Sentence examples for of fluvial style from inspiring English sources

The reconstruction of fluvial style changes provides evidence of four main aggradation periods.

Parts of the successions (Sinpyong Anpyong and Jotap units), formed in southward- or southeastward-draining fluvial systems, are documented in detail in terms of macroform-scale to stratigraphic-level architecture for the assessment of fluvial styles and evolution of non-marine depositional environments.

Evidence of changes in fluvial style attributable to base-level control has not been observed.

In this study the occurrence of thresholds in fluvial style changes during the Holocene are discussed for three different catchments: the Dijle and Amblève catchments (Belgium) and the Valdaine Region (France).

Overall, these examples demonstrate how changes in fluvial style depend on the crossing of thresholds in sediment supply and water discharge.

As a result of the climatic variations engendered by the last glacial cycle, the fluvial style repeatedly changed between a braided and anastomosing system.

Other changes in fluvial style appeared to be reversible.

The valley has undergone significant changes in fluvial style during the time humans have occupied its landscapes, including changes in channel pattern, location of depocenters, and sediment lithology.

Characteristics of these units throw more light on the fluvial styles, allowing inferences that ephemeral, mud-dominated river systems were also present.

Ancient braided fluvial systems were affected by a lack of binding vegetation, under variable paleoclimatic conditions, and possibly characterized by unique fluvial styles during the Precambrian.

The upper part of the Ecca Group reflects a filled stage of shallow marine sedimentation followed by the overfilled style of fluvial sedimentation of the overlying Beaufort and Stormberg groups (Catuneanu et al. 2005).