Tag Archives: volcanism

Terra Incognita. Southern Kamchatkan volcanoes: Koshelyov.

As our An-Kam-2015 inexorably approached its end, we had just one more volcano to check out: Koshelev – actually pronounced Koshelyov (accent on the lyov).

Though the name is in the singular, this isn’t a single volcano – it’s a set of five different volcanoes, each of which erupted at different times, and which together make up a single massive construction of varied volcanism. Since all the volcanoes are old, they’re all partly collapsed. But that’s just what makes them all the more photogenic.

The parts of Koshelyov we checked out (the western peaks) consist of lava stacks (the centers of former craters) colored with multicolored volcanic remains. Various shades of black, white, red and yellow almost glistening in the bright sunlight of the clear day we were lucky enough to be here on.

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Read on: It was getting really tough towards the end of the trip…

Terra Incognita. Southern Kamchatkan volcanoes: Kambalny.

Though Kamchatka isn’t the most well-known or accessible tourist destination in the world, it still has more than its fair share of ‘touristic meccas’, like the Valley of the Geysers, Tolbachik (especially during an eruption), and the Mutnovsky and Goreliy volcanoes. But it also has less-visited attractions too, for example the Ksudach volcano. Then there are places where a bear‘s paw print in the mud is observed without the slightest increase in heartbeat – as it would be just one among thousands of bear paw prints. And the sight of a human’s boot print similarly calls up zero emotions – as you see humans’ boot prints… never! For no one lives in such places, and only one or two groups of tourists visit… per year! These places are utterly barren, desolate, deserted and silent: Terra Incognita!

Oh, what a shame. For these incognito lands are all must-see! 

Two such must-see spots on Kamchatka’s Terra Incognita are the two volcanoes Kambalny and Koshelev.

Alas, we didn’t climb up to the very top of their crater rims as our schedule wouldn’t permit it. We settled instead for strolling about the area, and in doing so worked out our plan for the next Kambalny/Koshelev visit: to walk from Pauzhetka to Kambalny, then down to Kambalny Lake, and then… we’ll just have to see how much energy is left for onward volcano climbing…

Kambalny is a volcano 2161 meters high, but it also has a volcanic ridge some 15km long, which goes straight from north to south right in the middle of lower Kamchatka – directly between the Sea of Okhotsk and Kurile Lake.

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Oh my gorgeous. Fantastical spectacles…

Read on: Black rock, red rock, yellow rock, white rocks…

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Kamchatka-2015 – Ilynsky – the Kempinski of the volcanoes.

Next up on An-Kam-2015Ilynsky.

This is one grandiose volcano. There’s no arguing about it.

And the bigger – the better. Or so it seems at first… (more on the downside below). Anyway, we decided almost impulsively to get ourselves to its peak, for the views from up there are sure to be amazing – weather permitting.

Here’s what it looks like from the window of a helicopter, and also from the shore of Kurile Lake:

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Read on: we FINALLY MADE IT!…

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Kamchatka-2015: Ksudach – the Countach of the volcanoes.

The Ksudach volcano is one of the most unusual and breathtakingly beautiful places on our planet – I assure you. And since I’m lucky enough to have been practically everywhere on the planet, my assurances can be trusted, I do hope :).

All righty, what we got here?…

Basically, a colossal (7km – SEVEN KILOMETERS – in diameter!), almost perfectly round caldera of a very old volcano, which on maps looks like a crater on the moon. Inside the caldera there’s a cone of a new volcano (whose mouth is approx. one kilometer across); there are also two lakes, hot springs on a sandy beach, scrubby slopes on one side, gray-yellow volcanic slag on the other, and a sheer drop down to one side of the main lake. In all, the most out-of-this-world and unusual and heart-stirring and spine-tingling and goosebumps-giving sight you could ever possibly behold, at least on this planet.

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Read on: Stunning, moving, crazy, astounding…

Kamchatka-2015: Snowy peaks, hot springs.

