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sent on 17 Luglio 2013 (21:17) | This comment has been automatically translated (show/hide original)
Superb picture!
All photos of this series are very nice, and places, really sensational.
As always Zman, masterful in shooting.
Again congratulations, Greetings, Splibo.
Stupenda immagine!
Tutte le foto di questa serie sono molto belle,e i luoghi,davvero sensazionali.
Come sempre Zman, magistrale nelle riprese.
Ancora complimenti,Un saluto,Splibo.
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sent on 17 Luglio 2013 (21:20)
Greetings Splibo and a very good evening to you. Thank you for your kind words and nice compliments. Hallo |
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sent on 17 Luglio 2013 (23:54) | This comment has been automatically translated (show/hide original)
Also this beautiful, colors at the top.
Congratulations, Dino Bellissima anche questa, colori al top.
Complimenti, Dino |
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sent on 18 Luglio 2013 (9:58)
Thank you Dino. Hallo |
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sent on 18 Luglio 2013 (11:28) | This comment has been automatically translated (show/hide original)
beautiful pictures with colors really special, but you're sure this is a granite formation? I think these are basalts bellissima foto con colori veramente particolari, ma sei sicuro che sia una formazione granitica? secondo me questi sono basalti colonnari |
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sent on 18 Luglio 2013 (11:42)
Hi Mau. Thank you for nice compliment. You could be right it could be basalt I have no clear answer. Hallo |
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sent on 05 Gennaio 2014 (23:39) | This comment has been automatically translated (show/hide original)
Image, as well as beautiful, also very interesting and "teaching" that shows the internal structure of a lava flow very powerful; during cooling these flows can fracture more 'or less regularly and give rise to rectangular (columns) that have their basis a number of sides that depends on the thickness of the castings themselves.
It is not, therefore, granite but of an effusive magmatic rock.
Hello,
Emanuele
Immagine, oltre bella, anche molto interessante e "didattica" che mostra la struttura interna di una colata lavica molto potente; durante il raffreddamento queste colate si possono fratturare piu' o meno regolarmente e dare luogo a parallelepipedi (colonne) che alla loro base presentano un numero di lati che dipende dello spessore delle colate stesse.
Non si tratta, quindi, di granito ma di una roccia magmatica effusiva.
Ciao,
Emanuele
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sent on 06 Gennaio 2014 (0:15) | This comment has been automatically translated (show/hide original)
A beautiful palette of colors.
Hello Una bella tavolozza di colori.
Ciao |
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6.9 MEGAPIXEL
