126 J. D. Dana—Discharge of the flooded 
flooded streams; and that all the drift-deposits of the New 
Haven region, now thirty to fifty feet above mean tide, were 
included in the freshwater formations—the saltwater beds be- 
twenty feet has the revers cross-bedding. ow if it can be 
shown that Mill River was throughout its course a violent 
* Tbid., x, 191. + Ibid., x, 173. 
