4K 東京 江東区佐賀をアルク (朝) a-Walk in Tokyo Koto-ku Saga (AM)
10/ 9/2019 5:10 AM
東京都江東区佐賀1丁目。
Saga 1-chome(Tokyo Koto-ku).
4K.60p. dji osmo poket.
＊ご視聴頂きありがとうございます。
気まぐれなお散歩動画チャンネルです。
宜しければチャンネル登録をよろしくお願い致します。
＊Thank you for watching.
A whimsical Walk video channel.
Please Subscribe to the channel if you like.
#Saga#TokyoWalk#JapanWalk#東京散歩
a-Walk in Tokyo Monzennakachou(Koto-ku)門前仲町(江東区) #35 BGM入
江東区門前仲町をアルク。
Monzennajachou(Koto-ku).
7/30/2019. 5:55 a.m.
HD.30p. dji osmo poket.
＊気まぐれなお散歩動画チャンネルです。
毎日投稿しておりますので、良かったらチャンネル登録をよろしくお願いします。
＊a-Walk in video.
Im posting videos every day now.
So If you like. please Subscribe.
#Monzennakachou#Koto-ku#Japan
a-Walk in Tokyo Shiba-Park(Minato-ku)港区(東麻布.芝公園)#26 BGMあり
港区芝公園周辺をアルク。
Around Shiba-Park(Minato-ku).
7/23/2019. 9:30am.
気まぐれなお散歩動画です。
a-Walk in video.
HD.30p. dji osmo poket.
#Tokyo#Japan#Minato-ku
東京 根津(文京区) am.4K.a-Walk in Tokyo Nezu(Bunkyo-ku) No.65
※(動画内カタカナ表記✖️ズ○ヅの誤りがある事を、お詫び申し上げます)。
9.10.2019. 5:30 am. No.65
文京区根津1-2-丁目をアルク。
Nezu 1-2-chome(Bunkyo-ku).
4k.60p. dji osmo poket.
＊気まぐれなお散歩動画チャンネルです。
毎日投稿しておりますので、良かったらチャンネル登録をよろしくお願いします。
＊ a-Walk in video.
Im posting videos every day now.
So If you like. please Subscribe.
#TokyoWalk#JapanWalk#Nezu#東京散歩
JAPANTRIPGUIDE「五反田ゆうらく通りを歩く Gotanda Street」Shinagawa-ku, Tokyo 2015．4．6
Gotanda (五反田) is a busy neighbourhood in the Shinagawa ward of Tokyo, Japan. The name Gotanda can be literally translated as a (rice) paddy of half-hectare's size. The district straddles the Meguro river, and is located between the Meguro and Ōsaki stations on the JR Yamanote Line.
東京 西葛西(江戸川区) am.[4k] a-Walk in Tokyo Nishikasai(Edogawa-ku) No.19
8.13.2019. 5:40am.
江戸川区 (西葛西6丁目駅周辺)をアルク。
Edogawa-ku Nishikasai 6-chome.
4k.60p. dji osmo poket.
＊気まぐれなお散歩動画チャンネルです。
毎日投稿しておりますので、良かったらチャンネル登録をよろしくお願いします。
＊a-Walk in video.
Im posting videos every day now.
So If you like. please Subscribe.
#Nishikasai#TokyoWalk#Edogawa#WalkJapan#東京散歩
東京 中野(中野区) am.[4k] a-Walk in Tokyo Nakano Alley(Nakano-ku) No.33
中野区中野3丁目裏路地をアルク。
(レンガ坂)
(桃園通り)
(桃園川緑道)
8.21.2019. 6:00am.
Nakano-ku Nakano3-chome Alley.
Renga zaka.
Momozono dori.
Momozonogawa endo.
4k.60p. dji osmo poket.
＊気まぐれなお散歩動画チャンネルです。
毎日投稿しておりますので、良かったらチャンネル登録をよろしくお願いします。
＊a-Walk in video.
Im posting videos every day now.
So If you like.please Subscribe.
#Nakano#TokyoWalk#WalkJapan#東京散歩
a-Walk in Tokyo Ginza-2(5-6-7-chome)銀座をアルク#4
a-Walk in video
気まぐれなお散歩動画です。
#Japan#Ginza#銀座
5-6-7-chome. 6:30am.
7/8/2019. 6:30am. osmo A撮
a-Walk in Tokyo Akihabara(Taito-ku)秋葉原(台東区) #34 BGM入
台東区秋葉原をアルク。
Akihabara(Taito-ku).
