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1906
Contained within the 1st Edition (1906) of the Atlas of Canada is a map that shows the delineation of drainage basins. The geographic extent of each drainage basin is delineated and the total area drained for each basin is provided in square miles. This includes the great oceanic drainage basin and the Hudson Bay basin.
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Contained within the 1st Edition (1906) of the Atlas of Canada is a map that shows the delineation of drainage basins. The geographic extent of each drainage basin is delineated and the total area drained for each basin is provided in square miles. This includes the great oceanic drainage basin and the Hudson Bay basin.
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1915
Contained within the 2nd Edition (1915) of the Atlas of Canada is a map that shows the delineation of drainage basin. The total area drained is indicated in square miles for each basin, and drainage basins of the principal river systems of Canada, along with their areas. This includes the great oceanic drainage basins and the Hudson Bay basin. Only the
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Contained within the 2nd Edition (1915) of the Atlas of Canada is a map that shows the delineation of drainage basin. The total area drained is indicated in square miles for each basin, and drainage basins of the principal river systems of Canada, along with their areas. This includes the great oceanic drainage basins and the Hudson Bay basin. Only the
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DEVELOPMENT OF A DRAINAGE BASIN AND CHARAC-TERISTICS OF THE DRAINAGE BASINS OF JAPAN
Geographical Review of Japan, 1965By statistical analyses of the geometry of drainage basins formed by fluvial processes, the author obtained some important knowledge related to the development of a drainage basin, and made clear the hypsometrical characteristics of the drainage basins of Japan.
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The Geographical Journal, 1976
The geomorphological study of drainage basin changes can be visualized against the background of seven types of study. These include studies of morphometry, of basin characteristics and basin processes, of channel geometry, of theoretical approaches, of basin dynamics and of palaeohydrology.
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The geomorphological study of drainage basin changes can be visualized against the background of seven types of study. These include studies of morphometry, of basin characteristics and basin processes, of channel geometry, of theoretical approaches, of basin dynamics and of palaeohydrology.
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Drainage‐basin characteristics
Eos, Transactions American Geophysical Union, 1932Factors descriptive of a drainage‐basin as related to its hydrology may be classified broadly as:(1) Morphologic—These factors depend only on the topography of the land forms of which the drainage‐basin is composed and on the form and extent of the stream‐system or drainage‐net within it.((2) Soil factors—This group includes factors descriptive of the ...
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2016
The most conspicuous geomorphic feature of the Sunderbans is a low, alluvial plain intersected by an intricate network of tidal rivers, creeks, estuaries and minor tidal-water courses. The Thakuran River is one of the most important tidal rivers of a meso-macrotidal regime having no perennial freshwater supply, and it forms a drainage basin covering ...
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The most conspicuous geomorphic feature of the Sunderbans is a low, alluvial plain intersected by an intricate network of tidal rivers, creeks, estuaries and minor tidal-water courses. The Thakuran River is one of the most important tidal rivers of a meso-macrotidal regime having no perennial freshwater supply, and it forms a drainage basin covering ...
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