Posted on by Nancy Atkinson

Satellite Images Show Hurricane Igor Likely to Make Direct Hit on Bermuda

Hurrican Igor as seen by one of the GOES satellites, taken on Sept. 19, 2010 at 17:15 UTC. Credit: NOAA

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The massive Hurricane Igor is now a Category One storm, with maximum sustained wind speeds of 140 km per hour, (85 miles per hour). As of this writing at 2:30 EDT, it looks as if it is on a direct collision course with Bermuda and is about 220 km (135 miles) southwest of Bermuda. The intensity of the storm has decreased over the past few days, but the size and rotation of the Igor means that Bermuda will be hit repeatedly as the arms of the hurricane spin over the 54 square kilometer (21 sq mi) island nation. In the satellite image above, Bermuda is the small white dot near the center of the image.

Projected track of Hurricane Igor. Credit: NOAA

Damaging sustained winds of hurricane force will reach the Bermuda late Sunday afternoon, and they will continue into early Monday morning. Wind gusts are predicted to be near or just over 160 km/hour (100 mph) as Igor makes its closest approach to Bermuda. Here’s a link to even more hurricane images.

The hurricane threatens to leave widespread tree damage and power outages in its wake. Some structures will also sustain damage; but fortunately, many buildings on Bermuda are made of stone with foundations into bedrock.

Flooding is also a serious concern across Bermuda. Igor will not only drop 4 to 8 inches of rain but will also trigger a 6- to 10-foot storm surge. Worsening the situation is the fact that waves pounding Bermuda will rise to heights in excess of 40 feet into this evening.

The massive size of Igor will cause the hurricane to keep battering the island well into Monday afternoon.

This 3-D image of Igor's cloud heights and rainfall from NASA TRMM satellite. Credit: Credit: NASA/SSAI, Hal Pierce

This 3-D image of Igor’s cloud heights and rainfall from NASA TRMM data shows a large area of heavy rainfall (falling at about 2 inches per hour) shown here in red on Sept. 15 at 0353 UTC. The yellow and green areas indicate moderate rainfall between .78 to 1.57 inches per hour. The image reveals that Igor’s eye was still very distinct but the southwestern portion of the eye wall had eroded.

Sources: NOAA, AccuWeather, JPL

Posted on by Ryan Anderson

Extrasolar Volcanoes May Soon be Detectable

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We’ve all seen pictures of erupting terrestrial volcanoes from space, and even eruptions on Jupiter’s moon Io in the outer solar system, but would it be possible to detect an erupting volcano on an exoplanet? Astronomers say the answer is yes! (with a few caveats)

It’s going to be decades before telescopes will be able to resolve even the crudest surface features of rocky extrasolar planets, so don’t hold your breath for stunning photos of alien volcanoes outside our solar system. But astronomers have already been able to use spectroscopy to detect the composition of exoplanet atmospheres, and a group of theorists at the Harvard-Smithsonian Center for Astrophysics think a similar technique could detect the atmospheric signature of exo-eruptions.

By collecting spectra right before and right after the planet goes behind its star, astronomers can subtract out the star’s spectrum and isolate the signal from the planet’s atmosphere. Once this is done, they can look for evidence of molecules common in volcanic eruptions. Models suggest that sulfur dioxide is the best candidate for detection because volcanoes produce it in huge quantities and it lasts in a planet’s atmosphere for a long time.

Still, it won’t be easy.

“You would need something truly earthshaking, an eruption that dumped a lot of gases into the atmosphere,” said Smithsonian astronomer Lisa Kaltenegger. “Using the James Webb Space Telescope, we could spot an eruption 10 to 100 times the size of Pinatubo for the closest stars,” she added.

To be detected, exoplanet eruptions would have to be 10 to 100 times larger than the 1991 eruption of Mt. Pinatubo shown here. Image source: USGS

In 1991 Mount Pinatubo in the Philippines belched 17 million tons of sulfur dioxide into the stratosphere. Volcanic eruptions are ranked using the Volcanic Explosivity Index (VEI). Pinatubo ranked ‘colossal’ (VEI of 6) and the largest eruption in recorded history was the ‘super-colossal’ Tambora event in 1815. With a VEI of 7 it was about 10 times as large as Pinatubo. Even larger eruptions (more than 100 times larger than Pinatubo) on Earth are not unheard of: geologic evidence suggests that there have been 47 such eruptions in the past 36 million years, including the eruption of the Yellowstone caldera about 600,000 years ago.

