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Why 90% of Japan is "Empty"

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Why 90% of Japan is "Empty"

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Japan is one of the world's most

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populous countries. Home to around 123

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million people today, Japan is the

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world's 11th most populous country and

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it's also home to the world's second

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most populous island, Honshu. Home to

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more than 83% of the Japanese population

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and more than 102 million people all on

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its own. But when you look just beneath

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the surface of these statistics, you'll

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see that Japan is one of the most

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unusual and interesting population

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patterns in the world. Because the vast

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majority of Japan's population all just

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live within a relatively small and

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linear line that runs across the center

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and east of the country's south. Nearly

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twothirds of the entire Japanese

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population all just live within this

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line that encompasses most of Japan's

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largest metropolitan areas including

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Fukuoka, Hidiushu, Hiroshima, Okyama,

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Takamatsu, Kobe, Osaka, Kyoto, Nagoya,

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Hamamatsu, Shizuoka, and of course the

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biggest of all, Tokyo. Roughly 80

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million Japanese live within this long

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but narrow line that extends for around

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1,200 km across an area that only makes

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up less than 10% of Japan's total land

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area leaving behind the remaining 90% of

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the country that's significantly more

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sparsely populated. To help you

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visualize this divide better, roughly 80

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million Japanese live within the line

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that makes up less than 10% of the

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country's area, while only about 43

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million Japanese live within the rest of

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the 90% plus of the country. Nearly half

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of the population lives within the much

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much smaller line. The line of Japan

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contains an average population density

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that's nearly 17 times greater than the

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rest of the country has, which is one of

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the most astonishing differences between

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two different regions of the same

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country seen anywhere in the world. Put

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another way, the lion of Japan all

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throughout is even more dense than the

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crowded citystate of Vatican City is.

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While the rest of Japan has an average

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population density that's about the same

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as the US state of Pennsylvania.

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Economically, the line also accounts for

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an even more astonishing 70% of the

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entire Japanese economy. This highly

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populated and economically powerful line

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across Japan has been referred to by

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many different names. Sometimes it's

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referred to as the Thai belt, which in

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English means Pacific belt, and other

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times as the Tokaido corridor. I will

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continue referring to it from here on as

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the Taiheo Belt. And in many ways, it is

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fairly comparable in both size and scope

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to the northeast megalopouloolis in the

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United States. The most densely

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populated continuous urban area in North

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America that runs across the cities of

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Washington DC, Baltimore, Philadelphia,

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New York City, and Boston.

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Geographically, the Taio Belt is a bit

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larger. placed side by side with Fukuoka

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beginning where Washington DC begins,

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the Taiheo Belt would extend across the

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entire northeast coast well beyond

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Boston with Tokyo placed roughly in

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central Maine with around 80 million

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people living across it. The Thai belt

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is also significantly more populated

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than the Northeast Megalopouloolis is as

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well, which is home to only about 53

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million people by comparison. This

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difference in population density and

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scale between the two partly explains

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the dramatically superior rail

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connectivity across the Taio belt that

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exists today. Japan's famous Shingansen

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bullet train network connects the entire

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corridor together today and enables

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rapid transport from Tokyo to Fukuyama

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at only about 3 and 1/2 hours. Roughly

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half the time that it takes Amtrak

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Asella to cover the same distance from

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Boston to Washington DC at about 6 hours

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and 40 minutes. But all of this begs a

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fundamental question. Why does Japan's

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human geography look like this in the

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first place? Why does so much of Japan's

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population all live crammed together

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within a relatively narrow straight line

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across a small part of the country? And

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why is the rest of the country so much

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more relatively empty by comparison?

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First of all, it helps a lot to just

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simply look at a topographic map that

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shows Japan's elevation. Japan is one of

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the most mountainous countries in the

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world with about 73% of the country's

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total land area covered by them, leaving

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behind only about a quarter of the

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country left for significant human

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habitation in the few scattered areas of

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flatter land where urban development is

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easier and more affordable. Since time

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immemorial, this fact has left the

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people of the Japanese archipelago

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restricted to living within close

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proximity to each other along the

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coastal plains and across the few

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flatter areas within the interior where

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some stepped rice fields can be placed

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in the hills. There are pockets of flat

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land found all across the country from

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the west to the east and from the north

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to the south. But you will note how the

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Thai belt follows across what happens to

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be the three largest continuous areas of

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flat land found anywhere in the country.

