By A. L. Farley
The Atlas of British Columbia is the 1st significant cartographic research of the province to be released given that 1956. Created via shut co-operation among govt, the non-public zone, and the unviersity, it's the successor to the British Columbia Atlas of assets which, for two decades, has been the normal reference paintings utilized by colleges, undefined, executive, and most people. the newest facts to be had were used to offer a correct, complete photo of British Columbia’s economic climate because it is at the present time. Comparative reports express the improvement orf the province’s manpower and ordinary assets in addition to the fast progress of and know-how because the starting of the century. In occasion, the emphasis of the atlas displays millions of particular requests for updated source details rercorded during the last ten years.
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Additional resources for Atlas of British Columbia: People, Environment, and Resource Use
Moisture is insufficient to support tree growth under natural conditions. The annual addition of organic matter from grass items and roots results in a dark topsoil. Chernozemic soils are fertile but often droughty. The Brown, Dark Brown, Black soils form a sequence from the drier to the wetter parts of the grasslands. The Dark Gray soils occur along the grassland/forest margins. Cryosolic Soils contain permafrost (permanently frozen ground) because of their association with cold, exposed locations in higher latitudes.
Some aspects of the variation in quantity are outlined in the preceding text and on Map 15. Among the attributes of water quality that are readily measurable are clarity (expressed as turbidity), temperature, and chemical content. Depending upon the use to which the water is put, any or all of these and a number of other variables may be of considerable importance. For example, a sports fisherman is likely to prefer a clear stream to a turbid one regardless of the dissolved mineral content; the supervisor of a steam plant is likely to be more concerned about the relative water hardness of boiler feed than about its temperature.
The profiles from stream to stream vary largely because of differences in precipitation and temperature of the respective areas. The Cowichan River on Vancouver Island, for example, has a seasonal pattern that suggests it is rain-fed, the discharge being much higher in the fall and winter months than in the summer when rainfall is modest. Most of the graphs shown, though, display the characteristics of snow-fed streams, peak discharges occurring at the time of maximum snow (or glacial) melt. In the northeast especially, snowmelt is complemented by the precipitation regime, since maximum rainfall occurs in the summer months.
Atlas of British Columbia: People, Environment, and Resource Use by A. L. Farley
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