Posts
Sunday, May 9, 2010
Early this AM another aftershock 5.0 May 9, 2010
Our Bio-Bio region of Chile experienced another aftershock early today, 6:45 AM local time. This was reported by the USGS as a 5.0 magnitude. We didn't have any damages at our place.
Tuesday, May 4, 2010
New Strong 6.4 Aftershock on May 3, 2010
We felt another strong aftershock in our home in the Chile region of Bio-Bio at 7:10 last evening. This one measured 6.4 magnitude on the Richter Scale.
Monday, May 3, 2010
Sunday Morning - Another Strong Aftershock May 2, 2010
We experienced another strong aftershock on Sunday morning at 10:53 AM local time .... a 5.8 magnitude. This one caused a gentle, slow, back and forth movement of our entire home, and it was not even in our Bio-Bio region of Chile! It was to the north in the Maule region, but still scary here.
Thursday, April 29, 2010
Two New Aftershocks this Morning - April 29, 2010
We have felt two new aftershocks this morning - the first one was at 0356 AM local time here in Chile and was a 5.1 magnitude, the next one was at 0940 AM local time and measured 4.9. We felt both of these at our home in the Bio-Bio region near Chillan, just some shaking and rattling but thankfully no damage! The more recent 4.9 aftershock actually felt stronger because the epicenter was only about 25 miles from our home.
Friday, April 23, 2010
UPDATE - USGS Reports the Latest Aftershock was 6.1 Magnitude
USGS has just reported this latest strong aftershock was a 6.1 magnitude that happened about 20 minutes ago.
Another Strong Aftershock at 6:03 in Bio-Bio Region Chile April 23, 2010
This one was pretty strong. Our whole house shook, chairs starting moving, house plants were shaking. The preliminary USGS report says it was a 6.0 magnitude.
Wednesday, April 21, 2010
USGS Reported Another Aftershock in the Bio-Bio Region of Chile Aoril 21, 2010
The U.S. Geological Survey (USGS) reported another aftershock in our Bio-Bio region of Chile during the night just minutes before midnight at 23:52 local time that measured 4.7 on the Richter scale. No damage was reported in our area. Aftershocks in Chilean Spanish are called "replicas".
Monday, April 19, 2010
April 19, 2010 Another Aftershock this Morning
About 3:30 this morning there was another aftershock of 5.0 magnitude felt in the Bio-Bio region of Chile. There were no reported damages anywhere.
Sunday, April 18, 2010
More Aftershocks 18 Apr. 2010 at 0149UTC in BioBio Chile
We felt another aftershock from the recent big earthquake last evening, this time a 5.1 magnitude, about 9:49 PM local time here in Chile in the Bio-Bio Region near Chillan where we live. No damage....we just felt the slow back and forth movement of our solid brick and concrete home.
Saturday, April 17, 2010
Could Volcanic Eruptions Follow Chile's Earthquake? Experts Say "Yes"
We live almost directly on a line between the recent 8.8 massive Chile earthquake in the Bio-Bio region of Chile and the Chillan Volcano, or Volcán Chillán - also known as Nevados de Chillán. And this article indicates that volcanoes are more likely to be active within the next 12 months, especially volcanoes within a 500 km. radius of the epicenter of the big earthquake. From our home, we have a clear view of this Volcano.
According to Oxford University volcanologist, David Pyle, Chile's magnitude 8.8 earthquake may be a prelude to a series of volcanic explosions. "We expect to see an upsurge in volcanic activity over the next 12 months," said Pyle.
In his notebooks of the voyage of the HMS Beagle, Charles Darwin noted the link between large earthquake off Chile's coastline in February 1835 which resurrect previously inactive volcanoes, and cause active ones to increase their eruption rates: "The papers will have told you about the great Earthquake of the 20th of February. I suppose it certainly is the worst ever experienced in Chili (sic). It is no use attempting to describe the ruins--it is the most awful spectacle I ever beheld. The town of Concepcion is now nothing more than piles and lines of bricks, tiles and timbers-- it is absolutely true there is not one house left habitable."
