Leda clay is a soft clay, with a typical characteristics of varving (layered), high sensitivity (high ratio between peak and remolded strength), and it is usually associated with sediments which were deposited during the inundation of the glacial lakes in the prehistoric time. In some location in Canada, it has been associated with champlain or marine clays (eastern province), Leda clay (northern Ontario/Quebec areas), Lake Aggasiz clay (Winnipeg/Manitoba).
Because of the structure of the clay, in which upon disturbance it will loss its strength, lanslides occur in the areas which have this type of clay. There are lots of technical articles which were written over the years in Canadian Geotechnical Journals. Famous Canadian landslide failures, such as in Breckenridge Creek, Rockcliffe on Ottawa River, Orleans in Ontario, St. Jean - Vinney, toulnustouc river in Quebec, etc were associated with this type of soft clay.
You will see that highway cut or embankments in these areas have been cut or constructed with very flat slopes, such as 6H:1V of flatter. This is because in long term stability analysis, the remolded strength will govern, as the structure of the original clay will breakdown from disturbance, groundwater flow, loadings, etc.
Hope that this will give some insight about Leda clay.