Difficulty: Medium
Correct Answer: Valley deepening
Explanation:
Introduction / Context:
Rivers pass through different stages in their longitudinal profile: youthful, mature and old. Each stage is associated with particular erosional and depositional processes that shape the surrounding landscape. Understanding these processes is central to fluvial geomorphology and often forms part of physical geography questions in competitive exams. This question focuses on the youthful stage of a river and asks which geomorphic process dominates at this stage, testing your understanding of vertical versus lateral erosion and valley development.
Given Data / Assumptions:
Concept / Approach:
In the youthful stage, a river flows in steep gradients, has high velocity and actively erodes its bed vertically. This leads to valley deepening and the formation of narrow, V shaped valleys. Lateral erosion, which causes valley widening and prominent meanders, becomes more significant in the mature stage. River rejuvenation is a separate process where a river gains renewed erosive power due to uplift or fall in sea level, not a normal age stage. Meandering is most pronounced in later stages with gentler gradients. Therefore, the correct process for the youthful stage is valley deepening through dominant vertical erosion.
Step-by-Step Solution:
Step 1: Recall that in youth, a river usually flows in steep terrain with high energy.
Step 2: Understand that high energy streams primarily erode downward into their beds rather than sideways.
Step 3: This strong vertical erosion results in deep, narrow valleys, often described as V shaped valleys.
Step 4: Compare this with valley widening and meandering, which are characteristic of later, more mature stages.
Step 5: Select valley deepening as the dominant process during the youthful stage of a river.
Verification / Alternative Check:
Textbooks on geomorphology commonly illustrate the youthful stage with diagrams showing steep channels, waterfalls, rapids and V shaped valleys. They emphasise down cutting or vertical erosion as the main activity. Mature stages are described with wider floodplains and prominent meanders, indicating significant lateral erosion and valley widening. River rejuvenation is presented as an event caused by tectonic uplift or sea level change, not a standard age stage. Thus, by comparing descriptions across stages, it is clear that valley deepening corresponds to the youthful stage.
Why Other Options Are Wrong:
Valley widening is more typical of the mature stage of a river, when lateral erosion and floodplain development become prominent, rather than the youthful stage. River rejuvenating refers to a renewed phase of erosion after uplift or other changes, which can occur at different times and is not synonymous with youth. Meandering is most noticeable in later stages when the gradient is moderate and vertical erosion has reduced; it is not dominant in the steep youthful phase. Therefore, these options do not accurately describe the main process during the youthful stage.
Common Pitfalls:
Students sometimes confuse youthful and mature stages and may think that all visible river features like meanders occur throughout the course with the same intensity. Another pitfall is interpreting rejuvenation as the same as youth because both appear to suggest new energy, even though they are different concepts. To avoid such confusion, focus on the typical valley shape, type of erosion and channel pattern that characterise each stage. Creating a summary table of youthful, mature and old age river features with diagrams will help reinforce these distinctions.
Final Answer:
During the youthful stage of a river, the most dominant geomorphic process is valley deepening, so valley deepening is the correct option.
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