-lifted-during-orogeny-cools-down-during-erosion-cracks-appear-bright-dykes-dark-grey-brown-rock-293400.html https://www.aerialphotosearch.com/info/aerial-photos/rock-mountain-landscape-val-forno-graubuenden-switzerland-rock-breaks-during-orogeny-because-enormous-forces-which-act-hard-layers-rock-masses-cracks-open-deep-even-several-hundreds-thousand-meters-undergound-hot-fluids-circulate-there-hot-depth-earth-fill-cracks-cristallise-when-rockformation-lifted-during-orogeny-cools-down-during-erosion-cracks-appear-bright-dykes-dark-grey-brown-rock-293400.html

Rock and mountain landscape in Val Forno in Graubuenden, Switzerland. Rock breaks during orogeny because of the enormous forces which act on the hard layers and rock masses. Cracks open deep even several hundreds and thousand meters in the undergound. Hot fluids circulate there in the hot depth of the earth, fill the cracks and cristallise when the rockformation is lifted during the orogeny and cools down. During erosion, the cracks appear as bright dykes in the dark grey and brown rock. Restriction: No POD - Print on Demand uses allowed! Photo: Bernhard Edmaier

Aerial image ID: 293400
Image resolution: 6850 x 4090 pixels x 24 bit
compressed image file size: 15,18 MB
Image file size: 80,16 MB
Sources and credit: © euroluftbild.de/Bernhard Edmaier

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