The best candidates for detecting extrasolar volcanoes are super-earths orbiting nearby, dim stars, but the Kaltenegger and her colleagues found that volcanic gases on any earth-like planet up to 30 light years away might be detectable. Now they just have to wait until the James Webb Space Telescope is launched 2014 to test their prediction.

Posted on by Nancy Atkinson

NASA Satellites and Spacecraft Look Into the Eye of Hurricane Earl

Hurricane Earl on Sept. 2, 2010 as seen by NASA's Terra Satellite. NASA image courtesy Jeff Schmaltz, MODIS Rapid Response Team

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NASA scientists, instruments and spacecraft are busy studying Hurricane Earl from both the air and space, and an unmanned aircraft actually flew inside the giant storm. Above is a satellite image from NASA’s Terra satellite, and below is an image taken by one of the astronauts on board the International Space Station, Doug Wheelock. Three NASA aircraft carrying 15 instruments have been flying above, below and into Earl as part the new Genesis and Rapid Intensification Processes mission, or GRIP, which GRIP is designed to help improve our understanding of how hurricanes such as Earl form and intensify rapidly.

See below for a couple of NASA websites where you can see real-time data about Hurricane Earl.


Hurricane Earl as seen from the ISS, taken by astronaut Doug Wheelock. Credit: NASA

The Global Hawk is an unmanned aerial vehicle, and it made its first-ever flight over a hurricane on Sept. 2, and here’s the image of Earl as seen the morning of Sept. 2 from a high-definition camera aboard the aircraft.

NASA's Global Hawk in the Eye of Hurricane Earl on September 2, 2010. Credit: NASA

The photo show’s Hurricane Earl’s eye, and was taken from the HDVis camera on the underside of the Global Hawk aircraft at 13:05 UTC (9:05 a.m. EDT) on Sept. 2. The Global Hawk captured this photo from an altitude of 60,000 ft. (about 11.4 miles high). Here are some more hurricane photos.

Hurricane Earl's eye, as measured by NASA's HAMSR intrument on Sept. 2, 2010. credit: NASA-JPL/Data SIC/NOAA/U.S. Navy/NGA/GEBCO/Google

Among the instruments participating in GRIP is the High-Altitude Monolithic Microwave Integrated Circuit Sounding Radiometer, or HAMSR. The instrument is able to show the 3-D distribution of temperature, water vapor and cloud liquid water in the atmosphere.

Earl’s eye is visible as the blue-green circular area in the center of the image, surrounded by orange-red. The eye is colored blue-green because the instrument is seeing the ocean surface, which appears cool to the instrument. The surrounding clouds appear warm because they shield the cooler ocean surface from view. Just north of the ring of clouds is a deep blue arch, which represents a burst of convection (intense thunderstorms). The pink crosses in the image represent lightning in the area, as measured by a lightning network. Ice particles and heavy precipitation in the convective storm cell cause it to appear cold.

The early evolution of Hurricane Earl is shown in this pair of images from JPL's APR-2 instrument. Credit: NASA/JPL

A second GRIP instrument is the Airborne Precipitation Radar (APR-2), a dual-frequency weather radar that is taking 3-D images of precipitation aboard NASA’s DC-8 aircraft. APR-2 is being used to help scientists understand the processes at work in hurricanes by looking at the vertical structure of the storms.

The two APR-2 hurricane images above show the early evolution of Hurricane Earl from a rather disorganized storm (left) to a better developed hurricane with a more distinct and smaller eye and sharper eyewall (right). The data, taken during southbound passes over Earl’s eye on Aug. 29 and 30, respectively, are essentially vertical slices of the storm. They correspond to the intensity of precipitation seen by the radar along the DC-8’s flight track. Intense convective precipitation (shown in shades of red and pink) was observed on both sides of the hurricane’s eye. The eye is indicated by the dark region near the middle of the images. The yellow-green-colored regions indicate areas of lighter precipitation. The white lines near the bottom are the ocean surface.