7/29/2019. 5:55 p.m.
HD.30p. dji osmo poket.
＊気まぐれなお散歩動画チャンネルです。
毎日投稿しておりますので、良かったらチャンネル登録をよろしくお願いします。
＊a-Walk in video.
Im posting videos every day now.
So If you like. please Subscribe.
#Akihabara#Tokyo#Japan
東京 北千住(足立区) am.[4k] a-Walk in Tokyo Kita-Senju Alley(Adachi-ku) No.39
足立区北千住 千住2丁目裏路地をアルク。
Kita-Senju 2-chome Alley.
8.24.2019. 6:00am.
4k.60p. dji osmo poket.
＊気まぐれなお散歩動画チャンネルです。
毎日投稿しておりますので、良かったらチャンネル登録をお願いします。
＊a-Walk in video.
Im posting videos every day now.
So If you like. please Subscribe.
#Kitasenju#TokyoWalk#WalkJapan#東京散歩
a-Walk in Tokyo Akihabara-2秋葉原#9
秋葉原をアルク。
Akihabara.
7/13/2019. 7:00am.
HD.30p. dji osmo poket.
＊気まぐれなお散歩動画チャンネルです。
毎日投稿しておりますので、良かったらチャンネル登録をよろしくお願いします。
＊a-Walk in video.
Im posting videos every day now.
So If you like. please Subscribe.
#Akihabara#Japan#Akiba
[ENG sub] Haruto's First Love // Hana Nochi Hare ❀
Song: Hatsukoi by Utada Hikaru
I do not own any of the raw sources
All translations, editing, encoding by me
----
twi: kerrrrupuk
lj: kerupukk
TOKYO,TOKYO,TOKYO !（215）：Mejiro-dai〜Hyakunin-cho 〜目白台から高田馬場、百人町まで歩きました！
世界有数のメガポリス「東京」をイメージ動画で紹介。撮影動画本数2020本を目指しプロジェクト進行中。
URL ahead of “ TOKYO,TOKYO,TOKYO ! ”
youtube.com/NobuSynchroLab
2011 Tōhoku earthquake and tsunami
The 2011 earthquake off the Pacific coast of Tōhoku (東北地方太平洋沖地震, Tōhoku-chihō Taiheiyō Oki Jishin) was a magnitude 9.0 (Mw) undersea megathrust earthquake off the coast of Japan that occurred at 14:46 JST (05:46 UTC) on Friday 11 March 2011, with the epicentre approximately 70 kilometres (43 mi) east of the Oshika Peninsula of Tōhoku and the hypocenter at an underwater depth of approximately 30 km (19 mi). The earthquake is also often referred to in Japan as the Great East Japan Earthquake (東日本大震災, Higashi nihon daishinsai) and also known as the 2011 Tohoku earthquake, and the 3.11 Earthquake. It was the most powerful earthquake ever recorded to have hit Japan, and the fifth most powerful earthquake in the world since modern record-keeping began in 1900. The earthquake triggered powerful tsunami waves that reached heights of up to 40.5 metres (133 ft) in Miyako in Tōhoku's Iwate Prefecture, and which, in the Sendai area, travelled up to 10 km (6 mi) inland. The earthquake moved Honshu (the main island of Japan) 2.4 m (8 ft) east and shifted the Earth on its axis by estimates of between 10 cm (4 in) and 25 cm (10 in), and generated sound waves detected by the low orbiting GOCE satellite.
On 10 February 2014, a Japanese National Police Agency report confirmed 15,887 deaths, 6,150 injured, and 2,612 people missing across twenty prefectures, as well as 127,290 buildings totally collapsed, with a further 272,788 buildings 'half collapsed', and another 747,989 buildings partially damaged. The earthquake and tsunami also caused extensive and severe structural damage in north-eastern Japan, including heavy damage to roads and railways as well as fires in many areas, and a dam collapse. Japanese Prime Minister Naoto Kan said, In the 65 years after the end of World War II, this is the toughest and the most difficult crisis for Japan. Around 4.4 million households in northeastern Japan were left without electricity and 1.5 million without water.
This video is targeted to blind users.
