Sioux Falls Scientists endorse Restless Planet for describing some
of the foundamental forces that have shaped our planet.
Restless Planet (2005) - 275 minutes
Restless Planet at Amazon.com
Experience the devastating power of explosive volcanoes, ground-buckling earthquakes, deadly tornadoes, hurricanes and tsunamis as National Geographic heads into the field with scientists who risk their lives to study these fearsome natural phenomena. Featuring over five hours of programming, Restless Planet captures extraordinary scenes of destruction from the air, the ground and from inside a tornado and the moving, human side of the story from tales of heroism and tragedy to dedicated teams of experts racing to understand and ultimately better predict the deadly forces of nature.
Restless Planet includes:
- Disk 1: Volcano: Nature's Inferno
- Disk 2: Tsunami: Killer Wave
- Disk 3: Tornado Intercept
- Disk 4: Nature's Fury
- Disk 5: Storm of the Century
12-22-18 Mexico's deadliest volcano
It's a ticking time bomb, experts say — and its eruption could cause damage on the scale of Pompei. On the clear-sky morning of December 21st, 1994, Claus Siebe was standing at the foot of Popocatépetl, watching as elephantine plumes of black smoke and heaps of pyroclastic flow spewed out of Mexico's largest active volcano. Siebe stood silently next to a group of mountaineers, all of whom had their heads cocked upward. He'd never witnessed an eruption on this scale before; he was floored. Recalling that day now, nearly 24 years later, Siebe describes a scene of awe and confusion. "Everybody was watching," Siebe says. "Nobody panicked. We were all just kind of surprised that this was happening." For weeks leading up to the eruption, Siebe, a professor of volcanology at the Universidad Nacional Autónoma de México, had been busy reconstructing the eruptive history of Popocatépetl, a volcano that sits between Mexico City and Puebla and their collective 20 million people. Performing geological and gas measurements, Siebe and his team of researchers concluded that Popocatépetl (which translates to "Smoking Mountain" in the Nahuatl language) was now "reactivating." Four days before Christmas of that year, their hunch was proven correct. Over the next five years, Siebe and his colleagues would deduce that Popocatépetl's latest activity was its first in almost 1,000 years. In a 1996 paper in Geology, Siebe found, through hydrocarbon measurements and biometric dating, that the volcano experienced what's called a Plinian eruption — meaning an eruption that bears structural similarities to Mount Vesuvius' mythically destructive outburst; so named in honor of Pliny the Younger, the hawk-eyed Roman who witnessed the horror — around 215 B.C.E, and again around 823 C.E. In short, it had experienced its share of Big Ones, as he calls them. Siebe's research had estimated the occurrence of a Big One "every millennia or so," a calculation that, even with advances in monitoring technology, is a scientific shot in the dark. Among the wreckage his modeling predicts: the general devastation of everything in an eight-mile radius. In the years since the 1994 eruption, Siebe and his colleagues have witnessed a handful of eruptions placed in categories of "High Risk" to "Medium Risk" — categorizations that are determined by the expanding radius of a destruction zone from Popocatépetl's mouth — the worst being in 2000, 2003, 2013, and 2015. Theoretically speaking, the eruptions Siebe's categorized thus far from the volcano have been kind of like a treatable array of kitchen fires; a Plinian eruption, in line with its historical magnitude, would be sure to engulf the entire house. He and his team are certain that the question isn't if Latin America's deadliest volcano is going to have another Big One. It's when.
10-9-18 Falling rocks can explode so hard that only nuclear weapons beat them
If big rocks fall far enough they can explode with more energy than any non-nuclear bomb – and the ensuing shockwave can snap large trees half a kilometre away. If falling rocks are big enough and hit the ground hard enough they can create a blast so intense that the rocks are pulverised into powder. Such extreme rockfalls are followed by a shockwave that can snap trees hundreds of metres away. “They’re extremely weird phenomena, which have been somehow overlooked,” says Fabio De Blasio of the University of Milano-Bicocca in Italy. The first known example took place in Yosemite National Park, California, on 10 July 1996. Two large masses of rock fell from Glacier Point and plummeted 665 metres. When they hit the ground they released a blast of air that snapped or toppled about 1000 trees, including some half a kilometre away. This was followed by a cloud of abrasive sand, which scoured the fallen trees. The rockfall was described by researchers in 2000 but it remained a curiosity. Now De Blasio and his colleagues have identified 21 other “extremely energetic rockfalls” from the past two decades, mostly from the European Alps and the Dolomites in Italy. They argue that these extreme events are more common than had been thought. The crucial point is that the impact of the rocks on the ground is so violent that they are smashed into powder. This needs a big mass of rocks, on the order of 10,000 cubic metres, to pick up speed by falling several hundred metres. “Typically they will develop in areas where erosion has been quite fast,” says De Blasio. Yosemite is a steep gorge eroded by the Merced river, so it has lots of steep cliffs that are ideal.
