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  • This paper discusses three late Ordovician paleosols developed on andesite flows near Arisaig, Nova Scotia. These paleosols provide additional data for the Holland-Pinto model of soil development, and serve as a check on the model's validity.
  • 1989
  • In Holocene soils relict patterned ground and cryoturbated soil horizons were the most common relict soil properties. This paper provides a description of these relict soil properties and the environments under which they developed.
  • 1989
  • Soils are the product of soil forming factors, including climate and vegetation. Therefore, fossil soils are above all appreciated by geomorphologists, who wish to deduce past climates, conditions of the development of landforms. In this paper
  • 1989