Summary

Kansas: A Cyclopedia of State History… (1912)

Artesian wells are most readily obtained where the geological formations possess a moderate inclination or dip, and are composed of strata of materials impervious to water (rock or clay) , alternating with such as—like sand or gravel—allow it to pass more or less freely. The rain water falling where such strata approach to or reach the surface will in great part accumulate in the pervious strata, rendering them 'water bearing.' Thus are formed sheets of water between two inclined, impervious walls of rock or clay, above as well as below, and exerting great pressure at their lower portions.
Source: Wikisource

Kansas: A Cyclopedia of State History… (1912)

Recent developments tend to show that the early experiments in artesian wells in Kansas were only comparatively successful or altogether failures because the drillers did not go deep enough. Most of the wells have gone no further than the first pervious stratum. Somewhere there is a source of pressure sufficiently strong to furnish an abundant supply of water if the stratum connected with it can be reached.
Source: Wikisource

Kansas: A Cyclopedia of State History… (1912)

I have a 6-inch bored well in my door yard, 135 feet deep, with 8 feet of water. Over a year ago I noticed that at times a strong current of air came out of the openings around the pumpstock, and by observation find it to be an excellent barometer, as it blows from 6 to 20 hours preceding a storm. I have placed a brass whistle in the space, which at times can be heard a quarter of a mile. The harder and longer it blows the more intense the coming storm will be.
Source: Wikisource

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