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Where does your water cycle begin?

Does it start when you turn on your faucet in the morning to take a drink? When you jump in the shower or brush your teeth? Or is it when you wash your clothes, do the dishes, or water your lawn? Nope! In some cases, it starts hundreds of thousands of years ago.

For Mount Pleasant Waterworks customers, it starts 2,000 feet down into the earth with water that hasn’t seen light for thousands of moons. Watch our video to learn more.
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Join Our Team

Our team strives for an exceptional customer experience for all Mount Pleasant Waterworks customers. We are a diverse group of professionals working together each day to manage and operate a complex water and wastewater system. We are always looking for talented men and women to join our team.
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March Water Quality Report

pH BALANCE

8.51
S.U.
ACIDIC
NATURAL
ALKALINE
0-------------------7-------------------14
The optimal range for drinking water is between 6.5-8.5

TOTAL RESIDUAL
CHLORAMINE

3.31
PPM
0--------------------------------------4.0
The EPA sets a maximum level of 4.0 ppm in drinking water.

BACTERIOLOGICAL DATA

93
0
0
SAMPLES
minus
NEGATIVE SAMPLES
0
plus
POSITIVE SAMPLES
0
percent
% Positive Samples
0
Hardness
ppm
00 60 120 180
40
needle

Hardness is a measure of the amount of calcium and magnesium salts in water. Hard water creates scaling and soap scum. Soft water creates a better lather, but can be corrosive. Calcium chloride is added as a corrosion inhibitor.
Sodium
ppm
00 50 100
40
needle

Sodium is present in water and is one of the main salt-forming ions. Undetectable by taste at low concentrations, it helps replenish electrolytes in the body.
Chloride
ppm
00 125 250
30
needle

Chloride is found naturally in water as salt; typically as sodium chloride or calcium chloride.
Fluoride
ppm
0 2 4
0.53
needle

Fluoride occurs naturally on earth and is released from rocks into the soil, water, and air. All groundwater contains some fluoride.
Alkalinity
ppm
0 200
78
needle

Alkalinity is a measure of water's ability to neutralize acids. It results primarily from dissolving limestone or dolomite minerals in the aquifer.