Attribution:
Article text available under CC-BY-SA
Creative Commons image source in video
2011 Japan earthquake | Wikipedia audio article
This is an audio version of the Wikipedia Article:
00:05:12 1 Earthquake
00:07:49 1.1 Geology
00:12:28 1.2 Energy
00:13:47 1.3 Geophysical effects
00:18:13 1.4 Aftershocks
00:20:40 1.5 Earthquake Warning System
00:22:30 2 Tsunami
00:23:48 2.1 Japan
00:37:20 2.2 Elsewhere across the Pacific
00:42:26 3 Land subsidence
00:44:18 4 Casualties
00:44:27 4.1 Japan
00:50:17 4.2 Overseas
00:50:59 5 Damage and effects
00:53:11 5.1 Ports
00:54:33 5.2 Dams and water problems
00:55:45 5.3 Electricity
01:00:40 5.4 Oil, gas and coal
01:02:17 5.5 Nuclear power plants
01:05:52 5.5.1 Fukushima meltdowns
01:07:44 5.5.2 Incidents elsewhere
01:09:14 5.6 Wind power
01:09:39 5.7 Transport
01:14:09 5.8 Telecommunications
01:15:21 5.9 Defense
01:15:58 5.10 Space center
01:16:35 5.11 Cultural properties
01:18:02 6 Aftermath
01:20:11 7 Humanitarian response
01:20:40 8 Media coverage
01:23:39 9 Scientific and research response
01:28:17 10 See also
Listening is a more natural way of learning, when compared to reading. Written language only began at around 3200 BC, but spoken language has existed long ago.
Learning by listening is a great way to:
- increases imagination and understanding
- improves your listening skills
- improves your own spoken accent
- learn while on the move
- reduce eye strain
Now learn the vast amount of general knowledge available on Wikipedia through audio (audio article). You could even learn subconsciously by playing the audio while you are sleeping! If you are planning to listen a lot, you could try using a bone conduction headphone, or a standard speaker instead of an earphone.
Listen on Google Assistant through Extra Audio:
Other Wikipedia audio articles at:
Upload your own Wikipedia articles through:
Speaking Rate: 0.8806638741601678
Voice name: en-US-Wavenet-D
I cannot teach anybody anything, I can only make them think.
- Socrates
SUMMARY
=======
The 2011 earthquake off the Pacific coast of Tōhoku (東北地方太平洋沖地震, Tōhoku-chihō Taiheiyō Oki Jishin) was a magnitude 9.0–9.1 (Mw) undersea megathrust earthquake off the coast of Japan that occurred at 14:46 JST (05:46 UTC) on Friday 11 March 2011, with the epicentre approximately 70 kilometres (43 mi) east of the Oshika Peninsula of Tōhoku and the hypocenter at an underwater depth of approximately 29 km (18 mi).
The earthquake is often referred to in Japan as the Great East Japan Earthquake (東日本大震災, Higashi nihon daishinsai) and is also known as the 2011 Tōhoku earthquake, the Great Sendai Earthquake, the Great Tōhoku Earthquake, and the 3.11 earthquake.
It was the most powerful earthquake ever recorded in Japan, and the fourth most powerful earthquake in the world since modern record-keeping began in 1900.
The earthquake triggered powerful tsunami waves that may have reached heights of up to 40.5 metres (133 ft) in Miyako in Tōhoku's Iwate Prefecture, and which, in the Sendai area, traveled at 435 mph for up to 10 km (6 mi) inland. Residents of Sendai had only eight to ten minutes warning, and more than 19,000 were killed, many at the more than a hundred evacuation sites that washed away.The earthquake moved Honshu (the main island of Japan) 2.4 m (8 ft) east, shifted the Earth on its axis by estimates of between 10 cm (4 in) and 25 cm (10 in), increased earth's rotational speed by 1.8 µs per day, and generated infrasound waves detected in perturbations of the low-orbiting GOCE satellite.
Initially, the earthquake caused sinking of part of Honshu's Pacific coast by up to roughly a metre, but after about three years, the coast rose back and kept on rising to exceed its original height.The tsunami swept the Japanese mainland and killed over ten thousand people, mainly through drowning, though blunt trauma also caused many deaths. The latest report from the Japanese National Police Agency report confirms 15,897 deaths, 6,157 injured, and 2,533 people missing across twenty prefectures, and a report from 2015 indicated 228,863 people were still living away from their home in either temporary housing or due to permanent relocation.A report by the National Police Agency of Japan on 10 September 2018 listed 121,778 buildings as total collapsed, with a further 280,926 buildings half collapsed, and another 699,180 buildings partially damaged. The earthquake and tsunami also caused extensive and severe structural damage in north-eastern Japan, including heavy damage to roads and railways as well as fires in many areas, and a dam collapse. Japanese Prime Minister Naoto Kan said, In the 65 years after the end of World War II, this is the toughest and the most difficult crisis for Japan. Around 4.4 million households in northeastern Japan were left ...
