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Are old landslides in sensitive clay mapped near the home?

Parts of eastern Ontario, including much of Ottawa, sit on marine clay (Leda clay) that can fail in large slides along river valleys. The slopes concerned are part of the conservation authority's regulated hazard lands, and no open map of past slides is published for reuse.

Report check: Old landslides in sensitive clay. Entry reviewed 20 Oct 2026; each source below shows its own data date.

Land, soil and environment

How a report shows itsample, made-up home

Old landslides in sensitive clayNot published

No open map of old landslides in sensitive (Leda) clay covers this address for reuse. Unstable slopes are part of the conservation authority's regulated hazard lands, so the conservation authority for this address can say what its maps show.

Where we read it

  • Not in any report: where to look
Free checkfull report only
Full reportwhere to look
Dealbreakernot a pick

Published byConservation Ontario

What the record is

Natural Resources Canada and the Geological Survey have studied the clay and the historic slides along the Ottawa, South Nation and other rivers, and the conservation authorities map the unstable slopes they regulate. None of those maps is licensed for a product like this one.

Our reports don't read these maps. The report still lists the check, and its line points to the conservation authority for the address, whose regulated-area map shows the hazard lands.

Where it runs

No open map of old landslides in sensitive (Leda) clay covers this address for reuse. Unstable slopes are part of the conservation authority's regulated hazard lands, so the conservation authority for this address can say what its maps show.

Conservation Ontario: find a conservation authority

Sources

Look it up for one address

No record we may copy answers this check, so neither the free check nor the full report reads it. The full report still lists it, with the line above: where to look for that address.

Conservation Ontario: find a conservation authority

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