Kilauea: Ocean entry on Hawaii

 

On September 13, 2016, I set off for Hawaii. Of course direct flights were invaluable and so I booked one with 2 stopovers. Already on the first one my luggage got stuck: in the backpack there were not only clothes but also a part of my photo equipment. Until today the luggage remained lost.

On site I met with 2 friends. Together we explored the volcano Kilauea. It is the smaller of the large shield volcanoes of Big Island Hawaii. In the Halema’uma’u crater a lava lake was bubbling and it stood so high that it could be seen from the Jagger Museum.

In the west pit of the Pu’u ‘O’o crater cone a 2nd lava lake was boiling. The hike here was long and very humid due to the eternal rain. When I finally reached the crater and stumbled to the lava lake, it was foggy and I could see little. The lava lake had a diameter of about 50 meters and was covered in thick gas clouds. There were no useful shots and so I started the long way back. Back at my accommodation in Mountain View, the view of Pu’u ‘O’o was cloudless!

The ocean entry

From Pu’u ‘O’o the lava flows start towards the ocean. They have to travel 6 miles before they reach the Pacific Ocean. Recently, lava flow 61g started to enter the Pacific Ocean and wrest new land from it. This land, in the form of a delta of lava, is extremely unstable: the lava cliffs are washed under by the waves, or blown off by an underground lava flow. Thus, the HVO explicitly warns against entering the lava delta. This is also not reachable without a certain amount of effort. The emergency coastal road was closed and kept open for pedestrians only. Resourceful businessmen from Kalapana rented bicycles for 20 USD, with which the 4 miles to the “ocean entry” could be managed relatively fast. Lava flow 61g interrupted the coastal road on a width of 0.6 miles. The lava field was of course closed and who wanted to admire the “ocean entry” from next proximity had to sneak once again. Of course I did that several times. But you should not underestimate the heat on the coastal plain. My water consumption was enormous. It was increased then still with 2 marches on the Pali. 1.2 miles inland a little glowing lava found its way to the surface. Otherwise 61g flowed completely underground through tubes. I gave up the attempt to stay overnight on the fresh lava field. The underfloor heating was set too high.

The lava at the “ocean entry” was especially beautiful from the sea side. We went to sea 3 times, which was not a cheap pleasure. Depending on the boat you had to calculate with 200 – 250 USD per trip. The twilight trips were mostly booked out 2 days in advance. 2 trips were also cancelled on site. Nevertheless, the impressions burned into my memory, especially since the captain of the “Lava One” steered us right up to the cliffs. Officially this is of course forbidden in Hawaii!

 

Masaya: Lava lake in Nicaragua

Masaya is a volcano close to Nicaraguas capital Managua. In the crater Santiago an active lava lake is boiling since December 2015. I visited the volcano with a team of the Volcanological Society e.V. and we get a permit to stay on the crater rim during day and night. So, I was able to shot this stunning volcano footage of a boiling lava lake.

About Masaya volcano

Masaya is not just the most active volcano of Nicaragua, its a very unusual one, too. The volcano lies within the Las Sierras shield volcano and is a 6 x 11 km caldera with walls up to 300 m high. The basaltic caldera is filled on its NW end by more than a dozen vents that erupted along a circular, 4-km-diameter fracture system. The twin volcanoes of Nindirí and Masaya were constructed at the southern end of the fracture system and contain multiple summit craters. One of this is the currently active Santiago crater. A lava flow from the 1670 eruption overtopped the north caldera rim. (Source USGS)

Colima: volcanic lightning

In November 2015 I captured this volcano footage from Colima in Mexico. Colima was in a state of sporadic eruption from its main vent. The lava dome was blown out from explosions. So, instead of glowing avalances I observed volcanic lightning in the erupted ash clouds.

I traveled together with my colleagues from the Volcanological Society e.V. and meet with Hernando Alonso Rivera Cervantes who guided us. We rented a cabin, just 6 kilometers away from Colima’s summit.

More about Colima volcano

The Volcán de Colima is part of the Colima Volcanic Complex consisting of Volcán de Colima, Nevado de Colima and the eroded El Cantaro. It is the youngest of the three and is one of the most active volcanos in Mexico. It has erupted more than 40 times since 1576.

