The New Encyclopædia Britannica, Volume 19Encyclopaedia Britannica, 1981 - Encyclopedias and dictionaries |
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Page 170
... flow characteristics in existing valley gla- ciers reveals two general types of flow , extending flow and compressional flow . Both may occur in different reaches of the glacier stream . Extending flow occurs in the steeper reaches and ...
... flow characteristics in existing valley gla- ciers reveals two general types of flow , extending flow and compressional flow . Both may occur in different reaches of the glacier stream . Extending flow occurs in the steeper reaches and ...
Page 438
... flow , kinetic energy of groundwater is ne- glected because groundwater velocities are very small . During flow , groundwater experiences a frictional loss in energy caused by contact with the walls of the granular medium along its ...
... flow , kinetic energy of groundwater is ne- glected because groundwater velocities are very small . During flow , groundwater experiences a frictional loss in energy caused by contact with the walls of the granular medium along its ...
Page 707
... flows . The tubes are enclosed in a shell with provisions for the other fluid to flow through the spaces between the tubes . Fluid flowing outside the tubes can be directed either in the same direction as or counter to the effective flow ...
... flows . The tubes are enclosed in a shell with provisions for the other fluid to flow through the spaces between the tubes . Fluid flowing outside the tubes can be directed either in the same direction as or counter to the effective flow ...
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