The second set of amazing must-sees to the south of Paratunka are the hot springs near Khodutka volcano. In fact they’re not just hot springs, they make up a whole hot lake. And not just a hot lake; it’s more of a scalding lake: the temperature of the water hovers around 43°C. Now, if you’ve a heart as strong as an athlete’s, you could take a dip, but you won’t really fancy doing a fast crawl or anything – far too parching. Shame. All the same, just sitting in the lake – still a thoroughly satisfying way of taking in all the surrounding scenery.

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Read on: The Khodutkan hot springs work as follows…

Kamchatka-2015 – warm-up.

My Kamchatka-2015 vacation began in the town of Paratunka. This is a location commonly used by tourists for spending the first night on the peninsula after flying in from afar, before setting off for their first full-fledged destination the next day.

To the south of Paratunka are conveniently located two volcanoes, both of which are must-sees/climbs: Mutnovsky and Gorely. So this year, somewhat logically, we decided to start An-Kam (Annual Kamchatka) with visits thereto – kind of as a warm-up.

It’s just a 50-kilometer drive to get to the volcanoes; however the ‘road’ sure ain’t no smooth autobahn – it’s more a gravel track. Google claims it takes 50 minutes to get them, but in fact it’s more like two hours in a regular all-terrain vehicle – longer with stops. I guess 50 minutes is possible in one of those outsized off-roaders with the massive wheels – or a turbo-driven tank perhaps – but you’d have trouble keeping your breakfast inside you with all the violent jolting about.

After our two-hour cruise we finally arrived at Mutnovsky volcano: beautnovsky volcano.

Though this old volcano remains very active, it’s still possible to walk around the rim of its colossal crater. The sheer scale of the panoramic views, the colors, the rocks and cliffs, the glaciers and snow – fantastic. And there’s constant splashing and hissing to be heard – hot water spurting or hot steam blasting – and everywhere it stinks to high heaven low hell of sulfur. Infernally hellish beauty!

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Read on: The fabness of the sunny days…

Icelandic tectonic.

Everyone’s got a basic idea of how this planet of ours is constructed, even primary school kids. It goes something like this: in the middle of the planet is the core – the nucleus; then there’s the mantle, and on the outside there’s the hard crust, upon which you’re reading this blog.

But the earth’s crust isn’t a single whole piece – it consists of tectonic plates, which float around mostly imperceptibly on the surface of the magma. And they float around in different directions – into one another, perpendicularly, or away from each other. That is, they converge, chafe one another, or diverge from one another. Along the edges of the plates there are frequent earthquakes and all sorts of volcanic activity. For those interested, check out the links above.

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Where plates converge are to be found mountains, volcanoes, and their associated features of terra firma. We’re talking: Japan, Kamchatka, the Kurils, the Aleutians, the Andes, the Cordillera, the Himalayas, etc. Places where plates diverge are usually are on the seabed, visible on maps of sufficient quality and detail: here, under the Atlantic for example is the Mid-Atlantic Ridge. It’s here where tectonic plates move away from one another, with the space between them being filled with magma.

One of the few places where this divergence of plates occurs on land is Iceland: it’s situated along the seam between the North American and Eurasian plates. The former is moving ever-so slowly to the west, the latter ever-so slowly to the east – at a speed of 2cm a year. That is, the width of Iceland increases by two centimeters every year (not taking into account coastal erosion or, just the opposite, the expansion of the land mass on account of lava flows). 2cm a year – that’s two meters a century, 20 meters a millennium, 20 kilometers in a million years. So, if things keep going as they do, in 200 million years Iceland will become the length of Chile, and in in 300 million – the length of Russia!

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The crack in the ground along the fault line is best observed in Iceland at Þingvellir (Thingvellir).

Map of Thingvellir National Park, Iceland

There’s an uneven and craggy crack around five kilometers long that crosses the landscape here, plus a nice lake. This is how it all looks:

Thingvellir National Park, Iceland

Read on: Canyons, canyons, canyons!…

Four tickets to Aogashima – part 2. Hachijo-jima.

