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Pico
del Teide with its strombolian cone
view from top of Montaña Guajara at 2700 meters
Fumaroles are openings in the Earth’s crust, often
in the neighborhood of volcanos, from which volcanic gas escapes into
the atmosphere. Fumaroles may occur along tiny cracks or long fissures,
in chaotic clusters or fields, and on the surfaces of lava flows. From
the perspective of groundwater, fumaroles could be described as a hot
spring that boils off all its water before the water reaches the
surface and as such appear in the atmosphere as steam mixed up with
gases like carbon dioxide, sulfur dioxide, hydrochloric acid and
others. Depending on the heat source, fumaroles can be of short or long
term duration, ranging anywhere from weeks (if they occur above a fresh
volcanic deposit that quickly cools) over months and years up to many
hundreds of years (if they occur above a persistent heat source). The
hotter the source is, the longer the fumarole will persist. The
temperatures are between 70° C - 100° C (158° F
- 212° F) or even more and thus are often emitted with higher
temperatures than even geysers and hot springs, which are much more
known to the public. The gases are often dangerous and are always a
sign of active volcanism. Fumaroles also are not quiet, they however
produce different types of sounds, while they steam. The sound has been
described for example as hissing, roaring, and even thundering. The
sounds are dependent on the force of the steam being released into the
atmosphere. Slowly diffusing emissions will have lessened sounds.
Forceful, blasting emissions produce greater sounds. If there is enough
force, even the ground around the fumarole can tremble as the steam is
released.
Pico del Teide itself is a strombolian
type volcano with a cone of 150 meters height. With its summit (called
'Pilon de azúcar' - sugar loaf - have a detailed look at the
picture above to figure out why) being more than 3700 meters above sea
level it is the third highest volcanic complex on earth. It last
erupted in 1492, the year when Christopher Columbus detected America.
All later eruptions on the island were at different locations. Since
the volcano still permanently ejects high temperature fumaroles of
around 86° C (187° F) through tiny cracks inside the
crater after more than 500 years of no eruption, it is obvious that
there is still a huge and persistent magma source below the volcano.
The fumaroles at the crater are also one of the many things, which are
periodically measured to monitor volcanic activities in Tenerife. One
more point might be of interest. In 2004 was noticed a significant
increase in the number and severity of earthquakes (there were five
felt earthquakes) on the island along with increased fumarolic activity
at the summit of Pico del Teide. Everyone and even the scientists
feared a new eruption on the island. Meanwhile however all measured
values have been going back to normal at least for the time being.....
To get to the cache, you have two possibilities:
The hard way (Terrain difficulty 4)
Drive up to the National Park 'Cañadas del Teide' and park
near 28°15.569 N 016°36.188 W. Have enough water and
enough food with you. From there you just follow the well signed path
up to Pico del Teide, which will bring you to the Cache area after at
least 5 hours of climbing from around 2360 meters above sea level to
3717 meters above sea level. I do not say more about it, as it is
described in many books and on the Internet. There is also the
possibility to stay overnight in the 'Refugio de Altavista' 3250 meters
above sea level.
The easy way
(Terrain difficulty 3))
Drive up to the National Park 'Cañadas del Teide' and park
near the 'Teleferico' (cablecar) at 28°15.322 N
016°36.524 W. Buy a ticket. The 'Teleferico' gets you up to
3550 meters to 'La
Rambleta', from where you walk up to the top and the cache area.
No
matter, whether you
choose the hard or the easy way, prior to visiting this cache, you have
to get a free of charge but written permit, which allows you to walk up
the remaining 150 meters from 'La Ramblette' to the peak of the
volcano. Please
also note that the permit will only give you a two hour time window for
access to the top of the crater. So better be there, if the clock
starts to tick.
Note added
8/22/2010: Meanwhile you can also request
the permit for the access to the crater online here: Request
permit
To be
allowed to log the cache execute the following tasks:
- The
inside of the crater
is covered by the accumulation/accretion of the fumaroles. Looking at
the colours, what is the likely main chemical emitted by the fumaroles?
You can't avoid to smell it too.
- Try
to identify the
number of fumaroles, ejecting steam, during a 3 minutes time frame,
while you are there. How many did you count?
- How
would you describe
the sound, which you hear, when a fumarole ejects a steam cloud?
- What
would you say? Are
the emissions more 'slowly diffusing' or rather 'forceful blasting'?
- Send
me an E-Mail with
the answer to questions 1 to 4.
- OPTIONAL:
Make
a picture of you
with your GPSr from any point at the trail on the top (the crater in
the background). Upload it together with the log.
Please
note, that the cache coordinates point to the middle of the crater and
NOT to a point on the trail. NEVER leave the trail.
Note added 3/21/2013: Just send me the answers to the
questions and
log the cache. I will contact you, if one or more of your answers are
wrong