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Supplementary Notes: Stereonets

11 of 18 Erik Eberhardt UBC Geological Engineering EOSC 433 EOSC433: Geotechnical Engineering Practice & DesignSupplementary Notes: Stereonets2 of 18 Erik Eberhardt UBC Geological Engineering EOSC 433 Discontinuity MappingWindow mappingScanline mappingHudson & Harrison (1997)23 of 18 Erik Eberhardt UBC Geological Engineering EOSC 433 Discontinuity Mapping Remote SensingMahet al.(2013)3-D laser imagingis an emerging tool for discontinuity mapping. Acquisition is performed at a safe distance, including for inaccessible areas. Millions of high accuracy 3D data points are acquired in Cartesian space, and processed efficiently by automatic algorithms, leading to robust estimates of joint dipand dip of 18 Erik Eberhardt UBC Geological Engineering EOSC 433 Discontinuity MappingWyllie & Mah (2004)35 of 18 Erik Eberhardt UBC Geological Engineering EOSC 433 Stereographic ProjectionStereographic projection allows 3-D orientation data to be represented and analyzed in 2-D.

The pole (or normal vector) of a plane allows the plane to be represented on the stereonet as a single point. Pole plots are a convenient way to examine the orientation of a large number of discontinuities, such as that measured during a discontinuity scanline survey. 90° Wyllie & Mah (2004) When the tracing paper is rotated so

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