WEBVTT

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Most people around the world know the

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country of Nepal for one thing, Everest,

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the summit of the world. That photograph

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on the poster, that bucket list

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mountain, and the fact that it's used as

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a superlative for anything remotely

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challenging. But, despite the grandeur

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of this epic mountain, it kind of steals

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the spotlight from the rest of Nepal.

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Just knowing Nepal for Everest strips it

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of almost everything that makes it even

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more remarkable.

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Because Nepal is so much more than

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Everest.

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Surprisingly, it's a geographically

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diverse country.

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In the span of only 200 km, the land

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rises from the subtropical lowlands to

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the highest point on the planet.

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That is an elevation gain of nearly 9

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km. In those 200 km, you pass through

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several different climate zones, from

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alpine tundra to jungles, from monsoon

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forest with elephants and rhinos,

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through terraced hillsides and cloud

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forests, and through high-altitude

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grasslands and glacial valleys.

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So, let's today talk about the true

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geography of Nepal

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in all its glory.

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So, when we take a look at Nepal on a

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map, the first thing you'll notice is

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the shape, a long, narrow rectangle.

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It's oriented east to west, roughly 900

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km long and 200 km wide. To the south is

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a long, open border with India. And to

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the north is the Tibetan Plateau, the

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roof of the world.

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What this means is that Nepal is

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landlocked, completely surrounded by

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just two countries.

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For a nation of over 30 million people,

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this geographical reality has profound

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consequences.

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Most trade, most imports, and all access

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to the sea must pass through India, or

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to a much lesser extent, through the

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long and difficult routes into China.

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In terms of its size, it covers about

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147,000

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sq km.

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About the same size as neighboring

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Bangladesh. By area, it's small, but by

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topographic range, it's extraordinary.

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Home to eight of the world's 14 peaks

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over 8,000 m, including Everest,

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Kangchenjunga, Lhotse, Makalu, Cho Oyu,

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Dhaulagiri, Manaslu, and Annapurna. All

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epic peaks. No other country on Earth

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has eight 8,000ers. Those being peaks

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over 8,000 m high. But like I mentioned

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previously, Nepal is a lot more than the

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mountains. The Himalayas that run across

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the country are just the northern third

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of Nepal. The country is usually divided

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into three rough horizontal zones

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running east to west. The Terai lowlands

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in the south, the foothills of the

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Himalayas in the center, and the tall

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Himalayas in the north. Each zone is a

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different world, different climate,

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different ecology, and different

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culture. Which means to understand

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Nepal, you have to understand all three.

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So, let's do that, starting at the

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bottom, the Terai.

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Now, most people's mental image of Nepal

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begins somewhere in the high hills. You

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may have seen images of prayer flags

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strung between peaks, or monasteries

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climbing to clifftops. But the Terai

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doesn't fit that image.

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It's the flat southern strip of Nepal, a

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narrow plain sitting between the

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Himalayan foothills to the north and the

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Indian border to the south. It is the

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northern continuation of the great

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Indo-Gangetic Plain, one of the most

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fertile and densely populated

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agricultural landscapes on Earth. In

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Nepal, it is roughly 30 to 50 km wide

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and extends the full length of the

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country, east to west. Elevations in

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this region are low, mostly between 60

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and 300 m above sea level. The climate

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is subtropical, hot summers but cool

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winters, and a monsoon season from June

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to September that dumps enormous

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quantities of rain.

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This region can feel oppressively humid

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in summer with temperatures regularly

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exceeding 40° C.

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But this climate produces extraordinary

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biological richness.

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This region is home to Chitwan National

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Park, one of the finest wildlife areas

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in all of Asia. It protects a large

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remnant of the subtropical grasslands

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and riverine forest that once covered

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this entire region.

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Here live the one-horned rhinoceros,

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a species that came perilously close to

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extinction in the 20th century but has

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made a remarkable recovery in Nepal's

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protected areas. Also here, we find

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Bengal tigers and the extremely rare

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gharials, one of the strangest-looking

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crocodilian species on Earth.

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Sloth bears and leopards also call this

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area home.

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Now, surprisingly, Nepal is one of the

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few countries in the world where tiger

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populations are actually growing.

