. Carnegie Institution of Washington publication. FIG. 5 (Blackwelder).—Yen-chuaug, Shan-tung. Section of Cambrian strata in the western part of the Kiu- lung-shan. i =gray gneiss; 2=bright green shale; 3=gray earthy limestone; 4 = dense blue-black limestone; 5= brown and yellow shale; 6 = blue-gray limestone; 7=shaly gray limestone; 8= dense blue-black limestone; 9 = yellow shale; 10 = gray limestone and shale; n =slaty black limestone; 12 = chocolate slate; I3=brown shaly sandstone; I4 = yellow shale; is=buff earthy limestone; i6 = red shale. (Section continued in fig. 6.). 1718 19 ZO 21 z»
. Carnegie Institution of Washington publication. FIG. 5 (Blackwelder).—Yen-chuaug, Shan-tung. Section of Cambrian strata in the western part of the Kiu- lung-shan. i =gray gneiss; 2=bright green shale; 3=gray earthy limestone; 4 = dense blue-black limestone; 5= brown and yellow shale; 6 = blue-gray limestone; 7=shaly gray limestone; 8= dense blue-black limestone; 9 = yellow shale; 10 = gray limestone and shale; n =slaty black limestone; 12 = chocolate slate; I3=brown shaly sandstone; I4 = yellow shale; is=buff earthy limestone; i6 = red shale. (Section continued in fig. 6.). 1718 19 ZO 21 z» 25 Z6 2728 29 3O~ 31 ///25 2627 28 29 3031 32 FIG. 6.—I7=black limestone; i8=yellow shale; 19 = purple-gray limestone; 2O = gray limestone; 21 = yellow shale and thin limestone; 22 =red shale and thin limestcne: 23 = green-gray limestone; 24 = red and yellow shale; 25=maroon shale; 26 = greenish conglomeritic limestone; 27=brown shale; 28 = buff earthy limestone; 29 = olive-green shale; 30 = cross-bedded green-gray limestone; 31 =olive shale; 32 =gray sandy limestone; 33 =hard dark oolite; 34 = light and dark gray limestone; 35 =green shale; 36 = dense gray limestone; 37= green nodular shale and thin limestone; 38 = massive dark limestone. The scale of thickness of figures 5 and 6 is iudicated in 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 Carnegie Institution of Washington. Washington, Carnegie Institution of Washington
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