Sentence examples for bottom of fluvial from inspiring English sources

The stagnant layers always overlie the erosional bases and are located at the bottom of fluvial sedimentary cycle.

In near-surface settings, such as the bottom of fluvial channels or the top of mouth bars in braided river deltas, infiltration-related dissolution leads to more intergranular dissolution pores.

At the bottom of the fluvial channels in braided river delta plains or at the top of mouth bars in braided river delta fronts, eodiagenesis can inhibit compaction via early basal carbonate cementation, and the unfavorable reservoirs are extra-low-porosity and extra-low-permeability sandstones.

The evidence includes erosion and deformation of glaciolacustrine sediment that we interpret happened during draining of the lake, desiccation cracks that formed during exposure of the lake bottom, and fluvial sand deposited as the lake began to refill.

Unlike clasts commonly found at the bottom of a layer in a fluvial environment, these clasts are primarily found in the middle or upper parts of sandstones.

At present the basin is in a dry climate period which results in a lake level lowstand and progradation of fluvial systems such as the Río Colorado onto the former lake bottom.

And just when it was thought that all great challenges of fluvial exploration were over, there was one more: the river Bure in Norfolk.

When the sediment emptied into a river exceeds its carrying capacity, the river starts to "braid", in the language of fluvial geomorphology.

He disclaimed the theory of fluvial processes and held the biblical Deluge to be the agent of all erosion and sedimentation upon the Earth.

Deposition of fluvial sandbodies is controlled mainly by characteristics of the system, such as the rate of avulsion and aggradation of the fluvial channels and their geometry.

The incision of the spit and fluvial sediment supply was also observed, in October 2009, by Yamashita et al. (2011), who reported the northeastward transport of fluvial sediment into the sand flat by a fluvial flooding event.