4/25/2015 Nepal Quake

4/25/15 Nepal Quake

updated 5/15/15

The 7.8 Magnitude earthquake hit Nepal April 25, 2015 at 06:11 UTC (11:11 AM local time).  The epicenter was 50 miles NW of Kathmandu. It was the worst quake in Nepal in 81 years.  Over 8,000 have been confirmed dead, over 11,000 injured, 450,000 internally displaced and over 100,000 have been left homeless.  Many older buildings were destroyed.  Some modern buildings seem to have fared better. However a number of newer buildings have been built quickly without regard to building codes. These buildings have not stood up so well to the quake.   In the countryside, many areas are were cut off by landslides and avalanches.  Reports that have been received from villages suggest widespread devastation with most of the buildings destroyed by the quake or the landslides that followed. Resources are stretched thin as the government struggled to rescue survivors and provide aid. Rebuilding will take a long time due to the extent of the damage

Areas that are normally a 2 or 3 days trip from Kathmandu were completely cut off for days.  The army was mobilized to help in the rescue effort. International relief is being flown into the country. The airport was been closed intermittantly due to aftershocks. As is usual for a quake of this size, there have been frequent aftershocks.

On May 12, 2015 the worst aftershock yet with 7.3 Magnitude hit at 7:05 UTC (12:35 pm local time). Its epicenter was 50 miles east of Kathmandu.  The USGS classified the second quake as an aftershock because it occurred right at the eastern edge of the slip zone of the original quake.  At least 48 people were killed in Nepal from this second quake and possibly another 17 in India, according to the BBC.

An avalanche on Mt Everest killed 18 people at the 18,000 ft high Base Camp, where climbers begin the climb.  Survivors are being airlifted off the mountain.  Over 100 climbers were stranded above the avalanche. Helicopters were able to rescue them from Camp 1 at 20,000 ft.

Seismic activity in this area is driven by the same forces that raised the Himalaya mountains.  This area is feeling the effects of the collision between the Indian tectonic plate and the Eurasian plate. (See the Plate Tectonics page for more information on this process).  Over the past few millions of years the Indian plate traveled across the Indian Ocean, finally slamming into Eurasia with enough power to crumple the landscape and push the Himalaya mountains 5 miles above sea level.  This collision is still occurring. Stresses in the earth's crust continue to produce earthquakes. See the USGS report on the original quake. And the USGC report of the major aftershock of May 12.

Earthquakes are the result of pressure building up at a fault. When one section of the fault ruptures, it relieves the pressure in that section but can increase pressure in a neighboring section that didn't move.  That leads to a subsequent quake to relieve that pressure.  It can take many years for this to happen. The previous large quake in this area was in 1934 to the east of both of these recent quakes. The May 12 aftershock was located between the 1934 quake and the April 25 one, which increased the pressure likely triggering the May 12 shock.

News Stories about the quake:

Nepal Earthquake fears grow for remote villages as over 4,000 confirmed dead (The Guardian 4/27/2015)
Villages near the Nepal earthquake epicenter are desperate as death toll tops 4,000 (New York Times 4/27/2015)
A scene of destruction after ice thunders into Everest Base Camp (New York Times (April 27, 2015)
Nepal Earthquake Happened Right on Schedule, Scientists Say (Huffington Post April 27, 2015)
Fallen: Nepals Historic Landmarks After the Quake (CNNApril 27, 2015)
Nepal Earthquake Death Toll Hits 5,000 as Aid Starts Flowing (NBC 4/28/15)
Dozens die in new tremor near Everest (BBC 5/12/15)

8/3/14 Wenping China Quake

Updated 8/3/14

The 6.1 M quake struck at 08:30 UTC (4:30 PM Local Time) 8/3/14. The epicenter was near Wenping, 18 mi from Zhaotong in Yunnan province. This area is at the base of the Himalayas, in Southwestern China.

News reports put the death toll at 367, with 1300 injured. Over 12,000 buildings have collapsed and 30,000 were damaged. People ran into the street when the quake struck.  Rescuers worked with shovels in their search for survivors.  The government is sending at least 2,000 tents, cots, coats and quilts. Communication with the affected area has been hampered because electricity and phone lines have been damaged. The area has been hit with thunderstorms and landslides that have made the rescue efforts more difficult.

