Cheltenham Badlands

The Queenston shale here is red from iron oxide, and the green-grey bands running through it are where groundwater changed the iron to a different state. What makes the site unusual is the cause: this is not natural badlands but the result of poor farming practice in the 1930s that stripped the topsoil and let erosion cut the rippled gullies now visible. It became one of the most photographed spots in southern Ontario, and the trampling was destroying it, so the conservation authority closed direct access in 2015 and reopened in 2018 with a boardwalk and viewing platform only, plus timed parking reservations.

What you actually see

• The red shale - iron-stained rock cut into rippled gullies.
• The green bands - stripes where groundwater altered the iron.
• The boardwalk - a raised platform replacing the destroyed direct access.
• The erosion story - badlands created by 1930s farming, not by nature.

When to go

April to October; parking is by timed reservation in season and sells out on weekends. Low sun deepens the red. The site closes in winter.

Honest expectations

Walking on the shale is now prohibited and enforced; the visit is from a boardwalk. Parking reservations are required and limited. The site is small and takes half an hour.

Nearby

The Bruce Trail passes close; Toronto lies southeast.