3-24-18 Mount Etna is 'sliding towards the sea'
Europe's most active volcano, Mount Etna, is sliding towards the sea. Scientists have established that the whole structure on the Italian island of Sicily is edging in the direction of the Mediterranean at a rate of 14mm per year. The UK-led team says the situation will need careful monitoring because it may lead to increased hazards at Etna in the future. The group has published its findings in the Bulletin of Volcanology. "I would say there is currently no cause for alarm, but it is something we need to keep an eye on, especially to see if there is an acceleration in this motion," lead author Dr John Murray told BBC News. The Open University geologist has spent almost half a century studying Europe's premier volcano. In that time, he has placed a network of high-precision GPS stations around the mountain to monitor its behaviour. This instrumentation is sensitive to millimetric changes in the shape of the volcanic cone; and with 11 years of data it is now obvious, he says, that the mountain is moving in an east-south-east direction, on a general track towards the coastal town of Giarre, which is about 15km away. Essentially, Etna is sliding down a very gentle slope of 1-3 degrees. This is possible because it is sitting on an underlying platform of weak, pliable sediments. Dr Murray's team has conducted lab experiments to illustrate how this works. The group believes it is the first time that basement sliding of an entire active volcano has been directly observed.
1-25-18 These are the worst ready-made sandwiches for the climate
Producing ready-made sandwiches can generate twice as much carbon dioxide as simply making them at home, and one particular filling is egregiously bad. As well as saving money, making your sandwiches at home will help save the planet. Adisa Azapagic of the University of Manchester, UK and her colleagues have studied the carbon footprint of the 11.5 billion sandwiches eaten in the UK each year. They worked out how much greenhouse gas is released by making 40 types of sandwich. Overall, they found that the UK sandwich industry releases the equivalent of 9.5 million tonnes of carbon dioxide. However, homemade is better. “The main reason is that in commercial sandwiches you have longer refrigeration chains, plus packaging, and waste tends to be higher from bought sandwiches,” says Azapagic. The most climate-friendly sandwich studied is a plain, homemade cheese and ham sandwich. On average, depending on quantities in in the sandwich, it generates 550 grams of carbon dioxide equivalent, the same as driving a car for 6 kilometres. The worst is a commercial egg, bacon and sausage “all-day-breakfast” sandwich, with corresponding values of 1440g and 19km. The least harmful commercial sandwich was egg mayonnaise with cress, with carbon footprint figure of 740g, equivalent to driving 10km. The largest contributors are the farming and processing of ingredients, which account for 37 to 67 per cent of the footprints for ready-made sandwiches. Refrigeration in stores accounts for 25 per cent, and packaging 8.5 per cent.
1-25-18 Ring of Fire's volcanic and quake activity is normal, say scientists
Tens of thousands of people have had their lives disrupted in the past week by seismic and volcanic activity along the Ring of Fire. An earthquake off Alaska, an avalanche and volcanic eruption in central Japan and a volcano squirting lava in the Philippines all occurred within days of each other. It led the UN Office for Disaster Risk Reduction to send a tweet on Tuesday warning that the Ring of Fire was "active". Many are asking whether there is cause for concern that something more serious might happen. So is there reason to worry? The Ring of Fire refers to a string of volcanoes, earthquake sites and tectonic plates around the Pacific. It spreads across 40,000km (25,000 miles) from the southern tip of South America all the way to New Zealand. Roughly 90% of all earthquakes occur along the area and the ring is dotted with 75% of all active volcanoes on Earth, that's 452 individual active volcanoes. This week alone, a 7.9-magnitude earthquake struck off the coast of Alaska in the US. The quake briefly triggered a tsunami warning for coastal areas of Alaska and British Columbia in Canada. On the same day, one soldier was killed and at least 11 others injured in central Japan by an avalanche that may have been triggered by a volcanic eruption. The eruption of Mount Moto-Shirane, which is part of Mount Kusastsu-Shirane, also sent rocks raining down a kilometre-wide area near Kusatsu in central Japan, local media reported. Earlier last year, the eruption of Bali's Mount Agung led to the closure of the city's international airport and forced up to 100,000 people to evacuate.
