lo Bulletin of Laboratories of Denison University [Voi. xr. 
in any little creek, until our existing terraces stand as witnesses 
to their energy. 
At different times and places in the three southeastern 
counties of Indiana, men who seemed to know what they were 
talking about, agreed in their statements that from Dillsboro 
almost exactly south to near Vevay, the hills are capped with 
boulders and gravel ; and that none is to be found east of that 
line, except in the streams. Probably this is the real moraine. 
It remains an open question whether it crossed the Ohio near 
Vevay; or whether the material about the mouth of the Ken- 
tucky river may not have accumulated in the same manner as 
at Split Rock,'’ namely, by ice-borne and torrential deposit 
in a temporary lake caused by a col below Madison, Indiana. 
In all cases where drift is reported as existing on the 
“high lands,” or the “ highest hills, ” the person who essays 
to complete this unfinished work, should take pains to ascertain 
just how high they are. The suggestion seems scarcely neces- 
sary ; but in reading some of the articles on this matter one 
would infer that water, instead of hunting the lowest places 
and flowing through, sought the highest places and climbed 
over. 
Editorial Note. — Since the presentation of Mr. Fowler’s article before 
the Ohio State Academy of Science I have had the pleasure, through the kind- 
ness of the Cincinnati Society of Natural History, to visit the region around 
Cincinnati discussed by Mr Fowke and I take pleasure in stating that I believe 
Mr. Fowke has presented the best correlation of the complicated topographical 
features of the Cincinnati district that has been offered up to date. His broad 
generalizations as to the sequence of events are certainly suggestive of the vast 
amount of field work yet to be done before the full history can be written. 