Near-real-time images from HAMSR and APR-2 are being displayed on NASA’s TC-IDEAS website at . The website is a near-real-time tropical cyclone data resource and it integrates data from satellites, models and direct measurements from many sources, to help researchers quickly locate information about current and recent oceanic and atmospheric conditions. The composite images and data are updated every hour and are displayed using a Google Earth plug-in. With a few mouse clicks, users can manipulate data and overlay multiple data sets to provide insights on storms that aren’t possible by looking at single data sets alone.

The progress of NASA’s GRIP aircraft can be followed in near-real-time when they are flying at this website. “Click to start RTMM Classic” will download a KML file that displays in Google Earth.

Source: JPL

Here are some more hurricane pictures, and even more hurricanes pictures.

Posted on by Nancy Atkinson

Earth Moved Substantially in April 2010 Earthquake

Overview of the UAVSAR interferogram of the magnitude 7.2 Baja California earthquake of April 4, 2010, overlaid atop a Google Earth image of the region. Major fault systems are shown by red lines, while recent aftershocks are denoted by yellow, orange and red dots. Image credit: NASA/JPL/USGS/Google ›

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From a JPL press release.

NASA has released the first-ever airborne radar images of the deformation in Earth’s surface caused by a major earth quake — the magnitude 7.2 temblor that rocked Mexico’s state of Baja California and parts of the American Southwest on April 4, 2010. The data reveal that in the area studied, the quake moved the Calexico, Calif., region in a downward and southerly direction up to 80 centimeters (31 inches).

A science team at NASA’s Jet Propulsion Laboratory, Pasadena, Calif., used the JPL-developed Uninhabited Aerial Vehicle Synthetic Aperture Radar (UAVSAR) to measure surface deformation from the quake. The radar flies at an altitude of 12.5 kilometers (41,000 feet) on a Gulfstream-III aircraft from NASA’s Dryden Flight Research Center, Edwards, Calif.

The team used a technique that detects minute changes in the distance between the aircraft and the ground over repeated, GPS-guided flights. The team combined data from flights on Oct. 21, 2009, and April 13, 2010. The resulting maps are called interferograms.

The April 4, 2010, El Mayor-Cucapah earthquake was centered 52 kilometers (32 miles) south-southeast of Calexico, Calif., in northern Baja California. It occurred along a geologically complex segment of the boundary between the North American and Pacific tectonic plates. The quake, the region’s largest in nearly 120 years, was also felt in southern California and parts of Nevada and Arizona. It killed two, injured hundreds and caused substantial damage. There have been thousands of aftershocks, extending from near the northern tip of the Gulf of California to a few miles northwest of the U.S. border. The area northwest of the main rupture, along the trend of California’s Elsinore fault, has been especially active, and was the site of a large, magnitude 5.7 aftershock on June 14.

UAVSAR has mapped California’s San Andreas and other faults along the plate boundary from north of San Francisco to the Mexican border every six months since spring 2009, looking for ground motion and increased strain along faults. “The goal of the ongoing study is to understand the relative hazard of the San Andreas and faults to its west like the Elsinore and San Jacinto faults, and capture ground displacements from larger quakes,” said JPL geophysicist Andrea Donnellan, principal investigator of the UAVSAR project to map and assess seismic hazard in Southern California.

Each UAVSAR flight serves as a baseline for subsequent quake activity. The team estimates displacement for each region, with the goal of determining how strain is partitioned between faults. When quakes do occur during the project, the team will observe their associated ground motions and assess how they may redistribute strain to other nearby faults, potentially priming them to break. Data from the Baja quake are being integrated into JPL’s QuakeSim advanced computer models to better understand the fault systems that ruptured and potential impacts to nearby faults, such as the San Andreas, Elsinore and San Jacinto faults.

One figure (Figure 1) shows a UAVSAR interferogram swath measuring 110 by 20 kilometers (69 by 12.5 miles) overlaid atop a Google Earth image. Each colored contour, or fringe, of the interferogram represents 11.9 centimeters (4.7 inches) of surface displacement. Major fault lines are marked in red, and recent aftershocks are denoted by yellow, orange and red dots.

The quake’s maximum ground displacements of up to 3 meters (10 feet) actually occurred well south of where the UAVSAR measurements stop at the Mexican border. However, these displacements were measured by JPL geophysicist Eric Fielding using synthetic aperture radar interferometry from European and Japanese satellites and other satellite imagery, and by mapping teams on the ground.

