River bifurcation (Geomorphology 🏞️)

River bifurcation occurs when a river flowing in a single channel separates into two or more separate streams which then continue downstream. Some rivers form complex networks of distributaries, typically in their deltas. If the streams eventually merge again or empty into the same body of water, then the bifurca...

https://en.wikipedia.org/wiki/River_bifurcation

#RiverBifurcation #Hydrology #WaterStreams #Geomorphology #FluvialLandforms #RiverBifurcations

Knickpoint (Geomorphology 🏞️)

In geomorphology, a knickpoint or nickpoint is part of a river or channel where there is a sharp change in channel bed slope, such as a waterfall or lake. Knickpoints reflect different conditions and processes on the river, often caused by previous erosion due to glaciation or variance in lithology. In the cycle of erosion model, knickpoints advance one cycl...

https://en.wikipedia.org/wiki/Knickpoint

#Knickpoint #Geomorphology #ErosionLandforms #FluvialLandforms

Stream head cut (Geomorphology 🏞️)

In geomorphology, a stream head cut or simply head cut is an erosional feature of some intermittent and perennial streams. Headcuts and headward erosion are hallmarks of unstable expanding drainage features such as actively eroding gullies. Headcuts are a type of knickpoint that, as the name indicates, occur at the head of a channel. The knickpo...

https://en.wikipedia.org/wiki/Stream_head_cut

#StreamHeadCut #Geomorphology #ErosionLandforms #FluvialLandforms

River terraces (tectonic–climatic interaction) (Geomorphology 🏞️)

Terraces can be formed in many ways and in several geologic and environmental settings. By studying the size, shape, and age of terraces, one can determine the geologic processes that formed them. When terraces have the same age and/or shape over a region, it is often indicative that a large-scale geol...

https://en.wikipedia.org/wiki/River_terraces_(tectonic–climatic_interaction)

#RiverTerraces #Geomorphology #FluvialLandforms