体感！グレートネイチャー 2025年2月6日 名画が語る“地球の力”〜フランス・大地誕生の謎
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00:00:00I'm a little bit nervous, but I'll do my best.
00:00:04I'm not going to lose, I'll do my best.
00:00:08I'll do my best!
00:00:12I'll do my best!
00:00:16I'll do my best!
00:00:20I'll do my best!
00:00:24I'll do my best!
00:00:28I'll do my best!
00:00:59The father of contemporary painting, Cézanne,
00:01:03revealed himself to the public.
00:01:11Fontainebleau, which draws attention.
00:01:19Millet, which depicts the farmers living on the land.
00:01:28France, the land of art.
00:01:34What did the genius painters try to depict through the landscape?
00:01:47They sought the landscape depicted in the painting,
00:01:50and went all the way to France.
00:01:55Ah, here it is!
00:01:59What did Monet discover in his painting of the Beryl Island?
00:02:05This is what we call volcanic tissue.
00:02:09It's more or less 500 million years old.
00:02:15What about the Colossal Island, painted by Matisse?
00:02:21This deformation, the disappearance of the tissue,
00:02:24under the effect of a tectonic push coming from the south,
00:02:27from the African region.
00:02:30What about Fontainebleau, painted by Millet?
00:02:3635 million years ago, the sea left enormous amounts of sand.
00:02:44Monet.
00:02:47Cézanne.
00:02:51Matisse.
00:02:54Millet.
00:02:59From the landscape depicted in the famous painting,
00:03:02we approach the mystery of the formation of France in 500 million years.
00:03:21France
00:03:24Today, we will take you to France.
00:03:29Since the 19th century,
00:03:31the genius painters have drawn the landscape of this land.
00:03:39Monet's Beryl Island, representing the Impressionists.
00:03:44And Etolta's Danai.
00:03:52Millet's Fontainebleau, a peasant painter.
00:04:00Cézanne's modernist painting, Saint-Victor.
00:04:06Matisse's Colossal Island.
00:04:12What kind of charm is hidden there?
00:04:20First, let's go to Beryl Island, painted by Monet.
00:04:35Beryl Island, France
00:04:39About 500 kilometers from Paris,
00:04:42the Bretagne Peninsula in the western part of France.
00:04:49To the south of the peninsula,
00:04:51it takes about an hour by car ferry to Beryl Island.
00:04:55Beryl Island, France
00:05:01Beryl means a beautiful island.
00:05:06The center of the island, about 50 kilometers away,
00:05:09is the port town of Le Palais.
00:05:12About 2,500 people live there.
00:05:17There are quite a few shops for 2,500 people.
00:05:25This is a fishing shop.
00:05:28There are various things.
00:05:30Oh, there's a life jacket.
00:05:40Cute accessories.
00:05:43Cute accessories.
00:05:45Whales, fish, yachts.
00:05:50It's a port town after all.
00:05:58In 1886, he visited Beryl Island
00:06:03and painted about 40 paintings.
00:06:12This is Claude Monet, a representative of the Impressionists.
00:06:18He is famous for his series of watercolors, which he continued to paint in his later years.
00:06:24Watercolors
00:06:40Watercolors painted by Monet in 1903.
00:06:46What is very characteristic of this work
00:06:50is that the whole surface of the pond is painted.
00:06:56The water lily floats there,
00:06:59and the water lily is added a little red
00:07:02to accentuate the whole screen.
00:07:07And the characteristic of this work
00:07:11is the way of painting the water lily.
00:07:16This surface probably doesn't move that much,
00:07:20but by painting it moving little by little,
00:07:23I think it creates something lively on the screen.
00:07:32And another one.
00:07:36In 1886,
00:07:38this is a work by Monet when he was 45 years old.
00:07:41It's Beryl in the Rain.
00:07:47This island is very natural,
00:07:50especially because there are a lot of trees along the coastline.
00:07:53I'm very good at painting the scenery along the coastline.
00:07:56In the middle of the coastline,
00:07:59there is a very eerie rock.
00:08:02I'm very good at painting it.
00:08:05The word Ghibelle means
00:08:08a magnificent beauty in the ancient words of the British.
00:08:15This work is about a sudden rain,
00:08:18and then a dark, eerie scene.
00:08:21That's the kind of work I'm doing here.
00:08:24But it's a natural landscape in France,
00:08:27and I want to immerse myself in it
00:08:30and paint it myself.
00:08:38A magnificent beauty in a dark, eerie landscape.
00:08:42What kind of coastline is it?
00:08:45Hello, Dr. Delpont.
00:08:48Hello, sir.
00:08:51How are you?
00:08:54Very well, and you?
00:08:57Nice to meet you again.
00:09:00The guide is George Delpont,
00:09:03a geologist from Beryl Island.
00:09:06He is also familiar with the story of Monet's stay.
00:09:09I would like to go to the place
00:09:12where Monet painted the sea buffalo.
00:09:15Well, we can see this landscape
00:09:18on the wild coast,
00:09:21about 10 km from here, from Palais.
00:09:24The word wild is used
00:09:27to evoke the force,
00:09:30the violence of the winter storms.
00:09:33The sea buffalo is a wild animal
00:09:36with a very strong body.
00:09:39That's exactly it.
00:09:42If you want, we can go there.
00:09:45First, let's go to the village
00:09:48where Monet stayed,
00:09:51the Kervila Ouan village.
00:10:06This is the house
00:10:09where Claude Monet stayed
00:10:12before going to paint the different colors
00:10:15of the coast,
00:10:18varying with the different sunrises.
00:10:21I can show you the house
00:10:24where he lived.
00:10:27It's almost 150 years old.
00:10:30It's still there.
00:10:33Monet used the first floor
00:10:36as a storage room
00:10:39and slept on the second floor.
00:10:45Monet was accompanied
00:10:48by a man with a donkey.
00:10:51He put all his things on the donkey
00:10:54and then he walked
00:10:57to the coast.
00:11:04The road Monet took to the coast
00:11:07is almost a wild animal road.
00:11:12I wonder if Monet walked on this road.
00:11:17Monet wrote a letter
00:11:20about the impression of this land.
00:11:25I found a fascinating landscape
00:11:28so I decided to stay on the island.
00:11:32The rocks and caves are wonderful.
00:11:36It's a place where demons
00:11:39are likely to come out.
00:11:45A place where demons are likely to come out?
00:11:57That rock!
00:12:02I can see the sea!
00:12:06There are rocks in the sea!
00:12:10Perhaps more?
00:12:19From there it's not so bad.
00:12:22It's here!
