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Japan’s Tsunami History confirms What’s in Store

2 responses, Jun 28, 2010

Newly discovered tsunami deposits imply that the Japanese coastline was hammered by a series of massive waves thousands of years ago. The finding adds to growing proof that the region is regularly pounded by killer waves, and could help in planning for future inundations. The northern Japanese island of Hokkaido is huddled up against the Kuril-Kamchatka trench, a place where the Pacific tectonic plate dives beneath the Eurasian plate and home to terrible earthquakes in excess of magnitude 8.0. Tsunami at Japan
Now Wesley Nutter and a team of researchers say nine waves, each at least 33 feet high, thrashed the coastline before the dawn of civilization on the island. “In recorded history, tsunamis have hit the Hokkaido coast over and over again,” Wesley Nutter of Earlham College in Indiana said. “But something of that size has never been recorded here.”
Nutter and a team of researchers dug down into the sediments of a saltwater marsh on the island looking for signs of past tsunamis. Team member Kazuomi Hirakawa of Hokkaido University had first detected a series of sand deposits several years ago there that had no business in a marsh mostly made of peat. Tracing the sand deposits away from the coast, the team found they extend up to more than a mile inland and get thinner further from the sea.

Temperate earthquake strikes Puerto Rico

No response, May 27, 2010

Earthquake with a preliminary magnitude of 5.7 strike the Caribbean island of Puerto Rico early Sunday, the U.S. Geological Survey said.

 Earthquake

The quake hit at 1:16 a.m. (0516 GMT) four miles (six kilometers) from the small community of Espino on the western part of the island and 63 miles (101 kilometers) from the capital, San Juan. It was recorded at a depth of 68 miles (110 kilometers).

There were no immediate reports of damage and injuries.

The West Coast and Alaska Tsunami Warning Center said it did not guess a tsunami, but local tsunamis triggered by underwater landslides were possible in coastal areas close to the epicenter.

museum commemorating the victims of the 2004 Asian tsunami has been opened in the Indonesian province of Aceh

No response, May 18, 2010

It has been planned and designed as a symbolic reminder of the disaster, as well as an educational centre. In addition it will also serve as an Emergency disaster shelter in case the area is ever hit by a tsunami again.

Aceh served as home for more than half the 240,000 people who died in the disaster. The outburst of aid which followed was the largest in history. Almost all that aid money has now been spent - gone to pay for more than 130,000 houses and thousands of kilometers of road, bridges, as well as schools, and other infrastructure.

Yet this new museum building, paid for by Ache’s Reconstruction Fund, breaks with the tradition of post-disaster construction.

Earthquake generated Tsunamis

No response, May 14, 2010

Tsunamis can be generated when the sea floor hurriedly deforms and vertically displaces the overlying water. Tectonic earthquakes are a certain kind of earthquake that are associated with the earth’s crustal deformation; when these earthquakes occur beneath the sea, the water above the deformed area is relocated from its equilibrium position.

Waves are formed as the displaced water mass, which acts under the pressure of gravity, attempts to regain its equilibrium. When large areas of the ocean floor elevate or subside, a tsunami can be created. Huge vertical movements of the earth’s crust can occur at plate boundaries.

Plates act together along these boundaries called faults. Around the margins of the Pacific Ocean, for instance, denser oceanic plates slip under continental plates in a process known as subduction. Subduction earthquakes are mainly effective in generating tsunamis.

Illegal Haitians arrested at U.S. border

No response, Apr 06, 2010

Observers say the arrests reflect the growing fear among illegal Haitian immigrants in North America since the Jan. 12 damage. Among last 2 & half months, they have caught 115 Haitians trying to cross the border by foot into Vermont & New York, including 8 people over Easter weekend, border authorities said.

They may be tried re-entering the U.S. to take advantage of an 18-month ban on deportations to Haiti, passed by the Obama administration after the earthquake. Lots of were heading to New York City & Miami.

Haitians living in North American were paying among $50 & $100 a month for family at home, but many are now trying to double those amounts, said Villefranche. It’s not clear what will go on to the Haitians arrested at the border.

Red tape idle aid things at Haiti’s border

No response, Apr 02, 2010

Polanco drove the equipment for the International Committee of the Red Cross 11 hours from a harbor in the Dominican Republic, only to have the Haitian customs agent discover 1 problem later one more with his paperwork. As he remained in the shade of his truck’s cab in this dusty border town, dozens of others were lined up after him.

Haitian Prime Minister said that the border controls are compulsory to catch smuggled goods, & also lift revenues from commercial drivers’ trade in fees. “Some kind of control is needed,” said Bellerive, who put in that delays were to be waiting for. “There is a lot of traffic across a border that was not ready for that.”

A Haiti fit for its children & young people

No response, Apr 01, 2010

Haitian children & young people aged 5 to 24 shared their views on issues affecting them such as gender, disabilities, violent behavior & misuse, disaster risk reduction, & their own rights & responsibilities post-earthquake as their country come outs from recent earthquakes at a series of focus group thought held throughout the country from 26 February to 5 March.

In a recent situation disaster risk assessment study with more than 1,000 children, may said that go back to school & continue their education as soon as possible. I also want each to have access to schooling,” said quake survivor Daphmika at Port-au-Prince.

Nearly one in every 14 children did not live to see their 5th birthday & children who lived were troubled by high rates of malnutrition. Approximately 50% of all Haitian children did not attend primary school & only 18% of boys & 21% of girls attended secondary school.

