It’s not really an island, it’s actually what geologists call a “mud volcano,” which is caused by the pressure of sediment breaking up out from underneath the seabed. Basically an island of sand and mud, the mud volcano could last for anywhere from a couple of months to a few years, meaning it’s not here to stay long-term.According to local reporter Bahram Baloch, the island is about 250 to 300 feet in length, and about 60 to 70 feet above the water. You can walk on it, visitors to the island have also said that it is emitting flammable gas.
Within half an hour of the earthquake, inquisitive locals flocked to the island, which according to Rashid Tabrez, the director-general of the Karachi-based National Institute of Oceanography, is the fourth in the region since 1945. Geologists attribute that to the continuing process of continental drift that originally brought the Indian subcontinent to collide with Eurasia. In fact, 700 kilometers to the east of this new mud volcano lies the Makran coast, an area characterized by high seismic activity, and home to several other mud volcanoes.
In the northern Arusha region of Tanzania near the border with Kenya, a geological oddity pokes its nose out of the rift valley floor. It’s Ol Doinyo Lengai, the only volcano in the world that erupts with natrocarbonatite lava.
Natrocarbonatite is half the temperature of the glowing silicate lava you see oozing out of Hawaiian volcanoes and it flows many times faster. It spills forth like water in black frothing streams. If you don’t want to melt your Merrells in 950-degree rivers, you have to watch your step on the summit.
In the Maasai language, Ol Doinyo Lengai means “Mountain of God.” The Maasai’s supreme god and the creator of the world, Ngai, has resided there since time immemorial. Presumably it’s rent controlled.
From afar, the peak of Ol Doinyo Lengai looks like it’s puffing out small clouds, as would a cartoon train. Up close it’s apparent that little clouds have condensed around its cone. It’s not that high, though, at just under 10,000 feet. But height is not the only obstacle to summiting the volcano. When you travel to the middle of nowhere with no guide, luck is a huge factor.
Twenty of us were in Tanzania on a geological field trip with our university’s Earth and Planetary Sciences Department. As an aside, if you want to travel for work, don’t become a travel writer. Become a geologist. You’ll spend way less time in front of a computer and far more time in the middle of beautiful nowheres.
After landing in Nairobi, we rented a 4×4 and two vans to haul us – 19 students and one enduring, stoic professor – into and around Tanzania for two weeks. By the time we reached the turnoff from the paved road to Ol Doinyo Lengai, our luck had expired.
The road to ODL angled parallel to the shoulders of the Gregory Rift, part of East Africa’s Great Rift Valley, across flat expanses of grassy savannah and past a skeletal acacia trees. We were at the tail end of Tanzania’s brief dry season and the acacias had been picked clean months before. The new grasses had yet to take hold in most places, and the road rapidly deteriorated into fields of soft earth. Our vans constantly sunk deep into the loose soil and even our 4×4 lost its footing regularly.
On the uninterrupted African savannahs, you can see a plains storm from a long way off. The dark clouds billow across the sky and below them a torrent of rain dims a uniform trapezoid on the horizon. Dramatic to watch from afar, but impossible to drive through on the unprotected veld.
At this time of year a storm brought more than rain. In front of us on the road, a dark squall sagged heavily looking like a bubble waiting to burst. The fierce winds whipped up dust and sand from the parched fields in skinny sepia tornadoes. We eventually came to a complete halt as we plunged deeper into the storm. The visibility dropped to zero, and we had to sit it out with nothing to look at outside but a uniform swatch of cafe au lait dust.
By the time we arrived at where we thought the Maasai village was supposed to be, 9 hours had passed, and the sun had long since gone down. As we searched for the village in the pitch black nowhere, one van’s bash plate (the protective cover on the bottom of the engine) tore off and then the 4×4′s radiator went on the fritz, causing its engine to overheat and die.
Jerry-rigging a temporary fix for each took time and it was already midnight when we finally found the village. Our plan to begin climbing at 2 a.m. in order to avoid getting roasted by the equatorial sun was completely out the window. None of us had slept. The base of the volcano was still an hour’s drive away. And since we had two broken vehicles we that meant we had to shuttle three separate groups to the mountain in the one working van. Starting at 4 a.m. the first group set out on a couple hours of sleep. With any luck we would get everyone there before the sun launched a full assault on our climbing party.
No luck. The final group began the ascent at about 11 a.m., just as the sun came down on us like Thor’s hammer. I was part of the last group. It took me 5 hours to climb up the steep barren slope, feeling every step like Sisyphus, and clawing my way up on hands and knees near the top. The porters were up in only a few hours, bouncing from rock to rock as if they hadn’t heard of gravity.
At the top I crawled into a shaded tent and collapsed into dreamless sleep. The sun, sensing my respite, sought out my hiding place and began to suffocate me inside. Two ravens named Never and More then lived at the top of the volcano and they squawked with displeasure from their perch on the crater ridge as I burst from the tent gulping for air.
