Title: April 2015 Nepal earthquake
Content:   Nepal lies towards the southern limit of the diffuse collisional boundary where the Indian Plate underthrusts the Eurasian Plate, occupying the central sector of the Himalayan arc, nearly one-third of the 2400 km long Himalayas. Geologically, the Nepal Himalayas are sub-divided into five tectonic zones from north to south and, east to west and almost parallel to sub-parallel. These five distinct morpho-geotectonic zones are: (1) Terai Plain, (2) Sub Himalaya (Shivalik Range), (3) Lesser Himalaya (Mahabharat Range and mid valleys), (4) Higher Himalaya, and (5) Inner Himalaya (Tibetan Tethys). Each of these zones is clearly identified by its morphological, geological, and tectonic features. The convergence rate between the plates in central Nepal is about 45 mm per year. The location, magnitude, and focal mechanism of the earthquake suggest that it was caused by a slip 
Title: Nepal
Content:  Tarai Upatyaka) lie north of these foothills in several places. The Indian plate continues to move north relative to Asia at about 50 mm per year. This makes Nepal an earthquake prone-zone, and periodic earthquakes that have devastating consequences present a significant hurdle to development. Erosion of the Himalayas is a very important source of sediment, which flows to the Indian Ocean. Saptakoshi, in particular, carries a huge amount of silt out of Nepal but sees extreme drop in Gradient in Bihar, causing severe floods and course changes, and is, therefore, known as the sorrow of Bihar. Severe flooding 
Title: Nepal
Content:  Nepal is of roughly trapezoidal shape, about 800 km long and 200 km wide, with an area of 147516 km2. It lies between latitudes 26° and 31°N, and longitudes 80° and 89°E. Nepal's defining geological processes began 75 million years ago when the Indian plate, then part of the southern supercontinent Gondwana, began a north-eastward drift caused by seafloor spreading to its south-west, and later, south and south-east. Simultaneously, the vast Tethyn oceanic crust, to its northeast, began to subduct under the Eurasian plate. These dual processes, driven by convection in the Earth's mantle, both created the Indian Ocean and 
Title: Geology of Nepal
Content:   The geology of Nepal is dominated by the Himalaya, the highest, youngest and a very highly active mountain range. Himalaya is a type locality for the study of on-going continent-continent collision tectonics. The Himalayan arc extends about 2400 km from Nanga Parbat (8138 m) by the Indus River in northern Pakistan eastward to Namche Barwa (7756 m) by the gorge of the Tsangpo-Brahmaputra in eastern Tibet. About 800 km of this extent is in Nepal; the remainder includes Bhutan and parts of Pakistan, India, and China. Since 55 Ma the Himalayan orogeny beginning with the collision of Indian subcontinent and Eurasia at the Paleocene/Eocene epoch, has thickened the Indian crust to its present thickness of 70 km. The northwest tip of India after colliding with Asia seems to have met along the full length of the suture by about 40 Ma. Immediately prior to the onset of the Indo-Asian collision, the northern boundary of the Indian shield was likely a thinned continental margin on which Proterozoic clastic sediments and the Cambrian ±Eocene Tethyan shelf sequence were deposited.
