Wisconsin · Great Lakes & St. Lawrence Lowlands
Where your water goes
Your sub-basin
Rock
then
Mississippi River
then
Mississippi River system
It arrives here
Gulf of Mexico
This water joins the largest drainage in North America and travels south for thousands of kilometres to the Gulf. What runs off the fields upstream of you arrives there too, which is why a dead zone the size of a small country forms off Louisiana each summer.
Basin 070900 (USGS hydrologic unit)
The river right now
159%
of the ten-year median for this date · 1.8 m³/s against 1.1 normally
highRunning high for the date. Water will be pushy and coloured, fish will be tucked into the slack water at the edges and behind obstructions, and crossings that are normally easy are not. It is rising — about 244% more water by the end of the week.
Under your feet
About 541 million years old — from the age of the first forests, amphibians and reptiles.
All the kinds of rock, and how each one forms →
Paleozoic sedimentary rocks · Paleozoic
Cambrian sedimentary · Cambrian
Bedrock and soil figures are modelled from national geological surveys and global soil mapping, at a resolution of a few hundred metres — right for the shape of a district, not for a particular garden. River discharge is modelled, not gauged. For anything that matters, dig a hole and look.
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Cambrian, undivided · Cambrian
· Cambrian
The soil it made
What that means
The sweet spot for a vegetable garden. Nearly every nutrient is at its most available somewhere in this band, which is why it is the number every soil guide tells you to aim at.
Happy here without a fight
Almost everything: tomatoes, beans, squash, lettuce, apples, most perennials and most lawn grasses.
If you want the rest
Nothing needed. Compost keeps it here; heavy lime would push it past useful.
Working it
Fine and fertile, holding water better than sand without clay's stickiness. It caps over in heavy rain, so it wants a mulch or a cover crop rather than being left bare.