We spent the day exploring the summit, taking samples and clambering around the outer edge of the crater. The summit is filled with tiny peaks called hornitos, which are formed from solidified lava. We came across one spewing forth natrocarbonatite, black like oil. It gushed out of a wound in the hornito’s side and cascaded rapidly down the crater’s slope. Natrocarbonatite lava is completely dehydrated, so it reacts quickly with humidity in the atmosphere and turns white within hours. You can tell how old a lava flow is by its color.
The view from the crater’s ridge was superb. Storms lashed the sky at the depths of the scene, though it was calm and clear nearby. The volcanic ash that has landed around Ol Doinyo Lengai (and other long-dormant volcanoes in the region) creates an extremely fertile soil that grass thrives in, which in turn supports the expansive grasslands’ millions of wildebeest, antelope, zebras and a pantheon of famous predators. An apt name, the Mountain of God.
Night came quickly, as it does by the equator. I was looking forward to a night’s rest on the soft, pliant floor of the crater. Earlier, my friend and I hadn’t thought to tie down our tent because it was so calm in the shadow of the crater ridge…
… Our tent billowed as the gale-force winds became more powerful. We recognized when the tent was smothering us that someone would have to sort this out. I stepped out to pin it down and was immediately soaked and almost knocked over in the wind. None of the pins held when I stuck them in the soil. I called my friend out of the tent to hold it down. He emerged, got soaked, and clutched one corner as I gripped the other. The tent began to lift off the ground, pulling us up and away. We had idiotically attached ourselves to a massive sail. We dug our heels into the ground and braced against the wind. After a moment we looked at each other knowingly, and with a nod let go of the tent. It whipped away, plunging into the blackness.
We fled, pelted by the rain, to the nearest shelter, an occupied one-person tent that had already flooded. The three of us crammed close together to keep warm, knees to our chests, and tried to sleep under one sleeping bag in two inches of water. I listened to the others shivering and noted the cruel irony of being freezing cold while sleeping above a lake of lava.
In the morning light, we found the remains of our tent 20 meters away where it had sailed into the crater wall. I hope his few seconds of freedom were worth it.
With only one van at the bottom of the volcano to bring us back, we decided to retrieve the second van from camp, lack of bash plate be damned. We had driven about 3 miles from the volcano toward the camp when the rumble of a deflated tire brought us to a stop. We had a spare, but predictably the tools to remove it from the underside of the van were AWOL.
Incredibly, after a futile hour of trying to jar the bolts loose with a metal rod, another vehicle came by on the lonely road. A tour guide was scouting out the volcano for a hike the next week and he offered to drive one of us back to camp to fetch the other van. Several hours later, as we sauteed on the road in the no man’s land between the mountain and camp, the injured van came hobbling along, and we were able to use its tools to release the spare tire.
The group reconvened at camp by the early afternoon. We fixed the radiator leak in the 4×4 with an egg, strung up the bash plate with a bit of flimsy wire and negotiated down the porters, who were trying to fleece us for double what we had agreed to pay. As the sun winked out, we lurched away from camp, navigating through honking zebras in the dark, soft-soiled open plain.
The wire holding the bash plate in place promptly failed within 20 minutes and every time the metal intestines of the engine crunched against the hard ground we held our breath. Like an inauspicious totem, I changed vans and immediately my new transport was rendered immobile. I hopped out to check what was going on and saw the van was perched happily on solid ground. We tried four different gears and none would engage. Our clutch was shredded.
Under the van’s headlights we attached a tow strap to the 4×4, which snapped on cue each time we drove through a dip in the road, significantly shortening our lead. When we got up to speed again on the final gravel section, the front of our van was no more than four feet from the rear of the jeep. When the 4×4 braked, if we didn’t react we would careen into its bumper. As we hit 50 miles an hour on the last stretch of gravel road, I turned around to see everyone in the back snoring obliviously. Then I looked over to Jake in the driver’s seat, staring wide-eyed at the taillights of the 4×4, taking deliberately long breaths and blinking on purpose.
When we reached the paved road it was 5 in the morning, 11 hours after we left the village. Jake engaged the parking brake, stepped down unsteadily from the driver’s seat and collapsed in a deep sleep directly on the pavement.
Under a clear night sky next to a crackling fire on a Zanzibar beach two days later, we sipped cold Kilimanjaro beers and toasted our calamitous success. Some adventures are meant to be enjoyed in memory only.
Besides, it could have been worse. Thirteen months to the day that we had slept on the summit, Ol Doinyo Lengai blew its top, spewing ash and lava over the plain in the largest eruption seen in decades. Where we slept on the summit is now a deep crater.
The caves in Spain are famous for their variety and extent. Some delve more than a kilometer into the ground. Others are adorned with prehistoric cave art more than 10,000 years old. Almost all have beautiful rock formations. There’s a whole other world under the one we usually see.
