UPSC MainsGENERAL-STUDIES-PAPER-I202310 Marks150 Words
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Q6.

How are the fjords formed? Why do they constitute some of the most picturesque areas of the world?

How to Approach

This question requires a geographical explanation of fjord formation and an understanding of why these formations are aesthetically pleasing. The answer should begin by defining fjords and explaining their glacial origins. Then, it should detail the specific geological features that contribute to their scenic beauty. A concise and structured approach, focusing on both the 'how' and 'why' aspects, is crucial. Mentioning specific locations will enhance the answer.

Model Answer

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Introduction

Fjords are long, narrow, deep inlets of the sea between high cliffs, typically formed by submergence of a glacially eroded valley. These dramatic coastal landscapes are primarily found in regions that were heavily glaciated during past ice ages, such as Norway, Chile, New Zealand, and Alaska. Their unique formation and subsequent geological processes contribute to their breathtaking beauty, making them some of the most picturesque areas on Earth. Understanding their genesis is key to appreciating their aesthetic appeal.

Formation of Fjords

Fjords are formed through a complex interplay of glacial and geological processes. The process can be broken down into the following stages:

  • Glacial Erosion: During the Pleistocene epoch (the last ice age), massive glaciers carved out U-shaped valleys. Unlike rivers which erode vertically, glaciers erode both vertically and laterally due to their immense weight and the abrasive action of embedded rocks.
  • Deepening and Widening: The glaciers deepened and widened existing river valleys, creating steep-sided troughs. The erosive power was greatest at the base of the glacier, resulting in a deeper valley floor.
  • Isostatic Depression: The immense weight of the glaciers caused the land to sink (isostatic depression).
  • Sea Level Rise & Submergence: As the ice age ended, glaciers melted, causing sea levels to rise. The previously eroded valleys were then flooded by the sea, creating fjords. The isostatic rebound (land rising after the removal of weight) is still ongoing in some areas, influencing fjord depths.
  • Sill Formation: A characteristic feature of many fjords is a shallow underwater ridge or ‘sill’ at the mouth. This is formed due to reduced glacial erosion at the point where the glacier lost its power as it entered the sea.

Why Fjords are Picturesque

Several factors contribute to the exceptional scenic beauty of fjords:

  • Dramatic Topography: The steep, often near-vertical cliffs rising directly from the water create a dramatic and imposing landscape. These cliffs are often adorned with waterfalls.
  • Deep Blue Waters: The deep, still waters of fjords reflect the surrounding mountains and sky, creating stunning visual effects. The depth also contributes to the unique color.
  • Presence of Waterfalls: Meltwater from glaciers and snowfields cascades down the fjord walls as spectacular waterfalls, adding to the visual drama.
  • Unique Ecosystems: Fjords support diverse ecosystems, with lush vegetation clinging to the cliffs and abundant marine life in the waters.
  • Serene Atmosphere: The sheltered nature of fjords creates a calm and peaceful atmosphere, enhancing their aesthetic appeal.

Examples of Famous Fjords

  • Sognefjord, Norway: The longest and deepest fjord in Norway, known for its stunning scenery and charming villages.
  • Milford Sound, New Zealand: A famous fjord renowned for its dramatic cliffs, waterfalls, and wildlife.
  • Kenai Fjords National Park, Alaska: Features glaciers calving into the sea, creating a dynamic and breathtaking landscape.
Fjord Country Key Features
Sognefjord Norway Longest & deepest fjord in Norway, numerous branches
Milford Sound New Zealand Dramatic cliffs, waterfalls (Stirling Falls, Bowen Falls), Mitre Peak
Kenai Fjords USA (Alaska) Glacier calving, diverse marine wildlife (whales, seals)

Conclusion

In conclusion, fjords are remarkable geological formations created by glacial erosion and subsequent sea level rise. Their unique combination of dramatic topography, deep blue waters, cascading waterfalls, and serene atmosphere makes them exceptionally picturesque. These landscapes are not only aesthetically pleasing but also ecologically significant, representing a valuable natural heritage that requires careful preservation. Their continued existence is also a reminder of past climatic conditions and ongoing geological processes.

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

Isostatic Rebound
The process by which land rises after the removal of a heavy weight, such as a glacier. This is due to the Earth's mantle slowly flowing back to fill the space left by the removed weight.
U-Shaped Valley
A valley with steep, nearly vertical sides and a flat bottom, characteristic of glacial erosion. This shape contrasts with the V-shaped valleys formed by river erosion.

Key Statistics

Norway has approximately 86% of its coastline comprised of fjords.

Source: Norwegian Coastal Administration (as of 2023 knowledge cutoff)

Chile possesses over 30% of the world’s fjord coastline.

Source: National Geographic (as of 2023 knowledge cutoff)

Examples

Geirangerfjord, Norway

A UNESCO World Heritage site, Geirangerfjord is known for its steep cliffs, numerous waterfalls (like the Seven Sisters), and abandoned farms clinging to the mountainsides. It exemplifies the dramatic beauty characteristic of Norwegian fjords.

Frequently Asked Questions

Are fjords only found in cold regions?

While most fjords are found in high-latitude regions that were heavily glaciated, fjord-like features can also be found in other areas, though they are formed by different processes (e.g., submerged river valleys). However, the classic, dramatic fjords are predominantly associated with glacial activity.

Topics Covered

GeographyEnvironmentGeomorphologyCoastal GeographyGlacial Landforms