00:12:25We can see the little rock there.
00:12:28It's here!
00:12:34Wow!
00:12:38It's the same landscape
00:12:41as the Beryl of the rain!
00:12:46It's the same landscape
00:12:49as the Beryl of the rain!
00:13:00The rock of the beast king
00:13:03is that Giver!
00:13:06The rock of the beast king
00:13:09is that Giver!
00:13:18I'm sure that Monet
00:13:21stood here
00:13:24and drew pictures.
00:13:36Wow!
00:13:39The sea is full of rocks!
00:13:48Monet was fascinated by this landscape
00:13:51and drew 40 pictures.
00:13:54The sea is like a mosquito
00:13:57that refuses to come close to people.
00:14:00How did he draw it?
00:14:12The key to the mystery
00:14:15is discovered in another work.
00:14:18The key to solving the riddle was drawn on a different piece of paper.
00:14:31Look closely.
00:14:34Mone drew a part of the rock with green, white, and red.
00:14:41What on earth is this?
00:14:54Let's look for Mone's color on the beach.
00:14:58Wow!
00:15:04Wow!
00:15:07The rocks around here are a little bluish.
00:15:12Wow!
00:15:17Indeed, the green rocks are bluish.
00:15:20Wow!
00:15:23Moreover,
00:15:27the surface is thin and peeled off.
00:15:31The thickness is only a few millimeters.
00:15:36What on earth is this rock?
00:15:40We can't say these are micas, but they are part of the family of phyllites,
00:15:46which look like this.
00:15:49This is the result of deep pressure.
00:15:54Metamorphosis, that is, the minerals changed their composition
00:15:59and then recrystallized according to plans
00:16:03in order to form these rocks.
00:16:10This is a type of metamorphosis rock, called Senmai rock.
00:16:15It has a variety of colors, such as green, white, and red.
00:16:22This is the exact color Mone used to draw the rock.
00:16:27Even though they are the same rock, why is there a difference in color?
00:16:34The island was formed first by the accumulation of ash
00:16:40during volcanic eruptions more or less 500 million years ago.
00:16:46All of these are different alteration phenomena
00:16:53depending on the real mineral content of each part.
00:17:00So we will have different alteration sensitivities,
00:17:05which will give us different colors.
00:17:13Green is magnesium,
00:17:16white is silicon,
00:17:19red is iron,
00:17:22and so on.
00:17:25The difference in minerals contained in the original volcanic ash
00:17:30created different colors.
00:17:38Green, white, and red.
00:17:42The color of the rock drawn by Mone
00:17:46shows the volcanic activity that occurred 500 million years ago.
00:17:58But when did the volcanic ash turn into Senmai rock?
00:18:07When I told you earlier about the Gondwana and the Eurasia continents,
00:18:16when these two continents came together,
00:18:20this volcanic ash was metamorphosed
00:18:26and transformed into a rock that geologists call volcanic tuff.
00:18:36Let's go back to 500 million years ago and summarize the story of the volcanic ash.
00:18:46500 million years ago,
00:18:49it is believed that there were the large Gondwana continent in the south
00:18:54and several smaller continents in the north.
00:19:00Eventually, several continents in the north came together.
00:19:06It became the Eurasia continent.
00:19:09On the other hand,
00:19:12there was a land that would later become the foundation of Western Europe.
00:19:19The origin of the Beril Island
00:19:22is an ocean where volcanic ash was deposited
00:19:25due to the volcanic activity that occurred during that period.
00:19:29After that, the Gondwana continent and the Eurasia continent came together.
00:19:38Approximately 300 million years ago,
00:19:41when the supercontinent Pangaea was formed,
00:19:44the ocean that would later become the Beril Island
00:19:47sank into the supercontinent.
00:19:50The pressure from the sinking of the plate
00:19:53was applied to the ocean
00:19:56and the heat from the magma activity was also applied.
00:20:00Due to the heat and pressure,
00:20:03the ocean became a coniferous ocean.
00:20:08After that, the Beril Island took a long time
00:20:12to move to its current position.
00:20:21The remains of the Beril Island
00:20:24are the remains of the Gondwana continent.
00:20:27It is believed that the Gondwana continent
00:20:30and the Eurasia continent
00:20:33are the remains of the Beril Island.
00:20:36The Beril Island is a type of coniferous island.
00:20:39It is green, white, and red.
00:20:45It is the color of the history of the first coniferous island in 500 million years.
00:20:55Mone painted it.
00:21:02He was able to see different colors of rocks,
00:21:06even if he was not a geologist,
00:21:09that perhaps people today, who are always in a hurry,
00:21:13do not have time to see.
00:21:17The devil is about to appear.
00:21:20In the landscape that Mone felt,
00:21:23the vastness of the earth was hidden.
00:21:28Now that we have seen the landscapes of Beril,
00:21:32I advise you to go and see other territories
00:21:36that were painted by Claude Mone,
00:21:39including the cliffs of Etorta, in Normandy.
00:21:53The cliff of Etorta, painted by Mone.
00:21:56The cliff of Etorta,
00:21:59500 km north of Beril,
00:22:02in search of the original landscape.
00:22:08Look, it is the Seine river that flows on the right.
00:22:12The Seine River!
00:22:19The Seine River, which is the water source of the Alps,
00:22:23flows about 780 km
00:22:26along the coast of Normandy.
00:22:32The length of the Normandy Bridge over the river
00:22:36is 2,140 m.
00:22:45It is another 30 minutes across the Seine River.
00:22:57We can see the city of Etorta.
00:23:01It is a secret place by the sea in front of the Eiffel Tower.
00:23:14Trees, bricks,
00:23:18it is a serious building.
00:23:22It is almost the same as the middle of the 19th century
00:23:26but the landscape is different.
00:23:33This is the painting by Mone.
00:23:38There is a white cliff in the back of the coastline.
00:23:48This is also the coast of Etorta,
00:23:51painted by Mone.
00:23:54The cliff behind the sunset is painted black.
00:24:04Mone has painted almost 50 pieces of the Etorta cliff.
00:24:14Etorta is wonderful in itself.
00:24:18You can't express it well,
00:24:20but you can even remember your anger.
00:24:27To paint Etorta,
00:24:30you need hundreds of canvases with both hands.
00:24:39What is it that you can't express
00:24:42even if you do your best?
00:24:51Hello, Dr. Oez.
00:24:54Hello, sir. Nice to meet you.
00:24:57Nice to meet you, too.
00:25:00The guide is Mr. Bernhard Oez.
00:25:04He is a geologist who has studied the history of this land.
