the himalaya mountains are an example of what type of tectonic boundary
Convergent boundary In plate tectonics, a convergent boundary, also known as a destructive plate boundary, is a region of active deformation where two or more tectonic plates or fragments of the lithosphere are near the end of their life cycle. This is in contrast to a constructive plate boundary (also known as a mid-ocean ridge or spreading center). As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near destructive boundaries, where subduction zones or an area of continental collision (depending on the nature of the plates involved) occurs. The subducting plate in a subduction zone is normally oceanic crust, and moves beneath the other plate, which can be made of either oceanic or continental crust. During collisions between two continental plates, large mountain ranges, such as the Himalayas are formed. In other regions, a divergent boundary or transform faults may be present.
Himachal Pradesh Himachal is in the western Himalayas. Covering an area of 55,673 square kilometres (21,495 sq mi),[4] it is a mountainous state. Most of the state lies on the foothills of the Dhauladhar Range. At 7,025 m Shilla is the highest mountain peak in the state of Himachal Pradesh.[18]