Sentence examples for surface of the valley from inspiring English sources

The outer truncation index N dominates the fulfillment of continuity conditions (across the soil-bedrock interface) and zero-stress conditions (across the circular-arc surface of the valley).

Reflected waves from the inclined surface of the valley (displayed with white hollow triangles in Figure 10b,c,d,e) cross through the soil-bedrock interface, then interact with scattered waves from the lower corners of the valley, and finally trigger scattered waves R 2 and L 2 from the upper corners of the valley (see Figure 10f,g,h,i,j).

The Modesto area is situated on a belt of coalescing fluvial fans of low relief that lie between the dissected uplands to the east and the nearly flat surface of the valley floor.

For vertical incidence (α = 0°) in Figure 6a, the intense ground shaking (in the red region) appears almost near the center of the upper face of the alluvium and near the two intersections of the inclined and curved surfaces of the valley, especially when η ≥ 11.

Torque was mainly generated from the superior surface to the valley of the thread and the inferior and axial surfaces of the platform, while the inferior and axial surfaces of the thread did not significantly affect torque generation.

Associated surface lowering of the valley floor had a major impact on tributary stream incision but also on the available ice accumulation area at subsequent glaciations.

Primary ash fall deposits have sealed the pre-Toba surface of the Jurreru Valley, and subsequent deposition of remobilised ash has helped preserve this horizon.

The data obtained during this study provided evidence of a large conductive region beneath the surface of the Jigokudani valley that is underlain by a resistive layer at depths below 500 m.

New research aims to better understand how much methane – a potent greenhouse gas – is burbling to the surface of the Mackenzie Valley in Canada's Northwest Territories as the permafrost thaws.

The candidate arginine finger residue Arg444 is located in the loop between α3 and α4 on the concave surface of the V-shaped valley; its side chain is solvent exposed and projects from the valley bottom upwards to the open space.

These deposits are infrequently exposed at the land surface as most of the valley sides are draped by colluvial or landslide deposits derived from higher slopes.