A summary of part 1:

07:00. Flight from Tokyo (Haneda) to Hachijo-jima, then a tight connection – helicopter flight to Aogashima, a day there trekking and climbing about, and looking at and taking pictures of every nook and cranny. Beautiful!

The next morning I had a vague sense of déjà-vu: waking up at the impossible hour of 07:30, but this time ‘Boy Scout style’, accompanied by a lively announcer’s voice from speakers all over the hotel: peem paam poom puum ohayo gozaimasu (that’s ‘good morning ‘in Japanese). Followed by a lot more Japanese chatter, of which I only picked out ‘arigato’ and ‘kudasai’. Then rise and shine, get up from the straw mattresses, breakfast – and back to the helipad.

Just to recap: there’s only one helicopter flight a day – if the weather’s good. If it’s bad, no helicopter flight. The Hachijo-jima–Aogashima flight leaves at 09:15 and arrives at the destination around 09:40 (based on our observations). After landing, a regular helipad bustle: unloading/loading freight from/to the ‘mainland’, boarding new passengers – Aogashima natives and stray tourists – and flying back.

Thus, the return flight dropped us off on Hachijo-jima at some 11:30. Our flight to Haneda was at 17:20, so we had some six hours on our hands. How were we to spend that time? Rent a car and go to the onsen hot springs, of course! At least, that was what some of us thought. Wrong! I looked at the map, saw a track leading to the top of the local volcanic blister, and we all proceeded to climb this local Hachijo-Fuji (apparently, all sacred mountains in Japan are called ‘Fuji’) in accordance with this sudden plan.

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Read on: Not a bad sight at all!…

Four tickets to Aogashima.

The other day as I was browsing the Internet I came across a story about a most unusual place in Japan. It’s hard to get to but really worth the effort as it’s both beautiful and interesting. It’s the island of Aogashima, several hundred kilometers south of Tokyo, on the border between the Philippine Sea and the Pacific ocean. ‘That’s worth a look,’ I thought. Next thing… we were there – spending last Saturday on the island. A very curious place; highly recommended!

Now, let’s see what kind of an island it is…

Aogashima is a volcanic still-life made up of an ancient caldera that collapsed inwards, and the rather fetching cone of a new volcano that started to grow within it a few hundred years ago.

Aerial photos report the following:

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The first thing I did was call KL Japan to find out the details of this bizarre island, ask who might be ready to risk traveling there with me, and make other travel arrangements, which turned out to be rather complicated.

Read on: Yes, reaching that island proved anything but easy…

Cool your boots, Japan.

Tired after a seemingly endless journey, the long-distance traveler normally resorts to some kind of body of water first in his/her attempt at winding down, chilling out a bit, and returning from zombie state to kinda normal state. Usually a shower, sometimes a bath – sometimes even a banya and its attendant cold pool!

But only in Japan can one hope to reap the mega-chillage effects of a ryokan, which mixes bathing with a fantastic culinary experience to have you back all recharged and fully energized in no time at all. Which is what happened to me recently at Izukogen Hanafubuki Ryokan on the Izu Peninsula (伊豆), not far from Mount Fuji, Japan. Cool our boots, man, we sure did.

In case anyone doesn’t know what a ryokan is, let me tell you that it is a traditional Japanese hotel, usually not too big, with straw mattresses on the floor, offering super-duper Japanese food plus sometimes hot springs to dip in.

If you’re not Japanese, however, you have to be careful. You’ll need to bone up on the Japanese culture first, as it’s easy to put the proverbial foot in it with some faux pas that will cause upset at best, an international scandal at worst :). Best of all is to visit a ryokan with Japanese friends or colleagues, then there’s no chance of unintended mix-ups/offense. Accompanied by locals, you’re safely under their wing, so can feel just like a Japanese: blissfully content to recuperate for a few days, feed the soul, and revitalize the spirit.

And it’s not just the food and waters that act as a tonic to the body and soul – there’s also all the cherry blossoms still a-blooming here, picturesque little cottages, cozy little paths and an overall abundance of fauna and flora. Most fine.

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Why are we here?

Read on: Rainy day at volcano…