Are there volcanoes in the himalayan mountains

India and Pakistan for instance have fought three different wars over the control of the Kashmir region, and the region remains restive till today. The Arunachal Pradesh region for instance was administered by the Indian government until China claimed the region to be Southern part of Tibet- this is still generating conflicts till today.

Tensions between India and China were strained in the s when the Republic of China annexed the Tibetan Plateau and stationed its troops on the high altitude grey region. In , the relationship between the two countries was strained when the border war led to the development of more nuclear arms by the countries. The nuclearization of the countries sharing borders at the Himalayas has been one of the effects of the richness of the Himalayas.

The dispute between India and China over Himalaya control has placed smaller countries like Nepal, and Pakistan in more difficult positions. In for instance, India decided to incorporate the region of Sikkim into its territory- a decision that undermined the existence of Bhutan. Though Nepal used to have close ties to India now the small country is turning to China. Pakistan has also been closely aligned with China since the s.

In , China tried to wrestle Bhutan territories from India but failed. The joining of forces to China from Nepal and Pakistan has contributed even more to tensions between China and India in the past few years in the Himalayas.

The tension between different states of the Himalayas has led to the militarization of the Himalayas. In , some Chinese soldiers were caught after entering the Indian-controlled region of Sikkim and Ladakh. The tension between different states in the Himalayas has not only generated lots of strives but there have also been some positive vibes as each state is funding numerous infrastructural projects on their sides of the border intending to solidify their territorial control.

Though there are hundreds of thousands of troops from many countries stationed at the borders, this has not stopped tourists from visiting the Himalayas, and just that they are always warned strictly to stay away from the militarized zones. This militarization of the Himalayas is clearly understood, the countries involved class occasionally and compromise in the long run.

Experts see the conflicts on these mountains as mutual enmity, none of the governments of these countries is sufficient enough to understand the boundary demarcations for each country. Until the countries that share borders on the Himalayas understand the cultural diversity of the region, there may be no peace in sight even for many decades to come. Though international organizations like the UN have tried to resolve conflicts between warring factions, it seems India and China, the leading players in the battle will not shift grounds for a long time to come.

One under-appreciated space asset is the photography skills of the Russian cosmonauts on board the International Space Station. Oblique view of Mt. Now, for the first time in many years, Mt Everest was visible once again from Kathmandu Valley, even though it is km away. So much so that for the first time in many years, Mt Everest can be seen again from Kathmandu Valley even though it is km away.

The Kathmandu Valley is an undulating plateau on the southern side of the Himalayan divide. But as you can see, the skyline hangs in a dark smog and no snow-capped mountains are remotely visible. The Manual: What is the cost of climbing Everest? Begin typing your search term above and press enter to search.

Is it popossible that all that volume increasing the height of Himalaya? If so than how long? I thought the lack of volcanoes was more about continental plates colliding with no subduction. Prior to the collision of the Indian Plate with the Asian plate, when the ocean floor preceding the Indian plat was being subducted by the Asian Plate, there were lots of volcanic mountains.

Is this theory out the window??? The lack of subduction is certainly the main cause of volcanic cessation in the Himalaya. Subduction of Techyan oceanic lithosphere occurred between the Cretaceous and Tertiary, with volcanic and intrusive systems forming during two main phases volcanic-related porphyry and epithermal gold deposits exist in the Himalaya. Millions of years from present there will potentially being more volcanism or just intrusions associated with a decrease in lateral forces.

The role of subduction and pressure are just as important as water and dehydration of subducting crust. Water is only a piece of the volcano story. Like Liked by 1 person. You are commenting using your WordPress. You are commenting using your Google account. You are commenting using your Twitter account. You are commenting using your Facebook account. Notify me of new comments via email.

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As seen in the animation above not all of the Tethys Ocean floor was completely subducted; most of the thick sediments on the Indian margin of the ocean were scraped off and accreted onto the Eurasian continent in what is known as an accretionary wedge link to glossary.

These scraped-off sediments are what now form the Himalayan mountain range. From about Ma the rate of northward drift of the Indian continental plate slowed to around cm per year. This slowdown is interpreted to mark the beginning of the collision between the Eurasian and Indian continental plates, the closing of the former Tethys Ocean, and the initiation of Himalayan uplift.

Note that in the above animation the continental plates are shown to collide at 10 Ma; this should instead read 50 Ma.