Sentence examples for cycle of erosion from inspiring English sources

The dominant model for several decades was developed and widely disseminated by William Morris Davis, who conceived an idealized normal cycle of erosion in temperate climatic regions involving the erosive power of running water.

The overall aspect of relief, however, exhibits characteristics of an early, or juvenile, stage in the cycle of erosion.

"The end of the cycle of erosion and transport and the beginning of the generation (through burial and transformation) of new materials of great value to society".

It was further explained that such a cycle of erosion occurs under conditions of a rain-and-rivers environment (what present-day investigators would call a humid climate), which were assumed to reflect the normal climate for the Earth.

Humans have set in train their own great cycle of erosion, similar to that which beset many parts of western Europe in the 18th century and which has assailed many parts of the American West since the late 19th century.

Although it is still too early in the analysis to state with certainty, it appears from the work of several investigators that there is a regional, or semicontinental cycle, of erosion and deposition that occurs every 250 300, 500 600, 1,000 1,300, and possibly 6,000 years within the Holocene.

Cycles of erosion have repeatedly worn down the ancient and austere surfaces.

As cycles of erosion and mitigation iterate, coastline change and economically driven interventions become mutually linked.

Structurally, the Greater Caucasus represents a great uplift at the margin of the Alpine downwarp about 25 million years ago and subsequently altered by fresh cycles of erosion and uplift.

This ancient setting has been broken up by movements of the Earth's crust along several zones of structural weakness and also has been worn down by a number of separate cycles of erosion.

There also is a place for cycles of erosion of several kinds and for dynamic equilibrium, either as an end phase of enduring climatic morphogenesis and/or as an end phase of relief and elevation reduction by denudation following orogenesis.