00:25:09Mone made Etorta famous by his paintings,
00:25:13but Etorta also has a geological history.
00:25:17I will try to tell you about this geological history.
00:25:21Let's go and visit it together.
00:25:28Let's go and see the Etorta cliff.
00:25:31There are quite a few people.
00:25:34It's the sea!
00:25:39What a beautiful landscape!
00:25:47The Porte d'Amon is on your right.
00:25:54And the Porte d'Aval,
00:25:57with its needle behind it,
00:26:00is on your left.
00:26:06The painting Mone painted
00:26:09is the right hand of the coast,
00:26:12the cliff of Amon in the north.
00:26:17And the other painting is
00:26:20the left hand of the coast,
00:26:23the cliff of Aval in the south.
00:26:40Let's look at it from the sky.
00:26:42This is the cliff of Amon
00:26:45from the north side of the coast.
00:26:50And this is the cliff of Aval
00:26:53from the south side
00:26:56of the city of Etorta.
00:27:06And this is the cliff of Haliwa.
00:27:09And this is Haliwa.
00:27:21Wow!
00:27:24There are more cliffs in the back.
00:27:32It's 130 kilometers long.
00:27:39But how was this place
00:27:42built?
00:27:51To solve this mystery,
00:27:54let's get closer to the cliff.
00:27:59In front of this cliff,
00:28:02what do you see in the landscape?
00:28:05Wow!
00:28:08There are a lot of gray,
00:28:11or white,
00:28:14but also a lot of black lines.
00:28:17Yes.
00:28:20In the white,
00:28:23you see regular lines.
00:28:26These lines were already represented
00:28:29in the paintings of Mone.
00:28:34That's right.
00:28:37There are a lot of black lines
00:28:40on the white rocks.
00:28:48And the actual cliff
00:28:51has white and black layers
00:28:54overlapping each other
00:28:57like a thick millefeuille.
00:29:00Why?
00:29:05Let's get closer
00:29:08and find out.
00:29:12First, the white layers.
00:29:15So,
00:29:18we can see that this rock
00:29:21is made of...
00:29:24Here is a piece of chalk.
00:29:27Look.
00:29:30It's made of gas.
00:29:32This gas is carbonic gas,
00:29:35CO2.
00:29:38This rock is made of calcium carbonate.
00:29:41It's a carbonate
00:29:44that reacts with the acid
00:29:47and produces CO2.
00:29:50This white part is chalk.
00:29:53All the cliffs here
00:29:56are made of chalk.
00:29:59Is there a special chalk
00:30:02on the Seine?
00:30:05How was it made?
00:30:09All the chalk
00:30:12was deposited
00:30:15from 100 million years ago.
00:30:18There was a sea here,
00:30:21a warm sea.
00:30:24In this warm sea,
00:30:26there were algae
00:30:29called coccoliths.
00:30:32Most of the chalk
00:30:35was formed by these coccoliths.
00:30:40About 100 million years ago,
00:30:43the Earth was warm
00:30:46and the temperature was over 10°C.
00:30:49The water level was
00:30:52as high as 250 meters.
00:30:54At that time,
00:30:57Etorta was also
00:31:00in a warm sea.
00:31:03At that time,
00:31:06there were a lot of
00:31:09coccoliths in the sea.
00:31:12The coccoliths
00:31:15deposited
00:31:18in the sea
00:31:21and became a layer of chalk.
00:31:24The coccoliths
00:31:27were deposited
00:31:30in the sea
00:31:33and became a layer of chalk.
00:31:36The coccoliths
00:31:39were deposited
00:31:42in the sea
00:31:45and became
00:31:48a layer of chalk.
00:31:50The surface of this rock
00:31:53is very hard.
00:31:59This rock
00:32:02is a silex.
00:32:05This rock
00:32:08is made of silica.
00:32:11This silica
00:32:14comes from siliceous organisms.
00:32:17Silices only form
00:32:20when the temperature,
00:32:23oxygenation of water
00:32:26and the depth of the sea are low.
00:32:31About 100 million years ago,
00:32:34the water level rose
00:32:37and the sea level rose repeatedly.
00:32:43When the water level is low,
00:32:46sunlight reaches the seabed
00:32:48and a large number of
00:32:51coccoliths grow.
00:32:54The coccoliths have a hard silica shell
00:32:57and the coccoliths deposited
00:33:00and became a layer of chalk.
00:33:03When the water level is high,
00:33:06the coccoliths grow
00:33:09and the coccoliths deposited
00:33:12and become a layer of chalk.
00:33:15In this way,
00:33:18the coccoliths piled up
00:33:21and became a layer of chalk.
00:33:29The coast of Etorta
00:33:32where Monet was fascinated.
00:33:35100 million years ago,
00:33:38that was the bottom of the sea.
00:33:41And the bottom of the sea
00:33:44was a layer of chalk and flint.
00:33:47Two layers deposited alternately.
00:33:56Eventually, the sea level dropped
00:33:59and exposed to the ground.
00:34:02Because of erosion,
00:34:05it became what it is today.
00:34:07Etorta is wonderful itself.
00:34:10You can't express yourself well
00:34:13and even remember your anger.
00:34:16To paint Etorta,
00:34:19you need hundreds of canvases
00:34:22with both hands.
00:34:30The miracle scenery
00:34:33and the sea
00:34:35are hidden in Etorta.
00:34:38100 million years ago,
00:34:41that was the thickness of time.
00:34:44Monet kept fighting
00:34:47to express that.
00:35:05Etorta is a place
00:35:08where you can feel
00:35:11the beauty of nature.
00:35:14It is a place
00:35:17where you can feel
00:35:20the beauty of nature.
00:35:23It is a place
00:35:26where you can feel
00:35:29the beauty of nature.
00:35:32It is a place
00:35:35where you can feel
00:35:38the beauty of nature.
00:35:41It is a place
00:35:44where you can feel
00:35:47the beauty of nature.
00:35:50We can see the bell tower
00:35:53of the Church of Chagui-Lambière.
00:36:05It is a place
00:36:08where you can feel
00:36:11the beauty of nature.
00:36:14It is a place
00:36:17where you can feel
00:36:20the beauty of nature.
00:36:23It is a place
00:36:26where you can feel
00:36:29the beauty of nature.
00:36:32It is a place
00:36:35where you can feel
00:36:38the beauty of nature.
00:36:41It is a place
00:36:44where you can feel
00:36:47the beauty of nature.
00:36:50It is a place
00:36:53where you can feel
00:36:56the beauty of nature.
00:36:59It is a place
00:37:02where you can feel
00:37:05the beauty of nature.