This quake struck  in an area to the east of the Himalayas. Seismic activity in this area is driven by the same forces that raised the mountains.  This area is feeling the effects of the collision between the Indian tectonic plate and the Eurasian plate. (See the Plate Tectonics page for more information on this process).  Over the past few millions of years the Indian plate traveled across the Indian Ocean, finally slamming into Eurasia with enough power to crumple the landscape and push the Himalaya mountains 5 miles above sea level.  This collision is still occurring. Stresses in the earth's crust continue to produce earthquakes, some of them much larger than this one. See the USGS report on this quake.

Here are some news stories:

Chinese earthquake kills hundreds in Yunnan province (BBC 8/3/14)

Strong earthquake kills at least 367 in southern China (KING 5 8/3/14)

10/15/13 Philippines Quake

Updated 10/16/13

A 7.2M quake hit the Philippines on Tuesday, October 15, 2013 at 8:10 AM local time. The epicenter was near the city of Tagbilaran on the island of Bohol in the central Philippines. The worst damage as on the islands of Bohol and Cebu. There were panicked crowds trying to get out of buildings during the quake. One stampede on Cebu injured 19 people and killed a 4 year old girl. There was extensive damage, with many building damaged or destroyed. Among the damaged buildings were several historic churches, at least one of which, the Church of San Pedro in Loboc dating from 1602, had its roof collapse.   144 people have been confirmed dead and 291 injured. Cracks appeared in roads and power was out in the most affected area.  Authorities warned residents not to enter damaged buildings for fear that aftershocks could cause more damage.  Port facilities, and airport control tower were also damaged and closed while safety inspections were conducted.

The Philippines is a very active area seismically. Several tectonic plates jostle each other in this area, including the Philippines Plate, Sunda Plate, Pacific Plate and Eurasian Plate. A 6.8M quake hit the nearby island of Negros on 2/6/2012.  7.2M is a strong quake but by no means the strongest possible in this area. In 1948 an 8.1M quake hit not far away. See thePlate Tectonics Page for more on the processes involved.  The US Geological Survey (USGS) is an invaluable resource in understanding and tracking earthquakes. See the USGS report on this quake.

See these news stories about this quake:



9/24/2013 Pakistan Quake

On Tuesday September 24, 2013 at 16:29 UTC (9:29 PM local time) Southwestern Pakistan was hit by a 7.7M quake. The epicenter was 39 miles from the city Awaran in Bolochistan. This quake was followed two days later with a 6.8M quake in the same area. The quake was felt at far away as Delhi and Karachi.

366 people were killed in the first quake with another 7 dead from the second. Over 700 were injured. An estimated 21,000 buildings were destroyed. Relief efforts were hindered by the remoteness of the area with poor communications. There is also a separatist movement that hinders government access. There was a report that a government helicopter assessing damage was fired upon by separatists. Off the coast, a new rocky island was formed as the quake lifted the seafloor.

Survivors were afraid to stay inside hospital or other buildings, after the second quake in temperatures as high as 100ºF with little food, water or shelter.

These quakes occurred near the intersection of three tectonic plates, the Indian Plate to the east, the Arabian Plate to the west and the Eurasian plate to the north. Both the Indian and Arabian plates are moving northwards relative to the Eurasian plate at different rates. Although these complex plate movements lead to frequent small quakes, there has not been one this big in over 40 years. (See the Plate Tectonics page for more information on these processes.) The US Geological Survey (USGS) is an invaluable resource in understanding and tracking earthquakes. See the USGS summary of this quake 

News Reports:

New earthquake strikes hard-hit Pakistan (CNN 9/28/13)

Quake kills 45 in Pakistan creates new island in sea (Reuters 9/24/13)

11/7/2012 Guatemala Quake


Updated 11/7/2012

A 7.4M earthquake hit Guatemala at 16:35 UTC on 11/7/2012.  The epicenter was located in the Pacific Ocean 107 miles WSW of Guatemala City. It was felt as far away as Mexico City, 765 miles away, where office workers evacuated some skyscrapers. 

At least 39 people were killed in San Marcos state and Quetzaltenango, with 224,000 inhabitants the country's second largest city.  The worst hit area was in the mountains near the Mexican border, where buildings collapsed and landslides blocked roads. Rescuers  worked to rescue people buried in the debris.

In this area the Cocos tectonic plate is being forced under the neighboring North American and Caribbean plates near the intersection of the three plates of the the earth's crust. This quake was bigger than the 1983 7.1M quake in the same location almost 30 years ago, and bigger than anything in this area since.  A 7.5 M Quake killed 20,000 people in Guatemala in 1975. See The Earthquake Museum Plate Tectonics Page  for more on the root causes of earthquakes.  The US Geological Survey (USGS) is an invaluable resource in understanding and tracking earthquakes. See the USGS summary of this quake. This page now includes an interactive map, including plate boundaries. Zoom out all the way to see the whole earth with all the plates shown.

