ประกาศข่าวแผ่นดินไหว(&การคาดการณ์)

โรงเรียนภาษา /66 - ANSWERS OF AN ALIEN FROM ANDROMEDA - Nibiru - Elenin - Events

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Uploaded by atlanticobr on Oct 10, 2011

Friends of our channel and YouTubers welcome.
Answers of an alien from Andromeda -- video sixty six - October 10, 2011. Atlantic Time.
This video is a normal meeting with questions and answers.

 

ตีสามครึ่ง.....ฮอนชูมีไหวที่ระดับ5.. รอทั่นkiatp123มาว่าต่อครับ

2012-06-21 20:32:47 UTC
2012-06-22 03:32:47 THA
ศูนย์กลาง: Off East Coast of Honshu Japan
Lat: 39.41 , Long: 143.37
ขนาด : 5.1 , ลึก: 29 กม.
*(source:GEOFON)
--------------------------------------------------------------
<table border="0" cellpadding="0" cellspacing="0"><tbody><tr><td class="point">Magnitude</td><td class="point2">mb 5.3</td></tr><tr><td class="point">Region</td><td class="point2">OFF EAST COAST OF HONSHU, JAPAN</td></tr><tr><td class="point">Date time</td><td class="point2">2012-06-21 20:32:45.0 UTC</td></tr><tr><td class="point">Location</td><td class="point2">39.40 N ; 143.48 E</td></tr><tr><td class="point">Depth</td><td class="point2">5 km</td></tr></tbody></table>-------------------------------------------------------------------
ที่นี่ไม่มีอัพเดทในเวลานี้ 04.48 a.m.
Update time = Thu Jun 21 21:27:03 UTC 2012
<table border="0" cellpadding="1" cellspacing="1"><tbody><tr> <th>
</th> <th align="center">MAG </th> <th align="center">UTC DATE-TIME
y/m/d h:m:s </th> <th align="center">LAT
deg </th> <th align="center">LON
deg </th> <th align="center">DEPTH
km </th> <th> Region</th> </tr> <tr><td align="center" nowrap="nowrap" valign="top">MAP</td><td align="center" nowrap="nowrap" valign="top"> 2.7 </td><td align="center" nowrap="nowrap" valign="top">2012/06/21 18:48:06 </td><td align="right" nowrap="nowrap" valign="top"> 19.053 </td><td align="right" nowrap="nowrap" valign="top"> -66.414 </td><td align="right" nowrap="nowrap" valign="top"> 27.0 </td><td valign="top"> PUERTO RICO REGION</td></tr> <tr><td align="center" nowrap="nowrap" valign="top">MAP</td><td align="center" nowrap="nowrap" valign="top"> 4.6 </td><td align="center" nowrap="nowrap" valign="top">2012/06/21 16:22:47 </td><td align="right" nowrap="nowrap" valign="top"> -20.519 </td><td align="right" nowrap="nowrap" valign="top"> -69.144 </td><td align="right" nowrap="nowrap" valign="top"> 94.6 </td><td valign="top"> TARAPACA, CHILE</td></tr> <tr><td align="center" nowrap="nowrap" valign="top">MAP</td><td align="center" nowrap="nowrap" valign="top"> 2.6 </td><td align="center" nowrap="nowrap" valign="top">2012/06/21 13:20:09 </td><td align="right" nowrap="nowrap" valign="top"> 19.068 </td><td align="right" nowrap="nowrap" valign="top"> -66.405 </td><td align="right" nowrap="nowrap" valign="top"> 33.0 </td><td valign="top"> PUERTO RICO REGION</td></tr> <tr><td align="center" nowrap="nowrap" valign="top">MAP</td><td align="center" nowrap="nowrap" valign="top"> 4.8 </td><td align="center" nowrap="nowrap" valign="top">2012/06/21 12:22:19 </td><td align="right" nowrap="nowrap" valign="top"> 2.728 </td><td align="right" nowrap="nowrap" valign="top"> 123.062 </td><td align="right" nowrap="nowrap" valign="top">461.0 </td><td valign="top"> CELEBES SEA</td></tr> <tr><td align="center" nowrap="nowrap" valign="top">MAP</td><td align="center" nowrap="nowrap" valign="top"> 4.3 </td><td align="center" nowrap="nowrap" valign="top">2012/06/21 11:52:30 </td><td align="right" nowrap="nowrap" valign="top"> -3.042 </td><td align="right" nowrap="nowrap" valign="top"> 129.842 </td><td align="right" nowrap="nowrap" valign="top"> 41.4 </td><td valign="top"> SERAM, INDONESIA</td></tr> <tr><td align="center" nowrap="nowrap" valign="top">MAP</td><td align="center" nowrap="nowrap" valign="top"> 5.1 </td><td align="center" nowrap="nowrap" valign="top">2012/06/21 11:40:35 </td><td align="right" nowrap="nowrap" valign="top"> 2.647 </td><td align="right" nowrap="nowrap" valign="top"> 128.267 </td><td align="right" nowrap="nowrap" valign="top">114.7 </td><td valign="top"> HALMAHERA, INDONESIA</td></tr></tbody></table>
__________________

 

Update time = Thu Jun 21 23:23:46 UTC 2012

<TABLE border=0 cellSpacing=1 cellPadding=1><TBODY><TR><TH> </TH><TH align=middle>MAG </TH><TH align=middle>UTC DATE-TIME
y/m/d h:m:s </TH><TH align=middle>LAT
deg </TH><TH align=middle>LON
deg </TH><TH align=middle>DEPTH
km </TH><TH> Region</TH></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle> 2.8 </TD><TD vAlign=top noWrap align=middle>2012/06/21 22:58:13 </TD><TD vAlign=top noWrap align=right> 18.299 </TD><TD vAlign=top noWrap align=right> -64.352 </TD><TD vAlign=top noWrap align=right>18.0 </TD><TD vAlign=top> VIRGIN ISLANDS REGION</TD></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle> 4.9 </TD><TD vAlign=top noWrap align=middle>2012/06/21 22:34:38 </TD><TD vAlign=top noWrap align=right> -17.872 </TD><TD vAlign=top noWrap align=right> -178.103 </TD><TD vAlign=top noWrap align=right>545.7 </TD><TD vAlign=top> FIJI REGION</TD></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle> 4.6 </TD><TD vAlign=top noWrap align=middle>2012/06/21 22:17:11 </TD><TD vAlign=top noWrap align=right> -11.494 </TD><TD vAlign=top noWrap align=right> -76.329 </TD><TD vAlign=top noWrap align=right>38.3 </TD><TD vAlign=top> CENTRAL PERU</TD></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle> 5.4 </TD><TD vAlign=top noWrap align=middle>2012/06/21 20:32:50 </TD><TD vAlign=top noWrap align=right> 39.437 </TD><TD vAlign=top noWrap align=right> 143.339 </TD><TD vAlign=top noWrap align=right>33.1 </TD><TD vAlign=top> OFF THE EAST COAST OF HONSHU, JAPAN</TD></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle> 2.7 </TD><TD vAlign=top noWrap align=middle>2012/06/21 18:48:06 </TD><TD vAlign=top noWrap align=right> 19.053 </TD><TD vAlign=top noWrap align=right> -66.414 </TD><TD vAlign=top noWrap align=right>27.0 </TD><TD vAlign=top> PUERTO RICO REGION</TD></TR></TBODY></TABLE>

 