00:37:09It is a place
00:37:12where you can feel
00:37:15the beauty of nature.
00:37:20It is a place
00:37:23where you can feel
00:37:26the beauty of nature.
00:37:30It is a place
00:37:32The next is Saint-Victor-Le-Saint in southern France.
00:37:47The artist is the father of modern painting, Paul Cézanne.
00:37:52He has drawn more than 800,000 paintings of this mountain.
00:37:57What inspired him to paint Cézanne?
00:38:06The next is Aix-en-Provence, the hometown of Cézanne.
00:38:18This is a famous French town built by the Romans.
00:38:28Wow, it's a tall platanus.
00:38:34It's a suzu-kake-no-ki.
00:38:37It's quite big.
00:38:46Oh, there are many fountains.
00:38:51Aix-en-Provence has abundant groundwater.
00:39:01There are more than 100 fountains.
00:39:07In the middle of the town...
00:39:13In the middle of the town...
00:39:19Oh, it's a statue of Cézanne.
00:39:24He's got a cane, an easel on his back, and a painting tool.
00:39:29He actually carried his feet to the mountain and painted.
00:39:34It's a Cézanne-like statue.
00:39:43Paul Cézanne is said to be the father of modern painting.
00:39:49At first, he was a member of the Impressionists in Paris.
00:39:55He returned to his birthplace in the 1880s,
00:40:01and began to explore his own style of painting.
00:40:08His work had a great influence on the art of the 20th century.
00:40:20The representative work of Cézanne is Saint-Victor,
00:40:26which is located in the outskirts of his hometown, Aix-en-Provence.
00:40:32Cézanne says...
00:40:35In order to paint a good landscape,
00:40:39I must first find a geographical foundation.
00:40:45How does Saint-Victor lay his roots?
00:40:50The geographical characteristics of the soil
00:40:54move my heart and make me feel better.
00:41:01What did Cézanne try to express
00:41:05with his geographical knowledge?
00:41:14In order to solve this mystery,
00:41:17Cézanne went to the hills of Les Robes
00:41:21in order to paint Saint-Victor.
00:41:27How are you?
00:41:32The guide is Yves Dutour,
00:41:36director of the Aix-en-Provence Natural History Museum.
00:41:41He is a geographer who is also familiar with Cézanne's paintings.
00:41:46Is this the hill where Cézanne painted Saint-Victor?
00:41:52Look.
00:41:54In front of you.
00:42:00I couldn't see it from the city,
00:42:04but it's magnificent.
00:42:08In Cézanne's time, there were no cypress trees.
00:42:13It must have blown a lot at the top of Saint-Victor.
00:42:16It hides the mountain,
00:42:18and it's like the painting we see here.
00:42:24This is Saint-Victor,
00:42:27painted more than 800,000 times by Cézanne.
00:42:39At an altitude of 946 meters,
00:42:43a cross of Provence stands.
00:42:49Saint-Victor
00:42:55And this painting has a different characteristic from the actual landscape.
00:43:02Yes, because he really focused on Saint-Victor
00:43:06in order to enlarge it on the whole size of his painting.
00:43:10He completely hid the landscape around
00:43:13to really focus only on Saint-Victor.
00:43:18Cézanne needed knowledge of geology to paint the mountains.
00:43:24Who taught him?
00:43:27He had some knowledge,
00:43:29because he had a very good friend, Antoine Fortuné-Marion,
00:43:32who was a geologist,
00:43:34and he brought him knowledge.
00:43:39Geologist Fortuné-Marion
00:43:43is a 7-year-old childhood friend.
00:43:48He was a good consultant for Cézanne's creative activities.
00:43:56If you want, I can take you to the place
00:43:59where Marion explained to Cézanne how to form Saint-Victor.
00:44:03Please do.
00:44:11Mr. Dutour guided us to the town of Aix-en-Provence
00:44:16in the middle of Saint-Victor.
00:44:29What did Cézanne learn about the origin of Saint-Victor?
00:44:37Here it is.
00:44:41Wow!
00:44:43I can see Saint-Victor.
00:44:49This is where Antoine Fortuné-Marion
00:44:54drew and explained to Cézanne how Saint-Victor was formed.
00:45:00There, at an altitude of about 300 meters,
00:45:05was a cliff on the edge of the earth.
00:45:17This is what Cézanne learned from Marion.
00:45:22This is what he wrote.
00:45:30This is Cézanne's sketchbook.
00:45:38On the back of the sketchbook,
00:45:42Marion drew a map of Saint-Victor.
00:45:52On the top of the mountain,
00:45:55there is a cross of Saint-Victor.
00:46:04Compared to the actual Saint-Victor,
00:46:08Marion's sketchbook is longer,
00:46:11but it is definitely a map of Saint-Victor.
00:46:18What did Marion explain to Cézanne
00:46:22about the origin of Saint-Victor?
00:46:26All the rocks formed at the bottom of the water.
00:46:30The tectonic movements,
00:46:32the formation of the Alps,
00:46:34led to the formation of Saint-Victor.
00:46:37Marion wanted to explain to Cézanne
00:46:40that Saint-Victor was formed by a geological fold.
00:46:44He drew a fold to explain to Cézanne.
00:46:48And then he showed this fold from a geological point of view.
00:46:52Yes, yes.
00:46:56Originally, the limestone rocks deposited at the bottom of the sea
00:47:00were the extremities.
00:47:05And the deformities.
00:47:08Some were lost due to erosion,
00:47:11and Cézanne told Cézanne
00:47:14that this was the origin of Saint-Victor.
00:47:22I must first find a geological foundation.
00:47:30Cézanne knew the existence of the force that lifted the earth,
00:47:34and he made the sketchbook run.
00:47:45Now, let's go up to Saint-Victor
00:47:48and experience the force that lifted the earth.
00:47:59Hello.
00:48:01The guide is Thierry Tortosa,
00:48:04a student at the National Museum of Natural History.
00:48:09This is the route to Saint-Victor.
00:48:17First, we head to the National Nature Preserve.
00:48:23Here, we can see the amazing environment
00:48:26that existed before the mountains were built.
00:48:30Then, we climb up to the cross of Provence,
00:48:33which stretches to the west,
00:48:36and explore the true nature of the force
00:48:39that lifted the earth.
00:48:42It's 7 kilometers on one side,
00:48:45and 650 meters above sea level.
00:49:01The area of the National Nature Preserve
00:49:04in Saint-Victor is 1.4 square kilometers,
00:49:07which is equivalent to 30 Tokyo Domes.
00:49:14The amazing environment that existed
00:49:17before the mountains were built
00:49:20and the force that lifted the earth
00:49:23are all in this place.
