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Question

Which of the following statements regarding river meanders is/are correct?

1. It is a U-shaped bend in a river.

2. An extremely tight meander is called a goose neck; it is likely to become a cutoff, or oxbow lake, after a flood.

3. Tectonic uplift can cause a river to continue downcutting along its meandering course, producing incised or entrenched meanders.

Select the correct answer using the code given below. 

This question was previously asked in
CDS 2 2024 Maths Question Paper (01-Sep-2024)
The correct answer is

1, 2 and 3

River Meanders Explained

This solution delves into the characteristics and formation processes of river meanders, addressing the statements provided regarding their shape, evolution into oxbow lakes, and the impact of tectonic activity.

Statement 1: Meander Shape

The first statement describes a meander as a U-shaped bend in a river. This is an accurate description of the sinuous curves or bends that form naturally in a river's course, especially in its middle and lower stages where the river gradient is gentler and lateral erosion is more dominant than vertical erosion. The characteristic 'S'-shape of a meandering river is composed of multiple such bends.

Statement 2: Gooseneck Meanders and Oxbow Lake Formation

The second statement correctly identifies an extremely tight meander loop as a 'gooseneck'. This occurs due to the continuous process of erosion on the outer bank and deposition on the inner bank of a meander. Over time, the outer bank erodes, making the bend tighter and the neck of the meander narrower.

During periods of high flow, such as floods, the river's velocity increases, accelerating erosion across the narrow neck. Eventually, the river may breach the neck, taking a straighter, more direct path downstream. This event is called a 'cutoff'. The abandoned meander loop becomes isolated from the main river flow, often filling with water and sediment, forming a crescent-shaped lake known as an 'oxbow lake'.

Statement 3: Incised Meanders and Tectonic Uplift

The third statement accurately links tectonic uplift to the formation of 'incised' or 'entrenched' meanders. Tectonic uplift refers to the process where the land surface is raised relative to sea level due to movements within the Earth's crust. When tectonic uplift occurs in an area where a river is already meandering, it increases the river's gradient and its erosive power.

Consequently, the river begins to cut vertically downwards into the landmass while maintaining its existing meandering pattern. This downcutting action carves the river valley deeper, resulting in meanders that are set into the landscape with steep valley sides. These are known as incised or entrenched meanders, reflecting the river's history of lateral migration followed by renewed vertical erosion.

Conclusion on River Meander Statements

Based on the analysis, all three statements provided offer correct descriptions of key features and processes associated with river meanders:

  • Statement 1 correctly defines the basic shape of a meander bend.
  • Statement 2 accurately describes the evolution of tight meanders ('goosenecks') into oxbow lakes through the process of cutoff formation, often accelerated during floods.
  • Statement 3 correctly explains how tectonic uplift can lead to the formation of incised or entrenched meanders by causing the river to downcut along its established meandering course.

Therefore, all the given statements accurately reflect geomorphological concepts related to river meanders.

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