See also the following news stories:

8/11/2012 North Iran Quakes


Updated 8/12/2012

Northern Iran was hit with a 6.4 M earthquake at 12:23 UTC (4:53 PM local time) 8/11/2012. It was followed 11 minutes later with a 6.3 M quake at 12:34 UTC (5:04 PM local time). The epicenters of the two quakes were just 6 miles apart. The first quake's epicenter was 15 miles from the small city of Ahar and 36 miles from  Tabriz, Iran. This area is about 350 miles NW of Teheran, 180 miles SE of the Armenia capital Yerevan and 200 miles NE of Mosul, Iraq. This area is located on the southern edge of the Caucasian Peninsula between the Black Sea and the Caucasian Sea.

300 people have been reported dead, with over 5,000 injured in the two quakes.  The injuries were due to collapsed buildings. Aftershocks continue to keep people worried. The government has advised people to camp outdoors due to the danger that building that have been weakened by the quakes could collapse in an aftershock. Even in Tabriz, which did not sustain much damage, many people spent the night outside. Hospitals in the area are crowded with long lines of survivors needing treatment.  Roads to the affected area are crowded with people coming in to help in rescue efforts and survivors trying to get out. With transportation limited, it is difficult to get food, water and medical supplies to those in need. The Red Crescent has distributed 44,000 food packets and 5,600 tents. 36,000 people have been given emergency shelter. There are 1,000 small villages in the affected area, some of which have not been reached by rescue and relief crews.  The Iranian government announced Sunday evening that they did not expect to find more survivors and turned instead to  relief efforts.  Iran is subject to large quakes frequently and set up to respond quickly when they occur. The government explained that due to the small size of most of the damaged buildings and the sparse population, they were able to ascertain quickly that there were no more survivors in the rubble.

Tabriz is a city of 1.4 million  located in northeast corner of the country. It is the fourth largest city in Iran and an industrial and cultural center.  It is in a mountainous area at an elevation of 4,200 feet. The area affected by the quake is rural, comprised of small villages scattered over a wide area in the mountains.

Buildings in Tabriz came through the quakes without much damage but outside the city, construction relies on unreinforced masonry and concrete blocks that are cheap to build but very vulnerable to earthquake damage.  Worldwide, most earthquake damage, and casualties, is to this type of building. 

The two quakes had distinct epicenters so the second one was not considered and aftershock. It seems likely that the shock of the first triggered the second section of fault, which was also due to give way. These quakes are similar to last year's quake in eastern Turkey, about 200 miles to the west of these quakes. In this area the Arabian Plate is pushing northward into the Eurasian Plate, raising the Caucasus mountains to the north. It is causing stress in the surrounding crust as it is squeezed between these two plates and the Anatolian Plate, which is itself being squeezed between the African and Eurasian Plates. This earthquake is not located on a tectonic plate boundary  but the whole area is stressed due to the interactions between the surrounding plates. See The Earthquake Museum Plate Tectonics Page  for more on the root causes of earthquakes.  The US Geological Survey (USGS) is an invaluable resource in understanding and tracking earthquakes. See the USGS summary of this quake. This page now includes an interactive map, including plate boundaries. Zoom out all the way to see the whole earth with all the plates shown.

See also the following news stories:

5/20/12-5/29/12 Italy Earthquakes


Updated 5/31/12

Northern Italy felt a 6.0M quake on 5/20/12 followed by a   5.8M quake on 5/29/12 at 10:55 UTC (12:55 PM local time). The epicenter was in the Emilia Romagna region near Cavezzo, about 30 miles NW of Bologna.  The first quake killed 7 people and in the second 17 people died and 350 were injured. 14,000 are now homeless. Some of the victims were from a factory that had just been declared safe after the first quake. The quake was felt in Bologna, Milan, Venice and as far away as the Austrian border.

Many historic buildings collapsed but most modern buildings survived. The government is investigating whether building codes were followed with some of the modern buildings that did collapse.

Earthquakes in this region are generally due to stresses that accumulate as the African Plate moves northward, colliding with the Eurasian Plate.  This is the collision that is raising the Alps.  See the Plate Tectonics Page for more on the processes involved.  The US Geological Survey (USGS) is an invaluable resource in understanding and tracking earthquakes. See the USGS summary of this quake.


See also the following news stories: