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Page 2648, results 66176 - 66200

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Geology and geography of the Henry Mountains region, Utah
Charles B. Hunt, Paul Averitt, Ralph L. Miller
1953, Professional Paper 228
The Henry Mountains region in southeastern Utah is one of the classic areas in geology because of the study made there by Grove Karl Gilbert in 1875 and 1876. His report on the geology of the mountains was the first to recognize that intrusive bodies may deform their host rocks...
Water, frost, and frost resistance of natural and artificial building stones
H. Breyer, S. H. Britt (translator)
1953, Open-File Report 54-33
The worst enemy of construction engineering and of construction material is uncontrollable water, whether it be ground-, seepage-, rainwater, water of condensation, or melting snow and ice, exerting objectionable pressure upon tracks and roads. this applies as well to structures above the ground as to bridge piers and foundations, road...
Water resources of the Minneapolis-St. Paul area, Minnesota
Charles Henry Prior, Robert Schneider, W. H. Durum
1953, Circular 274
The water supply of the Minneapolis-St. Paul area is adequate to satisfy present requirements and requirements for many years to come if the area continues to develop at about the present rate. The flow of -the Mississippi River at the Twin Cities is more than sufficient to meet the demands of...
Irrigation and streamflow depletion in Columbia River basin above The Dalles, Oregon
Wilbur Douglas Simons
1953, Water Supply Paper 1220
The Columbia River is the largest stream in western United States. Above The Dalles, Oregon, it drains an area of 237,000 square miles, of which 39,000 square miles is in Canada. This area is largely mountainous and lies between the Rocky Mountains and the Cascade Range. The Kootenai, Pend Oreille,...
Floods of 1950 in the upper Mississippi River and Lake Superior basins in Minnesota
C. G. Paulsen
1953, Water Supply Paper 1137-G
In areal coverage and magnitude of peak discharge the floods of April-May 1950 in the Missouri River Basin in North and South Dakota were unprecedented in the area. These floods were characterized by an extremely late spring breakup of ice, by great flood peaks resulting from snow melt, and by...