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The Kai plane that encompasses the

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cities of Osaka, Kobe, and Kyoto. The

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Noi plane that encompasses Nagoya. And

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the single largest plane of all that can

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be found anywhere in Japan. The Kanto

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plane that encompasses the mega city of

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Tokyo. All three of these planes also

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have large rivers that flow through them

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that make them ideal centers for

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agriculture and supporting large

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populations. The Nagoya metropolitan

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area, crowded within the Novi plane, is

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Japan's third largest metro area, home

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to more than 9.3 million people. The

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Osaka metropolitan area crowded within

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the flat kai plane is the second largest

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home to more than 19.3 million people.

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While the Tokyo metropolitan area

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crowded within the Kanto plane is the

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largest not only in Japan but in the

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entire world with more than 41 million

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people living there today. More than

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double the population of the New York

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City metropolitan area in the United

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States. Collectively, these three planes

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alone are home to nearly 70 million

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people. Most of the population lives

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within the whole Taio belt and indeed

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more than half of the entire nationwide

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population. They've historically been

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the most major population, economic and

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political centers in Japan for centuries

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now that have long dominated over the

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rest of the country. But that's not just

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because they're the three largest areas

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of continuous flat land available for

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cityb building. The western side of the

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island of Hanju that faces the Sea of

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Japan has some areas of flat land around

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the coast, too. But on top of none of

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these areas being quite as large as the

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Kenai, Novi, and Kanto plains that are

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over on the Pacific side, they have

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multiple other disadvantages that have

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always made them less attractive places

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to settle in as well. For one thing, the

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Pacific side of Japan, for whatever

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reason, was also blessed by the RNG

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geography gods with significantly

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larger, deeper, and more useful natural

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harbors as well. Almost miraculously,

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Japan is home to not one but two of the

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most incredible natural harbors that can

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be found anywhere on the planet that are

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simultaneously huge, deep, exceptionally

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wellsheltered and directly connected to

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large flat hinderlands that can support

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huge adjacent population centers, Tokyo

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Bay and Osaka Bay, which of course are

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also directly connected to the huge flat

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Kanto and Kenai plains. Tokyo Bay in

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particular, large, very deep, very well

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sheltered, and surrounded by the flat

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Kanto plane that's home to Tokyo and

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it's 41 million people, is so comically

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overpowered from a commercial trade

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perspective that it alone handles around

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350 million tons of seaborn cargo

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annually, which is comparable to the

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entire maritime trade volume of the

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whole of Italy combined. While not quite

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as exceptional as the Tokyo and Osaka

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bays are, the Eay Bay that connects

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directly to the Nobi plane where Nagoya

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is concentrated is also still world

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class, being huge, deep, and fairly well

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sheltered with the huge Nobi plane

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directly adjacent. Obviously, these

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three worldclass natural harbors that

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just so happen to directly connect to

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the three largest flat planes in the

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country made them even more obvious

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centers to settle in in order to

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capitalize on the ridiculous commercial

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trade and naval potentials. But on top

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of these three, the Pacific side of

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Japan has many other excellent natural

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harbors as well, including the

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Kangoshima and Nagasaki bays on the

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Pacific facing side of Kiushu and

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Hiroshima Bay on Honu. The western sea

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of Japan- facing side of Honshu by

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comparison is nowhere near as jagged as

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the Pacific facing side is. It is

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significantly smoother and as a result

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it has nowhere near as useful of natural

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harbors and ports as the Pacific facing

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side has. The only notable harbors on

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the Sea of Japan side of Honshu are

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Misuru Bay and the Porta Nigatada, but

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both of them are still just a tiny

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fraction of the size of the massive

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natural harbors over on the Pacific side

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like the Tokyo and Osaka bays. And

