Ontario · Great Lakes & St. Lawrence Lowlands
Where your water goes
Your sub-basin
Northern Lake Erie
then
St. Lawrence River
It arrives here
Atlantic Ocean
Everything that falls here works its way east and north to the Atlantic. It is the drainage that carried the fur trade inland and the log drives back out, and the one Atlantic salmon and American eel still use — the eel travelling the whole length of it to spawn in the Sargasso Sea.
Basin 02G (Canadian sub-drainage area)
The river right now
150%
of the ten-year median for this date · 88.5 m³/s against 58.8 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 28% 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
Middle Devonian sedimentary · Middle Devonian
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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Hamilton Group · Middle Devonian
· Devonian
The soil it made
What that means
Easy ground for most vegetables and fruit. Iron and manganese start to get harder to reach at the top of this band, which shows up as yellowing between the veins on young leaves.
Happy here without a fight
Brassicas, beets, spinach, peas, lilacs, clematis and most herbs. Hydrangeas come out pink.
If you want the rest
Leave it. If acid-lovers are the point, grow them in containers or a made-up bed rather than fighting the whole garden.
Working it
A balance of sand, silt and clay — the texture that holds enough water to matter and still drains, which is why loam is the one everybody wants.