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A census conducted in 2022 recorded over

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350 wild tigers in the country, nearly

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double the number of a decade earlier.

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It is one of the genuine conservation

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success stories of our era. This region

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is also Nepal's breadbasket. Despite

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covering only about 17% of the country's

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land area, it produces roughly half of

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Nepal's agricultural output. There's

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rice, wheat, sugarcane, and lentils that

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grow here in the rich alluvial soil

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deposited over millennia by rivers

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flowing south of the Himalayas.

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This region of Nepal is home to the

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Madhesi people. They make up about 30%

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of the country's population and are

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predominantly Hindu.

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Now, the Tarai is where Nepal meets

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India. And for the majority of the

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population here, this is not really a

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border checkpoint, but more of a porous

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way of living. Many communities straddle

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the border. Families are divided by it.

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Languages, customs, and religious

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practices flow across it. Now, let's

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move north. Between the flat Tarai and

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the soaring Himalayas, lies a part of

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Nepal where most Nepalese have lived for

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most of its history, the middle hills.

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This is a zone of complex and folded

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terrain. These ridges and valleys

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running roughly east to west cut across

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by rivers flowing south from the

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mountains towards India. Elevations here

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typically range from 300 m to about

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3,000 m with most settlements clustered

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between 1,000 and 2,500 m. High enough

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to escape the Tarai's heat, but low

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enough to still grow some crops. The

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landscape of the middle hills is defined

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above almost anything else by one

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feature, terraces.

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Almost every hillside in the inhabited

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middle hills region has been terraced,

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cut into horizontal steps to create flat

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agricultural land on slopes that would

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otherwise be impossible to farm.

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Now, this practice of terracing in this

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region has been accumulating for over

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2,000 years. Generations of farmers

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cutting into the hillsides, building

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retaining walls of stone, channeling

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water from one terrace to the next. The

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result is one of the most

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interesting-looking agricultural

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landscapes on Earth.

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Rice is the staple crop here. Where

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water can be brought to irrigate the

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terraces, paddy rice dominates. On drier

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slopes and higher elevations, there's

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millet, maize, wheat, and buckwheat. The

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agricultural calendar is dictated

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entirely by the monsoon here. The

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arrival of the rains in June triggers

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planting. The end of the monsoon in

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September and October brings harvest.

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Within the middle hills, one place above

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all others has defined Nepali history

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and culture, the Kathmandu Valley.

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The Kathmandu Valley is a broad, flat

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basin sitting at around 1,300 m above

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sea level. Roughly oval in shape,

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surrounded by hills on all sides, it is,

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geologically speaking, a former lake

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bed, making it extraordinarily fertile.

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The Valley is home to Kathmandu,

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Lalitpur, and Bhaktapur, three ancient

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cities that were, until the 18th

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century, three separate rival kingdoms.

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The Kathmandu Valley today contains

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seven UNESCO World Heritage Sites, all

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within roughly 30 km of each other.

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Now, the Valley's position also made it

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a trade crossroads, sitting in the

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middle hills between the Indian plains

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and the Tibetan Plateau.

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It was a natural stopping point on the

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ancient trade routes carrying salt,

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wool, and grain south from Tibet, and

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cotton and spices north from India.

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Newar merchants controlled this trade

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for centuries and grew extraordinarily

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wealthy. That wealth built the famous

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temples in this region. Today, Kathmandu

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is the capital of Nepal and home to

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nearly 1.5 million people in the city

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proper, and with the greater Valley

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approaching 3.5 million. In its chaotic,

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traffic-choked, smog-hazed, and

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endlessly alive city.

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The city core survives alongside what

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looks like endless concrete sprawl. But,

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the beauty of the city is that on clear

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days, if you look to the north, the

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Himalayas are right there, towering over

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the city of Kathmandu.

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An epic reminder that this busy,

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complicated city sits at the base of the

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tallest mountain system on the planet.

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The middle hills are cut through by a

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series of major river systems, the

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Koshi, the Gandaki, and the Karnali. All

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of them drain from the Himalayas

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southward through the hills and into the

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Terai, and then eventually the Ganges

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River.

