All Natural Spring Water

Mountain Mist bottles all natural spring water right at our source. 

Spring (hydrosphere)

A spring is a point where groundwater flows out of the ground, and is thus where the aquifer surface meets the ground surface.  Dependent upon the constancy of the water source, rainfall or snowmelt that infiltrates the earth, a spring may be ephemeral, (intermittent) or perennial (continuous).

Formation

Water issuing from an artesian spring rises to a higher elevation than the top of the confined aquifer from which it issues. When water issues from the ground it may form into a pool or flow downhill, in surface streams. Sometimes a spring is termed a seep. 

Minerals become dissolved in the water as it moves through the underground rocks. This may give the water flavor and even carbon dioxide bubbles, depending upon the nature of the geology through which it passes. This is why spring water is often bottled and sold as mineral water, although the term is often the subject of deceptive advertising. Springs that contain significant amounts of minerals are sometimes called 'mineral springs'.

Classification

Springs are often classified by the volume of the water they discharge. The largest springs are called "first-magnitude," defined as springs that discharge water at a rate of at least 2800 L/s.

 

The scale for spring flow is as follows:

Magnitude

Flow (ft³/s, gal/min, pint/min)

Flow (L/s)

1st Magnitude

> 100 ft³/s

2800 L/s

2nd Magnitude

10 to 100 ft³/s

280 to 2800 L/s

3rd Magnitude

1 to 10 ft³/s

28 to 280 L/s

4th Magnitude

100 US gal/min to 1 ft³/s (448 US gal/min)

6.3 to 28 L/s

5th Magnitude

10 to 100 gal/min

0.63 to 6.3 L/s

6th Magnitude

1 to 10 gal/min

63 to 630 mL/s

7th Magnitude

1 pint to 1 gal/min

8 to 63 mL/s

8th Magnitude

Less than 1 pint/min

8 mL/s

0 Magnitude

no flow (sites of past/historic flow)

 

*Information obtained from Wikipedia, the free encyclopedia http://en.wikipedia.org/wiki/Spring_(hydrosphere)

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