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The northeastern US and Canada typically have acidic soils, often with a high percentage of organic matter due to the region's forests. These soils tend to be nutrient-poor and have a mixture of clay, silt, and sand particles. The specific soil type may vary depending on local geology and climate conditions.
Olof Tamm has written: 'Northern coniferous forest soils' -- subject(s): Soils, Forest soils
S. A. Wilde has written: 'Soils of Wisconsin in relation to silviculture' -- subject(s): Forest soils 'Russia of the tsars and poets' -- subject(s): History 'Forest soils' -- subject(s): Forest soils, Forests and forestry, Soils
Calcareous or chalky soilsPeatClay soilsSandy soils
The cast of Soils of Canada - 1978 includes: Walter Massey
George Filz has written: 'Engineering properties of Southeast Alaskan forest soils' -- subject(s): Forest soils
The Interior Plains of Canada are important because they contain both mineral and forest resources which provide raw materials for industry and rich soils for farming. The southern and eastern region contains fertile soils and sufficient rainfall to support wheat farming. The region is called the Bread Basket of Canada. The northern region contains forested lands, with the trees exploited for lumber, pulp, and paper.
Soils of Southern Colorado are mostly clay.
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Forest soils tend to be rich in organic matter, have higher acidity, and more microbial activity due to the decomposition of leaf litter and organic debris from trees. Prairie soils, on the other hand, are often characterized by a thicker topsoil layer, higher pH levels, and lower organic matter content, as grasses do not contribute as much organic material as trees.