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<br />Shelter at Laurie LaMotte Memorial Park <br /> <br />Included in your packet is a map of the park previously used when a concession building was being <br />consideedr. It is useful in this potential project too as it shows where the water and electricity come <br />into the area and where the shelter could be located. Remember, a water fountain can be placed in the <br />area, but there would not be sewer so it would have to be designed with a different water type runoff. <br />It would be possible to put electrical into the shelter. <br /> <br />1601 LaMotte Drive <br /> <br />The house and garage on this property were demolitioned the week of November 27, 2006. When the <br />foundation was removed it was discovered there was a capped well underneath the foundation that <br />appears to be an artesian well. Mr. Tedd Peterson questioned the 8t. Paul Water Utility who said there <br />were only like nine (9) artesian wells registered along Centerville Lake and this one was not registered, <br />but that is what it appears to be. Once the foundation was removed the cap on the well was broken and <br />cool, clear water is shooting out of the pipe continually. Public Works will cap it for now, but wanted <br />the committee to consider using this for perhaps some type of fountain. Below is a description of an <br />artesian well: <br /> <br />artesian well, deep drilled well through which water is forced upward under pressure. The water in an <br />artesian well flows from an aquifer, which is a layer of very porous rock or sediment, usually <br />sandstone, capable of holding and transmitting large quantities of water. The geologic conditions <br />necessary for an artesian well are an inclined aquifer sandwiched between impervious rock layers <br />above and below that trap water in it. Water enters the exposed edge of the aquifer at a high elevation <br />and percolates downward through interconnected pore spaces. The water held in these spaces is under <br />pressure because of the weight of water in the portion of the aquifer above it. If a well is drilled from <br />the land surface through the overlying impervious layer into the aquifer, this pressure will cause the <br />water to rise in the well. In areas where the slope of the aquifer is great enough, pressure will drive the <br />water above ground level in a spectacular, permanent fountain. Artesian springs can occur in similar <br />fashion where faults or cracks in the overlying impervious layer allow water to flow upward. Water <br />from an artesian well or spring is usually cold and free of organic contaminants, making it desirable for <br />drinking. <br /> <br />Committee Member Amundsen sent out the following email to the committee regarding the <br />property: <br /> <br />I'm meeting Maria Perez, Engineer Technician, Rice Creek Watershed District on Monday, December <br />4th @ 3:30pm on the site of the not yet named (Lake Park) property. Anyone or everyone is <br />welcome. It's an informal meeting to look at the property and discuss the lake shore erosion, possible <br />rain garden locations and any other program options that we might have available to us through the <br />RCWD. I will report back to the P&R group at Wednesday's meeting. <br /> <br />I walked the property for my first time on Thursday. For those of you who haven't walked it yet the <br />lake shore will need to be addressed. It's a two foot drop from the grass (where there is grass) to the <br />water. The waves are just working at the soil everyday. Roots are the only thing holding the dirt back <br />is some areas. There is also an 8" to 10" culvert sticking out of the ground about 25 feet from the <br />shore. I don't know where it starts. I'll look more closely on Monday. There is Black Locust growing <br />along the shoreline which is a non-native plant/treelbush that has very sharp thorns. <br /> <br />40f5 <br />