5 
yfayette, Ia, 
traversing the drift, and the bottom of the wel ssa : 
idea of 
the water comes from below the slate iA out at this local: 
iy: “A glance at the map will show by t 
ground at the well. It follows from this that we cannot - 6 
of reaching the marlite-waters. It was obtained im every 
other wells have been dug in the city for the expressed P ise 
stance, but did not overflow. 
«Physical 
taken freshly from the well. The deposit upon the peb 
is pleasantly brackish, resembling in taste, the liquor fro 
freshly opened. The density, from a mean of six ODE 
is 1:00523. : 