00:49:30What is Saint-Victor?
00:49:37We can see the red soil.
00:49:42We've arrived at a special site.
00:49:45It's a very important and interesting site.
00:49:48It's a scientific site where we work
00:49:51with the National Museum of Natural History
00:49:54to do research to understand the past of Saint-Victor.
00:49:57If you have a good eye,
00:50:00I'll write it down for you.
00:50:03If something is buried here,
00:50:06does that mean it's a fossil?
00:50:09Very likely.
00:50:12But not just any fossil.
00:50:15It's a specificity of the country.
00:50:18What kind of fossil is there?
00:50:21And even if you don't dig the ground,
00:50:24it's still exposed to the surface.
00:50:31It's like...
00:50:34I'm just picking it up randomly.
00:50:37It's red soil mixed with liquid.
00:50:43Let's compare.
00:50:46These are fossils, but not just any fossils.
00:50:49These are dinosaur egg fossils.
00:50:52What?
00:50:55Dinosaur egg fossils?
00:50:58What?
00:51:01We recognize them because they're always very flat.
00:51:05These fossils are full of egg shells.
00:51:12These are fragments.
00:51:15We have whole eggs that we can show you.
00:51:23These are for beginners.
00:51:26We put little labels on them.
00:51:29These are the results of last year's excavation.
00:51:32You can see the whole eggs here.
00:51:35They're in the wall.
00:51:38They could have been extracted.
00:51:43Dinosaur egg fossils with a clear outline.
00:51:47There are three ellipses, 20 cm in length and 10 cm in width.
00:51:58The shell is about 1 mm thick.
00:52:04Most of the egg's surface is broken and scattered,
00:52:07but inside...
00:52:10Can I touch it?
00:52:13Yes, of course.
00:52:16These are the fragments that fall from here.
00:52:19So this is how they were attached.
00:52:22I'm sure of it.
00:52:25More than 600 eggs were found
00:52:28from the 30-meter-wide excavation site.
00:52:31The eggs are in good condition.
00:52:34They're being carried out and stored.
00:52:37What kind of dinosaur eggs are they?
00:52:43We know that these are herbivorous dinosaur eggs,
00:52:46potentially titanosaur eggs,
00:52:49but we don't know for sure.
00:52:52We don't know for sure,
00:52:55but we know that these are herbivorous dinosaur eggs.
00:52:58We know that these are herbivorous dinosaur eggs,
00:53:01potentially titanosaur eggs,
00:53:04but we don't know for sure.
00:53:07That's why we're doing research to understand
00:53:10how these eggs were laid.
00:53:13If we have an idea of the laying strategy,
00:53:16we can maybe guess what the mother was that laid these eggs.
00:53:19I'm looking forward to the research that's to come.
00:53:22But when and how did the dinosaur eggs
00:53:26end up in the clay?
00:53:35We're in the red clay,
00:53:38which is typical of the upper Cretaceous of the province.
00:53:41We call it the Cretaceous, the Campanian stage.
00:53:44We're around 70 to 72 million years old.
00:53:47The plains were flooded after each rainy season,
00:53:50and the mud that overflowed from the rivers
00:53:53was brought in by the rain.
00:53:56The dinosaurs came to swim every year.
00:53:59Let's go back in time and sort out what Mr. Tortosa was saying.
00:54:02Let's go back in time and sort out what Mr. Tortosa was saying.
00:54:05150 million years ago,
00:54:08the earth was a warm and shallow sea.
00:54:11150 million years ago, the earth was a warm and shallow sea.
00:54:14The coral and other debris settled on the bottom of the sea
00:54:17and became a limestone coast.
00:54:20This limestone coast was later known as St. Victor's Island.
00:54:23This limestone coast was later known as St. Victor's Island.
00:54:28The place was the southern bottom of the Eurasian continent,
00:54:31The place was the southern bottom of the Eurasian continent,
00:54:34and the southern African continent was rising northward.
00:54:45About 70 million years ago,
00:54:48the power of the African continent rising northward
00:54:51and the power of the Eurasian continent opposing it
00:54:54were at stake.
00:55:04For this reason, the limestone coast of the seabed,
00:55:07which would later become St. Victor's Island,
00:55:10was strengthened and the bottom of the sea was flooded.
00:55:13The bottom of the sea was flooded and the bottom of the sea was flooded.
00:55:17In addition, due to the erosion caused by the rain and wind,
00:55:20the clay carried from the hillside to the river
00:55:23was deposited on the seabed.
00:55:27The dinosaurs laid eggs there,
00:55:30which later oxidized the iron and turned red.
00:55:33which later oxidized the iron and turned red.
00:55:39When the dinosaurs laid eggs,
00:55:42St. Victor's Island was not yet built.
00:55:46When the dinosaurs laid eggs,
00:55:49St. Victor's Island was not yet built.
00:55:52There was a first mountain,
00:55:55but it was not yet St. Victor's Island.
00:55:58All the formation of St. Victor's Island took place after the dinosaurs.
00:56:01In order to confirm this, we have to go up the mountain.
00:56:04In order to confirm this, we have to go up the mountain.
00:56:08How did St. Victor's Island become St. Victor's Island?
00:56:11How did St. Victor's Island become St. Victor's Island?
00:56:14How did St. Victor's Island become St. Victor's Island?
00:56:26The wind is strong.
00:56:32The height difference is 650 meters.
00:56:36We continue to climb the 4 km slope.
00:56:39We continue to climb the 4 km slope.
00:56:44Can we go? Continue?
00:56:51I didn't think it would be such a difficult mountain.
00:56:54I didn't think it would be such a difficult mountain.
00:57:04The cross of the province on the destination has become hazy with the clouds.
00:57:07The cross of the province on the destination has become hazy with the clouds.
00:57:25Finally.
00:57:44I can't see anything.
00:57:50What a pity.
00:57:55This is the Cross of the Provence.
00:57:58This is the most famous point in the St. Victor's Island.
00:58:01This is the most famous point in the St. Victor's Island.
00:58:08The Ones River continues to the west and east for a long distance.
00:58:11The Ones River continues to the west and east for a long distance.
00:58:14If we keep going, we will see all of the St. Victor's ridge.
00:58:20We are going to puit Louvier.
00:58:23And all along, it's the same thing.
00:58:25On one side, we have the cliff,
00:58:27and on the other side, a slope
00:58:29covered in vegetation.
00:58:35Let's take a look at the drone footage of a sunny day.
00:58:44It's true that the cut-off ridge
00:58:47continues from west to east.