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These rivers are among the most powerful

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on Earth in terms of sediment load. They

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carry millions of tons of eroded

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mountain material downstream every year,

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building the great alluvial plains of

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northern India. For the people of the

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hills, these rivers are both lifelines

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and barriers. They provide water, fish,

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and in some places hydroelectric power.

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But the deep gorges they carve have

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historically isolated communities from

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each other. A village on one side of the

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gorge might only be a kilometer from

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village on the other side as the crow

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flies, but hours of descent and ascent

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on foot. This geographical fragmentation

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has produced Nepal's extraordinary

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ethnic and linguistic diversity. Over

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120 languages are spoken in a country

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the size of New York state. And now we

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move to the Himalayas.

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Now to understand the Himalayas, you

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need to look at the geologic history of

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this region. And for that, you need to

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start about 100 million years ago. That

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time, what is now the Indian

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subcontinent was not attached to Asia at

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all. It was an island, a vast northward

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drifting landmass.

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Over tens of millions of years, the

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Indian subcontinent drifted north. Then,

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around 50 million years ago, India

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collided with Asia. The seafloor

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sediments that had accumulated in it

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were compressed and crumpled upwards.

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And the collision, which actually is

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still ongoing, began building the

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Himalayas. The Indian plate is still

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pushing north. The Himalayas are still

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rising about 5 mm per year. Nepal sits

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directly on this collision zone. The

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ground beneath Kathmandu is being

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compressed, uplifted, and periodically

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shattered by earthquakes that release

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the accumulated stress of two continents

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grinding against each other. And this is

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exactly what caused the 2015 Gorkha

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earthquake in Nepal. It was magnitude

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7.8, and it killed nearly 9,000 people,

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destroyed hundreds of thousands of

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homes, and triggered avalanches on

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Everest that killed climbers at base

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camp. It was a reminder, brutal and

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sudden, that Nepal does not sit on

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stable ground. It sits on one of the

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most geologically active zones on the

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planet.

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And here is something that you might

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find interesting. On the summit of Mount

00:11:43.399 --> 00:11:48.799
Everest is limestone, marine limestone

00:11:46.399 --> 00:11:51.399
full of fossils of tiny sea creatures,

00:11:48.799 --> 00:11:53.199
meaning the highest point on Earth

00:11:51.399 --> 00:11:56.120
was actually at the bottom of a tropical

00:11:53.200 --> 00:11:59.840
sea 450 million years ago. Tectonic

00:11:56.120 --> 00:12:02.879
forces lifted it nearly 9 km. But

00:11:59.840 --> 00:12:05.480
Everest is just but one mountain. Nepal

00:12:02.879 --> 00:12:08.519
is home to eight of the world's 14 peaks

00:12:05.480 --> 00:12:10.720
above 8,000 m. Each one is distinct in

00:12:08.519 --> 00:12:13.039
its character, in its difficulty, and in

00:12:10.720 --> 00:12:15.800
the history of human attempts on it.

00:12:13.039 --> 00:12:18.799
There is Annapurna in the west of Nepal.

00:12:15.799 --> 00:12:21.079
It was the first 8,000er ever summited

00:12:18.799 --> 00:12:23.000
by French climbers Maurice Herzog and

00:12:21.080 --> 00:12:25.200
Louis Lachenal. It was the first

00:12:23.000 --> 00:12:27.879
mountain above 8,000 m that any human

00:12:25.200 --> 00:12:30.400
being had ever stood on. And it remains,

00:12:27.879 --> 00:12:33.159
statistically, the most dangerous of all

00:12:30.399 --> 00:12:35.919
the 8,000ers. Its death rate is among

00:12:33.159 --> 00:12:38.719
the highest of any major Himalayan peak.

