Figure F8. Lithostratigraphy and selected lithologic and wireline log properties of sediments at Site 1186. Depths are in meters below seafloor (mbsf). There was no coring from 0 to 697.4 mbsf. High values of the lightness variable "L" are light-colored sediment in the L*a*b system (Blum, 1997), but many of the spikes to darker colors are caused by gaps among cored pieces or by other artifacts. The a-axis of chromaticity in the L*a*b color scheme shows variation between green (low values) and red (high values), and the b-axis shows variation between blue (low values) and yellow (high values). Higher values of magnetic susceptibility generally correlate with bands rich in volcanic ash (e.g., Core 192-1186A-13R) or with claystone (e.g., Core 192-1186A-26R). Natural gamma radiation intensity is from the FMS tool run, and medium-penetration resistivity and caliper of borehole diameter are from the geophysical tool run (see "Downhole Measurements," ). A key to the graphic lithology is on Fig. F4, p. 40, in the "Explanatory Notes" chapter.

Figure F8. Lithostratigraphy and selected lithologic and wireline log properties of sediments at Site 1186. Depths are in meters below seafloor (mbsf). There was no coring from 0 to 697.4 mbsf. High values of the lightness variable "L" are light-colored sediment in the L*a*b system (Blum, 1997), but many of the spikes to darker colors are caused by gaps among cored pieces or by other artifacts. The a-axis of chromaticity in the L*a*b color scheme shows variation between green (low values) and red (high values), and the b-axis shows variation between blue (low values) and yellow (high values). Higher values of magnetic susceptibility generally correlate with bands rich in volcanic ash (e.g., Core 192-1186A-13R) or with claystone (e.g., Core 192-1186A-26R). Natural gamma radiation intensity is from the FMS tool run, and medium-penetration resistivity and caliper of borehole diameter are from the geophysical tool run (see "Downhole Measurements"). A key to the graphic lithology is on Fig. F4 in the "Explanatory Notes" chapter.