HONSHU, JAPAN

<TABLE border=0 cellSpacing=1 cellPadding=1><TBODY><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>5.4 </TD><TD vAlign=top noWrap align=middle>2012/06/21 20:32:50 </TD><TD vAlign=top noWrap align=right>39.437 </TD><TD vAlign=top noWrap align=right>143.339 </TD><TD vAlign=top noWrap align=right>33.1 </TD><TD vAlign=top>OFF THE EAST COAST OF HONSHU, JAPAN</TD></TR></TBODY></TABLE>
10-degree Map Centered at 40°N,145°E



<TABLE border=0 cellSpacing=1 cellPadding=1><TBODY><TR><TD noWrap align=middle>MAP</TD><TD noWrap align=middle>5.4</TD><TD noWrap align=middle>2012/06/21 20:32:50 </TD><TD noWrap align=right>39.437</TD><TD noWrap align=right>143.339 </TD><TD noWrap align=right>33.1 </TD><TD>OFF THE EAST COAST OF HONSHU, JAPAN</TD></TR><TR><TD noWrap align=middle>MAP</TD><TD noWrap align=middle>4.6</TD><TD noWrap align=middle>2012/06/21 02:00:03 </TD><TD noWrap align=right>39.426</TD><TD noWrap align=right>143.258 </TD><TD noWrap align=right>32.7 </TD><TD>OFF THE EAST COAST OF HONSHU, JAPAN</TD></TR><TR><TD noWrap align=middle>MAP</TD><TD noWrap align=middle>4.6</TD><TD noWrap align=middle>2012/06/20 23:56:32 </TD><TD noWrap align=right>36.929</TD><TD noWrap align=right>141.105 </TD><TD noWrap align=right>35.1 </TD><TD>NEAR THE EAST COAST OF HONSHU, JAPAN</TD></TR><TR><TD noWrap align=middle>MAP</TD><TD noWrap align=middle>4.8</TD><TD noWrap align=middle>2012/06/19 22:28:47 </TD><TD noWrap align=right>37.628</TD><TD noWrap align=right>141.628 </TD><TD noWrap align=right>32.5 </TD><TD>NEAR THE EAST COAST OF HONSHU, JAPAN</TD></TR><TR><TD noWrap align=middle>MAP</TD><TD noWrap align=middle>6.4</TD><TD noWrap align=middle>2012/06/17 20:32:20 </TD><TD noWrap align=right>38.894</TD><TD noWrap align=right>141.946 </TD><TD noWrap align=right>31.8 </TD><TD>NEAR THE EAST COAST OF HONSHU, JAPAN</TD></TR><TR><TD noWrap align=middle>MAP</TD><TD noWrap align=middle>4.6</TD><TD noWrap align=middle>2012/06/17 07:13:15 </TD><TD noWrap align=right>36.149</TD><TD noWrap align=right>140.008 </TD><TD noWrap align=right>52.5 </TD><TD>NEAR THE EAST COAST OF HONSHU, JAPAN</TD></TR><TR><TD noWrap align=middle>MAP</TD><TD noWrap align=middle>4.7</TD><TD noWrap align=middle>2012/06/15 18:27:22 </TD><TD noWrap align=right>38.959</TD><TD noWrap align=right>143.417 </TD><TD noWrap align=right>19.0 </TD><TD>OFF THE EAST COAST OF HONSHU, JAPAN</TD></TR><TR><TD noWrap align=middle>MAP</TD><TD noWrap align=middle>4.7</TD><TD noWrap align=middle>2012/06/15 07:31:51 </TD><TD noWrap align=right>38.273</TD><TD noWrap align=right>141.779 </TD><TD noWrap align=right>51.1 </TD><TD>NEAR THE EAST COAST OF HONSHU, JAPAN</TD></TR><TR><TD noWrap align=middle>MAP</TD><TD noWrap align=middle>4.4</TD><TD noWrap align=middle>2012/06/15 05:09:47 </TD><TD noWrap align=right>37.024</TD><TD noWrap align=right>141.353 </TD><TD noWrap align=right>43.3 </TD><TD>NEAR THE EAST COAST OF HONSHU, JAPAN</TD></TR></TBODY></TABLE>

plate tectonics



ดู Plate tectonics ทั้งโลก ได้ ที่นี่

 

ขอบแผ่นออสเตรเลียตะวันออก

Update time = Fri Jun 22 2:00:04 UTC 2012

<TABLE border=0 cellSpacing=1 cellPadding=1><TBODY><TR><TH></TH><TH align=middle>MAG </TH><TH align=middle>UTC DATE-TIME
y/m/d h:m:s





</TH><TH align=middle>LAT
deg





</TH><TH align=middle>LON
deg





</TH><TH align=middle>DEPTH
km





</TH><TH>Region</TH></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>4.8 </TD><TD vAlign=top noWrap align=middle>2012/06/22 00:03:13</TD><TD vAlign=top noWrap align=right>-32.999 </TD><TD vAlign=top noWrap align=right>-179.833 </TD><TD vAlign=top noWrap align=right>35.1 </TD><TD vAlign=top>SOUTH OF THE KERMADEC ISLANDS</TD></TR></TBODY></TABLE>
<TABLE border=0 cellSpacing=1 cellPadding=1><TBODY><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>5.2 </TD><TD vAlign=top noWrap align=middle>2012/06/21 23:52:57</TD><TD vAlign=top noWrap align=right>-32.889 </TD><TD vAlign=top noWrap align=right>-178.637 </TD><TD vAlign=top noWrap align=right>37.4 </TD><TD vAlign=top>SOUTH OF THE KERMADEC ISLANDS</TD></TR></TBODY></TABLE>10-degree Map Centered at 35°S,180°E



<TABLE border=0 cellSpacing=1 cellPadding=1><TBODY><TR><TD noWrap align=middle>MAP</TD><TD noWrap align=middle>4.8</TD><TD noWrap align=middle>2012/06/22 00:03:12 </TD><TD noWrap align=right>-32.999</TD><TD noWrap align=right>-179.833 </TD><TD noWrap align=right>35.1 </TD><TD>SOUTH OF THE KERMADEC ISLANDS</TD></TR><TR><TD noWrap align=middle>MAP</TD><TD noWrap align=middle>5.2</TD><TD noWrap align=middle>2012/06/21 23:52:56 </TD><TD noWrap align=right>-32.889</TD><TD noWrap align=right>-178.637 </TD><TD noWrap align=right>37.4 </TD><TD>SOUTH OF THE KERMADEC ISLANDS</TD></TR><TR><TD noWrap align=middle>MAP</TD><TD noWrap align=middle>4.6</TD><TD noWrap align=middle>2012/06/21 03:25:53 </TD><TD noWrap align=right>-38.230</TD><TD noWrap align=right>176.493 </TD><TD noWrap align=right>172.9 </TD><TD>NORTH ISLAND OF NEW ZEALAND</TD></TR><TR><TD noWrap align=middle>MAP</TD><TD noWrap align=middle>4.8</TD><TD noWrap align=middle>2012/06/18 14:04:43 </TD><TD noWrap align=right>-33.220</TD><TD noWrap align=right>179.535 </TD><TD noWrap align=right>250.0 </TD><TD>SOUTH OF THE KERMADEC ISLANDS</TD></TR></TBODY></TABLE>

