



Granite Intrusions GCCB 5-8 resulting from the collision of the microcontinents of Ganderia and Avalonia in the Devonian Period.
When viewing on a PC, click on any image to enlarge it in a carousel of all the pictures.
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Granite Intrusions GCCB 5-8 resulting from the collision of the microcontinents of Ganderia and Avalonia in the Devonian Period.
When viewing on a PC, click on any image to enlarge it in a carousel of all the pictures.
Beautiful texture! I love these blog posts!
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Thank you, Fred.
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Special. Thank you.🙂
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Thank you, Sandy.
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