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neither of them are connected to as

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large of a flat plane in the interior

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that can support millions of people

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nearby to sustain trade. The Sea of

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Japan side of Honshu and the entire

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northern island of Hokkaido simply have

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nowhere near as ideal natural harbors to

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utilize for trade and commerce, on top

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of nowhere near as large of planes to

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build cities in, compounding other

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disadvantages to support huge

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populations even further. And to make

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the Pacific side of Japan even more

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advantageous, it also has the Sato

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inland Sea, which is without a

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coincidence placed directly in the

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center of the Taiheo Belt. Because the

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vast majority of Japan's land mass is

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mountainous, the islands have an

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abundance of water. But the dir of flat

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land also means that nearly all of the

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rivers running through the interior are

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rough and full of rapids and waterfalls

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that make them completely unsuitable for

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interior navigation and trade. Something

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that's made even worse by the fact that

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most of the rivers don't even connect

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together either. But what Japan does

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have that more than makes up for the

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lack of navigable rivers is the Sato

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Inland Sea. the largely enclosed body of

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water that's protected from the rest of

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the Pacific between the main islands of

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Honshu, Hyushu, and Shikoku. Between

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these main islands, there are only four

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very narrow straits that connect the

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Sato Windland Sea with the rest of the

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greater Pacific, which makes its water

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significantly more calm than anywhere in

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the surrounding ocean. While the tidal

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currents within the four narrow straits

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leading into and out of the sea can be

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strong and complex, the rest of the sea

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is exceptionally navigable and it

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blesses Japan's geography with one of

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the largest internal seas for navigation

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and trade that can be found anywhere in

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the world. To give you just a sense of

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the Sato Woodland Sea's scale, if you

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placed it over the northeast coast of

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the United States, it would stretch from

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Washington DC beyond New York City into

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a southern Connecticut. There's also

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around 700 separate smaller islands that

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can be found dotted all across the Sato

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Woodland Sea as well. Several of them

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complete with their own incredible deep

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natural harbors that provided abundant

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safe anchorage and stopovers for ship

10:48

steering storms [music]

10:49

which made the whole body of water

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perfect for early maritime trade during

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the ancient and medieval eras. [music]

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The sea also provides a moderating

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effect on the regional climate around it

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to the extent that it's often referred

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to as Japan's Mediterranean, an area

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with year round warm temperatures that

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supports yearround navigation and

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agriculture. During pre-industrial times

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in Japan, building roads across Japan's

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mountainous terrain to connect disperate

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flat areas together was extremely

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difficult. But the calm waters of the

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Sato Windland Sea provided a critical

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alternative for much easier and

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efficient sea-based transportation

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instead. Even better at the eastern edge

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of the sea, the presence of a waji

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island created the even further enclosed

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Osaka Bay within it, directly connected

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to the huge flat area of the Kenai plane

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in the interior. Thus, from early on

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within Japan's history, the Sato

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Windland Sea became the critical

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maritime trade artery that connected the

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Kenai plane in the Osaka Bay and all the

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other areas around its shorelines with

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the rest of Honshu to the east,

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including the Nobi and Kanto plains with

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their own ideal harbors. And with

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mainland Asia and Korea further to the

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west, all of this huge trade volume

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flowing through it transformed the Sato

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Windland Sea into the wealthiest area of

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Japan for centuries, which encouraged

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settlement around it and which in

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particular directly contributed to the

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massive population growth in the Kenai

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plane that gave rise to Japan's early

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political center in Kyoto and what

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eventually became the mega port city of

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Osaka. For centuries, it was Osaka that

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was the economic epicenter of Japan

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because of all of these advantages. And

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by the time of the Tokugawa shogunit,

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all of Japan's feudal lords, known as

12:30

Damio, had established an office in the

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city that were known as Osakaya Shiki,

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which were among the earliest forms of

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banks in Japan, which further reinforced

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Osaka's early importance. And by the

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time of the industrial age, the other

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cities around the sedland sea like Kobe,

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Okyama, Takamatsu, Fukuyama, Hiroshima,