ตรงจุดนี้คือด้านทิศตะวันออกของแผ่นอินโดออสเตรเลีย ที่ตั้งของหมู่เกาะตองก้า คามาเด็ด ไล่ลงไปจนถึงประเทศนิวซีแลนด์เกาะเหนือและใต้ แผ่นโซนที่แผ่นแปซิฟิคมุดสอดแผ่นออสเตรเลียพร้อมกับยกขอบแผ่นให้สูงขึ้น เฉพาะที่ร่องลึกตองก้า-คามาเด็ดจุดที่มีชื่อว่า Horizon Deep แผ่นแปซิฟิคยกขอบแผ่นออสเตรเลียให้สูงขึ้นไปแล้วกว่า 8 กิโลเมตร และยังมุดและยกขอบแผ่นอยู่ทุกวัน วันละหลายๆรอบ นักธรณีวิทยาไปวัดขอบแผ่นออสเตรเลียตะวันออกปรากฎว่าสูงขึ้นกว่า 13 ฟุตต่อวัน หรือเกือบ 4 เมตรต่อวัน

ลือกันว่าพื้นที่นี้คือทวีปลีมูเรียเก่า อาจมีเมืองแอตแลนติสอยู่บนทวีปนี้ด้วย ถ้าเป็นเช่นนั้นจริงอีกไม่กี่ปีเราก็จะได้เห็นทวีปนี้โผล่พ้นน้ำคืนชีพมาอีกครั้ง ถ้าไม่เป็นอะไรไปเสียก่อนอันนี้เรายังจะทันได้ดู

เท่านั้นยังไม่พอเวลาแผ่นแปซิฟิคยกขอบแผ่นตะวันออก ทำให้แผ่นออสเตรเลียเอียงไปทางทิศตะวันตกกดขอบแผ่นออสเตรเลียตะวันตกต่ำลงไปเรื่อย น้ำจากมหาสมุทรอินเดียใต้จะค่อยๆไหลบ่าเข้าท่วมทางตะวันตกของทวีปออสเตรเลีย ถ้าปรากฎการการเคลื่อนตัวของเปลือกโลกโซนนี้ยังไม่เปลี่ยนแปลง เราคงได้เห็นวีปออสเตรเลียด้านทิศตะวันตกหายไปอีกประมาณครึ่งทวีปเช่นเดียวกัน

 

ผมสังเกตุดู รอบๆ บ้านเราไหวแรงขึ้นเรื่อยๆ จาก 1 เป็น 2 - 3 ตอนนี้ 4 กว่าแล้ว

 

ก่อนเที่ยงเริ่มแรง....

Update time = Fri Jun 22 4:50:06 UTC 2012
<table border="0" cellpadding="1" cellspacing="1"><tbody><tr> <th>
</th> <th align="center">MAG </th> <th align="center">UTC DATE-TIME
y/m/d h:m:s </th> <th align="center">LAT
deg </th> <th align="center">LON
deg </th> <th align="center">DEPTH
km </th> <th> Region</th> </tr> <tr><td align="center" nowrap="nowrap" valign="top">MAP</td><td align="center" nowrap="nowrap" valign="top"> 6.0 </td><td align="center" nowrap="nowrap" valign="top">2012/06/22 04:31:17 </td><td align="right" nowrap="nowrap" valign="top"> -54.302 </td><td align="right" nowrap="nowrap" valign="top"> 158.727 </td><td align="right" nowrap="nowrap" valign="top"> 9.9 </td><td valign="top"> MACQUARIE ISLAND REGION</td></tr></tbody></table>----------------------------------------------------------------------------------------------
<table border="0" cellpadding="0" cellspacing="0"><tbody><tr><td class="point">Magnitude</td><td class="point2">Mw 6.0</td></tr><tr><td class="point">Region</td><td class="point2">MACQUARIE ISLAND REGION</td></tr><tr><td class="point">Date time</td><td class="point2">2012-06-22 04:31:17.3 UTC</td></tr><tr><td class="point">Location</td><td class="point2">54.30 S ; 158.73 E</td></tr><tr><td class="point">Depth</td><td class="point2">10 km</td></tr></tbody></table>-----------------------------------------------------------------------------------
2012-06-22 04:31:18 UTC
2012-06-22 11:31:18 THA
ศูนย์กลาง: Macquarie Island Region
Lat: -54.30 , Long: 158.79
ขนาด : 5.9 , ลึก: 10 กม.
*(source:GEOFON)

 

Large sinkhole opens up in Pikeville/Sinkhole swallows back half of home in Hudson

• Posted by khan on June 21, 2012 at 8:42am
• View Blog

June 20, 2012



Large sinkhole opens up in Pikeville

A 20 foot wide sinkhole has opened up in a field right near Highway 127, and local residents say that it is still growing.
http://timesfreepress.com/news/2012/jun/20/large-sinkhole-opens-pik...

....................................
Sinkhole swallows back half of home in Hudson
June 20, 2012





HUDSON — Susan Minutillo, 79, climbed out of her dark gray Mercury and saw the emergency trucks outside her house in Beacon Woods East. She'd left about half an hour before to run an errand for a friend, leaving a crew to do a survey of her home, checking for sinkholes. The survey was routine. Just like her day was supposed to be.
"I never thought this would happen to me," she said Wednesday afternoon, sitting at the kitchen table in her neighbor's home, voice thick with unshed tears. "I don't know where I'll go now."
At about 3 p.m., a sinkhole under the back half of her home began to collapse. Forty-five minutes later, half the house was gone, and county officials plastered a dark orange sign with black block letters spelling "condemned" on the garage door.
Emergency vehicles from the Sheriff's Office, Pasco County Ground Inspections, the fire department and others circled the property, surrounding the house with yellow tape and shutting down the electricity and water still pumping into the broken home.
Minutillo fled to her neighbor's home. It's probable she'll never be able to walk inside her own house at 14003 Shoal Drive.
Men from the fire department ventured inside her house — too dangerous for anyone else to enter — and brought out her cell phone charger and prescription medications.
She sat at the table in a corner of the kitchen while the fire department told her neighbors, Howard and Shirley Taylor, that their home was unsafe, as well. They had until 4:30 p.m. to evacuate. The rushed around their home, collecting medications and private documents, while Minutillo sat at the table, making phone calls.
Jim Johnston, operations coordinator for Pasco County emergency management, said more than 50 percent of Minutillo's home had been destroyed by 4 p.m. Wednesday. He said the next step is to determine what else in the area could be affected by the sinkhole, at which point they will be able to determine whether anyone else needs to be evacuated.
Minutillo said her insurance company promised to cover damages. Annette Doying, director of Pasco County emergency management, said a geotechnical engineering company surveyed the damage at the behest of the property insurance company. Due to the afternoon rain, however, the company could not use ground-penetrating radar to assess the sinkhole properly, so it could take several days to determine the damage.
Doying said a number of other homes in the neighborhood have had prior sinkhole activity that has been stabilized.
Minutillo called her sister in Port Richey, where she hopes to stay for the time being. She said she supposes she will have to rent an apartment, once she finds one. It's hard to say how long that could take, but she doesn't want to be a burden.
http://www.tampabay.com/news/environment/sinkhole-swallows-back-hal...

 

Without Satellites

The Zetas have long predicted that going into the Last Weeks, and well prior to some extent, that satellites will fail. They have been failing since Planet X arrived in the inner solar system in 2003, due to debris in the tail of Planet X but more due to electro-magnetic pulse. Recently, on April 8, 2012, Europe’s Envisat http://news.sciencemag.org/scienceinsider/2012/04/researchers-unabl...
satellite went out of control.

ZetaTalk Prediction 7/15/1995:
ZetaTalk: Internet
The months before the cataclysms, satellite failure will be sporadic, but enough to impact technology as it support lifestyles today. Land lines will be reliable, but cell phones will not.

ZetaTalk Prediction 9/15/1996:
ZetaTalk: Bill Gates
Satellites use magnets for alignment of their internal mechanisms, and if pointing in wrong directions, communications are halted. What good is a message intended for the Earth's surface when it is sent into outer space?

