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Removal of the landslide material which occurs mainly by water erosion results in steepening of the slopes within the scarp and upper transportation area of the landslide and also creates longer slopes below landslide parts that were described as unstable in 2009 (numbers 1, 2, 3 and 4 in Fig. 1).
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The red line roughly follows the longitudinal profile of the lower Saddle River (below the landslide).
The red line (cross-section) roughly follows the longitudinal profile of the lower Eureka River (below the landslide).
The results below show a landslide victory, and for Van Gaal it will be a welcome sigh of relief as the United faithful believe the squad are on course to achieve this season's target of a return to European football.
The dashed black line shows the suggested slip surface of the shallow landslide below the main scarp where the spring is also shown.
Their uncertainties are below 20%% for all the landslides except for nine of them, reaching a maximum of 68 % for small landslides.
The study area was limited to an altitude of 500 m, as no landslide data were found below this altitude (Fig. 2).
The volcano, Anak Krakatau — or "Child of Krakatoa" — caused a landslide either above or below the water's surface and created enormous waves.
Minimum values for S below which no landslides can occur at all are: 0.33, 0.36, 0.39, and 0.41, respectively in sub-area 1, 2, 3, and 4. By separating the data with shallow landslides and without shallow landslides in the S-C field, a factor T 2 from Fig. 6 can be obtained: {T}_2=S+0.8Cge {C}_{r2} (5)in which T 2 is the factor; C r2 is the critical value for triggering shallow landslides.
Minimum values for S below which no landslides can occur whatever the value of G are: 0.33, 0.36, 0.39, and 0.41, respectively in sub-area 1, 2, 3, and 4 with or without the free-face factor F. The critical value C r3 is 0.60, 0.65, 0.70, and 0.74, respectively in sub-area 1, 2, 3, and 4 for a free-face (F > 0) and 0.73, 0.78, 0.83, and 0.87 for sites without a free-face (F = 0) (Fig. 7a-d).
Prime Minister John Key flew over the destruction in Kaikoura by helicopter as aftershocks kicked up dust from the landslides below.
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