FC東京 チャント まとめ 20190310 【FC東京×サガン鳥栖】FC Tokyo football chants
【You'll never walk alone】
When you walk through a storm Hold your head up high
And don't be afraid of the dark At the end of a storm
There's a golden sky
And the sweet silver song of a lark
Walk on through the wind
Walk on through the rain
Though your dreams be tossed and blown
Walk on, walk on
with hope in your heart
And you'll never walk alone
you'll never walk alone
【東京こそすべて】
東京こそすべて 俺らを熱くする
情熱をぶつけろ 優勝を掴みとれ
バモ東京 バモ東京 バモ東京 バモ東京
バモ東京 バモ東京 バモ東京 バモ東京
【勝利を目指して】
それ行け 俺たちの東京
勝利を目指して ゴールを狙え
【負けるわけはないさ】
戦え俺の東京 今日も勝利を信じて
弾けよう｢飛田給｣ 負ける訳はないさ
【バモス東京】
バモス東京 バモス東京
バモバモス東京 バモバモス東京
【みんなで唄おう】
オー 俺の東京 誇りを持ち
立ち上がってみんなで歌おう
ララララララララララララ
【君の瞳に恋してる】
愛してる東京 ララララララ
愛してる東京 ララララララ
愛してる東京 ラララ ララ ララ
【ルパン東京】
男には自分の世界がある
例えるなら空を翔ける ひとすじの流れ星
東京ガス
【勝つのは俺たちだ】
青赤フラッグ掲げて
集まれ12飛田給
何色来たって
関係ねえ
勝つのは俺たちだー
VAMOS TOKYO！
GET KICK！THE GOAL！
勝つのは俺たちだー
【この気持ち とまらない】
この気持ち とまらない
俺たちは とまれない
さあみんな 立ち上がれ
荒れ狂え 飛び跳ねろ
東京 東京 東京 東京
東京 東京 東京 東京
【眠らない街】
東京 東京 眠らない町
青と赤の 俺らの誇り オオ
FC Tokyo 2 - 0 Sagan Tosu
89' [1-0] Hiromu Mitsumaru (own goal, auto-golo)
90' [2-0] Jael
FC Tokyo (FC東京) is a Japanese association football club playing in J1 League. Its hometown is Tokyo prefecture. The team is one of only four in the J. League to be simply called Football Club without an extended name.
FC Tokyo uses Ajinomoto Stadium as its home ground (the official name of this stadium is Tokyo Stadium). For a long time it did not have a home stadium of its own and played at various football fields such as the National Yoyogi Stadium, the National Nishigaoka Football Field, Edogawa Special Ward Stadium, and the Komazawa Olympic Park Stadium, but in 2001 it finally found a permanent home. Club's training grounds are Sarue Ground in Koto, Tokyo and Kodaira Ground in Kodaira, Tokyo.
FC Tokyo:Akihito Hayashi33,Diego Oliveira9,Kento Hashimoto18,
Ryoya Ogawa25,Msato Morishige3,Jang Hyun-Soo20,Takefusa Kubo15
Sei Muroya2,Keigo Higashi10,Kensuke Nagai11,Yojiro Takahagi8
#FC東京 #チャント #FCTokyo #Tokyo
2011 Tōhoku earthquake and tsunami | Wikipedia audio article
This is an audio version of the Wikipedia Article:
00:04:42 1 Earthquake
00:07:11 1.1 Geology
00:11:35 1.2 Energy
00:12:51 1.3 Geophysical effects
00:17:03 1.4 Aftershocks
00:19:21 1.5 Earthquake Warning System
00:21:06 2 Tsunami
00:22:20 2.1 Japan
00:35:28 2.2 Elsewhere across the Pacific
00:40:11 3 Land subsidence
00:41:59 4 Casualties
00:42:08 4.1 Japan
00:47:41 4.2 Overseas
00:48:21 5 Damage and effects
00:50:26 5.1 Ports
00:51:44 5.2 Dams and water problems
00:52:52 5.3 Electricity
00:57:32 5.4 Oil, gas and coal
00:59:04 5.5 Nuclear power plants
01:02:36 5.5.1 Fukushima meltdowns
01:04:23 5.5.2 Incidents elsewhere
01:05:49 5.6 Wind power
01:06:13 5.7 Transport
01:10:31 5.8 Telecommunications
01:11:39 5.9 Defense
01:12:13 5.10 Space center
01:12:50 5.11 Cultural properties
01:14:12 6 Aftermath
01:16:14 7 Humanitarian response
01:16:42 8 Media coverage
01:19:32 9 Scientific and research response
01:24:03 10 See also
Listening is a more natural way of learning, when compared to reading. Written language only began at around 3200 BC, but spoken language has existed long ago.