ZetaTalk Prediction 11/13/2010:
http://www.zetatalk13.com/7of10/7of10-20.htm
We have stated that total satellite failure can be expected as the last weeks approach, with increasing failure up until that point. Certainly, during the last weeks, the 9 of 10, total failure can be expected. Prior to this time electromagnetic surge and pulse will affect clear communication via satellite, and cell phone usage.

Most such failures are kept from the public view, with governments putting up additional satellites as a safety net in case of failure. Are they worried that their satellite views will fail, just when they need them the most? Per the Zetas, there is much evidence that the governments of the world are already setting up alternatives during the approach and passage of Planet X. Earth based arrays of telescopes are one such alternative.



Africa and Australia to Share Square Kilometre Array
May 25, 2012
BBC News - Africa and Australasia to share Square Kilometre Array
South Africa, Australia and New Zealand will host the biggest radio telescope ever built.

Super-Telescope Project Split Between South Africa and Australia
May25, 2012
http://www.rawstory.com/rs/2012/05/25/super-telescope-project-split...
Conceived more than two decades ago, the Square Kilometre Array aims at bringing together unprecedented size and new technology. It would use a forest of antennae, spread out over remote terrain, to pick up radio signals from cosmic phenomena that cannot be detected by optical telescopes. Stars that flare into life or explode at their death, black holes, mysterious “dark energy,” and relic traces of ancient events that occurred in the dawn of the Universe 14 billion years ago, are among its targets. According to plans that were made for a single-site project, the first phase of the scheme would be completed by 2019 and become operational in 2020.

Expensive NASA Equipment Found in North Texas
May 30, 2012
Expensive NASA equipment found in North Texas | wfaa.com Dallas - Fort Worth
Science equipment is missing, en route from Minneapolis to Palestine, Texas. The equipment is part of a NASA-funded experiment. A truck left The University of Minnesota's School of Physics and Astronomy Friday, but never made it to Palestine. It was last seen at truck stops in Dallas and Hutchins. The truck driver has been found, but the cargo is missing. It is a bizarre story that NASA doesn't even want to talk about.

ZetaTalk Comment 6/2/2012:
http://www.zetatalk15.com/ning/02ju2012.htm
What are the astronomers hoping to capture, with this massive new radio array in S Africa and Australia and New Zealand? Signals from outer space? Why is it necessary to point this massive array into the southern skies, and what relationship to the original inbound direction of Planet X, from Orion (in the southern skies) does this have? The entire project, supposedly to become operational in 2019 at the earliest but in fact operational immediately, is a front for tracking Planet X during its passage. The sites will set up, move equipment into place, and start scanning Planet X via numerous means – infrared visibility, radio waves, x-rays, and magnetic surge. The Southern Hemisphere arrays are not the only such arrangement being made. We have predicted almost since the start of ZetaTalk that satellites would fail as the time of the passage approached. This is their alternative!

Robotic planes, which have apparently been in operation for over a year, are another means of keeping track of Planet X when the satellites fail.

America's Mysterious Space Plane to Land after a YEAR in Orbit
June 4, 2012
http://www.dailymail.co.uk/sciencetech/article-2154405/Secret-missi...
Secret mission accomplished: America's mysterious space plane to land after a year in orbit - and no one knows what it did up there. The X-37B has been circling the Earth at 17,000mph and was due to land in California in December. Mission of highly classified robotic plane extended for unknown reasons.

ZetaTalk Comment 6/9/2012:
http://www.zetatalk16.com/ning/09ju2012.htm
How else to establish when it is time to duck into their bunkers? When satellites are blinded by debris, and man is left to peer through a dust clogged sky, how will they know when the hour of the Pole Shift has arrived? How are they to know when the largest moons of Planet X are slinging in their direction? Why reveal now, at this time, that this X-37B plane has already been in the skies, above the atmosphere? The time is rapidly approaching when the public will be aware of the presence of Planet X in the inner solar system, aware of the threat, and putting this all together with prophecy and legend. They will be demanding to know what their governments will do for them. At what point should they leave their jobs and head for the hills? The X-37B, and similar means of peering at the Planet X complex, will be trotted forth for reassurance. “We will tell you when it is time to panic” will be the reassurance. This will hardly reassure a public that now realizes they had been lied to for decades, but this is the establishment’s plan.

^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^
Photo Confirmation

There is nothing like photo confirmation - from different individuals who do not know each other, who are miles apart - to prove that Planet X and its components are very much visible in the skies. On June 4, 2012 Richard in Michigan noted a bright orb above the Sun, moving behind the clouds, and snapped a photo of this. He saw this naked eye, also. Bright Moon Swirls, the Monster persona that can form from Moon Swirls as well as from Planet X itself, are often seen around the Sun these days. On the same day, Elizabeth in S. Carolina took a snap using a red filter. She also caught the Monster Moon Swirl, halfway behind clouds. This shows, without a doubt, that the Monster is not a lens flare, as these always stand in FRONT of all objects being captured in the photos, as the flare is within the camera itself.

It was visible to the eyes. The sun is behind a cloud on the bottom.

A second sun photo taken with Canon Rebel X digital with a red filter.

 

Meteor Sightings Ground Flights, Reports From CO, NM, and KS... June 20, 2012

• Posted by Mistress Sindra on June 21, 2012 at 8:30pm
• View Blog

<iframe src="http://www.youtube.com/embed/eH8N63n9_us" allowfullscreen="" frameborder="0" height="315" width="560"></iframe>
Published on Jun 21, 2012 by Sheilaalien

 

Thailand: Villagers shocked the city to check the collapse of 10 meters

• Posted by khan on June 22, 2012 at 2:00am
• View Blog

June 21, 2012


Villagers shocked the city to check the collapse of 10 meters.

Today (20 Jun) reports that After the rain for several consecutive days. World. Result in the collapse of the school's front toe Huai Pa Rai Mon Tue Thong Pha Phum, Kanchanaburi yesterday (19 Jun), a depth of approximately 5 meters at 10.00 am on the last hole of the day. This was increased to more than 4 meters deep, approximately 10 meters in diameter and 5.6 meters in a stampede to see the students and the public in such vehicles. Fearing landslides. The local authorities have not allowed for security reasons. To wait for a geophysical survey tools, subsurface soils to determine the cause of the collapse of the soil. And find ways to prevent and resolve in this evening.
กรมธรณีฯวางแนวสำรวจหาจุดผ่านโพรงใต้ดินก่อนเกิดภัยพิบัติ | เดลินิวส์

 