1-23-18 Huge volcano eruption in the Philippi
More than 50,000 villagers were forced to flee their homes after the most active volcano in the Phillipines, Mount Mayon, spewed lava and ash plumes. The most active volcano in the Philippines spewed fountains of lava and massive ash plumes in a new eruption today that forced more than 50,000 villagers to evacuate. Fountains of lava fountains gushed 700m up above Mount Mayon’s crater and ash plumes rose up to 3km, according to the Philippine Institute of Volcanology and Seismology. An explosive eruption at noon local time on Monday was the most powerful since the volcano started acting up more than a week ago. Authorities warned that a violent eruption may occur in hours or days, characterised by more rumblings and pyroclastic flows – superheated gas and volcanic debris that race down the slopes at high speeds. After Monday’s explosion, officials raised Mayon’s alert level to four on a scale of five, and the danger zone was expanded 8km from the crater, requiring thousands more residents to be evacuated, including at least 12,000 who returned to their homes last week as Mayon’s rumblings temporarily eased and then scrambled back to the emergency shelters this week. At least 56,217 people were taking shelter in 46 evacuation camps on Tuesday and army troops and police were helping move more villagers from their homes, officials said.
1-15-18 Mount Etna may not really be a ‘proper’ volcano at all
Italy’s famous volcano Mount Etna may be fed mostly by hot water and carbon dioxide, with only a small dose of molten rock to make it resemble a classic volcano. Mount Etna, one of the world’s most famous volcanoes, may be misunderstood. According to one geologist, the material feeding the cone is mostly water, so Etna is effectively a giant hot spring. But other geologists are unconvinced. Mount Etna in Italy is almost constantly active. It’s been estimated that it spewed about 70 million tonnes of lava in 2011 alone. But what really puzzles Carmelo Ferlito at the University of Catania, Italy – about 30 kilometres from the volcano – is that Etna also belches out more than 7 million tonnes of steam, carbon dioxide and sulphur dioxide every year. The conventional explanation is that this gas bubbles out of magma as it loses pressure on its way up through the volcano’s vent. But Ferlito says Etna would need to erupt ten times more lava than it does to account for all the gas that burps out. Alternatively, maybe most of the molten rock in Etna loses its gas and sinks again, without erupting. But Ferlito’s calculations suggest that sustaining the gas emissions would require a fresh injection of 10,000 kilograms of magma every single second. This would “inflate the volcano like a children’s balloon”, he says. So instead, Ferlito argues the easiest way to explain Etna’s excess gas is to ditch the idea that it is fed only by magma. He has calculated that the volcano’s deep plumbing system could hold lots of water, carbon dioxide and sulphur, collectively making up about 70 per cent of the volume of material feeding the volcano. “Only 30 per cent is molten rock,” he says.
9-3-17 North America’s largest recorded earthquake helped confirm plate tectonics
North America’s largest recorded earthquake helped confirm plate tectonics
‘The Great Quake’ tells the story of the 1964 Alaska temblor. In 1964, the largest recorded earthquake in North American history shook Alaska to its core (damage in Anchorage, shown) and provided proof of tectonic plate movement. In the early evening of March 27, 1964, a magnitude 9.2 earthquake roiled Alaska. For nearly five minutes, the ground shuddered violently in what was, and still is, the second biggest temblor in recorded history. Across the southern part of the state, land cracked and split, lifting some areas nearly 12 meters — about as high as a telephone pole — in an instant. Deep, house-swallowing maws opened up. Near the coast, ground turned jellylike and slid into bays, dooming almost everyone standing on it. Local tsunamis swamped towns and villages. Not many people lived in the newly formed state at the time. If the quake had struck in a more developed place, the damage and death toll would have been far greater. As it was, more than 130 people were killed. In The Great Quake, Henry Fountain, a science journalist at the New York Times, tells a vivid tale of this natural drama through the eyes of the people who experienced the earthquake and the scientist who unearthed its secrets. The result is an engrossing story of ruin and revelation — one that ultimately shows how the 1964 quake provided some of the earliest supporting evidence for the theory of plate tectonics, then a disputed idea.
8-15-17 Seismologists get to the bottom of how deep Earth’s continents go
Seismologists get to the bottom of how deep Earth’s continents go
Analysis of seismic waves finds runny rock layer where landmass ends. Earthquake vibrations are revealing just how deep the continents beneath our feet go. Researchers analyzed seismic waves from earthquakes that have rocked various regions throughout the world, including the Americas, Antarctica and Africa. In almost every place, patterns in these waves indicated a layer of partially melted material between 130 and 190 kilometers underground. That boundary marks the bottom of continental plates, argue Saikiran Tharimena, a seismologist at the University of Southampton in England, and colleagues. Their finding, reported in the Aug. 11 Science, may help resolve a longtime debate over the thickness of Earth’s landmasses. Estimating continental depth “has been an issue that’s plagued scientists for quite a while,” says Tim Stern, a geophysicist at Victoria University of Wellington in New Zealand, who wasn’t involved in the work. Rock fragments belched up by volcanic eruptions suggest that the rigid rock of the continents extends about 175 kilometers underground, where it sits atop slightly runnier material in Earth’s mantle. But analyses of earthquake vibrations along Earth’s surface have suggested that continents could run 200 or 300 kilometers deep, very gradually transitioning from cold, hard rock to hotter, gooier material.
