6/29/84 Stercul Fjord Just downstream from the outcrop make a mile of the river is a same terrace glacial deposits with [illegible] proportion of reddish sediment for erosion in a few place probably derived from alluvium silt. The predominant aspect of this bed is grey at a reddish cast. Joining directly across the main or glacial valley from this point other same terrace deposits can be seen on the W side of it. All this appears that there are E.S. carbonaceous silt, below the strung plane of alluvium, fix and that other plane dips S at 5-6°. In addition to the E.S. mbr. DT silt, on the NE side of the Stercul Fjord also appear to be overridden by the alluvium. This high bed oriented and revealed that the folding at Stercul appears to be very associated with this orientation. Then Stercul Fjord is a F member not a Member.