หุ หุ วันนี้แรงขึ้นนะ 5+ตลอดในย่านนี้

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mso-para-margin-left:0cm; line-height:115%; mso-pagination:widow-orphan; font-size:11.0pt; mso-bidi-font-size:14.0pt; font-family:"Calibri","sans-serif"; mso-ascii-font-family:Calibri; mso-ascii-theme-font:minor-latin; mso-fareast-font-family:"Times New Roman"; mso-fareast-theme-font:minor-fareast; mso-hansi-font-family:Calibri; mso-hansi-theme-font:minor-latin;} </style> <![endif]--> [FONT=&quot]แผ่นดินไหว[/FONT]::[FONT=&quot] สำนักเฝ้าระวังแผ่นดินไหว[/FONT]
[FONT=&quot]แผ่นดินไหว [/FONT]Off West Coast of Northern Sumatra (1.31,92.32)
[FONT=&quot]ขนาด [/FONT]5.5[FONT=&quot] ลึก [/FONT]10[FONT=&quot] กม. วันที่ [/FONT]22[FONT=&quot] มิถุนายน [/FONT]2555[FONT=&quot] เวลา [/FONT]12.14[FONT=&quot] น.[/FONT][FONT=&quot] ตามเวลาประเทศไทย[/FONT]
2012-06-22 05:14:44 UTC
Lat. 1.31 , Long. 92.32
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[FONT=&quot]แผ่นดินไหว [/FONT]Macquarie Island Region(-54.30,158.79)
[FONT=&quot]ขนาด [/FONT]5.9[FONT=&quot] ลึก [/FONT]10[FONT=&quot] กม. วันที่ [/FONT]22[FONT=&quot] มิถุนายน [/FONT]2555[FONT=&quot] เวลา [/FONT]11.31[FONT=&quot] น.[/FONT][FONT=&quot] ตามเวลาประเทศไทย[/FONT]
2012-06-22 04:31:18 UTC
Lat. -54.30 , Long. 158.79
------------------------------------------------------------------------------------------------------------------------
[FONT=&quot]แผ่นดินไหว [/FONT]Tonga Islands(-18.18,-175.10)
[FONT=&quot]ขนาด [/FONT]5.1[FONT=&quot] ลึก [/FONT]177[FONT=&quot] กม. วันที่ [/FONT]22[FONT=&quot] มิถุนายน [/FONT]2555[FONT=&quot] เวลา [/FONT]11.25[FONT=&quot] น.[/FONT][FONT=&quot] ตามเวลาประเทศไทย[/FONT]
2012-06-22 04:25:39 UTC
Lat. -18.18 , Long. -175.10
[FONT=&quot]-------------------------------------------------------------------------------------------------------------------------[/FONT]
[FONT=&quot]แผ่นดินไหว [/FONT]South of Kermadec Islands(-32.73,-178.46)
[FONT=&quot]ขนาด [/FONT]5.4[FONT=&quot] ลึก [/FONT]10[FONT=&quot] กม. วันที่ [/FONT]22[FONT=&quot] มิถุนายน [/FONT]2555[FONT=&quot] เวลา [/FONT]09.20[FONT=&quot] น.[/FONT][FONT=&quot] ตามเวลาประเทศไทย[/FONT]
2012-06-22 02:20:08 UTC
Lat. -32.73 , Long. -178.46
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[FONT=&quot]แผ่นดินไหว [/FONT]South of Kermadec Islands(-32.75,-178.69)
[FONT=&quot]ขนาด [/FONT]5.1[FONT=&quot] ลึก [/FONT]121[FONT=&quot] กม. วันที่ [/FONT]22[FONT=&quot] มิถุนายน [/FONT]2555[FONT=&quot] เวลา [/FONT]07.03[FONT=&quot] น.[/FONT][FONT=&quot] ตามเวลาประเทศไทย[/FONT]
2012-06-22 00:03:15 UTC
Lat. -32.75 , Long. -178.69
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[FONT=&quot]แผ่นดินไหว [/FONT]Fiji Islands Region(-17.93,-178.19)
[FONT=&quot]ขนาด [/FONT]5.2[FONT=&quot] ลึก [/FONT]542[FONT=&quot] กม. วันที่ [/FONT]22[FONT=&quot] มิถุนายน [/FONT]2555[FONT=&quot] เวลา [/FONT]05.34[FONT=&quot] น.[/FONT][FONT=&quot] ตามเวลาประเทศไทย[/FONT]
2012-06-21 22:34:38 UTC
Lat. -17.93 , Long. -178.19
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[FONT=&quot]แผ่นดินไหว [/FONT]Off East Coast of Honshu, Japan (39.41,143.36)
[FONT=&quot]ขนาด [/FONT]5.0[FONT=&quot] ลึก [/FONT]29[FONT=&quot] กม. วันที่ [/FONT]22[FONT=&quot] มิถุนายน [/FONT]2555[FONT=&quot] เวลา [/FONT]03.32[FONT=&quot] น.[/FONT][FONT=&quot] ตามเวลาประเทศไทย[/FONT]
2012-06-21 20:32:50 UTC
Lat. 39.41 , Long. 143.36

 

เมื่อมีการเริ่มไหว ค่อยๆไหว ค่อยๆ ขยับ สุดท้ายก็คงพังทลาย เหมือนแก้วที่เริ่มร้าว สักวันก็คงแตก แต่การแตกไม่ได้เกิดจากการโดนกระทำครั้งเดียวแล้วแตก แต่หากเป็นการแตกเพราะรอยร้าวที่สะสม น่ากลัวเหมือนกันน่ะ

 

MACQUARIE ISLAND REGION

<TABLE border=0 cellSpacing=1 cellPadding=1><TBODY><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>6.0 </TD><TD vAlign=top noWrap align=middle>2012/06/22 04:31:17 </TD><TD vAlign=top noWrap align=right>

-54.302 ​

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</TD><TD vAlign=top noWrap align=right>158.727 </TD><TD vAlign=top noWrap align=right>9.9 </TD><TD vAlign=top>MACQUARIE ISLAND REGION</TD></TR></TBODY></TABLE></B>​

10-degree Map Centered at 55°S,160°E​

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Earthquake Location

<!-- b000amdx MACQUARIE ISLAND REGION -->Magnitude 6.0 MACQUARIE ISLAND REGION
Friday, June 22, 2012 at 04:31:17 UTC





<SMALL>Major Tectonic Boundaries: Subduction Zones -purple, Ridges -red and Transform Faults -green </SMALL>

<SMALL>Major Tectonic Boundaries: Subduction Zones -purple, Ridges -red and Transform Faults -green </SMALL>

Map of SOUTHERN OCEAN
Preliminary Earthquake Report
U.S. Geological Survey, National Earthquake Information Center
World Data Center for Seismology, Denver


Plate Tectonics

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The Geological Development of a Young Island ​

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Although Macquarie Island was first discovered by Captain Hasselburgh in 1810, the first geologist to study the island was Leslie Russell Blake, a member of the Australian Antarctic Expedition, who spent more that two years on the island from 1911 to 1914.
From the time the Australian National Antarctic Research Expedition (ANARE) set up a permanent station on Macquarie in 1948, there have been a considerable number of geologists keen to carry out detailed research into the origins of this tiny speck of land in the Southern Ocean.
Macquarie Island is geologically unique in a number of ways. Among subantarctic islands, it is the only one to be totally oceanic in origin and is a rare example of uplifted oceanic crust. It does not have large scale sedimentation and has not been built up from actual volcanic activity. It is also now thought that the island has been subjected to little or no glaciation during its development.
It all started some 12 million years ago. Basalt magma from deep inside the earth flowed from a fissure on the seabed at the abutting edges of two large tectonic plates, the Indian/Australian Plate, to which Macquarie Island belongs, and the Pacific Plate. A third tectonic plate, Antarctic, abuts the other two plates some 650 kilometres south of the island. Geologists now indicate that the Pacific Plate is being pushed, in an anticlockwise direction, under the Indian/Australian Plate at 2-3 centimetres a year. Consequently, the Indian/Australian Plate is riding up vertically over the Pacific Plate at 1 - 2 millimetres a year.
As a result of these complicated movements and pressures, the Macquarie Ridge complex has been growing upwards. Trending NNE in its northern part and curved towards the SE at its southern end, it runs from the New Zealand coastal shelf off the west coast of South Island to the triple plate junction at about 61�S, 162�E.
When the Macquarie Ridge had risen more than 2.5 kilometres from the sea floor, it broke through the ocean surface where it has since been subjected to the effects of the very strong winds and huge waves that are generated in the vast Southern Ocean. In spite of these eroding forces the island is now some 200 - 400 metres high. The date at which Macquarie Island broke through the sea surface is currently being debated by geologists. Some suggest 700,000 years ago while others think that it could be from 80,000 to 300,000 years ago.
Running parallel with and 40 km to the east of the Macquarie Ridge is the Macquarie Trench which is some 5,500 metres deep. This deep trench breaks through the ridge line nearly 100 kilometres to the south of the island and continues southwards as the Hjort Trench to about 60�S.
The age of the rocks which form the island have been calculated by geologists. Palaeomagnetic studies of the rocks suggest ages of 27 - 30 million years while Radiometric measurements yield ages of 9.7 to 11.5 million years. The age of the rocks is still extremely young in geological terms when you consider that the Australian mainland is mostly formed from rocks which are over 1,000 millions years old!
One of the rock types on the island, Harzburgite, suggest to geologists that the uplifting of Macquarie Island has been approximately 10 kilometres, as this rock type is normally formed 5 km below the ocean floor. (Selkirk, Seppelt & Selkirk)
P E Williamson (1987) considers that the detailed structure and stratigraphy of the extrusive rocks of the island are complex and poorly understood. Duncan and Varne (1987) suggest that the new maps and geological data show that the island is composed of a number of fault bounded blocks derived from different layers of the oceanic lithosphere. This implies that all the igneous rocks could have been formed at much the same time. The northern part of Macquarie Island is formed mainly of intrusive igneous rocks, whereas the remainder, south of a line Sandy Bay - Bauer Bay, is formed mainly of extrusive volcanic rocks and associated sedimentary rocks. ​