Scientists are still working to determine the exact northwest extent of the main fault rupture, but it is clear it came within 10 kilometers (6 miles) of the UAVSAR swath, close to the point where the interferogram fringes converge. “Continued measurements of the region should tell us whether the main fault rupture has moved north over time,” Donnellan said.

An enlargement of the interferogram is shown in another figure (Figure 2), focusing on the area where the largest deformation was measured. The enlargement, which covers an area measuring about 20 by 20 kilometers (12.5 by 12.5 miles), reveals many small “cuts,” or discontinuities, in the fringes. These are caused by ground motions ranging from a centimeter to tens of centimeters (a few inches) on small faults. “Geologists are finding the exquisite details of the many small fault ruptures extremely interesting and valuable for understanding the faults that ruptured in the April 4th quake,” said Fielding. Another figure, (Figure 3) shows a close-up of the region where the magnitude 5.7 aftershock struck.

“UAVSAR’s unprecedented resolution is allowing scientists to see fine details of the Baja earthquake’s fault system activated by the main quake and its aftershocks,” said UAVSAR Principal Investigator Scott Hensley of JPL. “Such details aren’t visible with other sensors.”

UAVSAR is part of NASA’s ongoing effort to apply space-based technologies, ground-based techniques and complex computer models to advance our understanding of quakes and quake processes. The radar flew over Hispaniola earlier this year to study geologic processes following January’s devastating Haiti quake. The data are giving scientists a baseline set of imagery in the event of future quakes. These images can then be combined with post-quake imagery to measure ground deformation, determine how slip on faults is distributed, and learn more about fault zone properties.

UAVSAR is also serving as a flying test bed to evaluate the tools and technologies for future space-based radars, such as those planned for a NASA mission currently in formulation called the Deformation, Ecosystem Structure and Dynamics of Ice, or DESDynI. That mission will study hazards such as earth quakes, volcanoes and landslides, as well as global environmental change.

See all the maps at this webpage.

Posted on by Nancy Atkinson

Gulf Oil Leak: Day 62 Update

Satellite image of the oil leak in the Gulf of Mexico, as seen on June 19, 2010. Credit: MODIS Rapid Response Team.

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Here’s the latest satellite image of the BP oil leak in the Gulf of Mexico. The oil keeps spreading towards the northeast, and appears as a maze of silvery-gray ribbons in this image from the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite. The MODIS team said that the spot of black just north of the location of the oil well may be smoke; reports from the National Oceanic and Atmospheric Administration say that oil and gas continue to be captured and burned as part of the emergency response efforts.

The MODIS team is putting out about two satellite images of the region a day, which can be seen at this link.

Below is a video from reporter David Hammer from the Times-Picayune newspaper in New Orleans, Louisiana, who is covering the BP oil spill, explaining the latest developments as of June 21,2010. Apologies for the 15 second ad at the beginning, but Hammer provides a good overview of what has been happening.

Oil spill video: Times-Picayune reporter update
Posted on by Nancy Atkinson

Latest Satellite Views of Oil Leak, Plus Dramatic Video of Where the Oil May End Up

Satellite view of the oil spill in the Gulf of Mexico on June 12, 2010, from the Aqua satellite. NASA image courtesy the MODIS Rapid Response Team.

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56 days into the the still-leaking Deepwater Horizon oil well spill in the Gulf of Mexico, satellite views are becoming a daily viewing habit. This latest image, taken on June 12, 2010 shows the oil particularly visible across the northern Gulf of Mexico when the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite captured this image at 1:55 p.m. CDT. Oil appears to have reached beaches and barrier islands in Alabama and the western Panhandle of Florida. The problem for wildlife, and particularly birds, is that from above, the water does not look different. And when they dive in for prey, the get soaked with oil. Estimates are that between 12,000 and 19,000 barrels a day are gushing from the damaged well. On June 3rd, BP lowered a containment cap onto a cut pipe to catch some of the flow. This cap, says the company, is now collecting more than 10,000 barrels of oil a day, ferrying it up to a tanker on the surface. But no one can be absolutely sure of the estimates.

As the oil is coming ashore along the gulf coast, everyone wonders how far the oil will travel. Researchers National Center for Atmospheric Research (NCAR) have completed a detailed computer modeling study that indicates the oil might soon extend along thousands of miles of the Atlantic coast and open ocean as early as this summer. The video of their results, captured in a series of dramatic animations, below, has caused quite a stir.