00:12:35.919 --> 00:12:41.000
Nearby is Dhaulagiri, also in western

00:12:38.720 --> 00:12:43.040
Nepal. It rises so dramatically from the

00:12:41.000 --> 00:12:44.799
surrounding terrain that early European

00:12:43.039 --> 00:12:47.360
surveyors briefly considered it as the

00:12:44.799 --> 00:12:50.159
highest mountain in the world. While far

00:12:47.360 --> 00:12:52.080
to the east of Nepal sits Kangchenjunga,

00:12:50.159 --> 00:12:54.240
the third highest mountain in the world

00:12:52.080 --> 00:12:57.240
at 8,586

00:12:54.240 --> 00:12:59.839
m. It is worshipped as a sacred deity by

00:12:57.240 --> 00:13:01.839
the Sikkimese people. And by tradition,

00:12:59.839 --> 00:13:03.920
climbers stop a few meters short of the

00:13:01.839 --> 00:13:06.400
actual summit out of respect, a

00:13:03.919 --> 00:13:08.279
remarkable act of restraint at the edge

00:13:06.399 --> 00:13:09.600
of one of humanity's greatest physical

00:13:08.279 --> 00:13:12.480
challenges.

00:13:09.600 --> 00:13:14.240
But the Himalayas are not uninhabited.

00:13:12.480 --> 00:13:15.759
People have lived in these mountains for

00:13:14.240 --> 00:13:17.600
thousands of years, and their

00:13:15.759 --> 00:13:19.480
adaptations to extreme altitude are

00:13:17.600 --> 00:13:21.680
among the most remarkable in human

00:13:19.480 --> 00:13:23.639
biology. These Sherpa people, who

00:13:21.679 --> 00:13:26.000
predominantly reside in the Khumbu and

00:13:23.639 --> 00:13:28.360
the Solo regions of Nepal, migrated from

00:13:26.000 --> 00:13:30.399
eastern Tibet roughly 500 years ago and

00:13:28.360 --> 00:13:32.800
settled in the high valleys of Northeast

00:13:30.399 --> 00:13:34.919
Nepal. They are famous worldwide for

00:13:32.799 --> 00:13:36.879
their role in Himalayan mountaineering,

00:13:34.919 --> 00:13:39.399
but their geographical significance goes

00:13:36.879 --> 00:13:41.439
far beyond guiding expeditions. They

00:13:39.399 --> 00:13:43.799
developed a civilization at elevations

00:13:41.440 --> 00:13:45.320
that would debilitate most humans.

00:13:43.799 --> 00:13:46.839
Sherpa communities have been in this

00:13:45.320 --> 00:13:49.040
environment long enough to develop

00:13:46.840 --> 00:13:52.639
genetic adaptations to altitude,

00:13:49.039 --> 00:13:54.199
including a variant of the EPAS1 gene

00:13:52.639 --> 00:13:55.919
that allows their bodies to use oxygen

00:13:54.200 --> 00:13:57.920
more efficiently at low partial

00:13:55.919 --> 00:13:59.879
pressures. Above the settlements, the

00:13:57.919 --> 00:14:02.159
landscape becomes one of the most severe

00:13:59.879 --> 00:14:04.320
on Earth. The high Himalayan valleys and

00:14:02.159 --> 00:14:05.199
passes are home to glaciers, thousands

00:14:04.320 --> 00:14:07.480
of them,

00:14:05.200 --> 00:14:09.759
covering an estimated 5,000 square

00:14:07.480 --> 00:14:11.080
kilometers of Nepal. And these glaciers

00:14:09.759 --> 00:14:13.039
are the source of the rivers that

00:14:11.080 --> 00:14:16.080
sustain hundreds of millions of people

00:14:13.039 --> 00:14:18.199
downstream in Nepal, India, Bangladesh,

00:14:16.080 --> 00:14:20.160
and Pakistan. The Himalayan glacier

00:14:18.200 --> 00:14:23.440
system is sometimes called the third

00:14:20.159 --> 00:14:25.519
pole after Antarctica and the Arctic.