Title: Nepal
Content:  Nepal (नेपाल ), officially the Federal Democratic Republic of Nepal (सङ्घीय लोकतान्त्रिक गणतन्त्र नेपाल), is a landlocked country in South Asia. It is mainly situated in the Himalayas, but also includes parts of the Indo-Gangetic Plain, bordering Tibet of China to the north, and India in the south, east, and west, while it is narrowly separated from Bangladesh by the Siliguri Corridor, and from Bhutan by the Indian state of Sikkim. Nepal has a diverse geography, including fertile plains, subalpine forested hills, and eight of the world's ten tallest mountains, including Mount Everest, the highest point on Earth. Nepal is a multi-ethnic, multi-lingual, multi-religious and multi-cultural state, with Nepali 
Title: Nepal
Content:  the Indian continental crust eventually to under-thrust Eurasia and to uplift the Himalayas. The rising barriers blocked the paths of rivers creating large lakes, which only broke through as late as 100,000 years ago, creating fertile valleys in the middle hills like the Kathmandu Valley. In the western region, rivers which were too strong to be hampered, cut some of the world's deepest gorges. Immediately south of the emerging Himalayas, plate movement created a vast trough that rapidly filled with river-borne sediment and now constitutes the Indo-Gangetic Plain. Nepal lies almost completely within this collision zone, occupying the central 
Title: Nepal
Content:  of the Himalayan arc, nearly one-third of the 2400 km-long Himalayas,     with a small strip of southernmost Nepal stretching into the Indo-Gangetic plain and two districts in the northwest stretching up to the Tibetan plateau. Nepal is divided into three principal physiographic belts known as Himal–Pahad–Terai. Himal is the mountain region containing snow and situated in the Great Himalayan Range; it makes up the northern part of Nepal. It contains the highest elevations in the world including 8848.86 m height Mount Everest (Sagarmāthā in Nepali) on the border with China. Seven other of the world's "eight-thousanders" are in Nepal 
Title: 1881 Nicobar Islands earthquake
Content:  The Nicobar Islands are a series of volcanic islands that are part of an active volcanic arc, formed above the subduction zone where the Indo-Australian Plate passes beneath the Burma Plate. The convergence along this plate boundary is highly oblique, with the plate vector running at a low angle to the boundary. Most of the strike-slip component of the convergence is accommodated by the Great Sumatran fault, which passes northwards into the Andaman Sea spreading centre. This plate boundary has been the location of many historical megathrust earthquakes. The 1881 rupture area lies almost entirely within that for the Mw = 9.2 2004 Indian Ocean earthquake, while rupturing less than a third of its down-dip width.
Title: Outline of Nepal
Content: Pronunciation:nɛpɑːl ; Common English country name: Nepal ; Official English country name: The Federal Democratic Republic of Nepal ; Common endonym(s): List of countries and capitals in native languages ; Official endonym(s): List of official endonyms of present-day nations and states ; Adjectival(s): Nepali ; Demonym(s): Nepalese (also 'Nepali') ; Etymology: Name of Nepal ; International rankings of Nepal ; ISO country codes: NP, NPL, 524 ; ISO region codes: See ISO 3166-2:NP ; Internet country code top-level domain: .np Nepal is: a landlocked country ; Location: ; Northern Hemisphere and Eastern Hemisphere ; Eurasia ; Asia ; South Asia ; Indian subcontinent ; Time zone: Nepal Time (UTC+05:45) ; Extreme points of Nepal ; High: Mount Everest 8848 m – highest point on Earth ; Land boundaries: 2,926 km ; 🇮🇳 India 1,690 km ; 🇨🇳 China 1,236 km ; Coastline: none ; Nepal Geological Society ; Population of Nepal: 29,609,623(2019 estimate) – 48th most populous country ; Area of Nepal: 147,516 km2 ; Atlas of Nepal Atlas of Nepal  Geography of Nepal
Title: Eastern South Asia
Content:  Nepal is the world's 93rd largest country. Nepal is commonly divided into three physiographic areas: mountain, hill, and southern lowland plains (the Terai). These ecological belts run east–west and are vertically intersected by Nepal's major, north to south-flowing river system. The southern lowland plains bordering India are part of the northern rim of the Indo-Gangetic Plain. The Hill Region (Pahad) abuts the mountains and varies from 800 to 4000 m in altitude with progression from subtropical climates below 1200 m to alpine climates above 3600 m. The Lower Himalayan Range reaching 1500 to 3000 m is the southern limit of this region, with subtropical river valleys and "hills" alternating to the north of this range. The Mountain Region (Himal), situated in the Great Himalayan Range, makes up the northern part of Nepal. It contains the highest elevations in the world, including eight of the ten highest mountains. The climate of Nepal includes subtropical, temperate, subalpine and alpine zones.

Question: what kind of plate boundary is nepal on?
Answer: orogenic belt.