Eastport quadrangle notebook # 5, 1908
Page 175
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Transcription
125 6/13 B2 + c Aug 7, 1908 The acid tuffs overlying S 1.6 A continue in a thick unbedded mass along the east side as far as the tiny core no. of the middle of S 1.3 where a series of banded stuccaceous sediments occur striking N 25 to 40° W and dipping NE 30°. On the west side of the corelet are observed a few bands with only Wilsonia - while both sides of the corelet are formed by about 75 feet of slightly sandy gray shales in which contain on the west side some Wilsonia? [complicate large] collectibles S 1.3 A unbedded S 1.3 B On the east side of the core beneath a mass of galber which form the point at no. S 1.3, the shales contain no Wilsonia's but instead common Leptostrophia elongata, wavelitus, "Chonetes cornuta common Spirifer var [x]crispus small), var simplex occasional Hypolithes sp Dalmanites of downinga rare Calymene sp # A couple of seams in the shale on the west side above the Wilsonia's con- tom Chonetes cornutus occasional S 1.3, B2 Dalmarella sp common Stereocisma common Wilsonia wilsoni (common) Spirifer crispus (small) , occasional Actinoptrella sp. rare (not seen) Hem