^'^^ KANSAS ACADEMY OF SCIENCE. 



For weeks, and in some cases even months, water would seep into 

 the cellars m the north part of Salina from the saturated soil, even 

 where the surface seemed comparatively dry. Certain it is that we 

 have had a great object-lesson on the power of water as a geological 

 agent, and a few repetitions of the flood of 1903 would bring about 

 vast changes m the topographical features of the state. 