There were reports of earthquakes from sealers who were working on the island from time to time, the first on 31 October 1815. The measurement of earthquakes in the area of Macquarie Island were initially made in Australia and New Zealand. Since 1950, the Bureau of Mineral Resources has been operating a seismograph on the island itself so that much more accurate data has been collected.

Dr. B. D. Goscombe and J. L. Everard of Mineral Resources of Tasmania carried out a detailed geological survey of Macquarie Island during 1994-96. The geology has been published in the form of 1:50,000, 1:25,000 and 1:10,000 geological maps in 1998 and the data is available in digital format. ​

There are many unanswered questions about the formation of Macquarie Island and much research remains to be done. ​

For further geological information please visit the following web site:- ​

Parks and Wildlife ​

Antarctic Division​

Glyn Roberts​

April 2000. ​

References:

Selkirk P.M., Seppelt R.D. & Selkirk D.R., 1990, "Subantarctic Macquarie Island, Environment and Biology", Cambridge University Press.

Williamson P.E. 1988, "Origin, Structural and Tectonic History of Macquarie Island Region", Papers & Proceedings of the Royal Society of Tasmania, 122(1).
Duncan R.A. & Varne R. 1988, "The Age and Distribution of the Igneous Rocks of Macquarie Island", Papers & Proceedings of the Royal Society of Tasmania, 122(1).
Jones T.D. & McCue K.F. 1988, "The Seismicity and Tectonics of the Macquarie Island Ridge", Papers & Proceedings of the Royal Society of Tasmania, 122(1).
Pemberton M., Davidson G. & Burdon J. 1998," Macquarie Island, a New Arrival", Parks & Wildlife Service Publication, Hobart. Mineral Resources Tasmania 1998, "Geology of Macquarie Island, Maps".​

<TABLE style="WIDTH: 22em" class="infobox vcard" cellSpacing=5><TBODY><TR><TH style="TEXT-ALIGN: center; BACKGROUND-COLOR: #cef2e0" colSpan=2>Geography</TH></TR><TR><TH style="TEXT-ALIGN: left" scope=row>Coordinates</TH><TD>54°30S, 158°57E<SUP id=cite_ref-aad.gov.au_0-0 class=reference>[1]</SUP></TD></TR><TR><TH style="TEXT-ALIGN: left" scope=row>Area</TH><TD>128 km<SUP>2</SUP> (49.4 sq mi)</TD></TR><TR><TH style="TEXT-ALIGN: left" scope=row>Length</TH><TD>34 km (21.1 mi)</TD></TR><TR><TH style="TEXT-ALIGN: left" scope=row>Width</TH><TD>5 km (3.1 mi)</TD></TR><TR><TH style="TEXT-ALIGN: left" scope=row>Highest elevation</TH><TD>410 m (1,350 ft)</TD></TR><TR><TH style="TEXT-ALIGN: left" scope=row>Highest point</TH><TD>Mounts Hamilton and Fletcher</TD></TR><TR><TH style="TEXT-ALIGN: center; BACKGROUND-COLOR: #cef2e0" colSpan=2>Country</TH></TR><TR><TD style="TEXT-ALIGN: center" colSpan=2>Australia</TD></TR><TR><TH style="TEXT-ALIGN: center; BACKGROUND-COLOR: #cef2e0" colSpan=2>Demographics</TH></TR><TR><TH style="TEXT-ALIGN: left" scope=row>Population</TH><TD>No permanent inhabitants</TD></TR></TBODY></TABLE>

จุดศูนย์กลางแผ่นดินไหวครั้งนี้อยู่บริเวณหมู่เกาะแมควารี่ ตั้งอยู่ด้านทิศใต้ของประเทศนิวซีแลนด์แต่อยู่ในเขตปกครองของประเทศออสเตรเลีย

โซนนี้เป็นรอยต่อขอบแผ่นอินโดออสเตรเลียกับแผ่นแปซิฟิคแต่ไม่ใช่แนวมุดสอด เป็นแนวที่แผ่นเปลือกโลกเคลื่อนที่ผ่านกัน(tranform Plate Boundary) การศึกษาวิจัยของนักธรณีวิทยามหาวิทยาลัย Adelaide ประเทศออสเตรเลียรายงานว่าแผ่นแปซิฟิคเคลื่อนที่แนวตะวันตกเฉียงเหนือด้วยความเร็วประมาณ 8 มม.ต่อปี ส่วนแผ่นอินโดออสเตรเลียเคลื่อนที่แนวตะวันออกเฉียงเหนือด้วยความเร็วประมาณ 6 มม.ต่อปี แต่ Peter bird นักธรณีวิทยาของ USGS บอกว่าโซนนี้แผ่นอินโดฯเคลื่อนที่ด้วยความเร็วประมาณ 66 มม.ต่อปี แผ่นแปซิฟิคเคลื่อนที่ 56 มม.ต่อปี ทิศทางเดียวกันกับการศึกษาของมหาวิทยาข้างต้น

ในขณะเดียวกันโซนนี้ก็เป็นโซนที่แผ่นเปลือกโลกทั้งสองแผ่นเคลื่อนที่ออกจากกัน(divergent plate Boundary) ด้วย ทำให้เกิดแนวร่องลึก Macquarie Ridge พาดผ่านหมู่เกาะนี้โดยเกาะเหนือของหมู่เกาะอยู่ด้านทิศตะวันตกของร่องลึกส่วนเกาะใต้อยู่ด้านทิศตะวันออก การขยายตัวออกของแผ่นเปลือกโลกแนวนี้เป็นสาเหตุหลักที่ทำให้เกิดแผ่นดินไหวในโซนนี้

นอกจากที่กล่าวมาแล้วทางด้านทิศตะวันตกของจุดศูนย์กลางแผ่นดินไหวห่างออกไปประมาณ 730 กม.มีแนว Ocean Ridge ซึ่งเป็นแนวแยกตัวออกจากกันของแผ่นอินโดออสเตรเลียกับแผ่นแอนตาร์คติคทำให้เกิดแรงผลักแผ่นเปลือกโลกออกสองข้างของแนวแยกตัวออกจากกัน อีกแนวหนึ่งด้วย

