UPSC MainsGEOGRAPHY-PAPER-I201310 Marks150 Words
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Q1.

Differences between Normal cycle and Arid cycle of Davis.

How to Approach

This question requires a comparative analysis of William Morris Davis’s Normal and Arid cycles of erosion. The answer should focus on the differences in landform development, controlling factors, and the resulting landscapes. A structured approach comparing the stages, dominant processes, and characteristic features of each cycle is crucial. Mentioning the climatic conditions and their influence on erosion is also important. The answer should be concise, sticking to the 150-word limit.

Model Answer

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Introduction

William Morris Davis proposed the ‘Geomorphic Cycle’ theory, explaining landscape evolution through stages of youth, maturity, and old age. He identified different cycles based on climatic conditions. The Normal cycle, prevalent in humid temperate regions, contrasts significantly with the Arid cycle, found in arid and semi-arid environments. Understanding these differences is fundamental to comprehending regional variations in landform development and the influence of climate on geomorphological processes.

Differences between Normal and Arid Cycles of Davis

The Normal cycle is characterized by a balanced interplay between erosion and deposition, leading to broad, gently sloping plains. It’s dominated by fluvial processes – vertical erosion in youth, lateral erosion in maturity, and peneplanation in old age. Conversely, the Arid cycle is marked by limited rainfall and significant temperature fluctuations.

Key Differences:

Feature Normal Cycle Arid Cycle
Climate Humid, temperate Arid, semi-arid
Dominant Process Fluvial erosion & transport Wind erosion, flash floods, limited fluvial action
Landforms V-shaped valleys, meanders, floodplains, peneplains V-shaped canyons, mesas, buttes, playas, alluvial fans
Erosion Rate Relatively slow and continuous Episodic and rapid (due to infrequent but intense rainfall)
Vegetation Cover Dense Sparse or absent

In the Arid cycle, vertical erosion is dominant due to infrequent but intense rainfall events, resulting in steep-sided canyons and angular landforms. Wind action plays a crucial role in shaping the landscape, creating features like yardangs and dunes. The lack of vegetation exacerbates erosion rates. The cycle often terminates in a bajada or playa rather than a peneplain.

Conclusion

In essence, the Normal cycle represents a landscape sculpted by gradual fluvial erosion in humid conditions, while the Arid cycle showcases a landscape carved by episodic, intense erosion and wind action in dry environments. These cycles highlight Davis’s attempt to link climate and landform development, though his model has been critiqued for its uniformitarian assumptions and rigid stages.

Answer Length

This is a comprehensive model answer for learning purposes and may exceed the word limit. In the exam, always adhere to the prescribed word count.

Additional Resources

Key Definitions

Peneplain
A peneplain is a low-relief plain formed by extensive erosion, representing the final stage of the normal cycle of erosion. It is almost a plain, with some low, residual hills.
Bajada
A bajada is a broad, gently sloping apron of alluvium deposited at the base of a mountain range in an arid or semi-arid region, often representing the final stage of the arid cycle.

Key Statistics

Approximately 30% of the Earth’s land surface is classified as arid or semi-arid (UNCCD, 2018).

Source: United Nations Convention to Combat Desertification (UNCCD), 2018

Desertification affects over 250 million people worldwide (FAO, 2017).

Source: Food and Agriculture Organization of the United Nations (FAO), 2017

Examples

Grand Canyon, USA

The Grand Canyon in Arizona, USA, is a prime example of a landscape shaped by the Arid cycle, showcasing deep canyons carved by the Colorado River and wind erosion.

Frequently Asked Questions

Is Davis’s cycle theory still relevant today?

While Davis’s cycle theory has been modified and critiqued, it remains a foundational concept in geomorphology, providing a framework for understanding landscape evolution and the influence of climate. Modern geomorphology incorporates plate tectonics and other factors not considered by Davis.

Topics Covered

GeographyGeomorphologyErosionLandformsCycle of Erosion