Deposited in a braided fluvial system.

The sinuosity of submarine channels is a characteristic instantly recognisable as being shared with fluvial systems.

As expected with this significant difference in scale, the dynamics of turbid current flows within submarine channels are significantly different to fluvial systems.

Lateral migration and accretion plays an important part in fluvial systems.

In this part of higher Himalaya, glacial melt-water dominates the fluvial system.

The Exner equation is a statement of conservation of mass that applies to sediment in a fluvial system such as a river.

The reservoir was deposited as a large braided fluvial system.

Meandering rivers, which form a sinuous path in a usually low-gradient plain toward the end of a fluvial system.

During the succeeding Bavel Interglacial the fluvial system reached its largest size but sedimentation rates already dropped at that time.

The strata were deposited in a fluvial and deltaic depositional system.