INDEX TO WATER LEVELS CHAMPLAIX-HUDSON VALLEYS 261 



Cook, G. H., Cited, 236% 245-, 247^ 

 Coolidge, P. T., cited, 213\ 

 Oopake, faults, 235\ 

 Corinth, delta at, 147^ 

 Cornelius, E., cited, 247^ 

 Cornwall terrace, 115'-16^ 

 Corson, J. P., cited, 247\ 

 Coveville outlet, 19(3^-97^ 

 Coveville stage of Lake Vermont, 



243^-44\ 

 Covey hill, evidence from the 



northern face of, 162--64^ ; shore 



lines about, 173"-74^ 

 Croll, J., cited, 247«. 

 Crosby, W. O., cited, 2471 

 Croton 'point, 102'-5® ; deposits 



south of, m'-98\ 

 Croton point stage, 98^ 

 Croton river, character of valley, 



230\ 

 Crown Point Peninsula, fossils on, 



213«. 

 Crugers, clays at, 105^-6^. 

 Cushing, H. P., cited, 168% 210% 247% 

 Cut cliff in till near Port Kent, 



204^-5% 

 Cylichna alba (?), 200% 213% 



Dana, J. D., cited, 72% 219*, 247% 



Dannemora mountain, southern 

 slope of, 160®. 



Danskammer terrace, 119*. 



Darwin, Charles, cited, 184% 



Davidson, G., cited, 72^ 



Davis, W. M., cited, 75% 247% 



Dawson, George M., cited, 167% 187% 



Dawson, Sir J. W., cited, 210% 215% 

 215% 218% 



Deformation by postglacial faults, 

 234^-36% 



Defreestville, faults, 235% 



De Geer, cited, 221% 



De Kay, J. E., cited, 247% 



Delebecque, cited, 72% 



Deltas, three, of Adirondack Hud- 

 son, 147^-49^ ; of the Champlain 

 valley, 168^-74. 



Desor, E., cited, 218% 248% 



Dewey, C, cited, 248% 



Dresden gravels, 153''-54% 

 Dryer, C. R., cited, 248% 

 Duparc, cited, 72^ 

 Durkeetown terrace, 138% 

 D wight, W. B., cited, 188% 248% 



East Bouquet mountain, parallel 



roads on, 168% 

 Eaton, A., cited, 248% 

 Eights, J., cited, 18G% 248% 

 Elevation of land in the southern 



Hudson valley, evidence of 



higher, 229^-31% 

 Elevation theory, possible objec- 

 tions to, 232^-34% 

 Emerson, B. K., cited, 181% 186% 



186% 

 Emmons, Ebenezer, cited, 76% 161% 



175% 188% 212% 215% 218% 221% 



248% 

 Englewood sand plain, 92^-93% 

 Esopus creek, character of valley, 



231% 

 Explanation of plates, 254-59. 



Fairchild, H. L., cited, 163% 248% 



Fairhaven Yt., delta of Poultney 

 river at, 150^-51% 



Far Rockaway gravels, 233*. 



Far Rockaway ridge, 89''-90% 



Faults, postglacial, deformation hj, 

 234^-36% 



Finch, J., cited, 248% 



Fishkill creek, character of valley, 

 230% 



Fitch, Asa, cited, 166% 176% 187% 

 229\ 



Flat Rock spillways, 161^-62% 



Forel, F. A., cited, 72% 



Fort Edward district, 138^-51^; be- 

 low the glacial terraces, 143--44% 



Fort EdAvard outlet, 198% 



Fossils, in Champlain deposits, dis- 

 tribution, of, 208'-W; depth of 

 submergence indicated by, 215*- 

 16% 



Fl-eydenburg's Mills, fossils at, 

 211«-12% 



Frontal moraine, '98^-100% 



Fuller, M. L., cited, 90% 233% 248% 



