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The southern flows were in an area marked by a difference between older sediments and newer, glassier rock, and the maximum ridge generated by the eruption, at the crest of the southern flow, was 13 m high.
Feature amplitude was reported as the difference between the maximum ridge value and the adjacent minimum groove value.
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The feature amplitude was measured as the difference between a maximum ridge value and an adjacent minimum groove value.
In Figures 4 and 5, CWT's ROC curves is limited in small FDR because two thresholds of the length of ridge lines and the scale corresponding to the maximum amplitude on the ridge line are used as default in MassSpecWavelet (Du et al., 2009).
However, the minimum runoff occurred at a ridge height of 6.7 cm, and the maximum sediment yield at a ridge height of 12 cm.
While for epitaxial side up ridges, the maximum temperature of heat sink is T sink (max) = 73 °C − 16 K/W*4.25 W = 5.0 °C.
For the presented epitaxial side down bonded DFB ridges, the maximum temperature to maintain CW operation is measured to be 25 °C.
The denudational pattern of the OBR (and Asahi Mountains?) can be explained if the bedrock uplift rate attains the maximum value at the ridges and decreases toward both bases (see Figure 12 of Sueoka et al. 2015).
The proposed tunnel crossing followed a mountain ridge, and the maximum depth was between 40 and, although the topography went steep down to those depths.
A secondary effect is to alter the magnitude of the maximum strain rate beneath the ridge, shifting the balance between grain growth and grain size reduction.
The strait is about 8 miles (13 km) wide at its narrowest point, and the maximum depth on its sill (submarine ridge between basins) is only a little more than 1,000 feet (300 metres).
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