O. N. Stoddard on Diluvial Stria. Sx7 
ArT. XXVI.—Diluvial Strie_on Fragments in Situ; by O. N. 
STODDARD, Prof. Nat. Science, Miami University. 
stone, hornblende and quartz, the whole em ed in com 
clay. The striated surfaces were in the same plane, and at one 
point the underlying rock was exposed, also striated. i- 
e. iat 2 as 
e bearing of this cage upon the different theories of 
the onditions 
. is region, holding the ded: 
neath frost-bound ; - |, while t heir enormous pressure down- 
wards, prevented di placement in an upward direction, their 
Motion towards the south, gro nd down, not only the rocks in 
y and no SecbeiiGi he meter eae ae Shas, that 
glaciers once overs meal ie ion, holding the beds under- 
d, 
