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Conglomerates and sandstones of the Eocene Carmelo Formation were deposited by sediment gravity flows, in relatively deep water, in a submarine canyon probably comparable to the present-day Monterey Canyon. Updated / edited version of an older panorama.
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GigaPan Comments (4)
Toggle Minimize gigapan_commentZoltan Sylvester (November 21, 2008, 03:05PM )
Thanks for the comments. Ron - it was not easy to get rid of the vignetting; I applied first Vignetting Reducer (vignetting.republika.pl
/) to each photograph,
and that helped quite a bit, but some vertical
dark bands were still visible. I tried to make
these less obvious in Photoshop. [It looks like I
will have to buy the real deal, Photoshop Elements
is unable to open these big files.]
Ron Schott (November 21, 2008, 02:56PM )
Looks great Zoltán! How did you get rid of the vignetting?
Tom Czerwinski (November 21, 2008, 12:19PM )
Great looking pano, Zoltan!
Ralph Fernandez (November 21, 2008, 12:06PM )
Magnificent,