The results seem fairly dramatic, but Dr. Synte Peacock, an oceanographer at NCAR said in an interview in EarthSky.org on that the simulations used a dye, and not oil. A dye would travel to the Atlantic Ocean, but oil would behave differently.

However, her team still thinks it’s very likely that oil will get into the Atlantic.

If it does, she said, people shouldn’t expect oil to coat Atlantic beaches and wildlife. That’s because, over the months it would take to travel there – if it does travel there – some oil will evaporate, be eaten by microbes, and become diluted in sea water.

Dr. Peacock added that in all the possible scenarios and simulations that were tested, oil from the oil spill traveled outside of the Gulf within 6 months. But she added that it’s still unclear if or how the oil will affect beaches on the Atlantic Coast. That eventual outcome is partially dependent on local weather around the time the oil reaches a beach.

NASA Earth Observatory image created by Jesse Allen, using data provided courtesy of NASA/GSFC/METI/ERSDAC/JAROS, and U.S./Japan ASTER Science Team.

This satellite image from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on NASA’s Terra satellite shows a false color image of on June 10, 2010, where parts of the oil slick are nearing the Mississippi Delta. Vegetation appears red and water appears in shades of blue and white.

Sources: NASA Earth Observatory, EarthSky

Posted on by Nancy Atkinson

More Up-Close Images of Eyjafjallajokull Volcano and Its Effect on Life in Iceland

View of volcanic ash spewing from the Eyjafjallajokull volcano. Image courtesy of and copyright Snaevarr Gudmundsson.

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Astronomer Snaevarr Gudmundsson from Iceland, who shared his incredible close-up images of the Eyjafjallajokull volcano with Universe Today back in April, has made another trek out to visit the region near the volcano. “Under the ash clouds the world takes strange turn,” he wrote in an email. “It is hard for residents to live in the neighborhood under these circumstances. When wind turns the ash clouds over their home village it gets unbearable to stay outside. It is absolutely essential to keep mask and goggles on to prevent sore throat and eyes filled with fine grained ash. The fine grained ash fills up every pore and penetrates into houses through every weakness, like joints around doors and windows, even though it is very well sealed. As you see where the bus is near the grill house at Vik (see below) a bad ash storm was making otherwise normal life awful.”

See more of Gudmundsson’s images of the Iceland volcano and how it is affecting life in Iceland.

View of volcanic ash spewing from the Eyjafjallajokull volcano. Image courtesy of and copyright Snaevarr Gudmundsson.

'A bad ash storm was making otherwise normal life awful.' Image courtesy of and copyright Snaevarr Gudmundsson.
Volcanic ash spewing from the Eyjafjallajokull volcano. Image courtesy of and copyright Snaevarr Gudmundsson.

Gudmundsson said that some images show the grass is green and one might assume everything is ok. “But the vegetation is growing through the ash layer which is up to 15 cm thick,” he said. When looking down into it the green color fades into grey ash with the grass sticking through.”

Ash on the ground. Image courtesy of and copyright Snaevarr Gudmundsson.
Lava flow and ash. Image courtesy of and copyright Snaevarr Gudmundsson.
Unusual clouds surround the Eyjafjallajokull volcano on a sunny day in Iceland. Image courtesy of and copyright Snaevarr Gudmundsson.
Eyjafjallajokull volcano in May 2010. Image courtesy of and copyright Snaevarr Gudmundsson.
Region near the Eyjafjallajokull volcano in May 2010. Image courtesy of and copyright Snaevarr Gudmundsson.
Going near the volcano requires protective gear and masks. Image courtesy of and copyright Snaevarr Gudmundsson.
This image was taken in 2005. Compare to the image below. Image courtesy of and copyright Snaevarr Gudmundsson.

These two photographs provide an idea of sediment disposal down into a the lagoon. “As I told you, it filled up the lagoon (believed to be 30 – 40 m deep before the eruption) in matter of two days by debris floods in the beginning of the eruption,” said Gudmundsson. “If you compare the two images from 2005 and now in May 2010 (not taken by same place) you can see how high the sediment plain reaches up to the glacier. Take note of the prominent gully and how high up it is . Indeed sediment has now buried the lower part of it so it will be curious to see what happens to the glacier in the future.”

