. Bulletin of the Geological Society of America. Geology; Geology -- United States. Figure 1.âSection near Great Barrington (after Dana). Julien, in a paper entitled "On the Geology at Great Barrington, Massachu- sctts," || has described the same locality. Mis views of the geologic structure are expressed in figure -yd*/ ii s, schi'bb or gneiss. q,q_uarUytc d* d* clolomyfce. a , an- e-n-cieivt fault Jo, 111. o fe 1-fcceii-t fa-ult. Figure 2.âSection near Great Barrington (pftei Julien). Mr. T. Nelson Dale,!] assistanl geologisl in the Archean division of the United states Geologi
. Bulletin of the Geological Society of America. Geology; Geology -- United States. Figure 1.âSection near Great Barrington (after Dana). Julien, in a paper entitled "On the Geology at Great Barrington, Massachu- sctts," || has described the same locality. Mis views of the geologic structure are expressed in figure -yd*/ ii s, schi'bb or gneiss. q,q_uarUytc d* d* clolomyfce. a , an- e-n-cieivt fault Jo, 111. o fe 1-fcceii-t fa-ult. Figure 2.âSection near Great Barrington (pftei Julien). Mr. T. Nelson Dale,!] assistanl geologisl in the Archean division of the United states Geological Survey, visited the Searles-Hopkins quarry al Great Barrington on October 5 and 14, L889, and Mr. J. !â¢'. Wolff examined the gneiss later microscop- *Now in the hands of tlie public printer at Washington. I l'h' Grej lock Synclinorium : \m. Geol., vol. \ iii, pp. l-T. [ On the Quartzite, Limestone and Associated Ro -k- of the vicinity of Gri i( Barrington, B shire eonnty, M if \m. Journ. Sci., 3d series, vol. v, 1873, p. 26, fig. 7. gOn Taconic Bo lis and Stratigraphy, with i logical Map ol the Taconic Region: Vm. Journ. Sci., 3d Beries, vol. \ \ \iii, 1887, p. WO, with plate 11. Trans New Ifork Acad. 8ci., vol. v, 1887, p ⢠i hi p ii i ji imIi and the ai npanying figure "â were prepared for this paper by Mr. Pale. I.\ III , 'â >.,,,. Soi . \ Vol .3 1891,. 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 Geological Society of America. [New York, etc. ] The Society
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