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Village Creek Artesian Springs Earthcache EarthCache

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geoaware: This EarthCache has been archived because it no longer meets the EarthCache guidelines. If you wish to update this EarthCache, please reference the guidelines at www.earthcache.org. Once you have updated your listing, please email the EarthCache Approver at earthcache@geosociety.org.

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Hidden : 3/24/2005
Difficulty:
1.5 out of 5
Terrain:
1.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

This spot is almost like quicksand as the artesian spring water comes through the ground. This artesian spring is nearly always visible, there is another spot (N 30 20.825 W94 14.329) with about 8 springs coming to the surface side by side which are visible so long as the creek isn't too high. There are some other ones in the area if you look around some. Unfortunately, people tend to dump trash around here, So take a little trash when you leave.


Artesian spring openings are very subtle, so doen't expect a strong water flow, that would be rare or more along the lines of an artesian well which is man made(see illustration). Several artesian springs may combine and make a larger spring that is easily seen, but an isolated artesian spring is often difficult to see, so don't expect a heavy water flow. Take a picture of any of these springs as proof of your find.

Artesian water is rain water which has fallen on some porous bed or stratum of earth and has followed the sloping course of this bed between other beds, which were sufficiently dense enough to trap water until it has found an opening to the surface, whether natural or manmade, at a lower level than its original source, so as to flow down-hill. When this opening is a natural one it is a spring; when artificial it is an artesian well.

In order to produce an artesian spring, there must be the proper conditions. These conditions depend upon the geology, topography, and its rainfall. The geologic conditions are that there shall be a continuous porous stratum enclosed between two strata that are impervious. Topographically it is necessary that the exposed portion of this porous stratum--the "catchment" basin--be at sufficient elevation above that of the mouth of the wells to force a steady flow of water by hydrostatic pressure; and finally the rainfall must be sufficient within the area covered by the catchment basin to secure the steady supply of water.

Unless all of these conditions be favorable there can be no constant supply of flowing water obtained. Below is how the artesian springs in Edwards are created, although the artesian spring for this cache is located on Village creek, rest assured that all artesian springs originate in a similar manner.

Click photo labeled How artesian springs are made
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