Archive image from page 60 of Description, analysis and predictions of. Description, analysis and predictions of sea floor roughness using spectral models descriptionanaly00foxc Year: 1985 105, 10- 10- 2 10' ' 1- z i 103 v s O 10' I 1— < u. UJ 10° O P B-B' A-A 10-3 10-2 10-' 10° NORMALIZED FREQUENCY (CYCLES/DATA INTERVAL) 10' Figure 4-10 Composite of Figures 4-8 and 4-9 Illustrating the anisot- ropy of the sea floor In the Mendocino Fracture zone. Although both spectra retain their power law form, there Is an obvious difference In slope and Intercept. Profile B-B' appears to contain m

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Archive image from page 60 of Description, analysis and predictions of. Description, analysis and predictions of sea floor roughness using spectral models descriptionanaly00foxc Year: 1985 105, 10- 10- 2 10' ' 1- z i 103 v s O 10' I 1— < u. UJ 10° O P B-B' A-A 10-3 10-2 10-' 10° NORMALIZED FREQUENCY (CYCLES/DATA INTERVAL) 10' Figure 4-10 Composite of Figures 4-8 and 4-9 Illustrating the anisot- ropy of the sea floor In the Mendocino Fracture zone. Although both spectra retain their power law form, there Is an obvious difference In slope and Intercept. Profile B-B' appears to contain more high spatial frequency energy, while profile A-A' contains more energy In lower spatial frequencies. 39

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