As I mentioned in a previous post, I’m taking a course on caving. My first experience was in Cañuela cave, an easy cave suitable for beginners. Last weekend we went to Coventosa in a remote valley in the Sierra de Cantabria, a tougher cave system that requires more rope work.
The first challenge is what you see in this photo. Here I am worming my way into a little tunnel that slopes down at a steep angle. As you can see I’m tied in with a pair of carabiners attached by ropes to my harness. Why? Because at the end, the tunnel opens out onto the edge of a cliff. Start sliding uncontrollably down this tunnel and you could fly right off the cliff, fall ten meters and smash into a bunch of jagged rocks.
Coventosa is an active cave with some amazing formations. Water seeping through cracks in the rock leaves mineral deposits that harden into stone. Over vast periods of time, these accumulated deposits create stalactites, stalagmites, columns and other formations. Several walls were full of shellfish fossils, evidence that the area was once underwater. Exploring caves gives you an appreciation for how incredibly old yet constantly changing our planet is.
%Gallery-183046%Normally as the water drips down it will create a stalactite hanging from the ceiling. The water hits the floor below, leaving more deposits to create a stalagmite rising from the ground. Eventually these two features will meet to form a column.
If the water is dripping more slowly, sometimes instead of a stalactite you’ll get a soda straw, which looks exactly like what it’s called. These tend to hang straight down or at a bit of an angle if the water is pushed by an air current. Some soda straws eventually turn into stalactites, while others cling to the side of existing stalactites and grow at crazy angles, with the water seemingly defying gravity. There are various theories as to how this could happen, which means that scientists really don’t know what’s going on. We still have a lot to learn about our world.
Caves are one of the last frontiers left to us for exploration. New caves are being discovered every year, and additional tunnels in existing caves are being explored regularly. Caving is pretty much the only way a regular person can discover a previously unseen part of the world.
While I’m years away from that level of skill, the caves in Spain are already giving me a taste of that feeling. How many people have been to the Beach, a stretch of sand next to an underground lake so large that it defied my attempts to photograph it? Or visited the Ghosts and the Virgin Mary, a cluster of eerie stalagmites in one of the deepest parts of Coventosa Cave?
Then there was my favorite, a low gallery with a forest of columns half submerged in water. Our lights couldn’t penetrate to the far wall. As we crouched there, one of the students asked how far it extended. The instructor said it didn’t go much further than we could see and was sealed off by a rock fall at the end. That made me wonder – what if we took away the rocks? Was there a tunnel on the other side? Where would it lead?
Passing between these sights got tricky at times. On one cliff we had to tie into the rope, get around a difficult outcropping, then secure our protection to a second rope. Going up that same route was even more difficult and a couple of us (myself included) made the rest wait as we fiddled around trying to find the best way to do it.
While caving can be physically demanding, it requires more balance and focus than pure strength. The best student in our class is a young woman who is a foot shorter than I am, who flies up and down the ropes with far more ease, and an obvious natural talent. This is a sport that any reasonably fit person can do.
Even so, by the end of the day we were all worn out. As we emerged from the cave entrance we were greeted by the deep blue sky of evening. We’d been in the cave for nine hours and the day had passed us by. Jupiter and a crescent moon shone high above the peaks. In that other world you lose track of time. Now that I’m back in the regular world with its sky and its clocks, I’m marking time again until next Saturday, when I’ll try an even more challenging cave.
The National Trust, which manages the geological marvel and UNESCO World Heritage Site, opened a new visitors center there in July. Soon there were numerous complaints about one segment of the audio tour that stated the dating of the rocks was controversial: “Young Earth Creationists believe that the Earth was created some 6000 years ago. This is based on a specific interpretation of the Bible and, in particular, the account of creation in the book of Genesis. Some people around the world, and specifically here in Northern Ireland, share this perspective.”
This segment was replaced with the statement that there was a, “clear understanding among scientists that the heat of the earth was the driving force behind the formation of the Giant’s Causeway … All the scientific evidence points to a volcanic origin for the columns of the Giant’s Causeway, around 60 million years ago. However, not everyone agrees with the scientific view. There are some people who believe – often for religious reasons – that the earth was formed more recently, thousands of years ago rather than billions. The National Trust supports the scientific view of the formation of the Giant’s Causeway.”
The exhibit is an interactive audio display. You can see the full revised transcript here, and the original transcript here.
Utah’s Monument Valley is home to some of the most iconic rock formations on earth, formations that have played host to numerous nature lovers, photographers and filmmakers who come to soak in their visual beauty. Today’s photo, taken by Flickr user oilfighter, offers us a magnificent and unique look at these world-famous geological oddities. Taken at sunrise, the two lone rock pinnacles lie in shadow, accentuated by the warm yellows and smoky oranges that herald the coming of a new day.
Taken any great sunrise photos during your travels? Why not share them on our Gadling group on Flickr? We might just pick one of yours as our Photo of the Day.