The New Encyclopædia Britannica, Volume 19Encyclopaedia Britannica, 1981 - Encyclopedias and dictionaries |
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Page 176
Sand dunes and loess deposits Lake Bonneville and Great Salt Lake Resigna- tion over Maynooth. centre polygons are indicative of actively growing ice wedges . The troughs surrounding the high - centre poly- gons indicate that the ...
Sand dunes and loess deposits Lake Bonneville and Great Salt Lake Resigna- tion over Maynooth. centre polygons are indicative of actively growing ice wedges . The troughs surrounding the high - centre poly- gons indicate that the ...
Page 436
... sand- stone or limestone , whereas soil or sediment refers to unconsolidated , uncemented material , such as sand , grav- el , or clay . Porosity is defined as the ratio of the volume of voids to the total volume of the material under ...
... sand- stone or limestone , whereas soil or sediment refers to unconsolidated , uncemented material , such as sand , grav- el , or clay . Porosity is defined as the ratio of the volume of voids to the total volume of the material under ...
Page 438
... sand that the flow rate Q was directly proportional to the energy loss , inversely proportional to the length of the flow path , and proportional to a coefficient K that de- pends on the type of sand . The coefficient K is also sub ...
... sand that the flow rate Q was directly proportional to the energy loss , inversely proportional to the length of the flow path , and proportional to a coefficient K that de- pends on the type of sand . The coefficient K is also sub ...
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