Learning by listening is a great way to:
- increases imagination and understanding
- improves your listening skills
- improves your own spoken accent
- learn while on the move
- reduce eye strain
Now learn the vast amount of general knowledge available on Wikipedia through audio (audio article). You could even learn subconsciously by playing the audio while you are sleeping! If you are planning to listen a lot, you could try using a bone conduction headphone, or a standard speaker instead of an earphone.
Listen on Google Assistant through Extra Audio:
Other Wikipedia audio articles at:
Upload your own Wikipedia articles through:
Speaking Rate: 0.9554487759653858
Voice name: en-US-Wavenet-C
I cannot teach anybody anything, I can only make them think.
- Socrates
SUMMARY
=======
The 2011 earthquake off the Pacific coast of Tōhoku (東北地方太平洋沖地震, Tōhoku-chihō Taiheiyō Oki Jishin) was a magnitude 9.0–9.1 (Mw) undersea megathrust earthquake off the coast of Japan that occurred at 14:46 JST (05:46 UTC) on Friday 11 March 2011, with the epicentre approximately 70 kilometres (43 mi) east of the Oshika Peninsula of Tōhoku and the hypocenter at an underwater depth of approximately 29 km (18 mi).
The earthquake is often referred to in Japan as the Great East Japan Earthquake (東日本大震災, Higashi nihon daishinsai) and is also known as the 2011 Tōhoku earthquake, the Great Sendai Earthquake, the Great Tōhoku Earthquake, and the 3.11 earthquake.
It was the most powerful earthquake ever recorded in Japan, and the fourth most powerful earthquake in the world since modern record-keeping began in 1900.
The earthquake triggered powerful tsunami waves that may have reached heights of up to 40.5 metres (133 ft) in Miyako in Tōhoku's Iwate Prefecture, and which, in the Sendai area, traveled up to 10 km (6 mi) inland.The earthquake moved Honshu (the main island of Japan) 2.4 m (8 ft) east, shifted the Earth on its axis by estimates of between 10 cm (4 in) and 25 cm (10 in), increased earth's rotational speed by 1.8 µs per day, and generated infrasound waves detected in perturbations of the low-orbiting GOCE satellite.
Initially, the earthquake caused sinking of part of Honshu's Pacific coast by up to roughly a metre, but after about three years, the coast rose back and kept on rising to exceed its original height.The tsunami swept the Japanese mainland and killed over ten thousand people, mainly through drowning, though blunt trauma also caused many deaths. The latest report from the Japanese National Police Agency report confirms 15,897 deaths, 6,157 injured, and 2,533 people missing across twenty prefectures, and a report from 2015 indicated 228,863 people were still living away from their home in either temporary housing or due to permanent relocation.A report by the National Police Agency of Japan on 10 September 2018 listed 121,778 buildings as total collapsed, with a further 280,926 buildings half collapsed, and another 699,180 buildings partially damaged. The earthquake and tsunami also caused extensive and severe structural damage in north-eastern Japan, including heavy damage to roads and railways as well as fires in many areas, and a dam collapse. Japanese Prime Minister Naoto Kan said, In the 65 years after the end of World War II, this is the toughest and the most difficult crisis for Japan. Around 4.4 million households in northeastern Japan were left without electricity and 1.5 million without water.The tsunami caused nuclear accidents, primarily the level 7 meltdowns at three reactors in the Fukushima Daiichi Nuclear Pow ...