During last years he activity was dominated by growth of an lava dome. In spring 2015 this dome was blown out by a series of explosions. Since then, explosive ash eruptions occur several time each day. This activity lasted several months. Then the explosions decreased and it began to grow a small dom again.

Kawah Ijen: blue burning sulfur

Incredible video footage of burning sulfur on Kawah Ijen in Java. Kawah Ijen volcano in Indonesia, is the own location you can certainly watch the electric blue fire of burning sulfur.

I traveled together with my indonesian friend and guide Andy. My friends Martin Rietze and Thorsten Böckel were also one of the party. We climbed the step crater walls short before sunset: just during night time the blue flames of the burning sulfur are visible.

About Kawah Ijen

The Ijen volcano complex is a group of stratovolcanoes in East Java, Indonesia. The volcanoes are inside a larger caldera, which is about 20 kilometers wide. Ijen volcano has a one-kilometer-wide acidic crater lake. The lake is the site of sulfur mining operation. Miners carried Sulfur-laden baskets by hand from the crater floor.

Karangetang: Eruption in 2015

Under the light of full moon. © Marc Szeglat

The small volcanic island of Siau is probably known to very few Europeans: it lies about 1/3 of the way between the Indonesian island of Sulawesi and the Philippines. It is one of the spice islands of Indonesia, because most people live from the cultivation and trade of nutmeg and cloves. The climate and the fertile volcanic soil create ideal conditions for the plants. There are also wonderful diving areas and extensive coral reefs off the coast of Siau. And then there is the all dominating volcano Karangetang! In extreme cases, you are nowhere safe from its eruptions on this small island.

The geonauts Thorsten, Martin and Marc set out there at the end of August 2015 to document the eruption of the volcano. When the news about the beginning of the eruption reached us, we were just at the Kawah Ijen in eastern Java. But even if you are already in Indonesia, the way is long and more complicated than e.g. the journey from Germany to Stromboli in Italy. First we had to take 3 domestic flights to Manado, where we arrived late in the evening. After a hotel night we went on an express ferry, which took almost 5 hours.

When we finally reached Siau and the volcano, the morphology of the island with its islets reminded me of a half-sunk caldera, on whose flank the new volcano with its 5 craters had formed. But in the scarce literature on Karangetang there is nothing about a caldera.

First Karangetang presented itself cloudy and we made our way from the harbor to the recommended hotel. This turned out to be adventurous and overpriced, but it was the only one here.

We went to the village to get something to eat and when we were done the clouds had cleared away. Only now we noticed how close the volcano was. From the roof of the hotel we had a box seat with an unobstructed view of the active fire slide: over the southern slope of the volcano, glowing lava avalanches kept coming down, fed by a lava tongue. This extremely tenacious lava flow poured down the slope from the south crater for about 200 m, where it stagnated at first. Some debris avalanches were so large that not much would have been missing and they would have become pyroclastic flows. Of course, we were aiming for these. However, the hotel, like the whole place, was not a safe place if really large pyroclastic flows were to occur. Even more exposed were some smaller places directly below the fire slide.

The next day Karangetang presented itself overcast. Only in the late evening did the curtain of clouds lift and allow a view of the fiery spectacle. The situation had changed significantly in the last hours. Two arms of the tenacious lava flow had left the upper volcanic flank and had almost reached the base of the fire slide. However, the surface of the flows had mostly cooled down and only one front was glowing. We positioned ourselves on a parking lot in a place directly below the fire slide and took pictures of the lava flows. Around midnight some drunken locals became unpleasantly pushy and I had to put them in their place, although I was afraid the situation could escalate. Fortunately our warung-host came by with his truck to check on us and brought us back to the hotel. Half an hour later there would probably have been a brawl.

The next unpleasant incident happened in the morning of our spontaneous departure: at the Lokon on Sualwesi there had been an eruption and we left in a hurry. In the rush Thorsten already paid the hotel and handed over the money to the employee behind the reception. Then he went packing and wanted to pick up the bill afterwards. Then we were told that he had not yet paid. The counter was searched umpteen times for the money and the employee leafed through a notebook several times. Only when Thorsten became energetic and hit the table with his fist did the money reappear. It was in the notebook, which had already been flipped through several times! The two incidents, coupled with the unkempt hotel and the dirt in the village, depressed a little the mood and the otherwise positive image of the volcanic island Api Siau.