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and Kea Kiushu all developed into major

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industrial shipping and naval centers as

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well, carrying over the Sato Windland

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Se's importance into the modern era and

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further solidifying the population

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concentration within what would become

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known as the Taihillo belt that runs

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directly across it. After the Tokugawa

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shogun had managed to largely unify

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Japan in the early 17th century, the

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shogun decided to establish the seed of

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their power away from the historical

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imperial capital at Kyoto towards the

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east at Ido within the larger Kanto

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plane. One of the most profound impacts

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on Japan's human geography and

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population pattern that has ever

13:25

happened. The shoguns relocated their

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administrative center to Ido, which

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would later be renamed to Tokyo during

13:30

the 19th century in order to distance

13:33

themselves from the emperor in Japan's

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traditional nobility in Kyoto so that

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they wouldn't be overshadowed by them.

13:39

While they also saw the potential for

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rapid urban development in the large and

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expansive Kanto plane that was still

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fairly underdeveloped by the time of the

13:47

early 17th century. At that time, Ido

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was nothing but a small castle town that

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was probably only home to a few tens of

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thousands of people. But within only a

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century of Tokugawa showing of rule with

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Ido as their de facto capital by around

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1700, its population had exploded to

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more than a million people, which

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transformed it from a small town into

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one of the largest cities in the world

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within only a couple of lifetimes.

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Fueling this enormous growth of people

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in Ido and the Kanto plane and elsewhere

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along the modern Taihio belt during the

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Tokugawa era was the shogunits centuries

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long policy that was known as Sanin Ko

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Thai which required all of Japan's

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feudal lords or doio to alternate living

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between their domain and Ido every other

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year. The hundreds of damio at any given

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time in Japan were forced by this policy

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to maintain a lavish residence both at

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their homes and in the shogun's capital

14:39

at Ido. And every other year when the

14:41

domino moved back and forth between

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them, they were forced to undergo

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expensive and lavish processions with

14:47

their full entouragees. For the Shogun,

14:50

the policy was a deliberate strategy to

14:52

force the domios and their families into

14:54

a state of surveillance in the capital.

14:56

[music] While the extreme financial

14:58

burden of maintaining lavish mansions in

15:00

both locations and moving back and forth

15:02

between them every other year was both

15:04

time and money that they couldn't spend

15:06

on plotting to overthrow the shogun.

15:09

Their frequent travel back and forth

15:11

with their full launchages also

15:12

incentivized road building and the

15:14

development of inns and other facilities

15:16

along the routes they took which helped

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generate early economic activity along

15:20

them. Over time, five primary routes

15:23

were developed that the domios took

15:25

between their domains in Ido. And the

15:27

most used route out of all of them falls

15:29

directly along the Taihi belt today

15:31

between Ido and the old imperial capital

15:33

at Kyoto. Which meant that this route

15:35

became rapidly economically developed

15:37

across the Tokugawa era into the 19th

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century and was already the most

15:42

developed part of the country leading

15:43

into the era of industrialization that

15:45

accelerated its growth even further.

15:48

Another major key to the puzzle that

15:50

influences the location of Japan's

15:52

population across the Taihill belt today

15:54

are the presence of ocean currents which

15:56

dramatically influence Japan's regional

15:58

climates. This is a map of the average

16:00

winter sea surface temperatures that are

16:02

found in the western Pacific using

16:03

satellite data. From the south, the

16:06

Kiroio current functions in a similar

16:08

manner to the Gulf Stream in the North

16:09

Atlantic, carrying warm waters from the

16:12

Philippines northward along the eastern

16:13

shores of Japan. This current brings

16:16

warm and moist air along with it, which

16:19

highly contributes to the mild winters

16:21

and humid summers that are experienced

16:23

in Kyushu, Shikoku, and southeastern

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Honshu, basically immediately along the

