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It can be seen that decreasing the coupling strength advances phase across all photoperiods.
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The biomechanical measurements of reaching in the absence of vision showed that all groups were impaired in the advance phase of the reach, but only the advanced PD subjects were additionally impaired in the withdrawal phase of the reach.
Control and mild PD subjects did not differ in the time to complete the skilled reaching task, whereas the advanced PD subjects displayed increased movement times for both the advance phase and withdrawal phase of the reach [8].
In contrast to the slow advance phase, the retreat phase may take only a few decades.
Fig. 3 Upthrust advance phase glacial lacustrine sediment (LTA3) at the toe of the Eureka River landslide.
LTA5 retreat phase glaciolacustrine sediment; LTA4 glacial sediment (including till); LTA3 advance phase glaciolacustrine sediment; LTA2 massive sands (with bone dates of 25.1 ka BP); and.
Each of the landslides we described had a basal rupture surface within the advance phase glaciolacustrine sediment (LTA3) or near the base of the glacial sediment (LTA4).
The landslide's rupture surface, in advance phase glaciolacustrine sediment (LTA3), extended under the channel creating a Type VI landslide dam (Cruden et al. 1997, Fig. 9).
The landslide rupture surfaces, in advance phase glaciolacustrine sediment or glacial sediment, extend under the channel causing the channel to be elevated and forming Type VI dam.
The landslide's rupture surface, in advance phase glaciolacustrine sediment (LTA3), extended beneath the streambed causing it to be elevated by approximately 20 m, creating a Type VI landslide dam.
Our main findings for Peace River area landslide dams are as follows: The landslide rupture surfaces, in advance phase glaciolacustrine sediment or glacial sediment, extend under the channel causing the channel to be elevated and forming Type VI dam.
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