[aprox 20 seconds to load] [repeats 5 times] In the animation above, you will fly into the sample locality on the cliffs below SIO. The scene mixes multibeam bathymetry, DEMs, air photos, helicopter oblique photos, chirp seismic lines, and underwater dive photography. As you approach the cliff, you will see figures from Schwehr and Tauxe (2003). Schwehr and Tauxe (2003) uses bootstrapped eigen values to distinguish fabric shape. Natural sedimentary fabrics should be oblate or spherical. Based on fabric shape we were able to differentiate between normal, crypto-slumped, and slumped layers. The Fledermaus scene used for this movie is available at my La Jolla demo site.