2011 Tōhoku earthquake | Wikipedia audio article
This is an audio version of the Wikipedia Article:
00:06:39 1 Earthquake
00:09:55 1.1 Geology
00:15:54 1.2 Energy
00:17:35 1.3 Geophysical effects
00:23:20 1.4 Aftershocks
00:26:23 1.5 Earthquake Warning System
00:28:44 2 Tsunami
00:30:24 2.1 Japan
00:48:06 2.2 Elsewhere across the Pacific
00:54:35 3 Land subsidence
00:56:56 4 Casualties
00:57:06 4.1 Japan
01:04:41 4.2 Overseas
01:05:35 5 Damage and effects
01:08:25 5.1 Ports
01:10:09 5.2 Dams and water problems
01:11:41 5.3 Electricity
01:18:00 5.4 Oil, gas and coal
01:20:04 5.5 Nuclear power plants
01:24:39 5.5.1 Fukushima meltdowns
01:27:03 5.5.2 Incidents elsewhere
01:28:58 5.6 Wind power
01:29:28 5.7 Transport
01:35:20 5.8 Telecommunications
01:36:54 5.9 Defense
01:37:39 5.10 Space center
01:38:27 5.11 Cultural properties
01:40:16 6 Aftermath
01:43:00 7 Humanitarian response
01:43:34 8 Media coverage
01:47:23 9 Scientific and research response
01:53:22 10 See also
Listening is a more natural way of learning, when compared to reading. Written language only began at around 3200 BC, but spoken language has existed long ago.
Learning by listening is a great way to:
- increases imagination and understanding
- improves your listening skills
- improves your own spoken accent
- learn while on the move
- reduce eye strain
Now learn the vast amount of general knowledge available on Wikipedia through audio (audio article). You could even learn subconsciously by playing the audio while you are sleeping! If you are planning to listen a lot, you could try using a bone conduction headphone, or a standard speaker instead of an earphone.
Listen on Google Assistant through Extra Audio:
Other Wikipedia audio articles at:
Upload your own Wikipedia articles through:
Speaking Rate: 0.7056265830443723
Voice name: en-GB-Wavenet-D
I cannot teach anybody anything, I can only make them think.
- Socrates
SUMMARY
=======
The 2011 earthquake off the Pacific coast of Tōhoku (東北地方太平洋沖地震, Tōhoku-chihō Taiheiyō Oki Jishin) was a magnitude 9.0–9.1 (Mw) undersea megathrust earthquake off the coast of Japan that occurred at 14:46 JST (05:46 UTC) on Friday 11 March 2011, with the epicentre approximately 70 kilometres (43 mi) east of the Oshika Peninsula of Tōhoku and the hypocenter at an underwater depth of approximately 29 km (18 mi).
The earthquake is often referred to in Japan as the Great East Japan Earthquake (東日本大震災, Higashi nihon daishinsai) and is also known as the 2011 Tōhoku earthquake, the Great Sendai Earthquake, the Great Tōhoku Earthquake, and the 3.11 earthquake.
It was the most powerful earthquake ever recorded in Japan, and the fourth most powerful earthquake in the world since modern record-keeping began in 1900.
The earthquake triggered powerful tsunami waves that may have reached heights of up to 40.5 metres (133 ft) in Miyako in Tōhoku's Iwate Prefecture, and which, in the Sendai area, traveled at 435 mph for up to 10 km (6 mi) inland. Residents of Sendai had only eight to ten minutes warning, and more than 19,000 were killed, many at the more than a hundred evacuation sites that washed away.The earthquake moved Honshu (the main island of Japan) 2.4 m (8 ft) east, shifted the Earth on its axis by estimates of between 10 cm (4 in) and 25 cm (10 in), increased earth's rotational speed by 1.8 µs per day, and generated infrasound waves detected in perturbations of the low-orbiting GOCE satellite.
Initially, the earthquake caused sinking of part of Honshu's Pacific coast by up to roughly a metre, but after about three years, the coast rose back and kept on rising to exceed its original height.The tsunami swept the Japanese mainland and killed over ten thousand people, mainly through drowning, though blunt trauma also caused many deaths. The latest report from the Japanese National Police Agency report confirms 15,897 deaths, 6,157 injured, and 2,533 people missing across twenty prefectures, and a report from 2015 indicated 228,863 people were still living away from their home in either temporary housing or due to permanent relocation.A report by the National Police Agency of Japan on 10 September 2018 listed 121,778 buildings as total collapsed, with a further 280,926 buildings half collapsed, and another 699,180 buildings partially damaged. The earthquake and tsunami also caused extensive and severe structural damage in north-eastern Japan, including heavy damage to roads and railways as well as fires in many areas, and a dam collapse. Japanese Prime Minister Naoto Kan said, In the 65 years after the end of World War II, this is the toughest and the most difficult crisis for Japan. Around 4.4 million households in northeastern Japan were left ...
