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Victoria University Antarctic Research Expedition Science and Logistics Reports 1984-85: VUWAE 29

Figure 8. Cross-section of Ferrar Valley through the CIROS 2 site, showing water depth and 3 estimates of the geometry of the valley fill. 1 is from Burdelik (1981) and based on 3 seismic refraction profiles (shown by arrow heads) parallel to the valley axis. 2 is a reinterpretation of Burdelik's data by F.J.Davey (letter to P.J.Barrett, October 1982). 3 is a sketch by Barrett based on the valley slopes above sea level and on profiles across the east-trending Dry Valleys, all of which have thei…

Figure 8. Cross-section of Ferrar Valley through the CIROS 2 site, showing water depth and 3 estimates of the geometry of the valley fill. 1 is from Burdelik (1981) and based on 3 seismic refraction profiles (shown by arrow heads) parallel to the valley axis. 2 is a reinterpretation of Burdelik's data by F.J.Davey (letter to P.J.Barrett, October 1982). 3 is a sketch by Barrett based on the valley slopes above sea level and on profiles across the east-trending Dry Valleys, all of which have their lowest point just north of the middle of the valley. Basement was encountered at 377m below sea level, between estimates 2 (330m) and 3 (430m).

Figure 8. Cross-section of Ferrar Valley through the CIROS 2 site, showing water depth and 3 estimates of the geometry of the valley fill. 1 is from Burdelik (1981) and based on 3 seismic refraction profiles (shown by arrow heads) parallel to the valley axis. 2 is a reinterpretation of Burdelik's data by F.J.Davey (letter to P.J.Barrett, October 1982). 3 is a sketch by Barrett based on the valley slopes above sea level and on profiles across the east-trending Dry Valleys, all of which have their lowest point just north of the middle of the valley. Basement was encountered at 377m below sea level, between estimates 2 (330m) and 3 (430m).