00:58:54The diagonal lines left behind by the rocks
00:58:59are the boundary between the extreme
00:59:02and the pressed-down vegetation.
00:59:09What kind of geological change
00:59:12struck Saint-Victor?
00:59:17Africa is starting to move towards Europe
00:59:20and it's forming large folds.
00:59:23Here, we're at about 45 million years.
00:59:26It continues to grow,
00:59:28and so the fold is getting stronger.
00:59:31After a while,
00:59:33by force of growth, it will break.
00:59:36Then, we have the growth of the Alps,
00:59:39which will lift up all of Provence.
00:59:43I love you.
00:59:46This is what Mr. Dutour said.
00:59:53About 65 million years ago,
00:59:56between the Italian peninsula
00:59:59and the Eurasian continent,
01:00:01there was the sea.
01:00:04There was a boundary line of plates.
01:00:08Then, the African plate rose to the north.
01:00:14By the force of the plate,
01:00:17the Alps increased in size.
01:00:23Its influence reached
01:00:25the place where Saint-Victor was built.
01:00:31Let's look at the cross-section.
01:00:34The mountain range is a clay layer
01:00:37where dinosaurs laid their eggs.
01:00:42The cross-section is made of
01:00:44the tremendous power of the plate collision.
01:00:47The stone coastline,
01:00:49which was already collapsed,
01:00:51has been twisted even more.
01:00:5645 million years ago,
01:00:58the power of the cross-sectional movement
01:01:01continued even after the collapse of the Alps,
01:01:04and the ground layer was tilted
01:01:06by nearly 90 degrees
01:01:08to make the cross-section.
01:01:12After that, the oak was cut off
01:01:14due to erosion,
01:01:16and the present-day Saint-Victor was built.
01:01:26First, I have to find
01:01:28the foundation of the cross-sectional movement.
01:01:35Cezanne, who put the power
01:01:37that worked on the ground into painting,
01:01:40knew that the sculpture,
01:01:42which had been made over a long time,
01:01:45would change with the change of the sun,
01:01:48and the beauty of thought would appear.
01:01:59Cezanne left these words.
01:02:05Look at that Saint-Victor.
01:02:09What a momentum!
01:02:12What a fierce activity of the sun!
01:02:17And at night,
01:02:19when all that weight comes down,
01:02:23what a melancholy!
01:02:29To be continued
01:02:38The next destination is
01:02:4012 hours by ferry from Marseille,
01:02:44the Gorgia Island.
01:02:53Half the size of Shikoku
01:02:55there is a mountainous landscape.
01:03:03At the end of the 19th century,
01:03:05there is a painter who visited the Gorgia Island
01:03:08and painted 55 paintings in 4 months.
01:03:15He is Henri Matisse,
01:03:17a representative painter of the 20th century.
01:03:21He is called the colorist magician.
01:03:24His work, Jazz,
01:03:26is a masterpiece
01:03:28that pursues pure colors.
01:03:39Matisse, born in Northern France,
01:03:42met the sun of the Mediterranean Sea for the first time
01:03:45and awakened to bold colors.
01:03:48It was the Gorgia Island.
01:03:57What kind of painting did Matisse paint on the Gorgia Island?
01:04:08The painting was kept in a museum on the island.
01:04:19Mmm!
01:04:37The painter came to Corsica on his honeymoon
01:04:41and he stayed in Corsica a few months.
01:04:44He painted several paintings,
01:04:47not big ones,
01:04:49almost this size,
01:04:51and then he came back in France.
01:04:56And here in Corsica,
01:04:58he learned a lot about the light.
01:05:04This is what Matisse said.
01:05:08I learned about the scenery of the Mediterranean Sea
01:05:12in this wonderful place.
01:05:17Everything is shining
01:05:19and overflowing with colors and light.
01:05:27In this painting,
01:05:29Matisse painted the sea of Corsica
01:05:32in blue-green,
01:05:34the grass in dark green,
01:05:36the rocks in red,
01:05:38the sun in yellow,
01:05:40the clouds in red,
01:05:43and the sky in gray,
01:05:45a white gradation.
01:05:49It's a painting like the origin of Matisse,
01:05:52a colorist.
01:05:57I think there are a little more buildings now,
01:06:01but I think you will see almost a part of it,
01:06:06and it will be the same that Matisse has seen.
01:06:13Let's go to the Scudo beach,
01:06:15where this painting was painted.
01:06:22Actually, it may be a little higher,
01:06:26but I can't enter because it's a private property,
01:06:30so let's go to the coastline.
01:06:35There is a cape over there,
01:06:39and it continues all the way to the ocean,
01:06:43so it's around there.
01:06:49Oh!
01:06:50If the sun goes down as it is,
01:06:54there is a sea in front of you,
01:06:56and it's dazzling.
01:07:01Everything is shining
01:07:03and overflowing with colors and light,
01:07:06that's Matisse.
01:07:10The sea of Corsica, Scudo,
01:07:13depicts the unique colors of this island
01:07:16without exception.
01:07:23On the coast,
01:07:25as it is written,
01:07:27the rocks by the sea are reddish.
01:07:33Indeed,
01:07:34Matisse paints the coastline in red.
01:07:38What kind of rock is this red rock?
01:07:46Oh, there is a red rock over there, too.
01:07:50Oh, people are sitting.
01:07:53Let's ask.
01:07:56Good evening!
01:07:59Good evening!
01:08:04Do you know what this red rock is?
01:08:07Yes, these are rocks that you can find everywhere in Corsica,
01:08:11and if you want to see more rocks like this,
01:08:14you have to go to the Gulf of Porto,
01:08:16which is listed as a World Heritage Site.
01:08:19There are landscapes full of red rocks like this.
01:08:22World Heritage Porto?
01:08:28Matisse encountered a variety of colors.
01:08:31Let's see what red is like in Porto.
01:08:45Porto is 80 kilometers north of the coast of Scudo.
01:08:50It takes more than two hours by car.
01:08:58As we approach Porto Bay,
01:09:01the rocks along the road are getting much redder.
01:09:13What does this red rock have to do with the birth of France?
01:09:20What does this red rock have to do with the birth of France?
01:09:27How are you?
01:09:29Hello!
01:09:32Our guide is Frédéric Younon-Hacq,
01:09:35who has lived in Corsica and the Gulf of Porto.
01:09:43Absolutely, it's true.
01:09:45The region is engulfed by red.
01:09:48The rocks are beautiful,
01:09:50especially at this time of day.
01:09:52The color is very vivid and really beautiful.
01:09:58A special red rock?
01:10:07What a vivid red!