The government of Haiti has notified that more than one million children in the earthquake zone were already in vulnerable circumstances & now face increased risks due to loss, separation from, or displacement of their families, malnutrition, illness, psychological trauma & abuse.

NASA scientist says Chilean Quake may have shortened Earth Days

1 response, Mar 03, 2010

JPL research scientist Richard Gross computed how Earth’s rotation should have changed as a result of the Feb. 27 quake. Using a complex model, he and fellow scientists came up with a preliminary calculation that the quake should have shortened the length of an Earth day by about 1.26 microseconds (a microsecond is one millionth of a second).

Perhaps more impressive is how much the quake shifted Earth’s axis. Gross calculates the quake should have moved Earth’s figure axis (the axis about which Earth’s mass is balanced) by 2.7 milliarcseconds (about 8 centimeters, or 3 inches). Earth’s figure axis is not the same as its north-south axis; they are offset by about 10 meters (about 33 feet).

By comparison, Gross said the same model estimated the 2004 magnitude 9.1 Sumatran earthquake should have shortened the length of day by 6.8 microseconds and shifted Earth’s axis by 2.32 milliarcseconds (about 7 centimeters, or 2.76 inches).

Gross said that even though the Chilean earthquake is much smaller than the Sumatran quake, it is predicted to have changed the position of the figure axis by a bit more for two reasons. First, unlike the 2004 Sumatran earthquake, which was located near the equator, the 2010 Chilean earthquake was located in Earth’s mid-latitudes, which makes it more effective in shifting Earth’s figure axis. Second, the fault responsible for the 2010 Chiliean earthquake dips into Earth at a slightly steeper angle than does the fault responsible for the 2004 Sumatran earthquake. This makes the Chile fault more effective in moving Earth’s mass vertically and hence more effective in shifting Earth’s figure axis. Gross said the Chile predictions will likely change as data on the quake are further refined.

Magnitude 5.7 - near Kyrgyzstan-Xinjiang border region

No response, Jun 29, 2009

Kyrgyzstan To Xinjiang

The most important pass in border between Kyrgyzstan and Xinjiang is Torugart Pass, which is “Central Asia’s most exhilarating overland crossing. Scenically extraordinary but logistically difficult and potentially expensive.” (Lonely Planet: Central Asia (2000))

By Crossing the Torugart Pass, travellers get to Kezilesu in westerm Xinjiang and might head eastwards to Kashi and Hetian. Xinjiang’s Akesu is also bordering Kyrgyzstan.

Wednesday, December 25, 2002 at 12:57:07 (UTC)

Magnitude : 5.7
Time : Wednesday, December 25, 2002 at 12:57:07 (UTC)
Distance from : 106 km (66 miles) ESE (108 degrees) of Kyrgyzstan-Xinjiang
Coordinates : 39 deg. 42.2 min. N (39.703N) Depth 33.0 km (20.5 miles)
border region
Quality : Error estimate: horizontal +/- 6.1 km; depth fixed by location program

Earthquake Facts

No response, Jun 01, 2009

1. The largest recorded earthquake in the United States was a magnitude 9.2 that struck Prince William Sound, Alaska on Good Friday, March 28, 1964 UTC.

2. The largest recorded earthquake in the world was a magnitude 9.5 (Mw) in Chile on May 22, 1960.

3. The earliest reported earthquake in California was felt in 1769 by the exploring expedition of Gaspar de Portola while the group was camping about 48 kilometers (30 miles) southeast of Los Angeles.

4. Before electronics allowed recordings of large earthquakes, scientists built large spring-pendulum seismometers in an attempt to record the long-period motion produced by such quakes. The largest one weighed about 15 tons. There is a medium-sized one three stories high in Mexico City that is still in operation.

5. The average rate of motion across the San Andreas Fault Zone during the past 3 million years is 56 mm/yr (2 in/yr). This is about the same rate at which your fingernails grow. Assuming this rate continues, scientists project that Los Angeles and San Francisco will be adjacent to one another in approximately 15 million years.

6. The East African Rift System is a 50-60 km (31-37 miles) wide zone of active volcanics and faulting that extends north-south in eastern Africa for more than 3000 km (1864 miles) from Ethiopia in the north to Zambezi in the south. It is a rare example of an active continental rift zone, where a continental plate is attempting to split into two plates which are moving away from one another.

7. The first “pendulum seismoscope” to measure the shaking of the ground during an earthquake was developed in 1751, and it wasn’t until 1855 that faults were recognized as the source of earthquakes.

8. Moonquakes (”earthquakes” on the moon) do occur, but they happen less frequently and have smaller magnitudes than earthquakes on the Earth. It appears they are related to the tidal stresses associated with the varying distance between the Earth and Moon. They also occur at great depth, about halfway between the surface and the center of the moon.

9. Although both are sea waves, a tsunami and a tidal wave are two different unrelated phenomenona. A tidal wave is a shallow water wave caused by the gravitational interactions between the Sun, Moon, and Earth. A tsunami is a sea wave caused by an underwater earthquake or landslide (usually triggered by an earthquake) displacing the ocean water.

10. The hypocenter of an earthquake is the location beneath the earth’s surface where the rupture of the fault begins. The epicenter of an earthquake is the location directly above the hypocenter on the surface of the earth.


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