Last year, Pyle and his colleagues found that after a magnitude 8.3 in 1906 and a magnitude 9.5 earthquake in 1960, there were three or four more volcanic eruptions within about 500 kilometres of the epicentre in the following year than would normally be expected.
Chaiten1
Last week's earthquake occurred on the same section of fault that caused the earthquake Darwin observed in 1835. "We'll be using satellite measurements of heat and deformation to keep an eye on the entire arc of volcanoes, from Llaima in the south to Tupungatito in the north," said Pyle.
The image above shows a plume of ashes spewed by the Chaiten volcano as seen from the city of Chaiten, 1,200km south from Santiago, Chile on May 5, 2008 -its first activity in over 9,000 years.
The image below shows local residents are helped to board during evacuation operations following the eruption of the Chaiten volcano, in the locality of Chaiten on May 2, 2008. About 1,500 people had to be evacuated after the eruption, which caused a red alert in neighbouring regions of Chile and Argentina.
Pyle and Oxford University colleagues studied the massive Chaitén volcano in southern Chile that began to erupt explosively on 2 May 2008 -the biggest volcanic eruption in almost 20 years. The study showed that the impact of past eruptions is likely to have been significantly underestimated as so much of the evidence quickly disappears, For six days afterwards the volcano pumped huge volumes of ash high into the atmosphere before its activity began to decline to a low intensity eruption
"The area around a volcano immediately after an eruption is like a crime scene where the evidence can quickly be destroyed by the elements,’ said Pyle of Oxford University’s Department of Earth Sciences. ‘Ash deposited on land will rapidly be removed by rain or wind, while ash deposited out to sea is only accessible by collecting core samples of the sea-floor sediment. This makes it extremely difficult for volcanologists to accurately reconstruct a past eruption from the available evidence and say how much fine ash was deposited, and over what area, during an eruption.’
Chaiten3 The team’s work on Chaitén has shown that the several millimetres thickness of ash deposited across Argentina have been lost from wide areas – of at least 50,000 square kilometers – in only nine months. A geologist attempting to map the region affected by ash fallout now would significantly underestimate the size of the area affected, and as a result would underestimate the size of the eruption and the amount of ash erupted.
‘By using satellite imagery to guide us, we were able to map the ash fallout across Argentina to a thickness of less than one tenth of a millimetre,’ said Sebastian Watt, a PhD student in Oxford’s Department of Earth Sciences, who led the team. ‘We collected samples from over 220 sites across an area of 100,000 square kilometres and with these field data and samples we were able to make the first scientific assessment of the size and impact of the eruption.’
The Chaitén eruption had immediate social and economic impacts across Patagonia (southern Chile and Argentina), with more than 5,000 people evacuated from settlements up to 75 km from the volcano, and extensive ash deposition leading to regional disruption of agriculture and aviation. The volcano was not routinely monitored, and there was no recognised warning before the eruption started.
The Andes Mountains along the western coastline of South America include numerous active steep-sided, cone-shaped stratovolcanoes. The majority of these volcanoes were formed and are still fed by magma generated as the Nazca tectonic plate under the southeastern Pacific Ocean moves northeastward and plunges beneath the South American continental plate—a process known as subduction. The Nazca plate is the source of last week's earthquake. The line of Andean volcanoes marks the approximate location of the subduction zone.
This astronaut photograph (below) highlights two volcanoes located near the southern boundary of the Nazca–South America subduction zone in southern Chile. Dominating the scene is the massive Minchinmávida Volcano (image upper right). Charles Darwin observed an eruption of this glaciated volcano during his Galapagos Islands voyage in 1834; the last recorded eruption took place the following year. When this photo was taken, the white, snow-covered summit of Minchinmávida was blanketed by gray ash erupted from its much smaller but now-active neighbor to the west, Chaitén Volcano.
According to Oxford University volcanologist, David Pyle, Chile's magnitude 8.8 earthquake may be a prelude to a series of volcanic explosions. "We expect to see an upsurge in volcanic activity over the next 12 months," said Pyle.
