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Owing to this clear ambiguity, the present compilation retains only the inclination from Malta. Figure 3 exhibits together the 41 historical geomagnetic directions discussed above.
Detailed examination of the inclination from both cores shows a fluctuation in the high-temperature component at the basal part of the crystalline rhyolite namely, greater than ~70 m below the ground level for each core (Fig. 5).
The more the horizontal spacing between the wells, the more the inclination from the vertical orientation between them (if the vertical spacing is constant) and in turn, the later the communication between the wells is established.
This observation is based on plots of volume vs. angle of reach (defined as the inclination from horizontal of the line connecting the highest point on the failure scarp to the distal end of the deposit), suggesting that higher volume events have greater mobility.
These contradictory findings might be explained by differences in lung recruitability, distribution and extension of lung volume alterations, differences in chest wall compliance, the influence of abdominal weight and heart compression, the inclination from the horizontal plane and the use or not of ventral supports [3, 9, 34, 35].
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In the developed model, fibres have been added in great detail, respecting the distribution in layers, as well as the variable inclination from the interior to the exterior of the annulus, making it possible to obtain precise stresses distributions.
The dip slope has an average incline of approximately 15°, and the inclination varies from 10° to 20°.
We then compare the inclination stack from the Okhotsk Sea with the stacks of relative paleointensity and inclination from the West Caroline Basin in the western equatorial Pacific (Yamazaki et al. 2008; Fig. 5).
The inclination angles from the vertical position are 0, 145 45, and 67° clockwise (leeward direction).
In particular, the inclination factors from the Meyerhof theory appear to be inaccurate, whilst the Vesić theory does not take proper account of the self-weight.
However, non-dipolar fields (as noted in models of the Holocene geomagnetic field) are likely to contribute to the difference between an instantaneous measurement of inclination and the inclination expected from a dipolar field at the measurement site.
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