. Annual report. New York State Museum; Science; Science. state Museum Plate 7 Bulletin 77. H. P. Gushing, photo. The Dolgeville fault exposed in the bank of East Canada creek. At the right the fault is at the base of the vertical cliff, which consists entirely of Beekmantown layers, the Lowville capping not showing in the view. Over most of the cliff the fault breccia is still in place, so that the stratification shows only here and there. The fault plane is seen to diagonally ascend the cliff face from right to left, commencing at the dark bush and following the line of bushes. The sloping s
. Annual report. New York State Museum; Science; Science. state Museum Plate 7 Bulletin 77. H. P. Gushing, photo. The Dolgeville fault exposed in the bank of East Canada creek. At the right the fault is at the base of the vertical cliff, which consists entirely of Beekmantown layers, the Lowville capping not showing in the view. Over most of the cliff the fault breccia is still in place, so that the stratification shows only here and there. The fault plane is seen to diagonally ascend the cliff face from right to left, commencing at the dark bush and following the line of bushes. The sloping surfaces below are those of the updragged layers of Utica shale, whose stratification may be made out at the extreme Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original New York State Museum. Albany : University of the State of New York
Size: 1506px × 1659px
Photo credit: © Library Book Collection / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1900, bookdecade1900, booksubjectscience, bookyear1902