In his notebooks of the voyage of the HMS Beagle, Charles Darwin noted the link between large earthquake off Chile's coastline in February 1835 which resurrect previously inactive volcanoes, and cause active ones to increase their eruption rates: "The papers will have told you about the great Earthquake of the 20th of February. I suppose it certainly is the worst ever experienced in Chili (sic). It is no use attempting to describe the ruins--it is the most awful spectacle I ever beheld. The town of Concepcion is now nothing more than piles and lines of bricks, tiles and timbers-- it is absolutely true there is not one house left habitable."
Last year, Pyle and his colleagues found that after a magnitude 8.3 in 1906 and a magnitude 9.5 earthquake in 1960, there were three or four more volcanic eruptions within about 500 kilometres of the epicentre in the following year than would normally be expected.
Chaiten1
Last week's earthquake occurred on the same section of fault that caused the earthquake Darwin observed in 1835. "We'll be using satellite measurements of heat and deformation to keep an eye on the entire arc of volcanoes, from Llaima in the south to Tupungatito in the north," said Pyle.
The image above shows a plume of ashes spewed by the Chaiten volcano as seen from the city of Chaiten, 1,200km south from Santiago, Chile on May 5, 2008 -its first activity in over 9,000 years.
The image below shows local residents are helped to board during evacuation operations following the eruption of the Chaiten volcano, in the locality of Chaiten on May 2, 2008. About 1,500 people had to be evacuated after the eruption, which caused a red alert in neighbouring regions of Chile and Argentina.
Pyle and Oxford University colleagues studied the massive Chaitén volcano in southern Chile that began to erupt explosively on 2 May 2008 -the biggest volcanic eruption in almost 20 years. The study showed that the impact of past eruptions is likely to have been significantly underestimated as so much of the evidence quickly disappears, For six days afterwards the volcano pumped huge volumes of ash high into the atmosphere before its activity began to decline to a low intensity eruption
"The area around a volcano immediately after an eruption is like a crime scene where the evidence can quickly be destroyed by the elements,’ said Pyle of Oxford University’s Department of Earth Sciences. ‘Ash deposited on land will rapidly be removed by rain or wind, while ash deposited out to sea is only accessible by collecting core samples of the sea-floor sediment. This makes it extremely difficult for volcanologists to accurately reconstruct a past eruption from the available evidence and say how much fine ash was deposited, and over what area, during an eruption.’
Chaiten3 The team’s work on Chaitén has shown that the several millimetres thickness of ash deposited across Argentina have been lost from wide areas – of at least 50,000 square kilometers – in only nine months. A geologist attempting to map the region affected by ash fallout now would significantly underestimate the size of the area affected, and as a result would underestimate the size of the eruption and the amount of ash erupted.
‘By using satellite imagery to guide us, we were able to map the ash fallout across Argentina to a thickness of less than one tenth of a millimetre,’ said Sebastian Watt, a PhD student in Oxford’s Department of Earth Sciences, who led the team. ‘We collected samples from over 220 sites across an area of 100,000 square kilometres and with these field data and samples we were able to make the first scientific assessment of the size and impact of the eruption.’
The Chaitén eruption had immediate social and economic impacts across Patagonia (southern Chile and Argentina), with more than 5,000 people evacuated from settlements up to 75 km from the volcano, and extensive ash deposition leading to regional disruption of agriculture and aviation. The volcano was not routinely monitored, and there was no recognised warning before the eruption started.
The Andes Mountains along the western coastline of South America include numerous active steep-sided, cone-shaped stratovolcanoes. The majority of these volcanoes were formed and are still fed by magma generated as the Nazca tectonic plate under the southeastern Pacific Ocean moves northeastward and plunges beneath the South American continental plate—a process known as subduction. The Nazca plate is the source of last week's earthquake. The line of Andean volcanoes marks the approximate location of the subduction zone.
This astronaut photograph (below) highlights two volcanoes located near the southern boundary of the Nazca–South America subduction zone in southern Chile. Dominating the scene is the massive Minchinmávida Volcano (image upper right). Charles Darwin observed an eruption of this glaciated volcano during his Galapagos Islands voyage in 1834; the last recorded eruption took place the following year. When this photo was taken, the white, snow-covered summit of Minchinmávida was blanketed by gray ash erupted from its much smaller but now-active neighbor to the west, Chaitén Volcano.
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