Sentence examples for meltwater into from inspiring English sources

The Shyok, Shigar, Gilgit, and other streams carry glacial meltwater into the Indus.

The recharge of subglacial meltwater into underlying bedrock and sediment aquifers created transient reversals in the long-term equilibrium flow directions of basinal fluids.

Based on the TiO2-normalized plots of Al2O3 and Fe2O3, the similarity of the source rocks in the two lakes is high (Figure 4d), suggesting the discharge of homogenous meltwater into both lakes.

The recharge of meltwater into the ice sheets bed was instrumental in generating poorly sorted diamict sediments (till) by sliding-induced shearing and deformation of overpressured sediment and soft rock.

So far, the AMOC has not suffered a dramatic shutdown, but it is slowing, and scientists worry that a rapid increase in Greenland ice melt as the Arctic continues to warm will pour ever more meltwater into the North Atlantic, severely disrupting the conveyor system.

Gentle mounds were separated by valleys, and these led down to waterfalls of meltwater cascading into the ocean.

In the Arctic, summer gravity drainage is enhanced by flushing, as snow and ice meltwater percolate into the ice.

As we cover clumpy, sometimes boggy, terrain, Huw points out Lennox Falls, plunging over the Forbes mountains, and Mount Earnslaw, whose meltwater runs into the Rees: "They say no man ever steps in the same river twice and that's never been truer than for the Rees".

Unfortunately for the 1m people who live around the lake's shore, the conclusion of this research is that something similar could easily happen again.The tsunami of 563 started at the opposite end of the lake from Geneva, at the point where it is fed by glacial meltwater carried into it by the Rhône.

The kame belt demonstrates the development of a complex glacier karst typified by the evolution of subglacial meltwater tunnels into an englacial and supraglacial meltwater system dominated by ice-walled lakes and migrating ice-contact drainage networks.

A subsequent major change in alluvial architecture resulted from fundamental changes in seasonal water and sediment input that marked the end of glacial meltwater input into the valley about 12.4 ka (10,500 14C yr B.P).