Tohoku earthquake | Wikipedia audio article
This is an audio version of the Wikipedia Article:
00:06:13 1 Earthquake
00:09:21 1.1 Geology
00:14:50 1.2 Energy
00:16:24 1.3 Geophysical effects
00:21:38 1.4 Aftershocks
00:24:34 1.5 Earthquake Warning System
00:26:46 2 Tsunami
00:28:17 2.1 Japan
00:44:32 2.2 Elsewhere across the Pacific
00:50:27 3 Land subsidence
00:52:42 4 Casualties
00:52:51 4.1 Japan
00:59:44 4.2 Overseas
01:00:33 5 Damage and effects
01:03:11 5.1 Ports
01:04:48 5.2 Dams and water problems
01:06:13 5.3 Electricity
01:12:06 5.4 Oil, gas and coal
01:14:02 5.5 Nuclear power plants
01:18:21 5.5.1 Fukushima meltdowns
01:20:35 5.5.2 Incidents elsewhere
01:22:20 5.6 Wind power
01:22:48 5.7 Transport
01:28:10 5.8 Telecommunications
01:29:35 5.9 Defense
01:30:17 5.10 Space center
01:31:00 5.11 Cultural properties
01:32:42 6 Aftermath
01:35:16 7 Humanitarian response
01:35:48 8 Media coverage
01:39:22 9 Scientific and research response
01:44:57 10 See also
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Speaking Rate: 0.7529985707519036
Voice name: en-US-Wavenet-E
I cannot teach anybody anything, I can only make them think.
- Socrates
SUMMARY
=======
The 2011 earthquake off the Pacific coast of Tōhoku (東北地方太平洋沖地震, Tōhoku-chihō Taiheiyō Oki Jishin) was a magnitude 9.0–9.1 (Mw) undersea megathrust earthquake off the coast of Japan that occurred at 14:46 JST (05:46 UTC) on Friday 11 March 2011, with the epicentre approximately 70 kilometres (43 mi) east of the Oshika Peninsula of Tōhoku and the hypocenter at an underwater depth of approximately 29 km (18 mi).
The earthquake is often referred to in Japan as the Great East Japan Earthquake (東日本大震災, Higashi nihon daishinsai) and is also known as the 2011 Tōhoku earthquake, the Great Sendai Earthquake, the Great Tōhoku Earthquake, and the 3.11 earthquake.
It was the most powerful earthquake ever recorded in Japan, and the fourth most powerful earthquake in the world since modern record-keeping began in 1900.
The earthquake triggered powerful tsunami waves that may have reached heights of up to 40.5 metres (133 ft) in Miyako in Tōhoku's Iwate Prefecture, and which, in the Sendai area, traveled at 435 mph for up to 10 km (6 mi) inland. Residents of Sendai had only eight to ten minutes warning, and more than 19,000 were killed, many at the more than a hundred evacuation sites that washed away.The earthquake moved Honshu (the main island of Japan) 2.4 m (8 ft) east, shifted the Earth on its axis by estimates of between 10 cm (4 in) and 25 cm (10 in), increased earth's rotational speed by 1.8 µs per day, and generated infrasound waves detected in perturbations of the low-orbiting GOCE satellite.
Initially, the earthquake caused sinking of part of Honshu's Pacific coast by up to roughly a metre, but after about three years, the coast rose back and kept on rising to exceed its original height.The tsunami swept the Japanese mainland and killed over ten thousand people, mainly through drowning, though blunt trauma also caused many deaths. The latest report from the Japanese National Police Agency report confirms 15,897 deaths, 6,157 injured, and 2,533 people missing across twenty prefectures, and a report from 2015 indicated 228,863 people were still living away from their home in either temporary housing or due to permanent relocation.A report by the National Police Agency of Japan on 10 September 2018 listed 121,778 buildings as total collapsed, with a further 280,926 buildings half collapsed, and another 699,180 buildings partially damaged. The earthquake and tsunami also caused extensive and severe structural damage in north-eastern Japan, including heavy damage to roads and railways as well as fires in many areas, and a dam collapse. Japanese Prime Minister Naoto Kan said, In the 65 years after the end of World War II, this is the toughest and the most difficult crisis for Japan. Around 4.4 million households in northeastern Japan were left ...
