Tag Archives: volcanism

Now for some detail on our expedition to the top of Kilimanjaro: pics, commentary, impressions and debunkings…

Ready, steady, go!…

Day 1: Lemosho Gate – Mti Mkubwa.

• Altitude: 2400m > 2800m
• Distance: 4km
• Average speed: 2km/h

And we’re off. Ahhhh, so nice to be in Africa at Christmastime. With Moscow under a foot of snow and Western Europe wet and cold and miserable, what better place to be? :)

Our first day was suitably equatorial to get us into the African spirit…

Read on: Five days and one night to the top…

At Christmastime (“ho, ho, ho”), what better to do than… climb a volcano in Africa? That’s what I asked myself in November of last year… 

…Wind forward six weeks, and there I was, at the summit of Kilimanjaro!

“The first stage of altitude sickness is euphoria: the individual becomes animated, excited, amiable, chatty… almost ecstatic. The second stage is lethargy: the person becomes despondent, sad, bored, subdued and sluggish, with no wish to converse and no appetite.”

Those are the notes I wrote based on the talk our guide in Tanzania, O.R., gave us not long after our arrival in the country. But I think she left the next stage out (she didn’t want to frighten us, after all); so let me add it: The third stage is fatal: a swift worsening of one’s physical and mental state and… hmmm, like O.R., I’d prefer not to go into it. Let me just mention what you’d need if approaching this third stage: oxygen mask, injected medicine, and a call to an SOS medical helicopter service – all ASAP.

http://instagram.com/p/BAZe3gQuiQI/

Read on: Oh my Google Maps! What an adventure we had…

Hello to everyone in this new year!

I hope the holidays went off well, without too much collateral damage, and that the winter break has proved useful for the mind, body and cultural development. All the usual stuff. But now it’s time to return to my tales, travel notes, reports and photos.

Starting the year as I mean to carry on – quietly… Yeah, right!

You need to start the year with a bang! Like this:

No matter who I talk to about Kilimanjaro, they’ve either been to the summit (the majority) or intend to go there in the near future (the minority). A few days ago I joined the majority – on 31 December 2015, to be precise, I stood at the highest point of this volcano. And saw in the new year on Kili!

Due to Internet and time constraints here, the details will have to wait. For now, all I can do is have a little moan about the fact that for this kind of expedition you need to prepare well in advance and very thoroughly. It wasn’t easy.

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.

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

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.

Oh my gorgeous. Fantastical spectacles…

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

Next up on An-Kam-2015 – Ilynsky.

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:

Read on: we FINALLY MADE IT!…

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.

Read on: Stunning, moving, crazy, astounding…

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.

Read on: The Khodutkan hot springs work as follows…

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!

Read on: The fabness of the sunny days…

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.

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!

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

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:

Read on: Canyons, canyons, canyons!…