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Nova Scotia | What you're dealing with is a layer of soil(current ground level) deposited on top of the original ground level. You can dig down and see where the soil changes. It looks like there was a huge deposit of soil or mudflood at some point in recent history.The original ground level has its own contours and water paths. Where the water paths on the original ground level meet current ground level a spring develops. I see it all the time here. We tile those wet spots here. | |
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