16:28

Taihi belt. And it's what keeps Tokyo in

16:31

particular relatively warm for a city at

16:33

its latitude. At the same time, an

16:36

opposite oceanic current also comes down

16:38

to Japan from the north that's known as

16:40

the Oashio current. A cold subarctic

16:43

current that flows south from the Arctic

16:45

Ocean through the Bearing Straight that

16:47

carries frigid but nutrientrich Arctic

16:49

waters along with it. Almost immediately

16:52

northeast of Tokyo Bay, the cold Oshhio

16:55

current collides with the warm Kiroio

16:58

current, creating one of, if not the

17:00

richest fishery areas on the planet that

17:03

has always been easy to capture and

17:05

exploit from the relative safety of

17:07

nearby Tokyo Bay to help support the

17:09

population across the Kanto plane. The

17:12

cold air above the Oshio current

17:14

contributes substantially to the colder

17:16

climate that can be found in the

17:17

northern island of Hokkaido and along

17:19

the western coast of Honshu that faces

17:21

the Sea of Japan. But there's a lot of

17:24

other complex climatic effects going on

17:26

here that makes them even worse. A

17:28

branch of the warm Kiroio current known

17:31

as the Tsushima current breaks off and

17:33

flows into the Sea of Japan from the

17:35

south. But during the winters, when cold

17:37

and dry air originating from Siberia

17:39

will blow across the Sea of Japan, the

17:41

cold air masses will pick up the

17:43

moisture and warmth from the relatively

17:45

mild Tsushima current and become

17:47

saturated. When that saturated air then

17:49

hits the mountains in western Honshu and

17:51

Hokkaido, it'll rapidly cool and then

17:54

dump an absolutely enormous amount of

17:57

snow in the process. like to the point

17:59

that northwestern Honchu and Hokkaido

18:01

are among the snowiest locations that

18:03

can be found anywhere on the planet. It

18:06

also means that eastern Honshu that

18:08

faces the warmer waters of the Pacific

18:10

along with Shikoku and Kiushu experience

18:13

dramatically less snowfall than the

18:15

western side of Honshu and Hokkaido

18:17

suffer throughout the winter. An area of

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Japan that's literally referred to by

18:21

the Japanese as the snow country. From a

18:24

North American perspective, the climate

18:26

found in Hokkaido is more similar to the

18:28

area around Lake Ontario, like Toronto,

18:30

Buffalo, and Rochester. The northern and

18:32

western sides of Honshu are generally

18:34

more comparable to coastal New England

18:36

and the Mid-Atlantic. While the eastern

18:38

side of Honshu, along with Shikoku and

18:40

Kiushu, are much warmer and rainier and

18:42

are more comparable to Georgia and South

18:44

Carolina. Northwestern Honshu is so

18:47

snowy because of this effect during the

18:49

winter that Ali city in the north of the

18:51

island holds the distinction of being

18:53

the snowiest major city in the world.

18:56

It's 265,000

18:58

people experience a whopping average of

19:00

8 m or 26 ft of snowfall every winter.