2011 Tohoku earthquake and tsunami | Wikipedia audio article
This is an audio version of the Wikipedia Article:
00:04:45 1 Earthquake
00:07:11 1.1 Geology
00:11:31 1.2 Energy
00:12:46 1.3 Geophysical effects
00:16:51 1.4 Aftershocks
00:19:04 1.5 Earthquake Warning System
00:20:46 2 Tsunami
00:22:00 2.1 Japan
00:34:40 2.2 Elsewhere across the Pacific
00:39:16 3 Land subsidence
00:41:02 4 Casualties
00:41:11 4.1 Japan
00:46:37 4.2 Overseas
00:47:17 5 Damage and effects
00:49:21 5.1 Ports
00:50:39 5.2 Dams and water problems
00:51:45 5.3 Electricity
00:56:15 5.4 Oil, gas and coal
00:57:43 5.5 Nuclear power plants
01:01:02 5.5.1 Fukushima meltdowns
01:02:47 5.5.2 Incidents elsewhere
01:04:11 5.6 Wind power
01:04:35 5.7 Transport
01:08:50 5.8 Telecommunications
01:09:56 5.9 Defense
01:10:30 5.10 Space center
01:11:07 5.11 Cultural properties
01:12:28 6 Aftermath
01:14:29 7 Humanitarian response
01:14:57 8 Media coverage
01:17:42 9 Scientific and research response
01:21:56 10 See also
Listening is a more natural way of learning, when compared to reading. Written language only began at around 3200 BC, but spoken language has existed long ago.
Learning by listening is a great way to:
- increases imagination and understanding
- improves your listening skills
- improves your own spoken accent
- learn while on the move
- reduce eye strain
Now learn the vast amount of general knowledge available on Wikipedia through audio (audio article). You could even learn subconsciously by playing the audio while you are sleeping! If you are planning to listen a lot, you could try using a bone conduction headphone, or a standard speaker instead of an earphone.
Listen on Google Assistant through Extra Audio:
Other Wikipedia audio articles at:
Upload your own Wikipedia articles through:
Speaking Rate: 0.9985378624446191
Voice name: en-GB-Wavenet-C
I cannot teach anybody anything, I can only make them think.
- Socrates
SUMMARY
=======
The 2011 earthquake off the Pacific coast of Tōhoku (東北地方太平洋沖地震, Tōhoku-chihō Taiheiyō Oki Jishin) was a magnitude 9.0–9.1 (Mw) undersea megathrust earthquake off the coast of Japan that occurred at 14:46 JST (05:46 UTC) on Friday 11 March 2011, with the epicentre approximately 70 kilometres (43 mi) east of the Oshika Peninsula of Tōhoku and the hypocenter at an underwater depth of approximately 29 km (18 mi).
The earthquake is often referred to in Japan as the Great East Japan Earthquake (東日本大震災, Higashi nihon daishinsai) and is also known as the 2011 Tōhoku earthquake, the Great Sendai Earthquake, the Great Tōhoku Earthquake, and the 3.11 earthquake.
It was the most powerful earthquake ever recorded in Japan, and the fourth most powerful earthquake in the world since modern record-keeping began in 1900.
The earthquake triggered powerful tsunami waves that may have reached heights of up to 40.5 metres (133 ft) in Miyako in Tōhoku's Iwate Prefecture, and which, in the Sendai area, traveled at 435 mph for up to 10 km (6 mi) inland. Residents of Sendai had only eight to ten minutes warning, and more than 19,000 were killed, many at the more than a hundred evacuation sites that washed away.The earthquake moved Honshu (the main island of Japan) 2.4 m (8 ft) east, shifted the Earth on its axis by estimates of between 10 cm (4 in) and 25 cm (10 in), increased earth's rotational speed by 1.8 µs per day, and generated infrasound waves detected in perturbations of the low-orbiting GOCE satellite.
Initially, the earthquake caused sinking of part of Honshu's Pacific coast by up to roughly a metre, but after about three years, the coast rose back and kept on rising to exceed its original height.The tsunami swept the Japanese mainland and killed over ten thousand people, mainly through drowning, though blunt trauma also caused many deaths. The latest report from the Japanese National Police Agency report confirms 15,897 deaths, 6,157 injured, and 2,533 people missing across twenty prefectures, and a report from 2015 indicated 228,863 people were still living away from their home in either temporary housing or due to permanent relocation.A report by the National Police Agency of Japan on 10 September 2018 listed 121,778 buildings as total collapsed, with a further 280,926 buildings half collapsed, and another 699,180 buildings partially damaged. The earthquake and tsunami also caused extensive and severe structural damage in north-eastern Japan, including heavy damage to roads and railways as well as fires in many areas, and a dam collapse. Japanese Prime Minister Naoto Kan said, In the 65 years after the end of World War II, this is the toughest and the most difficult crisis for Japan. Around 4.4 million households in northeastern Japan were left ...