Call Number (LC) Title Results
I 19.16:264-F Permafrost and ground water in Alaska 2
I 19.16:264-G A new species of Merychippus 2
I 19.16:264-H Studies of some early Tertiary red conglomerates of central Mexico 1
I 19.16:264-I A biofacies of Woodbine age in southeastern Gulf Coast region 2
I 19.16:264-J Fossil birds from Manix Lake, California 2
I 19.16:265 Geology of the Quartz Creek pegmatite district, Gunnison County, Colorado 2
I 19.16:266 Late Paleozoic stratigraphy of central Cochise County, Arizona
Late Paleozoic stratigraphy of central Cochise County, Arizona : a report giving detailed descriptions of rocks of Mississippian, Pennsylvanian, and Permian ages, with representative sections and faunal lists of the formations concerned
2
I 19.16:267-A Geology of the Brandywine area and origin of the upland of southern Maryland 2
I 19.16:267-B Hardpan soils of the Coastal Plain of southern Maryland 1
I 19.16:268 The central Kuskokwim region, Alaska
The central Kuskokwim region, Alaska; an account of its geography, geology, geomorphology, and mineral resources including the occurrence and mining of quicksilver
2
I 19.16:269 Water-loss investigations, Lake Hefner studies : technical report 2
I 19.16:270 Water-loss investigations : Lake Hefner studies, base data report
Water-loss investigations: Lake Hefner studies, base data report
2
I 19.16:271 The natural channel of Brandywine Creek, Pennsylvania 2
I 19.16:272-A The effect of salinity on evaporation 2
I 19.16:272-B The effect of the addition of heat from a powerplant on the thermal structure and evaporation of Lake Colorado City, Texas 1
I 19.16:272-C Review of literature on evaporation suppression 2
I 19.16:272-D Evaporation from the 17 Western States 2
I 19.16:272-E A practical field technique for measuring reservoir evaporation utilizing mass-transfer theory 2
I 19.16:272-F Methods to compute long-wave radiation from the atmosphere and reflected solar radiation from a water surface 2
I 19.16:272-G Evaporation study in a humid region, Lake Michie, North Carolina 2