01:10:13The world heritage sites in Porto Bay
01:10:17are the sea and land,
01:10:19about 160 square kilometers in total.
01:10:23This Scandola region is one of them.
01:10:26It is only accessible by boat
01:10:29for its natural scenery and ecological protection.
01:10:42The Scandola Region
01:10:52These are the prisms.
01:10:54These are the prisms of Rhyolite.
01:10:56There are a lot of pillars.
01:11:04It's true.
01:11:06How were these red prisms made?
01:11:14These prisms are like hexagonal columns
01:11:19that correspond to the cooling of a stream of volcanic rocks.
01:11:24They are part of a volcanic building
01:11:27that you can see here in Scandola,
01:11:30which is quite old, dating from the Permian period,
01:11:33between 300 and 250 million years ago.
01:11:35So these are really old rocks.
01:11:37There are also many volcanic ash deposits
01:11:41that are more or less compact.
01:11:44And there are also flows,
01:11:46like mud flows,
01:11:48but composed of volcanic ash and debris,
01:11:50called lahars.
01:11:52These are minerals with geoclastic beaches.
01:11:54It's a type of feldspad,
01:11:56so it can be different things.
01:11:58I can't tell you exactly how far it is.
01:12:03What?
01:12:05The red rock is a giant volcano from 300 million years ago?
01:12:10Why did it erupt?
01:12:17There is another red rock that solves this mystery
01:12:21in Porto.
01:12:24The next destination is the village of Girolata,
01:12:28at the base of the Scandola Peninsula.
01:12:38This village is a tourist attraction
01:12:40that goes around the Scandola Peninsula by boat.
01:12:53This area is also red.
01:13:02What is the other red rock
01:13:04that tells the story of the giant volcano
01:13:06from 300 million years ago?
01:13:15In the granite,
01:13:17we will find several types of minerals,
01:13:19essentially three families.
01:13:21We will find quartz grains,
01:13:23which are gray grains.
01:13:25We will find red and pink minerals,
01:13:30which are feldspads.
01:13:32And we will also find dark spots,
01:13:34which are ferromagnetic minerals,
01:13:36like mica.
01:13:41What is the relationship
01:13:43between this rock and the giant volcano
01:13:45from 300 million years ago?
01:13:48This granite is a very old granite,
01:13:51older than the volcanism of Scandola,
01:13:54which we discovered earlier.
01:13:56These granites are dated to about 330 million years.
01:14:00There was only one main continent,
01:14:03which was called the Pangea.
01:14:05The Ercinian granite chain
01:14:07spread over several tectonic plates.
01:14:11The volcanism of Scandola
01:14:15was caused by this type of rock,
01:14:18this type of environment.
01:14:23This is what happens
01:14:25when we summarize the story of the Ercinian granite.
01:14:32Approximately 330 million years ago,
01:14:35the southern continent of Gondwana
01:14:38and the northern continent of South America
01:14:40came close together.
01:14:45The Pangea, the supercontinent,
01:14:47was being formed.
01:14:51Iron ore was mined near the equator,
01:14:54and the plates of the sea
01:14:56sank into the supercontinent.
01:15:01The Corsica Island
01:15:03was on the edge of the supercontinent.
01:15:07Let's take a look at the cross section.
01:15:15When the plates of the sea sank into the supercontinent,
01:15:19the seawater was drawn in,
01:15:21and the melting point of the mantle decreased,
01:15:23causing magma to form.
01:15:27The magma slowly cooled down
01:15:29and solidified deep in the ground,
01:15:31and became limestone.
01:15:36The limestone is lighter than the surrounding rocks,
01:15:39so it begins to rise slowly.
01:15:44Eventually, the plates of the sea became stronger
01:15:47and entered the supercontinent.
01:15:53As a result, more magma was formed.
01:15:59As a result,
01:16:00about 300 million years ago,
01:16:02there was a huge eruption.
01:16:08The lava cooled and solidified,
01:16:10and became limestone.
01:16:15After that, the lava rose to the surface.
01:16:21Together with the iron ore,
01:16:23it became a red land.
01:16:31The red rocks on the coast drawn by Matisse
01:16:38were left behind by the Corsica Island.
01:16:41The Corsica Island was the birthplace of the Earth,
01:16:45which began more than 300 million years ago.
01:16:5680% of the Corsica Island is made up of granite,
01:16:59but about 20% of the Corsica Island
01:17:01is made up of very original rocks,
01:17:03which are complementary to the color red.
01:17:06It's the color green,
01:17:08the metamorphic rocks, like schist,
01:17:10that can be seen in the north and east parts of Corsica.
01:17:15Green rocks!
01:17:21In addition to the red rocks,
01:17:23the green rocks make up 20% of the island.
01:17:28What a colorful island!
01:17:32The goal is the Dugnell Cape,
01:17:34which is at the top of the northeastern part of the island.
01:17:44To reach the Dugnell Cape,
01:17:46you have to walk along the coast for more than 30 minutes.
01:17:51The Dugnell Cape
01:17:58I've walked about 2 km,
01:18:01and I'm tired.
01:18:11Here we are.
01:18:13This is our destination,
01:18:15the Dugnell Cape.
01:18:18It's green!
01:18:26Wow!
01:18:28It's beautiful!
01:18:32The blue sea of the Mediterranean Sea
01:18:34is full of green rocks.
01:18:38The stone tower was built by the Republic of Genoa,
01:18:42who once ruled the island of Corsica,
01:18:45at the end of the 16th century.
01:19:08How did they come up with these green rocks?
01:19:20The original rock was a basalt.
01:19:24But this basalt was metamorphosed
01:19:27in conditions of pressure and temperature
01:19:30so that the minerals of the basalt were reorganized
01:19:34into lighter colors, greener colors,
01:19:37and darker colors.
01:19:43The rock was transformed into a green rock
01:19:46when the magma solidified.
01:19:51When and how was it transformed?
01:19:57The basalts that we see here,
01:19:59which were transformed,
01:20:01were found at the bottom of an ocean,
01:20:04the Alpine Ocean,
01:20:06the Tethys.
01:20:08This deformation,
01:20:10the disappearance of the Tethys
01:20:12due to a tectonic push
01:20:14coming from the south,
01:20:16from the South-East,
01:20:18the African region,
01:20:20or the current Mediterranean-Eastern region,
01:20:23is due to this tectonic constraint
01:20:25of the disappearance of the Alpine Sea
01:20:28in the mountains.
01:20:30And Corsica had to adapt
01:20:32to this alpine deformation.
01:20:34And for this,
01:20:36these rocks collapsed
01:20:38on the Ercinian Granitic Massif.
