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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