Entrenched meanders are evidence for a sequence of geologic events that includes episodes of uplift and erosion, followed by a period of deposition and then a period of downcutting. This sequence of events creates a meandering river with entrenched meanders, which are meanders that have been cut deeper and wider than the surrounding landscape.

Entrenched river

entrenched snakes of virgin river at the top end of Zion Canyon, zion national park, Utah.

One entrenched riveror entrenched flow is a river or stream flowing into a narrow ditch or valley cut into a flat or relatively level plateau. Because of lateral erosion, streams flowing over gentle slopes over time develop a meandering course (snake-like pattern). Meanders form where the gradient is very smooth, for example in the floodplain and delta. intricacies it is the characteristic of the middle and final course of the river. But very deep and wide meanders can also be found cutting through hard rock. These meanders are called item or entrenched meanders. The exception is that entrenched meanders are formed during land uplift where the river is young. They widen and deepen over time and can be found as deep canyons or canyons on hard rock. In the case of an entrenched stream or river, it is often assumed that the watercourse inherited its course by cutting through the bedrock of a pre-existing plain with little modification of the original course. Downsizing of the river system can be the result not only of tectonic uplift, but also of other factors such as river piracy, decreased head, increased runoff, extension of the drainage basin, or change in base level such as a drop at sea level. The general, non-generic terminology for a river or stream flowing in a narrow ditch or valley, for which evidence of a pre-existing plain or relatively level plateau may be absent or present is meander valley or winding valley the latter being the preferred term in the literature.

The snakes that form part of an entrenched river or meander valley are more commonly known as item snakes. They are commonly classified as a jammed meander or one entrenched meander. For a long time, it was argued that interlocking meander occurs when reduction process is slow and the river can cause erosionleading to a asymmetrical valley. Furthermore, it has also been argued for a long time that an entrenched meander it forms when there is a rapid incision in the river bed so that the river does not have the opportunity to erode the side. This leads to symmetry valleys common canyon-like appearance. However, more detailed studies have shown that the development of ingrown meanders versus entrenched meanders depends on a complex mix of factors, such as bedrock lithology, tectonic activity, and climate.


As noted above, a entrenched river can be caused by tectonic uplift in the area or when lowering the sea ​​level occurs. It can also be caused by the increased level of reduction or a collapse of moraine– dammed lake downstream, or capture of the river by another river. In addition, the river’s rejuvenation process can also be the cause of the entrenchmentespecially when the process occurred due to tectonic uplift. River rejuvenation increases the force of flowing water and therefore the process of erosion it is accelerated.

Studies show that tectonic movementparticularly the movement associated with elevatecan influence spatial patterns of erosion and sedimentation. Although it is very difficult to provide detailed information about tectonic activity, the basic temporal and spatial scale can show evidence of how this movement leads to the formation of an entrenched river. Several authors have used an entrenched river as evidence of tectonic movement in the past, and in this way they proved the significant role of tectonic elevations in the formation of an entrenched river.

Several studies have cited incised meander an important feature of river entrenchment, as an impact of river rejuvenation. On the other hand, scholars argue that the incision snakes and entrenched snakes are features formed before the rejuvenation of the river. item snakes occur at the base of the river and occur when the level of the base of the river is reduced, thus giving the river sufficient strength to erosion happen. Some studies also indicate that anthropogenic factors such as cleanliness vegetationdevelopment of damsand reservoir and urbanization are also causes of river entrenchment. For example, gravel mining along the russian river developed the Middle Reach well, which in turn led to the creation of the Entrenched River. According to Posamentier, in the 1950s and 1980s, the Russian River had gravel wells and dry Stream. However, over time, the river became entrenched due to mining (p. 1777).

Urbanization and cleaning of vegetation increase water runoff, which in turn increases water volume, especially during the rainy seasons. Therefore, the increase in the level of verticalization erosion of the river increases the force of the water, leading to erosion From Rio. a study of São Pedro river and another river in the southwest indicated that flooding was the main cause of river entrenchment in the 18th century. The study shows that the increase in population and human activities in these places has increased floods and, consequently, the volume of water drainage (Hereford 43).


Rosgen indicates that the consequences of the incision meander are associated with the accelerated flow bank erosion, loss of landaquatic habitat loss, as well as the reduction of the water table. Furthermore, the study also found that the incision snakes also cause loss of land productivity and downstream sedimentation (pg. 2). The factors can affect not only the economic development of the land it passes through, but it is also very expensive when restoration is about to be started. the entrenchment of the river happens because the water has the power to cause erosion on the riverbed. that increased velocity showed a negative effect on the river habitatbecause of the increase erosion of the area. For example, a study by Simon revealed that canal incision is an important feature of riversand affects variables in riparian forests vegetation and fish growth in the areas (p. 528). The lowering of the channels means that the water table has also dropped. Specifically, entrenched river development reduces the amount of groundwater due to water loss through infiltration. Base level movement changes tributaries and the entrenchment of a affluent channel. studies of various rivers revealed that the process of river entrenchment has been associated with the adjustment of river positions through erosionas well as enlargement.

river restoration

The entrenchment of the river causes negative impacts, such as chain Bank erosionland loss, water loss habitatloss of land productivity, lowering of the water table and sedimentation of the river downstream. However, to compensate for these problems, there are canal restoration measures focusing on restoring the river to its original or former characteristics. However, to achieve good results, a good understanding of river patterns and the profile of stable channels is a critical requirement. The process also needs an elaborate procedure to follow to ensure that all important factors and actions are followed. Numerous projects around the world involving river restoration have been undertaken, and a good example of such projects is Maggie Creek, Nevada. The project was completed in 1990 at Upper Maggie Creek in Nevada. It was a partnership between the government and a private farm, and the project involved rectifying many kilometers of unstable land. gravel bed considered as type C4/D4.

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