History of the Water Supply of the World: arranged in a comprehensive form from eminent authorities, containing a description of the various methods of water supply, pollution and purification of waters, and sanitary effects, with analyses of potable waters, also geology and water strata of Hamilton county, Ohio, statistics of the Ohio river, proposed water supply of Cincinnati. — John Shaqi
History of the Water Supply of the World: arranged in a comprehensive form from eminent authorities, containing a description of the various methods of water supply, pollution and purification of waters, and sanitary effects, with analyses of potable waters, also geology and water strata of Hamilton county, Ohio, statistics of the Ohio river, proposed water supply of Cincinnati.Bell, Thomas J. (Thomas Jefferson)
History
History of the Water Supply of the World: arranged in a comprehensive form from eminent authorities, containing a description of the various methods of water supply, pollution and purification of waters, and sanitary effects, with analyses of potable waters, also geology and water strata of Hamilton county, Ohio, statistics of the Ohio river, proposed water supply of Cincinnati.
Bell, Thomas J. (Thomas Jefferson)
Water-supply -- History; Water-supply -- Ohio -- Hamilton County
---+-------------+------------+------------------------------+----------
| SYSTEM. | GROUP. | STRATA. |THICKNESS.
---+-------------+------------+------------------------------+----------
| | | | FEET.
1 | Drift. | Alluvial | Clay, sand, and gravel. | 123
| | drift. | |
| | | |
| { | Base of | |
2 | Devonian. { | Hamilton. | Dark bituminous shale. | 15
| { | Helderberg.| Dark and gray limestone with |
| | | bands of chert. |
| | | |
| { | Niagara. | Sandy above, darker and | 626
3 | Upper { | | argillaceous below. |
4 | Silurian. { | Clinton. | Red, brown, and gray shales | 162
| { | | and marls. |
| | | |
| { | Hudson | |
5 |Lower { | Trenton. | Greenish calcareous shale. | 1058
6 |Silurian. { |Calciferous.| Light drab sandy magnesian | 475
7 | { | | limestones. |
| { | Potsdam. | White sand-rock, calcareous. | 316
---+-------------+------------+------------------------------+----------
Temperature of well at bottom, 88 degrees, being uniform for 90
feet, at 53 degrees, will make an increase of one degree for every
additional 71 feet. It was the opinion of Prof. Newberry, that, if
water was successfully struck, it would be of a saline character.
Dubuque, Iowa, is supplied by a spring accidentally struck while
tunneling in a neighboring drift.
At the upper basin of the Thames River there are seven springs, whose
capacity is estimated at 32,000,000 gallons daily.
Liverpool, England, has four wells, with a combined capacity of
6,000,000 gallons daily.
Birmingham, England, has four wells, from which the water company
derives 8,000,000 gallons daily.
Washington has over 400 wells, and Cincinnati about 300, nine of
which are artesian, that were bored by private enterprise.
The deepest well in the world is near Berlin--4194 feet deep without
piercing the salt formation.
WELL BORING.
The art of boring into the earth was practiced by the Chinese 2,000
years ago, the feature of their system being the percussive action of
a tool suspended by a flexible rope.
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