00:14:23.440 --> 00:14:27.440
Now, let's leave behind the high peaks

00:14:25.519 --> 00:14:30.559
of the Himalayas and talk a little bit

00:14:27.440 --> 00:14:32.280
about Nepal's climate. And you cannot

00:14:30.559 --> 00:14:34.838
talk about Nepal's climate without

00:14:32.279 --> 00:14:36.679
mentioning the monsoon. The South Asian

00:14:34.839 --> 00:14:38.760
monsoon is one of the most powerful

00:14:36.679 --> 00:14:40.439
atmospheric systems on Earth. It is

00:14:38.759 --> 00:14:42.480
driven by the differential heating

00:14:40.440 --> 00:14:44.960
between the Indian Ocean and the Asian

00:14:42.480 --> 00:14:46.680
landmass. In summer, the land heats

00:14:44.960 --> 00:14:48.360
faster than the ocean,

00:14:46.679 --> 00:14:51.519
causing the air over the Indian

00:14:48.360 --> 00:14:53.519
subcontinent to rise. This causes moist

00:14:51.519 --> 00:14:55.919
air from the Indian Ocean to take its

00:14:53.519 --> 00:14:57.639
place. When the air hits the Himalayas,

00:14:55.919 --> 00:15:00.439
the greatest topographic barrier on

00:14:57.639 --> 00:15:02.559
Earth, it's forced upward. It cools and

00:15:00.440 --> 00:15:04.720
releases its moisture as rainfall,

00:15:02.559 --> 00:15:06.639
enormous, torrential, and possibly

00:15:04.720 --> 00:15:08.720
months-long rainfall.

00:15:06.639 --> 00:15:11.039
The monsoon typically arrives in Nepal

00:15:08.720 --> 00:15:13.639
in June and lasts through September. And

00:15:11.039 --> 00:15:16.039
in that 4-month window, roughly 80% of

00:15:13.639 --> 00:15:17.919
Nepal's annual precipitation falls.

00:15:16.039 --> 00:15:20.120
Rivers that were quiet mountain streams

00:15:17.919 --> 00:15:22.719
become raging torrents. Terraced

00:15:20.120 --> 00:15:26.200
hillsides green up almost overnight. But

00:15:22.720 --> 00:15:28.200
the monsoon is not uniform across Nepal.

00:15:26.200 --> 00:15:30.960
The middle hills and the Terai region

00:15:28.200 --> 00:15:33.720
receive more than 2,000 mm of rain

00:15:30.960 --> 00:15:35.879
annually, and over 80% of that is during

00:15:33.720 --> 00:15:37.800
the monsoon. However, the complex

00:15:35.879 --> 00:15:39.480
topography of the middle hills region

00:15:37.799 --> 00:15:41.839
means that there's a lot of local

00:15:39.480 --> 00:15:44.200
variation. But the rain shadow effect

00:15:41.840 --> 00:15:45.920
behind the Himalayas is dramatic. The

00:15:44.200 --> 00:15:48.120
high valleys of northern Nepal,

00:15:45.919 --> 00:15:50.120
sheltered by the main Himalayan range,

00:15:48.120 --> 00:15:53.080
receive only a fraction of the monsoon

00:15:50.120 --> 00:15:54.639
rainfall. Places like Mustang and Dolpo,

00:15:53.080 --> 00:15:56.720
upper valleys tucked behind the

00:15:54.639 --> 00:15:59.319
mountains, receive an almost central

00:15:56.720 --> 00:16:01.879
Asian dryness, receiving less than 200

00:15:59.320 --> 00:16:04.480
mm of rain per year.

00:16:01.879 --> 00:16:07.399
And this dry, arid region is home to one

00:16:04.480 --> 00:16:10.080
of Nepal's most extraordinary places.

00:16:07.399 --> 00:16:12.679
This is Lo Manthang, the walled city of

00:16:10.080 --> 00:16:14.400
Upper Mustang. It sits in a desert at

00:16:12.679 --> 00:16:16.839
3,840

00:16:14.399 --> 00:16:18.840
m. Its mud-brick architecture and

00:16:16.840 --> 00:16:21.120
Tibetan Buddhist culture feel entirely

00:16:18.840 --> 00:16:23.000
different from the rest of Nepal.

00:16:21.120 --> 00:16:25.799
The monsoon also defines Nepal's

00:16:23.000 --> 00:16:28.000
economy. Agriculture, still the primary

00:16:25.799 --> 00:16:30.599
livelihood for the majority of Nepalese,

00:16:28.000 --> 00:16:33.759
depends entirely on monsoon timing and

00:16:30.600 --> 00:16:36.519
intensity. A late monsoon or a weak one

00:16:33.759 --> 00:16:38.439
means poor harvests and food insecurity.

