Sentence examples for seaward surface from inspiring English sources

Sixty kilometers landward from the most seaward surface breaks, the fault patterns become more intricate (Figures 2 and 3), presumably a reflection of these faults' interacting with the pre-existing fabric of the Pacific Plate and each other as they propagate (e.g., Ranero et al. 2003).

In our study area, however, BSRs are distributed seaward of the surface probe data (Kinoshita et al. 2011) and cannot be used for comparison.

When an enhanced river flow and a strong down-estuary wind both occur at the spring tide, the surface seaward advective salt flux increases significantly, whereas the tidal salt flux is also enhanced, becoming the main contributor to the landward salt transport.

For a higher, more consistent bounce, Seaward needed a firmer surface, without the weed grass that caused dead spots.

This terrace surface is inclined seaward.

A floating ice sheet of considerable thickness attached to a coast (usually of great horizontal extent with a level or gently undulating surface); often a seaward extension of ice sheets.

In a steadily subsiding basin in which accommodation balances sediment flux, the depth of a eustatic lowstand determines the paleo-depth of the deepest clinoform inflection point and the seaward limit of the erosional transgressive surface, whereas the duration of a lowstand controls the amount of progradation that takes place.

Consistent with previous field observations, friction does not significantly alter the gradient of the water surface elevation and a seaward-dipping water surface elevation is observed during the majority of the swash process.

The basal surface of this incision extends seawards under six to seven Late Quaternary depositional sequences preserved on the mid and outer shelf.

The study provides explicit data on how dynamic pressures vary vertically from the seabed to the still water surface and on the resulting forces, both seaward and shoreward.

This study provides explicit data for the vertical variation of the dynamic pressures from the seabed to the still water surface and for the resulting forces, both seaward and shoreward.