Mame hunter - Hanscam's Bowling Center (klamath Falls Oregon)
address - 3319 S 6th St, Klamath Falls, OR 97603
Microtel Inn & Suites by Wyndham Klamath Falls - Klamath Falls Hotels, Oregon
Microtel Inn & Suites by Wyndham Klamath Falls 2 Stars Hotel in Klamath Falls, Oregon Within US Travel Directory Nestled in the scenic Cascade Mountains, this hotel features rooms with free Wi-Fi and a 32-inch flat-screen TV. A free shuttle is offered to Klamath Falls Airport, just 3.9 km away.Decorated in cool tones, all rooms at Microtel Inn & Suites by Wyndham Klamath Falls feature a bay window with cushioned seating and a spacious work desk. A coffee maker is provided in every room.This hotel boasts an indoor/outdoor pool and a relaxing hot tub. Guests can enjoy free access to an off-site fitness center or use the hotel’s 24-hour business center.Microtel Inn & Suites by Wyndham Klamath Falls offers a daily breakfast and discount coupons are available to the Aftershock Bar and Grill, located next door.The Epicenter Family Entertainment Complex is within easy walking distance of this hotel. Shield Crest Golf Course is a 15-minute drive away.
Microtel Inn & Suites by Wyndham Klamath Falls - Klamath Falls Hotels, Oregon
Location in : 2716 Dakota Court, OR 97603, Klamath Falls, Oregon
Booking now :
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The Elks Americanism Essay and The Elks Eye Injury Prevention Poster Contests Awards 2019
The Elks Americanism Essay and The Elks Eye Injury Prevention Poster Contests Awards.
The Elks will be at Shasta Elementary to give out awards to the participants for the essay and poster contest.
Awards up to $1800.
A Special Thanks to:
Jumping N Jax, Epicenter, Klamath Museum, Abby's Pizza, C&D Burger shoppe and Chicken shack
All donated certificates.
Klamath Network Radio will be covering the Event as a Proud Sponsor of Klamath Falls Elks #1247.
The eye injury prevention poster contest is to educate on eye injury prevention.
There will be a Eye screening at Klamath Family Head Start in the fall.
Lyncho Ruiz
Oregon State Elks Association S.E. District Americanism and Visual Chairman
Local Klamath Falls Elks #1247
Applying the Evidence: Afternoon Sessions
HFO-TV: Oregon State Economist Mark McMullen on Oregon's 2017 Economy
According to McMullen, Oregon's median household income has finally recovered from losses suffered when all the mills closed in the 1970s. The state and the country are currently in the middle of the latest economic expansion. Jobs are continuing to increase although at a slower pace. All that and more in this latest Roundtable video. [Runtime: 24:08]
Global Warming Effects on Extreme Weather
Global Warming Effects on Extreme Weather - Select Committee on Energy Independence and Global Warming - 2008-07-10 - In the aftermath of severe storms across America and throughout the world, and with Bertha strengthening to the first hurricane of the season, extreme weather is on the minds of people around the globe. And while storms, floods and droughts have always occurred, science points to our changing climate as having a real effect on the severity and frequency of extreme weather events. Extreme precipitation events have increased over North America over the past 50 years. For the past decade, the West and Southwest regions have experienced drought conditions which are impacting agriculture, and contributing to the wildfire epidemic in the Western United States. On Thursday, Chairman Edward J. Markey (D-Mass.) and the Select Committee on Energy Independence and Global Warming will hold a hearing examining the links between global warming, extreme weather events, and how these events affect the world now and will in the future. WITNESS LIST: Jimmy O. Adegoke, Ph.D, Associate Professor, University of Missouri - Kansas City; Heather Cooley, Senior Research Associate, Pacific Institute; Dr. Jay S. Golden, Director, National Center of Excellence, SMART Innovations for Urban Climate and Energy, Global Institute of Sustainability, Arizona State University; Angela Licata, Deputy Commissioner, New York City Bureau of Environmental Planning and Analysis; Dan Keppen, Executive Director, Family Farm Alliance. Video provided by the U.S. House of Representatives.
President Rahmat Shoureshi Inauguration
Visit Portland State University at
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
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: 0.7529985707519036
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 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 ...
1993 Scotts Mills earthquake | Wikipedia audio article
This is an audio version of the Wikipedia Article:
00:00:42 1 Earthquake
00:01:55 2 Damage
00:02:52 3 Previous events
00:03:21 4 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: 0.9240195662654174
Voice name: en-GB-Wavenet-C
I cannot teach anybody anything, I can only make them think.
- Socrates
SUMMARY
=======
The 1993 Scotts Mills earthquake, also known as the Spring break quake, occurred in the U.S. state of Oregon on March 25 at 5:34 AM Pacific Standard Time. With a moment magnitude of 5.6 and a maximum perceived intensity of VII (Very strong) on the Mercalli intensity scale, it was the largest earthquake in the Pacific Northwest since the Elk Lake and Goat Rocks earthquakes of 1981. Ground motion was widely felt in Oregon's Willamette Valley, the Portland metropolitan area, and as far north as the Puget Sound area near Seattle, Washington.
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 ...
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 ...
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 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.
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