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Dorothy H. Radbruch

Publications and source records attributed to Dorothy H. Radbruch.

6 recordsLinked to original sources

Status of engineering geologic and environmental geologic mapping in the United States

1. Engineering geologic maps in the United States may be one map prepared as part of a larger study of environmental geology, individual areal geologic maps containing additional engineering geologic data, or engineering geologic maps of single construction sites. 2. No systematic methodology for engineering geologic or environmental geologic maps has been developed. 3. Environmental geology studies combine the efforts of workers in a number of geologic fields to produce many maps of basic data, as well as various interpretative maps, only one of which may be an engineering geologic or foundation conditions map. Maps of many scales may be prepared for a single study, depending upon the geologic conditions, the main problems of the area, and the principal needs. 4. New technology, including computers and various types of aerial photography, is constantly being developed, and its use is being encouraged to increase the speed and efficiency of map preparation. 5. The use of engineering geologic and environmental geologic maps in the United States is constantly growing; such maps will continue to be made in increasing numbers.

Bulletin of the International Association of Engin

Map showing recently active breaks along the Hayward fault zone and the southern part of the Calaveras fault zone, California

This map is one of a set that shows the traces of the inferred most recently active faults of the San Andreas and related fault zones of the San Andreas fault systems (Cromwell, 1962.) It was compiled primarily to provide information for those concerned with land use and development on or near these fault zones. The map shows the locations of all known or suspected fault traces formed by recent tectonic displacements of the ground surface along the Hayward and the southern part of the Calaveras fault zones. The displacements may have been due to violent rupture during earthquakes, to imperceptible movement not accompanied by felt earthquakes (slippage or "creep"), or to some combination of both. Map users should keep in mind that the lines shown on the map are primarily guides for locating fault traces on the ground and are not necessarily located with the precision needed for every engineering or land-use project.

California