. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. 400 I 0= , Structure, from \ gravity study 675 81 Fig. 22. Crustal sections computed to fit the seismic and gravity data for Bermuda and Oahu. (After Woollard, ) -400 S TRUCTURE -300 SECTION THROUGH HAWAIIAN ISLANDS Distance kilometers -200 -100 0 100 200 300 400. Fig. 23. Crustal section computed for Hawaii. (After Worzel and Talwani, unpublished.) another mass distribution to account for the gravity anomalies for Hawaii. In this case there were considerably more gravity data available. Fig. 23 shows the resultin
. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. 400 I 0= , Structure, from \ gravity study 675 81 Fig. 22. Crustal sections computed to fit the seismic and gravity data for Bermuda and Oahu. (After Woollard, ) -400 S TRUCTURE -300 SECTION THROUGH HAWAIIAN ISLANDS Distance kilometers -200 -100 0 100 200 300 400. Fig. 23. Crustal section computed for Hawaii. (After Worzel and Talwani, unpublished.) another mass distribution to account for the gravity anomalies for Hawaii. In this case there were considerably more gravity data available. Fig. 23 shows the resulting section. The asymmetry indicated in the section would be more exaggerated if the section were made farther to the southeast and less exag- gerated if it were made farther to the northwest. A continuous gravity profile has been obtained on an east to west crossing. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Hill, M. N. (Maurice Neville), 1919-. New York : Interscience Pub.
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