00:16:36.519 --> 00:16:40.600
A particularly violent monsoon could

00:16:38.440 --> 00:16:43.280
mean flooding, landslides, and the loss

00:16:40.600 --> 00:16:45.320
of everything a family has built. Nepal

00:16:43.279 --> 00:16:47.838
sits almost exactly at the point where

00:16:45.320 --> 00:16:49.800
the monsoon hits the Himalayas hardest,

00:16:47.839 --> 00:16:52.080
which means the stakes of every year's

00:16:49.799 --> 00:16:53.719
rains can be enormous.

00:16:52.080 --> 00:16:56.320
Now that we've explored the physical

00:16:53.720 --> 00:16:58.720
geography of Nepal, let's talk about the

00:16:56.320 --> 00:17:00.839
cities of Nepal. What are they like, and

00:16:58.720 --> 00:17:03.080
where are they located? We already spoke

00:17:00.839 --> 00:17:05.400
a little bit about Kathmandu, but what

00:17:03.080 --> 00:17:07.480
other large cities are in Nepal?

00:17:05.400 --> 00:17:10.160
Well, Nepal's second largest city is

00:17:07.480 --> 00:17:12.759
Pokhara. It sits in a broad valley like

00:17:10.160 --> 00:17:14.920
Kathmandu at around 820 m above sea

00:17:12.759 --> 00:17:17.240
level. It's lower and warmer than

00:17:14.920 --> 00:17:20.318
Kathmandu, and its defining feature is

00:17:17.240 --> 00:17:22.160
probably Fewa Lake, a large blue-green

00:17:20.318 --> 00:17:24.000
lake whose southern shore has become the

00:17:22.160 --> 00:17:26.519
spine of Nepal's tourism industry

00:17:24.000 --> 00:17:28.640
outside of the Everest region. To the

00:17:26.519 --> 00:17:32.960
north of Pokhara lies the Annapurna

00:17:28.640 --> 00:17:35.160
Massif, which rises to over 8,000 m. So,

00:17:32.960 --> 00:17:37.160
just imagine on a clear morning standing

00:17:35.160 --> 00:17:39.840
at the lakeside of Fewa Lake, looking to

00:17:37.160 --> 00:17:41.759
your north and you see the massive

00:17:39.839 --> 00:17:43.599
Annapurna. And because of this

00:17:41.759 --> 00:17:45.799
proximity, Pokhara is actually the

00:17:43.599 --> 00:17:48.279
gateway to the Annapurna Circuit and the

00:17:45.799 --> 00:17:50.159
Annapurna Sanctuary, two of the world's

00:17:48.279 --> 00:17:51.879
most celebrated trekking routes.

00:17:50.160 --> 00:17:53.800
Hundreds of thousands of trekkers pass

00:17:51.880 --> 00:17:55.600
through this city each year, either

00:17:53.799 --> 00:17:58.079
setting out into the hills or returning

00:17:55.599 --> 00:18:00.119
from them. But Pokhara is not just a

00:17:58.079 --> 00:18:02.960
gateway for Annapurna. It's an actual

00:18:00.119 --> 00:18:04.639
city with over 600,000 people, and it

00:18:02.960 --> 00:18:07.079
has a different character than the

00:18:04.640 --> 00:18:09.520
larger Kathmandu. Less congested,

00:18:07.079 --> 00:18:11.159
greener, and significantly wetter.

00:18:09.519 --> 00:18:13.440
Pokhara receives more rainfall than

00:18:11.160 --> 00:18:16.000
almost anywhere else in Nepal. And the

00:18:13.440 --> 00:18:18.600
result of this are lush hills, full

00:18:16.000 --> 00:18:20.680
rivers, and dramatic waterfalls.

00:18:18.599 --> 00:18:23.519
Beyond Kathmandu and Pokhara, there are

00:18:20.680 --> 00:18:26.240
other cities, particularly in the Terai

00:18:23.519 --> 00:18:28.839
region near the Indian border. Here lies

00:18:26.240 --> 00:18:30.559
Biratnagar, home to jute mills, sugar

00:18:28.839 --> 00:18:33.279
factories, and a growing manufacturing

00:18:30.559 --> 00:18:35.240
sector. There is also Birgunj, the main

00:18:33.279 --> 00:18:38.000
gateway for goods crossing from India

00:18:35.240 --> 00:18:39.640
into Nepal. Now, this city processes an

00:18:38.000 --> 00:18:42.000
enormous proportion of the country's

00:18:39.640 --> 00:18:44.000
imports and has grown into a substantial

00:18:42.000 --> 00:18:46.720
commercial city entirely on the back of

00:18:44.000 --> 00:18:48.440
its border position. But Nepal's cities

00:18:46.720 --> 00:18:50.720
are not yet dominant in the way the

00:18:48.440 --> 00:18:53.640
cities of India and China or Southeast

00:18:50.720 --> 00:18:56.200
Asia are. But the trajectory is clear.

