
Kilauea

The explosion debris covered part of Crater Rim Drive and damaged Halema’uma’u overlook, but didn’t release any lava, which suggests to scientists that it was driven by hydrothermal or gas sources.
This explosion event followed a dangerous increase of sulfur dioxide gas levels from the Halema’uma’u crater which prompted closures of Crater Rim Drive between Kilauea Military Camp south/southeast to Chain of Craters Road, Crater Rim Trail from Kilauea Military Camp south/southeast to Chain of Craters Road, and all trails leading to Halema’uma’u crater.
Early in the morning of March 24, 2008, the white gas ejection changed to brown-gray ash, and lava particles were thrown from the vent, forming Pele’s Hair, Pele’s Tears, and 4-inch (10 centimeter) lava spatters around the vent. This is the first time fresh lava has been erupted in the crater since 1982.



Kilauea is a very low, flat shield volcano — vastly different in profile from the high, sharply sloping peaks of stratovolcanoes like Mt. Fuji, Mount Hood, and Mount St. Helens.
It lies against the southeast flank of much larger Mauna Loa volcano. Its massive size and elevation of 13,677 feet (4,169 meters) is a stark contrast to Kilauea, which rises only 4,091 feet (1,247 meters) above sea level, and thus from the summit caldera appears as a broad shelf of uplands well beneath the long profile of occasionally snow-capped Mauna Loa, 15 miles (24 kilometers) distant.


An interesting phenomenon seen at Kilauea is “gas pistoning” — gas-driven rise and fall of the magma — caused by accumulation of gas beneath a column of lava, such as in Pu`u `O`o’s crater vents. As the accumulated gas rises, it pushes up the overlying lava (the “piston”). When the gas bubble reaches the surface, it bursts, sometimes as a forceful jet of fume and spatter, and the lava then drains back into the vent.
Magma erupts because of gas dissolved in it at depth. The gas forms bubbles or vesicles and tries to escape at the low pressures near the earth’s surface. The technical term for this bubble formation is “vesiculation.” Trapped in the magma, the bubbles expand and force the magma toward the surface.
If the cone and its surroundings are highly fractured, the magma may rise only partway in the vent’s throat. The gas escapes through the fractures before the magma expands enough to erupt in the crater. Blockages may occur intermittently at the point where the lava tube normally drains magma away from Pu`u `O`o. Blockages cause changes in pressurization, allowing the magma to reach the surface and spill onto the crater floor as lava.
The ponded lava rarely overtops the crater rim, draining back into its conduit. Drainback occurs due to the lava cooling and losing its gas to the atmosphere. This colder, denser lava forms a cap that stalls further vesiculation in the underlying magma column. Meanwhile, bubbles coalesce within the maturing magma column. As they grow in size they rise more rapidly, hollowing out the core of the column.
Kilauea Volcano Dramatic Eruption
Sidaorjo’s Man-Made Mud Volcano Lusi
For 2 years, a hole in the earth has been oozing enough mud to fill 50 Olympic size swimming pools daily, covering villages and factories roof deep in mud and forcing the evacuation of thousands in Sidoarjo, East Java, Indonesia.

above the dried mud that now covers all traces of its former neighborhood, near the
volcano in Sidoarjo, East Java on May 27, 2008.
On the 2nd anniversary of Sidaorjo’s mud volcano eruption that displaced tens of thousands of villagers in central Indonesia, scientists claim to be almost certain it was caused by faulty drilling of a gas exploration well — not an earthquake as the gas company claimed.
“We are more certain than ever that the Lusi mud volcano is an unnatural disaster and was triggered by drilling.” said Richard Davies, lead author of a study published in early June in the journal Earth and Planetary Science Letters.


East Java province May 29, 2008.

On 28 May 2006, gas company PT Lapindo Brantas exploring for gas in Sidoarjo, in East Java, Indonesia, drilled a borehole. At 5am, a secondary stage of drilling began and the drill string went about 9,300 feet down, after which the first small eruption of water, steam and a small amount of gas occurred at a location just southwest of the well. Several more eruptions followed the next few days, and the flow of hot mud hasn’t stopped since.
Fourteen people have been killed and 30,000 have been evacuated. At least 12 villages, with more than 10,000 homes have been destroyed while schools, offices and factories have also been wiped out and a major impact on the wider marine and coastal environment is expected.


which used to be their village.

mud volcano and its surrounding area.

caldera of the mud volcano.

Brimstone Pit
What lives 1,800-feet undersea, spews molten rock and sounds like a rumbling tractor trailer? The erupting Brimstone Pit in the North Pacific, recently recorded by NOAA.
A giant, eruptive plume pours from the Brimstone Pit during a 2004 expedition to
NW Rota-1. Submarine Ring of Fire 2004 Exploration.
A submarine volcano called NW Rota-1 was detected during a 2003 NOAA survey of the Mariana Island arc in the northern Pacific Ocean not far from a gigantic undersea trench where one continent-sized piece of the Earth’s crust is grinding underneath another, and found to be hydrothermally active.
The basaltic to basaltic-andesite seamount rises to within 517 m of the sea surface SW of Esmeralda Bank, lying about 42 miles (64 kilometers) NW of Rota Island and about 60 miles (100 kilometers) north of Guam.
In 2004, a minor submarine eruption from the vent Brimstone Pit intermittently ejected a plume several hundred meters high containing ash, rock particles, and molten sulfur droplets that adhered to the surface of the remotely operated submersible vehicle. The active vent was funnel-shaped, about 65 feet (20 meters) wide and 40 feet (12 meters) deep.
Brimstone Pit Eruption
Glowing, red lava shoots out of the Brimstone Pit crater near the summit of NW Rota-1
volcano, Submarine Ring of Fire 2006 Exploration. Photo NOAA Vents Program
For 2 years now, a team of scientists with the National Oceanic and Atmospheric Administration (NOAA) have been doing what no one else has ever done — watching an underwater volcano up close.
This is the first time a video and audio of such an event has ever been recorded simultaneously which was released earlier this month.
Researchers dove to the Brimstone Pit, taking recordings from a submersible vehicle using an underwater microphone to capture the explosions.
Even at a depth of more than 1,800 feet below the surface, the classic signs of a volcano eruption were there — flowing lava and huge plumes of what looks like smoke. But that smoke is actually the rapid steam formation caused by the undersea interaction of magma and water. The most explosive bursts were 2 to 6 minutes long.
Antarctic Volcano