จากผลการของเคลื่อนที่ผ่านกันและแรงผลักของแนว Ridge ทั้งสองแนวข้างต้น ทำให้เกิดแผ่นดินไหวในโซนนี้ต่อเนื่องมาโดยตลอด

 

แผ่นดินไหวในพม่า

กรณีศึกษา Myanmar earthquake of March 24, 2011 - Magnitude 6.8 เปรียบเทียบการไหววันนี้
When continents collide, there are far-reaching consequences. A magnitude 6.8 earthquake struck eastern Myanmar, near the border with Thailand and Laos, at a depth of 10 km, at 20:25 local time (13:55 UTC) on Thursday, March 24th, 2011. As of Sunday, March 27, the death toll had reached 104. There is no evidence that this earthquake is related to recent earthquakes in Japan. Rather, the earthquake in Myanmar occurred on an active fault that is part of a broad zone of deformation resulting from the collision of the Indian subcontinent with the Eurasian landmass.
The most dramatic manifestations of the collision of India with Asia are the Himalaya, the tallest mountain range in the world, and the Tibetan Plateau, the tallest and largest plateau in the world. However, the effects don't stop there; this collision has been forcing blocks of the Eurasian landmass toward the east-southeast for over 35 million years. Thus active earthquake faults riddle not only the Himalaya and Tibetan Plateau, but also regions far to the north and east, toward Mongolia and Beijing, and also to the southeast, through Sichuan and Yunnan into Myanmar, Thailand, Vietnam, and Laos. (Figures 1 and 2


Figure 1. Map of the regional tectonic setting of the March 24th Tarlay (Myanmar) earthquake (Figure modified from Tapponnier and others, 1982). The red dot within the white square shows the location of the earthquake. The white square outlines the area shown in Figure 3.

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Figure 2. Animation showing the tectonic evolution of India and Asia over the past 50 million years. (Produced in 2002 by Prof. Paul Tapponnier and a team from the French Centre National de la Recherch Scientifique for the exhibition "Himalaya-Tibet: Le Choc de Continent" at the Muséum National d'Histoire Naturelle in Paris. Based on the work published in Replumaz and Tapponnier, 2003.)
Zooming closer in to eastern Myanmar and northern Thailand and Laos, we find the crust* of the Earth behaving a bit like a stack of books that is toppling over on a shelf (Figures 3, 4, and 5). Unlike subduction zones where one plate dives under another, in this region the rocks on either side of the earthquake faults are sliding side-to-side as India continues is northward voyage. Side-to-side motion along two major earthquake faults, the Sagaing Fault in Myanmar and the Red River fault in Vietnam and Yunnan (Figure 1), is accomodating both of the northward motion of India and the southeasterly motion of China. In between these two major faults, the Earth's crust is broken into a series of blocks that are slowly rotating clockwise as a result. The edges of the blocks themselves are faults; it appears that the March 24th earthquake occurred on one of these faults, the Nan Ma fault (as mapped by Le Dain and others, 1984, and Lacassin and others, 1998; Figure 4).


Figure 3. (Click the image for a higher-resolution version.) Location map of Tarlay (Myanmar) earthquake of March 24th. The northward motion of India, shown as the largest white arrow at about 40 millimetres per year, is causing motion on the Sagaing and Red River Faults (this relative motion is shown by the smaller white arrows). The motion on these major faults is driving motion on a series of faults in between, including the Nan Ma fault where the earthquake occurred. An analogy of this fault motion is shown in Figure 5. The white square indicates the area shown in Figure 4. Figure modified from Tapponnier and others (2001).


Figure 4. (Click the image for a higher-resolution version). Map of the local tectonic setting of the March 24th Mong Hpayak (Myanmar) earthquake. The earthquake epicentre is shown by the red star; the portion of the Nam Ma fault that is likely to have slipped in the earthquake is shown by the red line. The two white arrows show where the Mekong River has been offset (shifted) by 12 km over the past few million years by motion on the Nan Ma Fault. The areas shaded in yellow are extensional sedimentary basins.


Figure 5. Analogy of the style of deformation in the region around the March 24th Tarlay (Myanmar) earthquake. Motion along the major Sagaing and Red River faults has caused the crust in between to deform as rotating blocks, as when a row of books topples over to the side on a shelf. A series of left-lateral faults slip in between the blocks; the Nan Ma Fault is one of these faults. This mechanism is aptly called "bookshelf faulting." For reference, the Sagaing Fault runs roughly north-south.

Over the past few million years, motion on the Nan Ma Fault has offset (shifted) the Mekong River by 12 kilometres (Figure 4, between the two white arrows; see Lacassin and others, 1998). This 12-km offset would not have occurred smoothly, nor all at once, but rather in a series of small jumps as earthquakes periodically caused the rocks to shift. Imagine travelling in a boat down the Mekong River as you approach this fault from the north; once you reach the fault, you would turn left to follow the river. For this reason, we call these kinds of faults "left-lateral" faults, meaning that if you stand on one side of the fault, it looks like land on the other side has shifted to the left.

Based on inital estimates of the earthquake location, it appears likely that the earthquake was caused by motion on the western segment of the Nan Ma Fault. The direction of motion inferred from seismograph readings is also consistent with the left-lateral motion that is typical of this fault. We do not yet know how much the rocks may have slipped in the March 24th earthquake, nor do we know for sure whether the fault actually broke to the surface. Other earthquakes on similar faults at similarly shallow depths (10 km) and similar magnitude (6.8) are typically accompanied by a couple of metres of slip at the surface over a segment of the fault a few tens of kilometres long. Field study at the site of this earthquake would shed important new light on the nature of this earthquake.

There is no evidence to connect earthquakes that occur far apart on the Earth, such as this earthquake and the Tohoku (Japan) earthquake of March 11th. There are cases, however, of earthquakes on one portion of a fault increasing the stresses on other portions of the fault and on closely neighbouring faults. This earthquake in Myanmar likely increased stresses on the eastern part of the Nan Ma Fault. Unfortunately, we don't have enough information about these faults to say whether the earthquake hazard has changed in neighbouring areas. Scientists from the Earth Observatory of Singapore are currently undertaking projects, both at a regional scale and in western Myanmar, Nepal, India/Bangladesh, and China, to learn more about the earthquake faults associated with the great collision of India and Asia. These faults have been much less well-studied than faults in areas such as Japan and California, yet can be at least as devastating, as the 2008 Wenquan (Sichuan) earthquake (Figure 3) showed all too clearly.




Figure 6: Left lateral offset of paddy boundaries caused by slippage of the Nam Ma fault during the earthquake of March 24th. Photo courtesy of Soe Thura Tun of the Myanmar Earthquake Committee.



* It is actually the lithosphere of the Earth that is involved in fault and plate motions, which includes the crust and the very uppermost part of the mantle. We use the term "crust" in this article because it is more widely understood.