The same area in May 2010. Image courtesy of and copyright Snaevarr Gudmundsson.

Thanks once again to Snaevarr Gudmundsson for sharing his images and insight of the Eyjafjallajokull volcano and how it is affecting life in Iceland.

Listen to a podcast on 365 Days of Astronomy of Snaevarr Gudmundsson interviewed by Col Maybury from radio station 2NUR in Australia, talking about the volcano.

Posted on by Nancy Atkinson

Volcano Cam Now Available

Eyjafjallajökull on May 12, 2010. NASA image by Jeff Schmaltz, MODIS Rapid Response Team at NASA GSFC.

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Via the Bad Astronomer, there is now a live video feed of the Eyjafjallajökull volcano in Iceland. It comes in two flavors: regular (visible) and infrared, so you can see a thermal version of the feed as well. It’s not an embeddable feed, so here’s the link. I’ve been watching it for awhile, and so far, there have always been people visible in the field of view, too. Scroll down on the page, and there’s also a map that shows the location of the camera relative to the volcano.

Above is the latest satellite imagery of Eyjafjallajökull, the Iceland volcano, taken on May 12, 2010, taken by the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite. It shows the plume reaching a height of 4 to 5 kilometers (13,000-17,000 feet), even going above the clouds. The plume has switched directions from yesterday’s image, where the plume was blowing south and slightly southest; now it is blowing more easterly.

According to the Iceland Meteorological Office and the Institute of Earth Sciences at the University of Iceland, the eruption had changed little from previous days and showed no signs of stopping.

Sources: NASA Earth Observatory, About Miles

Posted on by Nancy Atkinson

Latest Satellite Images of Eyjafjallajokull, the Volcano that Keeps on Giving

Eruption of Eyjafjallajökull Volcano in Iceland continues, seen in this NASA image by Jeff Schmaltz, MODIS Rapid Response Team at NASA GSFC, taken on May 11, 2010.

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Iceland’s Eyjafjallajökull Volcano continues to spew out a thick plume of ash. Seen here on May 11, 2010, the ash was streaming almost directly south, visibly extending at least 860 kilometers (530 miles) from Eyjafjallajökull. According to the NASA’s Earth Observatory website and the London Volcanic Ash Advisory Center, the ash reached altitudes of 14,000 to 17,000 feet (4,300 to 5,200 meters). CNN reported that some Spanish and Moroccan airports were closed at the time. On May 10th, the Icelandic Met Office reported continuous ash fall south of the volcano, with as depths reaching 2-3 millimeters (roughly 0.1 inches). “Presently there are no indications that the eruption is about to end,” the Met Office said yesterday.

Astronomer Snaevarr Gudmundsson from Iceland who shared his amazing close-up images of the volcano a few weeks ago, sent an update on how Iceland is coping with continued eruption.

“By now ash has covered all surface snow and ice so the mountains looks quite different from the photographs what I mailed to you,” he said. “The eruption is affecting people in a small village southeast of Eyjafjallajokull, named Vik. There it is stopping normal life of people. They are leaving their homes and elementary school is forced to shut down, only because of the fine grained ash. But the people are not in a threat of anything serious like pyroclastic flow or poisoned gases.”

Gudmundsson said he would be venturing out for the next few days to try and take more images of the volcano, and will send us another update soon.

Here is another satellite image, of the Iceland volcano taken by Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite on May 10, 2010.

The Eyajafjallajokull volcano on May 10, 2010. NASA image courtesy Jeff Schmaltz, MODIS Rapid Response Team at NASA GSFC.

Source: NASA Earth Observatory

Posted on by Nancy Atkinson

Shock Waves, Volcanic Bombs From Eyjafjallajokull

The volcano in Iceland keeps producing eye-popping effects. Now that the ash isn’t spewing quite so dramatically,the mouth of the volcano itself is visible. Here’s close-up aerial footage of the crater at Eyjafjallajokull, with glowing red lava and shockwaves of the eruptions in the ash cloud. Incredible.

If you haven’t yet seen images taken by Astronomer Snaevarr Gudmundsson from Iceland, he was just a few kilometers away from the volcano last Saturday, at the height of the action — including lighting in the plume. So check them out.

There are many other great images on across the webs — take a look at The Daily Mail website of the eruption with a unique backdrop of a stunning aurora, or these on Discovery News.