A layer of volcanic ash and glass shards frozen within an ice sheet in West Antarctica which extends across an area larger than Wales was identified in an article published in the journal Nature Geosciences by Hugh F. J. Corr and David G. Vaughan.
The volcanic eruption from beneath rated “severe” to “cataclysmic” on an international scale of volcanic force, punching a massive breach in the ice sheet and spitting out a plume about 8 miles (12,000 meters) into the sky. The subglacial volcano has a ‘volcanic explosion index’ of around 3 to 4.
“We believe this was the biggest eruption in Antarctica during the last 10,000 years.” Corr said.

“This is the first time we have seen a volcano beneath the ice sheet punch a hole through the ice sheet.” Vaughan said.
Heat from a volcano could still be melting ice and contributing to the thinning and speeding up of the thinning Pine Island Glacier which passes nearby, but Vaughan doubted that it could be affecting other glaciers in West Antarctica, which have also thinned in recent years.

The discovery is another vital piece of evidence that will help determine the future of the West Antarctic Ice Sheet and refine predictions of future sea-level rise.
The volcano is located beneath the West Antarctic ice sheet in the Hudson Mountains. Volcanoes are an important component of the Antarctic region, forming in diverse tectonic settings, mainly as a result of mantle plumes acting on the stationary Antarctic plate.
The region also includes some of the world’s best examples of a long-lived continental margin arc (Antarctic Peninsula), a very young marginal basin (Bransfield Strait) and an oceanic island arc (South Sandwich Islands). Many extinct volcanoes are very well preserved and others are still active, such as Deception Island, Mount Erebus, and the South Sandwich Islands.
Volcanic eruptions were common during the past 25 million years, and coincided with the great period of climatic deterioration that resulted in the formation of the Antarctic ice sheet.
Chaiten Llaima Volcano

“There’s been additional volcanic activity that we’re really worried about” said regional governor Sergio Galilea.

May 4 2008.
Luis Lara, a government geologist, said he did not expect a catastrophic collapse of the volcano, but “the eruptive column could, and that is sufficient material to be displaced down its sides and into areas nearby.”
The government declared the town of Chaiten — only 6 miles (10 kilometers) from the erupting volcano — off-limits for 3 months and reported that about 90% of the town had been flooded by the Blanco and Raya Rivers.

and ash flowing southeast from the summit of the volcano across the Andes mountains,
across part of Argentina and then dissipating over the Atlantic ocean.
“The flooding has receded in terms of water. But there’s a lot of material left, more mud than water.” Galilea said.
There were no deaths, but thousands of people have been evacuated within a 30 mile (48 kilometer) radius, including the 4,500 residents of Chaiten.
Ash has contaminated water supplies and coated houses, vehicles and trees. Authorities have also moved thousands of head of cattle from the area.
Futaleufu has also been coated with up to 6 inches of ash. About 1,000 residents had crossed into neighboring Argentina, where some areas have also been showered with hot debris, treating some for breathing problems.
Chaiten Volcano Eruption
Volcanoes for Alternative Energy

The state Division of Oil and Gas hopes the lease sale slated for August will be the first of many, and is considering to permit exploration of the 4,134 foot (1260 meter) Augustine Volcano, 171 miles (275 kilometers) southwest of Anchorage.

“High prices and climate change are definitely creating a renaissance in geothermal interest, particularly on a state and local level.” said Karl Gawell, executive director of the Geothermal Energy Association (GEA). “There really is a tremendous amount going on right now.”

“It’s only the tip of the iceberg in terms of what is possible. If we really want to go all out for it, we could easily achieve a substantial amount, 20, 25% of US energy needs within a few decades. We’re limited more by public policy than the resource — the resource is enormous.”

But he estimates 80% of geothermal systems remain undiscovered as they have no tell-tale surface feature such as a hot spring. “We’re still just finding the obvious stuff.”

The biggest challenge to harnessing underground power is working out how to access and tap heat buried deep under earth or rock.

“The problem is it’s only being produced in a handful of states. It’s well known in those states but it’s unknown in others.” Gawell said.

The GEA estimates that the number of countries producing geothermal energy will more than double by 2010 to 46 countries.
Volcano Vacations
For those weary of boring cruises where you eat yourself into oblivion and stroll around tropical paradises, a cruise for those with lava running through their veins is now available.

A superliner will set to sail to the remote Russian port of Petropavlovsk, departing from Sydney on July 14th 2008, which will visit 29 ports.

Kronotsky is a major stratovolcano of the Kamchatka Peninsula, Russia that stands 10,168 feet (3,100 meters) above the surrounding plain, located to the east of Kronotskoe Lake, considered to be the one of the most scenic volcanoes in Kamchatka.

The main crater has been completely destroyed. The cinder cones appear to have formed during lateral eruptions of the volcano on the southeast, southwest and north sides of the foot. It has been long considered extinct, but according to the local inhabitants of the area in November of 1922, black smoke erupted from its southern slope, as the volcano “hummed” and shot flames.