01:20:40And it was this pressure
01:20:42and these particular tectonic conditions
01:20:45that allowed for this type of deformation.
01:20:51Let's listen to the explanation
01:20:53by Mr. Yuno Haku.
01:20:59200 million years ago,
01:21:01the supercontinent Pangaea
01:21:03was divided into the northern Laurasia
01:21:05and the southern Gondwana.
01:21:09The island of Corsica
01:21:11was on the Laurasian side.
01:21:15The continent was further divided.
01:21:19Approximately 70 million years ago,
01:21:21during the process of moving
01:21:23to the current continent,
01:21:26the island of Corsica
01:21:28was on the edge of the Eurasian continent.
01:21:32Let's take a closer look.
01:21:38The island of Corsica
01:21:40was separated from the Eurasian continent
01:21:42by the Alps,
01:21:44and later by the Italian Peninsula.
01:21:50At the bottom of the Alps,
01:21:52there was a plate boundary
01:21:54between Africa and Eurasia.
01:21:58Let's take a look at the cross section at the time.
01:22:04At the edge of the Eurasian continent
01:22:06was the island of Corsica.
01:22:10It was pushed by the African plate
01:22:12to the north,
01:22:14and approximately 40 million years ago,
01:22:16the tip of the Eurasian plate
01:22:18that had sunk
01:22:20collapsed.
01:22:25Then, magma rose from the boundary.
01:22:29The lava cooled and solidified,
01:22:31and it became the Aegean Sea.
01:22:36After that,
01:22:37the north of the African plate continued,
01:22:40and the Aegean Sea collided with the island of Corsica.
01:22:45Due to the pressure and heat at that time,
01:22:48magma formed
01:22:50and turned green.
01:23:01The green of the island of Corsica
01:23:06was hidden by the tremendous power
01:23:08of the two plates
01:23:10attacking each other.
01:23:19The light and color of the island of Corsica
01:23:22gave a shock to the colored magician Mathis.
01:23:27Finally, let's approach the origin of white.
01:23:34Actually, the white rock
01:23:36has something to do with the magnetic field
01:23:39that made the island of Corsica
01:23:41an island floating in the Mediterranean Sea.
01:23:44Let's go to St. Florent,
01:23:46the port town at the base of the island of Corsica.
01:23:56When we go to the seaside,
01:24:01So, here we are on the white rocks.
01:24:03Oh, it's true.
01:24:06So, here we are on the white rocks.
01:24:08Oh, it's true.
01:24:15Oh, the white rocks are
01:24:17rising up to the surface of the sea.
01:24:25So, we are on limestone rocks,
01:24:28carbonated rocks.
01:24:30Limestone rocks.
01:24:33For example, we can see
01:24:35the debris of the seashells here.
01:24:37It's a marine environment
01:24:39at the level of a fairly warm sea,
01:24:41a tropical sea.
01:24:46The white limestone rocks.
01:24:49How are they related to the birth of the island of Corsica?
01:24:54A deformation of the earth's crust
01:24:56that slowly caused the migration of this block,
01:25:00Corsica, Sardinia and northern Algeria,
01:25:03to position itself much further south.
01:25:06So, during this migration,
01:25:08this movement,
01:25:10there were places in Corsica
01:25:12that found themselves a little low,
01:25:15that sank
01:25:17and were invaded by the sea.
01:25:21Separation from the south of France?
01:25:24What does this mean?
01:25:30The tremendous power of the Alps Migration Movement
01:25:33reached southern France as well.
01:25:39Approximately 30 million years ago,
01:25:41this area was stretched out.
01:25:44For this reason,
01:25:46the islands of Corsica and Sardinia
01:25:48that followed
01:25:50split up and began to migrate.
01:25:55During the migration,
01:25:57a part of it sank
01:25:59and the limestone rocks
01:26:01settled on the shallow seabed.
01:26:04Approximately 15 million years ago,
01:26:06the current population
01:26:08of the island of Corsica
01:26:10and Sardinia
01:26:12reached their current position.
01:26:17They appeared on the surface
01:26:19as a white land.
01:26:3230 million years ago,
01:26:34the island of Corsica
01:26:36and Sardinia
01:26:38split up
01:26:40and became a white island.
01:26:47Over 300 million years ago,
01:26:49the island of Corsica
01:26:51became red
01:26:53and 40 million years ago,
01:26:55the island of Sardinia
01:26:57became green.
01:27:01The natural colors of the landscape
01:27:03reminded us of the talent
01:27:05of the color magician
01:27:07Mathis.
01:27:11In the 19th century,
01:27:13the genius painters
01:27:15were fascinated
01:27:17by the landscapes
01:27:19of France.
01:27:26He was able to see
01:27:28different colors of rocks,
01:27:30even if he was not a geologist,
01:27:32that perhaps people today,
01:27:34who are always in a hurry,
01:27:36do not have the opportunity
01:27:38to see.
01:27:42And in geology,
01:27:44we have this ability
01:27:46to travel in time
01:27:48and space-time.
01:27:50Because here,
01:27:52we are at the bottom
01:27:54of an ocean
01:27:56under a tropical climate.
01:27:58When we were in the middle
01:28:00of the dinosaurs,
01:28:02we were in a river.
01:28:04The age and power of the earth
01:28:06were hidden in the sea.
01:28:13In order to express this,
01:28:15the artists continued
01:28:17to fight.
01:28:35The struggle for a more
01:28:37vivid picture
01:28:39has been a state of the art
01:28:41for the last few years.
01:28:43At the end of the pandemic,
01:28:45people were forced
01:28:47to choose whether
01:28:49to live to 40,000 or 50,000.
01:28:59Over 59,000 were killed
01:29:02It's been two years since the Turkish-Syrian earthquake.
01:29:05We're approaching the site of the disaster.
01:29:07This is the International News at 10 p.m.
01:29:13Last Family, discovered on the island!
01:29:16A fisherman is stranded on the island?
01:29:19And then...
01:29:20About 40% of the blood flow goes to the island of surprise!
01:29:23Friday, February 7th, at 6 p.m.
01:29:26Huh?
01:29:29The goal is to run 1,000 km on a bicycle!
01:29:35NHK BS, Friday, February 7th, at 11.30 p.m.
01:29:39It's beautiful!
01:29:43The 10-episode journey of Japan!
01:29:45The journey of spring goes from Miyazaki to Iwate!
01:29:48We're looking for letters from Miyazaki!
01:29:51We're looking forward to seeing the scenery of your precious hearts!
01:29:54The deadline is February 17th!