00:18:53.640 --> 00:18:58.400
Nepal is urbanizing faster than most

00:18:56.200 --> 00:19:00.400
people realize. And the cities being

00:18:58.400 --> 00:19:02.759
built now, how they are planned, and how

00:19:00.400 --> 00:19:04.519
they manage their growth will shape much

00:19:02.759 --> 00:19:06.519
of Nepal's future.

00:19:04.519 --> 00:19:08.920
So, we started this video talking about

00:19:06.519 --> 00:19:11.279
a mountain, or rather, the reduction of

00:19:08.920 --> 00:19:14.880
an entire country to a single iconic

00:19:11.279 --> 00:19:18.119
peak. But, like I said, Nepal cannot be

00:19:14.880 --> 00:19:20.640
defined by just one mountain. It is so

00:19:18.119 --> 00:19:22.879
much more than that. It is a country and

00:19:20.640 --> 00:19:25.840
a land that compresses much of Earth's

00:19:22.880 --> 00:19:27.680
environments into a small region.

00:19:25.839 --> 00:19:30.240
From tropical lowlands to the Earth's

00:19:27.680 --> 00:19:32.120
highest peaks, it tells the story of a

00:19:30.240 --> 00:19:33.920
collision between continents still

00:19:32.119 --> 00:19:35.159
unfolding underneath this beautiful

00:19:33.920 --> 00:19:37.720
country.

00:19:35.160 --> 00:19:39.800
It tells the story of people who learned

00:19:37.720 --> 00:19:42.120
to live in a place that most people

00:19:39.799 --> 00:19:43.879
would not even survive in.

00:19:42.119 --> 00:19:46.479
Its resourceful people terraced

00:19:43.880 --> 00:19:48.800
impossibly steep slopes and built cities

00:19:46.480 --> 00:19:50.720
on ancient lakebeds. Despite being

00:19:48.799 --> 00:19:53.079
landlocked, earthquake-prone, and

00:19:50.720 --> 00:19:55.039
dependent on monsoon rains, the people

00:19:53.079 --> 00:19:58.159
of this country carved out their unique

00:19:55.039 --> 00:20:01.119
culture. So, let's not just limit Nepal

00:19:58.160 --> 00:20:03.000
to Everest or the Himalayas. It is so

00:20:01.119 --> 00:20:05.439
much more than that, and I hope this

00:20:03.000 --> 00:20:06.839
video helped you realize that.

00:20:05.440 --> 00:20:08.400
And as always, if you'd like content

00:20:06.839 --> 00:20:09.679
like this, give this video a like.

00:20:08.400 --> 00:20:11.519
Subscribe to the channel if you haven't

00:20:09.680 --> 00:20:12.840
done so already, and let me know in the

00:20:11.519 --> 00:20:14.799
comments below if you want me to

00:20:12.839 --> 00:20:17.119
continue making videos about different

00:20:14.799 --> 00:20:19.000
countries and their geography.

00:20:17.119 --> 00:20:20.959
And thank you to each and every one of

00:20:19.000 --> 00:20:22.160
you who's followed me over the past year

00:20:20.960 --> 00:20:24.759
and a half.

00:20:22.160 --> 00:20:26.759
I've now passed 100,000 subscribers, and

00:20:24.759 --> 00:20:28.879
when I first started this channel, I had

00:20:26.759 --> 00:20:30.640
no idea that I'd be getting here.

00:20:28.880 --> 00:20:31.400
So, thank you to each and every one of

00:20:30.640 --> 00:20:33.240
you.

00:20:31.400 --> 00:20:35.800
And I'll catch you in the next one.

00:20:33.240 --> 00:20:35.799
Peace.
