According to the College Board, there are 5 test centers for SAT and SAT Subject Tests in Nepal. Please note that before you register either of the SAT exams, you should choose your test date and test location. Each testing location is affiliated with an educational institution, such as high school, community college, or university. The following test centers administer one or more of 2019 and 2020 SAT tests in Nepal.
2019 – 2020 SAT Test Dates in Nepal
- March 9, 2019
- May 4, 2019
- June 1, 2019
- August 24, 2019
- October 5, 2019
- November 2, 2019
- December 7, 2019
- March 14, 2020
- May 2, 2020
- June 6, 2020
- August 29, 2020
- October 3, 2020
- November 7, 2020
- December 5, 2020
SAT Testing Centers in Nepal
KATHMANDU INTERNATIONAL STUDY CENTRE
RATO BANGALA SCH
ST XAVIER’S SCH
TRINITY INTERNATIONAL COLLEGE
More about Nepal
Nepal borders China (Tibet) to the north, India to the west, south and east.
Nepal stretches for around 880 km in a west-east direction. The glaciated High Himalayas with deeply carved river valleys run through the middle of the western half of the country (Dhaulagiri 8,167 m above sea level, Annapurna (8,091 m above sea level), the Manaslu (8,163 m above sea level) in central Nepal already has a smaller one Distance to the northern border; in eastern Nepal the highest peaks are border mountains to Tibet (Mount Everest [Sagarmatha] 8,848 m, according to other information also 8,846 or 8,850 m above sea level, Lhotse 8 516 m above sea level, Makalu 8,463 m) above sea level, Cho Oyu 8 201 m above sea level) and to India (Kangchenjunga 8 586 m above sea level).
In the lower front of the Himalayas, on the southern edge of which the Mahabharat chain runs through the whole country, is the Kathmandu valley (approx approx. 20 km wide) and the valley of Pokhara. The Siwalik chain (in Nepal: Churia) extends parallel to and south of the Mahabharat chain, in front of which the 15–50 km wide, once malaria-infested alluvial plain of the outer Tarai which merges into the north Indian Ganges plain. In two places the mountain ranges of the Siwalik chain push themselves up to the Indian border, whereby the Nepalese plains are divided into a western, middle and eastern Tarai. The inner Tarai is formed by tectonic basins, the so-called duns (e.g. Rapti Dun), between the Siwalik and Mahabharat ranges.
- ACEINLAND: Modern history of Nepal from World War I to today, covering all major events on politics, economy, society, and technology.
Nepal is influenced by the summer southwest monsoon, which blows in Nepal due to the topographical conditions from the southeast and brings 80-90% of the annual rainfall, as well as the dry, winter northeast monsoon, which blows in Nepal from the northwest. Winter rains fall in connection with low pressure areas coming from the west. The mean annual precipitation in Nepal is 1,627 mm. However, behind this number there are considerable local differences: in sloping rain on the southern flank of the Himalayas, up to 6,000 mm can fall during the monsoons, while the annual precipitation from stations in the rain shadow on the north side of the Himalayas is only up to 250 mm. From a climatic point of view, Nepal shows a very pronounced differentiation in altitude. The hot tropical zone extends from the Tarai to altitudes of around 1,000 m above sea level. This is followed by a subtropical level between around 1,000 m and 2,000 m above sea level and a moderate level between around 2,000 and 4,000 m above sea level. The high mountain range is characterized by particularly cold winters and lower amounts of precipitation. Check thedresswizard to see Nepal As a Tourist Country.
The only remnants of the rain-green monsoon forests and the grasslands of the Tarai are replaced upwards by evergreen deciduous and coniferous forests, which form a cloud forest level in the area of highest rainfall between 2,000 and 3,600 m above sea level ; the tree line is formed at 4,200 to 4,400 m above sea level by fallen deciduous forests (birch) and coniferous forests or by rhododendron and juniper forests. In addition, the alpine mat level follows. In the rain shadow on the north side of the Himalayas, alpine steppes are predominant.
The tourism began in 1954 with the opening of Tribhuvan Airport from Kathmandu. Initially, Nepal was only a destination for expedition and trekking tourism. Today’s trend is towards mass tourism. In 2014, 790,100 foreign guests visited the country, most of them from India, China, Sri Lanka, Great Britain and the USA. Important tourist attractions are the Kathmandu Valley (UNESCO World Heritage Site) with the cultural cities of Kathmandu, Patan and Bhadgaon (Bhaktapur), the Pokhara Valley at the foot of Annapurna and Lumbini (UNESCO World Heritage Site).
However, trekking and mountaineering tourism posed major ecological problems. By decentralizing the flow of tourists and setting up national parks (Chitwan, Sagarmatha [both UNESCO World Heritage Sites] and others), environmentally friendly tourism is to be pursued.