<p>It mostly has to do with the type of convergent boundary the  Himalayas are, continental crust to continental crust. Most convergent boundaries are oceanic to continental or oceanic to oceanic. In both cases there is a dense oceanic plate that can get subducted. But in a continental crust to continental crust collision neither can really dive under the other and get reworked*, since both are low density, thick, and roughly equal in density, so they just compress together like pushing two wads of clay together. They build both up and down since they sort of float on the rock below. Think of it kinda like a geologic iceberg, it is too light to sink. All compressive collisions  thicken like this to a lesser extent, due to the compressive forces, it is just far more intense with continental to continental collisions because there is no other outlet for the energy but compression because all the material involved is to light to be subducted. . </p>

<p>the Eurasian and Indian plates are both large continental plates so as long as they are getting forced together they can only get thicker and thicker. This is the only boundary like this on earth right now, so it seems weird to us, but this type of collision has happened before they are just rarer. </p>

<p>*sometimes one does go down more than the other but it does not get reworked, they just get fused together in a lopsided fashion. </p>

CC BY-SA 3.0
2017-09-05T05:01:55.117Z
2017-09-05T15:37:58.867Z
2017-09-05T15:37:58.867Z
John
<p>In addition to previous answers, there will be some degree of partial melting at the base of the collision zone of two continental plates (Indian &amp; Eurasian plates). Subsequently, this initiates deep lithospheric thickening, which has an upward component that could lift the crust. </p>

CC BY-SA 3.0
2017-10-13T03:54:48.213Z
2017-10-13T03:54:48.213Z
HammerKid073
<p>Of course the mountains were caused by moving tectonic plates. But in case of the Himalaya mountains was the speed of the plates just higher so more energy got 'into' the mountains. Or was the continental plates just slightly more loose on the plates? Or did the plates just submerge more, if so what caused that? Or....</p>

CC BY-SA 3.0
2017-09-04T22:01:23.323Z
Possible duplicate of [Himalayas are currently rising. What will be the highest point they can reach?](https://earthscience.stackexchange.com/questions/8910/himalayas-are-currently-rising-what-will-be-the-highest-point-they-can-reach)
Spencer
CC BY-SA 3.0
2017-09-05T07:32:22.357Z
(The answer to) that other question only explains why there is a maximum height approx. that of the Himalayas, but does not explain why no other mountain ranges are as high as the Himalayas. Not a dupe IMO
Jan Doggen
<geology>
What allowed the Himalaya to become so high?
Marijn 
# What allowed the Himalaya to become so high?

(Asked by: username_0 on 2017-09-04)

Of course the mountains were caused by moving tectonic plates. But in case of the Himalaya mountains was the speed of the plates just higher so more energy got 'into' the mountains. Or was the continental plates just slightly more loose on the plates? Or did the plates just submerge more, if so what caused that? Or....

**Tags:** geology

> **Comments:**
> **username_1**: Possible duplicate of [Himalayas are currently rising. What will be the highest point they can reach?](https://earthscience.stackexchange.com/questions/8910/himalayas-are-currently-rising-what-will-be-the-highest-point-they-can-reach)  
> **username_2**: (The answer to) that other question only explains why there is a maximum height approx. that of the Himalayas, but does not explain why no other mountain ranges are as high as the Himalayas. Not a dupe IMO  

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## 2 answers

### Answer by username_3 on 2017-09-05. Score: 1

It mostly has to do with the type of convergent boundary the Himalayas are, continental crust to continental crust. Most convergent boundaries are oceanic to continental or oceanic to oceanic. In both cases there is a dense oceanic plate that can get subducted. But in a continental crust to continental crust collision neither can really dive under the other and get reworked\*, since both are low density, thick, and roughly equal in density, so they just compress together like pushing two wads of clay together. They build both up and down since they sort of float on the rock below. Think of it kinda like a geologic iceberg, it is too light to sink. All compressive collisions thicken like this to a lesser extent, due to the compressive forces, it is just far more intense with continental to continental collisions because there is no other outlet for the energy but compression because all the material involved is to light to be subducted. .

the Eurasian and Indian plates are both large continental plates so as long as they are getting forced together they can only get thicker and thicker. This is the only boundary like this on earth right now, so it seems weird to us, but this type of collision has happened before they are just rarer.

\*sometimes one does go down more than the other but it does not get reworked, they just get fused together in a lopsided fashion.


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### Answer by username_4 on 2017-10-13. Score: 0

In addition to previous answers, there will be some degree of partial melting at the base of the collision zone of two continental plates (Indian & Eurasian plates). Subsequently, this initiates deep lithospheric thickening, which has an upward component that could lift the crust.


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