1-4-17 Molten iron river discovered speeding beneath Russia and Canada
Molten iron river discovered speeding beneath Russia and Canada
DEEP below our planet’s surface, a molten jet of iron, nearly as hot as the surface of the sun, is picking up speed. This stream of liquid some 420 kilometres wide has been discovered by telltale magnetic field readings 3000 kilometres below North America and Russia. It has trebled in speed since 2000, and is now circulating westwards at between 40 and 45 kilometres per year, heading from deep under Siberia towards the underside of Europe (see diagram). That is three times as fast as the typical speeds of liquid in the outer core. No one knows yet why the jet has got faster, but the team that made the discovery thinks it is a natural phenomenon, and can help us understand the formation of Earth’s magnetic fields, which keep us safe from solar winds. “It’s a remarkable discovery,” says Phil Livermore at the University of Leeds, UK, who led the team. “We’ve known that the liquid core is moving around, but our observations haven’t been sufficient until now to see this jet.” “We know more about the sun than the Earth’s core,” says team member Chris Finlay from the Technical University of Denmark in Kongens Lyngby. “The discovery of this jet is an exciting step in learning more about our planet’s inner workings.” What made the discovery possible was the combined monitoring power of the European Space Agency’s trio of satellites, called Swarm, which were launched in 2013. From orbit, they can measure magnetic field variations down to 3000 kilometres below Earth’s surface, where the molten core meets the solid mantle.
1-3-17 'Better estimate' of volcanic ash cloud return
'Better estimate' of volcanic ash cloud return
Potentially disruptive volcanic ash clouds across Northern Europe occur more frequently than previously thought, according to new research. Scientists investigated known and newly identified records of ash fall deposits over the past few thousand years and concluded the average return rate to be about 44 years. Previous research had put the recurrence at roughly 56 years. The source of the ash is almost always from Iceland. In 2010, the island’s Eyjafjallajökull volcano erupted, throwing some 250 million tonnes of fine particles into the atmosphere that grounded planes across Europe. The eruption of Grímsvötn the following year also disrupted air traffic - albeit on a much smaller scale. But despite these two recent, closely spaced events, the team behind the latest research says the general frequency of volcanic ash clouds over Northern Europe is still generally quite low.
11-4-16 Huge lake discovered 15 kilometres under a volcano
Huge lake discovered 15 kilometres under a volcano
The discovery of a vast reservoir of water – as big as the largest freshwater lakes – could help reveal how eruptions occur, and how continental crust forms. Our planet is blue inside and out. A massive reservoir of water has been discovered deep beneath a volcano in the Andes, and Earth’s interior may be dotted with similar wet pockets lurking below other major volcanoes. The unexpected water, which is mixed with partially melted magma, could help to explain why and how eruptions happen. This water may also be playing a role in the formation of the continental crust we live on, and could be further evidence that our planet has had water circulating in its interior since its formation.
11-1-16 Mount St. Helens is a cold-hearted volcano
Mount St. Helens is a cold-hearted volcano
Scientists are still searching for the source of volcano’s heat. While a volcano called Mt. Adams is fed by an obvious heat source, Mount St. Helens sits above a wedge of rock formed at the edge (or “cold nose”) of the North American tectonic plate. Below most volcanoes, Earth packs some serious deep heat. Mount St. Helens is a standout exception, suggests a new study. Cold rock lurks under this active Washington volcano. Using data from a seismic survey (that included setting off 23 explosions around the volcano), Steven Hansen, a geophysicist at the University of New Mexico, peeked 40 kilometers under Mount St. Helens. That’s where the Juan de Fuca tectonic plate melts as it sinks into the hot mantle beneath the North American plate, fueling an arc of volcanoes that line up like lights on a runway. All except for Mount St. Helens, which stands apart about 50 kilometers to the west. Still, Hansen and colleagues expected to see a heat source under Mount St. Helens, as seen at other volcanoes. Instead, thermal modeling revealed a wedge of a rock called serpentinite that’s too cool to be a volcano’s source of heat, the researchers report November 1 in Nature Communications. “This hasn't really been seen below any active arc volcanoes before,” Hansen says.
Sioux Falls Scientists endorse Restless Planet for describing some
of the foundamental forces that have shaped our planet.