References:
Lacassin, R., Replumaz, A., Leloup, P. H., 1998, Hairpin river loops and slip-sense inversion on southeast Asian strike-slip faults, Geology, 26, 703.
Le Dain, A. Y., Tapponier, P., and Molnar, P., 1984, Active faults and tectonics of Burma and surrounding regions, Journal of Geophysical Research, 89, 453.
Replumaz A. and P. Tapponnier, Reconstruction of the deformed Collision Zone between India and Asia by backward Motion of Lithospheric Blocks, Journal of Geophysical Research, vol. 108, N°B6, 2285, 2003.
Tapponnier, P., Peltzer, G., Le Dain, A. Y., Armijo, R., and Cobbold, P., 1982, Propagating extrusion tectonics in Asia: New insights from simple experiments with plasticine, Geology, 10, 611.
Tapponnier P. , Xu Zhiqin, F. Roger, B. Meyer, N. Arnaud, G. Wittlinger, Yang Jingsui, Oblique, Stepwise Rise and Growth of the Tibet Plateau, Science, vol 294, pp. 1671-1677, 2001

 

Update time = Fri Jun 22 10:03:17 UTC 2012

<TABLE border=0 cellSpacing=1 cellPadding=1><TBODY><TR><TH></TH><TH align=middle>MAG </TH><TH align=middle>UTC DATE-TIME
y/m/d h:m:s
</TH><TH align=middle>LAT
deg
</TH><TH align=middle>LON
deg
</TH><TH align=middle>DEPTH
km
</TH><TH>Region</TH></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>3.8 </TD><TD vAlign=top noWrap align=middle>2012/06/22 09:16:04 </TD><TD vAlign=top noWrap align=right>-34.229 </TD><TD vAlign=top noWrap align=right>148.713 </TD><TD vAlign=top noWrap align=right>10.0 </TD><TD vAlign=top>NEW SOUTH WALES, AUSTRALIA</TD></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>5.1 </TD><TD vAlign=top noWrap align=middle>2012/06/22 07:58:43 </TD><TD vAlign=top noWrap align=right>39.406 </TD><TD vAlign=top noWrap align=right>143.509 </TD><TD vAlign=top noWrap align=right>19.1 </TD><TD vAlign=top>OFF THE EAST COAST OF HONSHU, JAPAN</TD></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>4.8 </TD><TD vAlign=top noWrap align=middle>2012/06/22 07:50:17 </TD><TD vAlign=top noWrap align=right>56.773 </TD><TD vAlign=top noWrap align=right>-152.954 </TD><TD vAlign=top noWrap align=right>15.0 </TD><TD vAlign=top>KODIAK ISLAND REGION, ALASKA</TD></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>3.7 </TD><TD vAlign=top noWrap align=middle>2012/06/22 06:01:28 </TD><TD vAlign=top noWrap align=right>18.883 </TD><TD vAlign=top noWrap align=right>-68.750 </TD><TD vAlign=top noWrap align=right>170.0 </TD><TD vAlign=top>DOMINICAN REPUBLIC</TD></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>3.0 </TD><TD vAlign=top noWrap align=middle>2012/06/22 05:37:15 </TD><TD vAlign=top noWrap align=right>38.011 </TD><TD vAlign=top noWrap align=right>-111.086 </TD><TD vAlign=top noWrap align=right>0.3 </TD><TD vAlign=top>UTAH</TD></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>3.2 </TD><TD vAlign=top noWrap align=middle>2012/06/22 05:23:58 </TD><TD vAlign=top noWrap align=right>17.890 </TD><TD vAlign=top noWrap align=right>-64.110 </TD><TD vAlign=top noWrap align=right>38.0 </TD><TD vAlign=top>VIRGIN ISLANDS REGION</TD></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>4.9 </TD><TD vAlign=top noWrap align=middle>2012/06/22 05:22:40 </TD><TD vAlign=top noWrap align=right>-17.822 </TD><TD vAlign=top noWrap align=right>167.720 </TD><TD vAlign=top noWrap align=right>35.2 </TD><TD vAlign=top>VANUATU</TD></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>4.8 </TD><TD vAlign=top noWrap align=middle>2012/06/22 05:14:46 </TD><TD vAlign=top noWrap align=right>1.213 </TD><TD vAlign=top noWrap align=right>92.476 </TD><TD vAlign=top noWrap align=right>30.6 </TD><TD vAlign=top>OFF THE WEST COAST OF NORTHERN SUMATRA</TD></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>5.1 </TD><TD vAlign=top noWrap align=middle>2012/06/22 05:02:07 </TD><TD vAlign=top noWrap align=right>-32.832 </TD><TD vAlign=top noWrap align=right>-178.340 </TD><TD vAlign=top noWrap align=right>10.0 </TD><TD vAlign=top>SOUTH OF THE KERMADEC ISLANDS</TD></TR><TR><TD vAlign=top noWrap align=middle>MAP</TD><TD vAlign=top noWrap align=middle>2.7 </TD><TD vAlign=top noWrap align=middle>2012/06/22 04:45:42 </TD><TD vAlign=top noWrap align=right>18.922 </TD><TD vAlign=top noWrap align=right>-67.715 </TD><TD vAlign=top noWrap align=right>20.0 </TD><TD vAlign=top>PUERTO RICO REGION</TD></TR></TBODY></TABLE>

 

Land Slide By USGS

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[Music]

Peter Lyttle: Almost every citizen in the United States could potentially experience a landslide.

Types of Landslides

Peter Lyttle: Landslides come in quite a few different flavors, and even with our small group of 20 here at the USGS, we have some of the world experts in each of the different kinds of landslides. There are very slow-moving, deep-seated landslides, which don’t threaten lives too often, but they can do a huge amount of damage to property. If you imagine your house slowly moving down a hill. We have very fast moving landslides, which are a danger to human beings. These are called debris flows. These move at 30 miles an hour, and if you imagine sort of a consistency of concrete with huge boulders in it rushing at you at 30 miles an hour, you’re not going to get out of the way. These kill a few people around the world every year. And finally there are rock falls, which probably are the kind of landslide that most people are familiar with, when huge boulders fall off of a cliff along the side of a highway and smash a car.

USGS Science

Sue Cannon: Within the Landslides Hazards Program we have three specific tasks. One is developing tools and methodologies that can be used to characterize landslide hazards. The second is to respond to landslide disasters, to provide expertise and assessments. And then the third is outreach to try to educate the public about landslides and landslide hazards as best we can.

Details

Title: Landslide Hazards

Description:
Landslides occur in all 50 states and U.S. territories, and cause $1-2 billion in damages and more than 25 fatalities on average each year. USGS scientists aim to improve our understanding of landslide hazards to help protect communities and reduce associated losses.


Video Sections:

• Types of Landslides
• USGS Science
• Did You See It?
• Debris Flow Early Warning System (NOAA Partnership)
• Tips for Homeowners
• Conclusion

Location: Washington, DC, USA
Date Taken: 6/11/2012
Length: 6:12
Video Producer/Videographer: Don Becker (U.S. Geological Survey)
Note: This video has been released into the public domain by the U.S. Geological for use in its entirety. Some videos may contain pieces of copyrighted material. If you wish to use a portion of the video for any purpose, other than for resharing/reposting the video in its entirety, please contact the Video Producer/Videographer listed with this video.
Additional Video Credits:
Video Credits:
David Applegate (USGS)
Sue Cannon (USGS)
Lynn Highland (USGS)
Peter Lyttle (USGS)
Maureen O’Leary (NOAA)
Pedro Restrepo (NOAA)
Chris Vaccaro (NOAA)
Producers:
Don Becker
Heidi Koontz
Clarice Nassif Ransom
Jessica Robertson

Source:
Visit the USGS Landslide Hazards Program websitefor more information.

File Details:

• Quicktime (MP4 Video - 51.52 MB)
• Flash Video (FLV File - 28.89 MB)
  • W3C Timed-Text captions file (XML Document - 7.55 KB)
  • Text transcript (Text Document - 4.03 KB)
• YouTube version

 

โรงเรียนภาษา / 67 - ANSWERS OF AN ALIEN FROM ANDROMEDA - Nibiru - Elenin - Events

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Uploaded by atlanticobr on Oct 18, 2011

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Answers of an alien from Andromeda -- video sixty seven - October 18, 2011. Atlantic Time.