19:04

Nearly 6 times as much snowfall as

19:07

Minneapolis experiences on average in

19:09

the United States. Snowfall gets so deep

19:12

in some parts of the snow country that

19:14

some buildings are designed and built

19:16

with a special entrance through their

19:18

second story. All kinds of special

19:20

infrastructure considerations have to be

19:22

made in the snow country. Residents have

19:24

to remove the piles of snow that

19:26

accumulate on their roofs in order to

19:28

prevent its weight from crushing and

19:29

caving them in. Streets are often lined

19:32

with covered sidewalks to make sure that

19:34

residents can still get around in the

19:35

winter. Streets are equipped with

19:37

sprinklers that deploy warmer

19:39

groundwater to keep them passible by

19:41

melting snow. And in some towns, people

19:43

even used to tunnel paths through the

19:45

snow in order to get to each other's

19:47

homes. All of this means the development

19:49

in the snow country is just more

19:51

expensive and timeconuming than it is

19:52

elsewhere in Japan. And thus, when you

19:55

put this all together, it's pretty easy

19:57

to see why the area that became the

19:59

Taiho Belt is by far the most densely

20:02

populated part of the country and why it

20:05

has been for a very long time now. The

20:07

Taiho Belt has the advantages of the

20:09

Sato inland Sea for a large, calm, and

20:12

easily navigable body of water to

20:14

facilitate trade, movement, and

20:16

commerce. It encompasses by far the best

20:19

natural harbors that can be found in the

20:20

islands and some of the best anywhere in

20:22

the entire world like Tokyo and Osaka

20:24

bays. Both of which are directly

20:26

connected to large flat hindrlands in

20:28

the Kenai and Kanto plains with another

20:31

worldclass harbor at Eay Bay in between

20:33

them connected to another large flat

20:35

hinderland in the Noi plane which

20:37

enabled a sort of leaprogging ability

20:39

for ships early in history to take

20:41

between them in the Sato Windland Sea

20:43

that established early modern Japan's

20:44

commercial superighway. It has by far

20:48

the more milder climate in Japan

20:49

compared to the western sea of Japan

20:51

side of Honshu that gets buried by snow

20:54

during the winter. And it's also closest

20:56

to what's arguably the richest fishery

20:58

in the world off the coast of eastern

21:00

Honshu where the warm Kiroio and

21:03

coldosio currents clash together. One of

21:06

the very few notable cons of the Taihi

21:09

belt in the Pacific side of Japan from a

21:11

geographic perspective is that it's also

21:13

located across the most natural

21:14

disasterprone area of Japan as well

21:17

which experiences more damaging

21:19

earthquakes and tsunamis than anywhere

21:21

else in the country does due to the

21:22

locations of the Japanese archipelago

21:24

subsurface fault lines and the

21:26

coastline's exposure to the vast open

21:29

Pacific on this side. But these natural

21:31

disasters are sporadic enough that the

21:33

numerous advantages of concentrating

21:35

within the Taiho belt have repeatedly

21:38

outweighed them enough across the

21:40

centuries to be decisive. And that in a

21:43

nutshell is why Japan's population

21:46

exists where it does today. Now, there's

21:49

a lot of data that goes into producing

21:50

these kinds of videos. Whether it's

21:52

visually showing you the scale of the

21:53

Taihei belt compared to the US northeast

21:55

coast, detailing out how the system of

21:57

ocean currents, mountains, and wind

21:59

patterns contribute to northwestern

22:00

Japan's enormous snowfall levels, or

22:03

showing you the risk of natural

22:04

disasters across Japan that are heavily

22:06

concentrated within the Tahoe belt. The

22:08

ability to actually visualize raw data

22:10

like this on the map instead of just

22:12

reading about it in text format is

22:14

exactly what makes learning about these

22:15

kinds of geography based subjects so

22:18

fascinating to me. And it's why the

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Interactive Summary

Japan, one of the world's most populous countries, has a unique population distribution where a vast majority of its 123 million people, around 80 million, reside within a narrow, linear region called the Taiheiyo Belt (Pacific Belt or Tokaido corridor). This belt, covering less than 10% of Japan's land, is extremely densely populated, accounting for 70% of the nation's economy. This concentration is largely due to several geographical advantages on the Pacific side of Honshu, including the presence of the three largest continuous flat plains (Kanto, Kenai, Nobi) ideal for urban development and agriculture, world-class natural harbors (Tokyo Bay, Osaka Bay, Ise Bay) for trade, and the calm, navigable Seto Inland Sea which served as a crucial historical trade artery and features a mild, Mediterranean-like climate. Political factors, such as the Tokugawa Shogunate's relocation of its capital to Edo (Tokyo) and the Sankin Kōtai policy, further spurred development along this route. Additionally, warm ocean currents (Kuroshio) contribute to milder winters on the Pacific side, while the collision of warm and cold currents creates rich fisheries. Conversely, the Sea of Japan side suffers from a lack of large flatlands, inferior harbors, and immense winter snowfall due to cold Siberian air picking up moisture from the Tsushima current and hitting the mountains, making development challenging and expensive. Despite the Taiheiyo Belt being prone to natural disasters like earthquakes and tsunamis, its numerous advantages have historically outweighed these risks, solidifying its status as Japan's most populated and economically vital region.

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