The Mighty Himalayas

 Discovering the Hidden Facts about the Great Himalayan Mountains

 


 The Himalayan Mountain Range: Description: Luciano’s painting is what we can call a geological marvel

     The many-crossed Himalayas, that south Asian mountainous system, that has always mesmerized people of the globe. These snowy giants demonstrate that some of the highest points on planet Earth are located here and can be also seen as a direct indicator of the powerful processes that has been taking place on our planet for millions of years.

In this blog, I am planning to write on geological aspects of Himalayas; the layout, fact, analysis, and the details that have created the Himalayas that we see today. Starting from the marine stratum of Mesozoic origin to the existing forces of the earth movements shaping these mountains, it can be viewed that Himalayan story is one of profound transformation and survival.

 

The Himalayan Origin: From the great deep and sea, To the mountain high and free

Many people will be surprised, but the Himalayas were not always so high as are now While still growing, the older ranges of the world are recognized by geologists as being now in process of degradation. Thus, the highest point in the world’s number one mountain system, the Himalay; Mount Everest was once at the bed of the ocean.

The story of the Himalayas has been traced as far back as 200 million years ago when the Indian plate was still mobile and was moving northwards. In the course of the earth’s history, the Indian plate moved northwards and eventually underthrust the Eurasian plate, which is referred to as the Himalayan orogeny. The collision which happened over a period of about 50 million years pushed the oceanic crust up and formed the Himalayan range.

The first tectonic contact was continent-ocean, that is, among the colliding plates there were parts of both an ocean and a continent; the oceanic plates were the first to be collapsed and uplifted. After the collision progressed further, it became a continent-continent collision and resulted into thrust faults and further emersion of the mountains.

Even today, in the Himalayas, there is evidence or existence of marine shelf and much even marine fossils at the heights of lofty summits. Thus, such an extraordinary geological history illustrates that geology indeed refracts the complex and constantly evolving processes of our Earth.

The Himalayan Range: A World That is so Vast & Vastly Different

The Himalayas are not a range but a huge and varied structure operating throughout various countries that people should not confuse with other ranges. It consists of a number of ranges of mountains which are in parallel to one another and which are quite different in size geology and structure.

Stretching for about 2,400 km across the south Asian region, the Himalyan range runs from the Indus River in the west to the Brahmaputra River in the east. Across this expanse of earth, it has some of the tallest mountain elevations of the world; Mount Everest for example is 8,848 meters above the sea level.

Besides mountain heights the range has much more for example different climates starting from the sal-forested hills of northern India and Pakistan to the cold and unfertile snow-capped mountains. This diversity is due to the fact that the climate of the range as well as its altitude changes even within small distances sometimes.

 

The Himalayan Tectonic Activity: Contemporary Evolution

In fact, the Himalayas are not this kind of static environment or remains untouched in this way during the world. However, they are the result of constant tectonic movements where the Indian plate is still moving northward and slides under the Eurasian plate.

This collision is behind slow shedding of the Brahmaputra sediment which has been shaping the uplift of the Himalayan range over thousands of years with the mountains moving upwards at a rate of one centimeter annually. This process continuation has caused the formation of numerous thrust faults and other kinds of geologic structures that can be seen throughout the range.

It is the tectonic movement that not merely provided for the strenghth of the Himalayas but also for the regular earth quakes that take place in the region. The Himalayan region is typically prone to earthquakes and even ranks as one of the most dangerous occasions of the world’s most lethal and strongest earthquakes.

However, despite these challenges posed by this tectonic activity, the himalayas remain to be a beautiful wonder of nature intriguing the world’s population. Contemporary changes in this mountain structure, make one realize the ever dynamic nature of the earth and how important forces of the earth have shaped the actual world we live in.

 

Exploring the Himalayan Wonders

The Himalayas are not only the highest mountain ranges of the world but also the centuries-old active cultural and symbols of dynamism of ecological systems. Trekking through the beautiful landscapes of the rick Buddhist monasteries to exploring the forests and alpine meadows; Himalayas have it all to offer.

For those who are fascinated by such feelings that these mountains can give those who are eager to conquer them, the Himalayas offer such a possibility and the opportunity to defy human physiology. Climbing adventures to some of the tallest mountains in the world including the Mount Everest is one of the oldest adventure fantasies that lovers of adventure have always dreamt of, and each time someone conquers the mountain, it is always a conquer of the human spirit.

Nevertheless, people and civilizations other than mountain climbers are also part of the Himalayas, and they are as impressive and extraordinary as the mountains themselves. From the cattle breeders of the alpine meadow to the black smiths who follow the profession inherited from the ancestors, people of the Himalayas extend a handshake with the nature.

These are just some of the mysteries and marvels of the Himalayas that have been discovered so far; we will find more as we keep on researching them and wandering in the world of mountains. Whether one is a geologist, a climber or just someone with awe in facing the Himalayan facade, it provides a discovery for the explorer.

 

Conclusion: The names of the Buddhist countries may change, but the mountains remain the same: the Allure of the Himalayas.

In terms of the strength and over-archingly the ever-evolving nature of the earth, there could be no better example than the Himalayas, as evidences the wonderful world we live in. These mountains, created in Pre-Cambrian times at the bottoms of seas and oceans and changing even today, attract and influence people all over the globe.

As we move progressively into the mysteries of the Himalayas, more other wonders of this beautiful region would be revealed. It is the amazing physical geography of the great peaks, the historical and ethnological aspects of the population, and much more, or even the breathtaking, piping spiritual geography that each part of the Himalayas holds the prospect of discovery and growth.

Consequently, let the world, researchers, and myself keep on admiring the beautiful outlook of the Himalayas, deep and versatile geological background necessary for further researches. Such is the case for this action as they not only expand knowledge regarding Earth but also find a link with the soul of these everlasting mountain ranges.

 

Reference

1.      Zurick, David; Pocheco, Julsun (2006), Illustrated Atlas of the Himalaya, University Press of Kentucky, p. 8,11,12, ISBN 9780813173849

2.      "Himalayan"Oxford English Dictionary (Online ed.). Oxford University Press. Retrieved 5 August 2021. Etymology: < Himālaya (Sanskrit < hima snow + ālaya dwelling, abode) + -an suffix) (Subscription or participating institution membership required.)

3.      Bishop, Barry"Himalayas (mountains, Asia)". Encyclopaedia Britannica. Retrieved 30 July 2016.

4.      A.P. Dimri; B. Bookhagen; M. Stoffel; T. Yasunari (8 November 2019). Himalayan Weather and Climate and their Impact on the Environment. Springer Nature. p. 380. ISBN 978-3-030-29684-1.

5.      Wadia, D. N. (1931). "The syntaxis of the northwest Himalaya: its rocks, tectonics and orogeny". Record Geol. Survey of India. 65 (2): 189–220.

6.      Apollo, M. (2017). "Chapter 9: The population of Himalayan regions – by the numbers: Past, present and future". In Efe, R.; Öztürk, M. (eds.). Contemporary Studies in Environment and Tourism. Cambridge Scholars Publishing. pp. 143–159.

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