Sentence examples for and uplift in the from inspiring English sources

The orogeny was completed by strong deformation and uplift in the late Neogene.

But when it clicks, there's an optimism and uplift in the music that makes pointing out these obvious influences seem like nit-picking.

Restraining steps show compression and uplift in the zone between the segments (Biddle and Christie-Blick 1985; Wakabayashi et al. 2004).

In contrast, viscoelastic relaxation of the oceanic mantle produces an almost opposite deformation pattern to that of the mantle wedge, characterized by westward (landward) motion across the entire area, subsidence in the Tohoku district and offshore area, and uplift in the southern Hokkaido, Kanto, and Chubu districts and in the area beyond the trench (Fig. 4e).

These results, combined with previous work, indicate that strong winds, hyper-aridity, exposure of friable Neogene strata, and ongoing rock deformation and uplift in the western Qaidam Basin have created an environment where wind, instead of water, is the dominant agent of erosion and sediment transport.

People want hope and uplift in the White House and not just expressions of outrage.

Migration processes depend mainly upon the tectonic activities which have occurred through fault elements and uplifting in the study area.

Over geological history, sedimentary depressions, slopes, and uplifts may have migrated or converted between depression and uplift in a "seesaw" movement, where the fulcrums are linearly distributed in the plane, forming a hinge zone for tectonic activity.

Now let your real distaste show, too, as Michael Billington does in the Guardian by saying that "the romantic sentiment and uplift inherent in the musical sit uneasily with a story of not just heroic resistance but starvation, suffering and the death of more than 100,000 Polish Jews".

Vertical deformation at the present time, before the Tohoku-Oki earthquake, is characterized by rapid subsidence in the fore-arc side and gentle uplift in the back-arc side, with a hinge line (zero vertical velocities) running along the middle of the NE Japan arc (Fig. 5a) (Suwa et al. 2006; Nishimura 2014).

During the second stage (late syn-rift II; 143.5 138.2 Ma), the shelf-margin was affected by increasing rates of accommodation and high sediment supply, which reflects an active period of rifting triggering both tectonic subsidence in the basin, and active uplift in the hinterland.