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Mt. Tambora Sumbawa
A big vulcano that erupted in the 19th century
The paroxysmal eruption of Mt. Tambora on the island of Sumbawa in
April 1815 – despite having triggered a world wide historic event
– is astonishingly neglected in studies of volcanic activity. The
world wide event referred to was the so-called "Year without a
Summer" - the exceptionally cold months of 1816. In addition to
this, Mt. Tambora's eruption far-eclipsed in violence and ejecta
the more famous eruption of Krakatau (Krakatoa) in 1883, which
also had an impact on the world's weather.
Though disappointing, the reason for part of this neglect is not
hard to find. There exist few contemporary records of the eruption
and what there is has seen little reprinting in modern works.
Nonetheless, enough data is now available that a more definitive
study can and should be undertaken. The intent of this posting is
to synthesize and integrate what is available and hopefully
inspire further investigation.
Sir Thomas Stamford
Raffles, later founder of Singapore, was at the time of the
eruption serving as Lt. Governor of Java, based at his capital in
Batavia. He had occupied this post since September 1911, a month
after the British had wrested Batavia from control of Napoleon's
France. Having heard of the great human distress and disastrous
phenomena accompanying the outbreak, he gave orders that British
residents gather information and report if possible to him on the
effects of the eruption On April 18, Lt. Owen Phillips was
dispatched with a shipload of rice for relief to the disaster
zone. It is from Phillips' findings, and Raffles subsequent
submission of his report to the Natural Historical Society of
Batavia in September 1815 that we learn after-the-fact of the
details of the eruption. It is important to note that no native
accounts save one are known to survive, and the character and form
of the eruption must be reconstructed "retroactively" working
backwards from the Raffles report and the physical aftermath on
the islands. With this challenge in mind, we proceed.
The eruption Even allowing for the scant documention, the
characteristic about the eruption that immediately jumps out at
the researcher is its terrifying speed and brevity. When this is
contrasted with its stupendous scale and effects, the event
becomes a singularly sobering and daunting one. Perhaps only the
Mt. Tarawera eruption of 1886 in New Zealand compares in modern
times for sheer suddenness and destructive force of eruption. A
word of explanation is in order here. Though such celebrated
eruptions as Krakatau, Mt. St. Helens, Mt. Pelee, and more
recently El Chichon and Pinatubo, capture the public eye and
respect, all of those powerful eruptions had fairly lengthy
eruptive sequences. In short, for those with mind to do so, there
was ample time if not always means to vacate the danger zone. With
Tarawera it was different---in 1886 in the space of one night a
triple peak mountain range near Lake Rotomahana suddenly split
open and erupted. Literally some 4,000 people who had gone to
their beds that evening would never again wake up. Such a
disastrous and only slightly less deadly suddenness accompanied
the Tambora eruption.
The Setting Almost nothing is reliably known about the form and
history of Mt. Tambora prior to the 1815 eruption. (Some
indication of the lack of exploration of the region is gained by
noting that the famous Komodo Dragons on the adjacent island of
Komodos were only discovered in 1911!). However, mountains being
what they are, the remnants tell a great deal to the expert eye.
Although the top of the mountain collapsed in 1815, what still
stands is unusual and provocative in its features. According to
the best available evidence, before the eruption Mt. Tambora was a
volcanic cone 4,000 meters high and 60 kilometers in diameter at
sea level; densely blanketed in forest. It is reported to have
originally had two summits, and there were several parasitic cones
on the east and northeast slopes. What is unusual is that studies
indicate that in its first phase of activity Tambora was a shield
volcano, not unlike those of Iceland or Hawaii. Later, a bedded
cone was built up on top of this, possibly the result of a change
in the composition of the magma. The mountain, which may well have
begun life as an island separate from Sumbawa, in time rose to
dominate a peninsula joining it to Sumbawa on the southwest flank.
By the time the Europeans came to occupy Sumbawa in the 18th
century Mt. Tambora had lapsed into a deep dormancy. This state of
affairs continued for a decade more into the 19th century. Then
the volcanic energies once again burst forth.
At the time of the Tambora eruption, some 140,000 natives were
reported to be living on Sumbawa. Sumbawa is long vaguely
rectangular island running nearly from west to east. About a third
the way from the eastern end, on the north side, a large peninsula
projects northwestward like the trigger of a gun. But this trigger
belonged to a cannon capable of force like no general of the age
could ever have imagined. For it is on this penninsula, the
Sanggar Peninsula, that Mt. Tambora stands. Scattered around in
1815 some 12, 000 people lived in a handful of villages and towns
clustered on the peninsula of Tambora. Forty miles to the
eastward, a small British contingent headed by a Resident resided
at the village port of Bima, the capital of the European
colonists. Bima was located beside Bima Bay, a deep indentation in
the northern side of the east end of Sumbawa, and about 40 miles
east of Tambora's peninsula.
Though some mild spewings of ash were alleged to have occurred at
the summit in the spring of 1814, the first real and almost only
warnings were a rolling succession of deep shocks through the
Dutch East Indies on the evening of April 5. In Dutch Macassar the
warship Benares of the East India Company lay at anchor, the
officers and crew perturbed by what seemed to be a naval battle
taking place just over the horizon to the south. As dusk neared,
the barrage seemed closer, with heavy artillery seemingly
sprinkled with intermitent rifle volleys; just then a detachment
of troops arrived aboard, and the Benares was ordered to put to
sea to investigate. But they found nothing nor the source of the
"cannonade", although they remained at sea for three days. In the
words of a modern author, "that was just as well. For if they had,
there was nothing they, nor all the troops and ships in the world,
could have done about it." Indeed, for their quarry was no pirate
over the horizon: but more than 200 miles south, and what was fast
becoming the most explosive eruption of recorded history.
With sunrise on April 6 light ashes began falling on Batavia. The
sun became obscured in the skies over Java, "having the appearance
of being enveloped in a fog. The weather was sultry and the
atmosphere close, and still the sun seemed shorn of its rays, and
the general stillness and pressure of the atmosphere seemed to
forebode an earthquake. This lasted several days." Oddly enough,
the rumblings and explosions – though they continued – now seemed
to come less frequently and with less noise. The Europeans were
perplexed and concerned, but some of the Java natives, however,
were delighted: priests declared with confidence and satisfaction
that the thunder and dark was the sign that the gods of the
mountains were coming forth to free the island from foreign rule.
However as the ash fall grew and persisted, while the rumblings
and explosions continued, all those in-the-know now realized it
must be a volcanic outbreak, and the speculation was that Merapi,
Kelut, or Bromo was the likely culprit. With the cause if not the
source of the disturbance identified, the Europeans at least
became less concerned and ceased to pay much attention to it, for
this volcanic outbreak was not yet "considered of greater
importance than those which have occasionally burst forth in
Java".
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Mount Tambora
Trekking Top |
Top of Mount
Tambora |
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Top of Mount
Tambora |
Start Trek to
Tambora Mountain |
I,M SUNNY RED JACKET WE ARE AT SUMMIT OF Mt TAMBORA, i DO GUIDE TO
Mt TAMBORA FOR Mr ,Alex Cohan USA and Ms,Natalie at mt Tambora on
April 2007 Great Mountain This educated complacency abruptly
shattered on April 10. As if rebuking their hubris, as the
afternoon came, suddenly the roar and detonations like blasting
gravel and cannon renwed, even stronger than before, and this time
a truly menacing and darkened cloud of ash billowed over from the
east. This time it was even greater than before, so that the sun
was almost blotted out. In the eastern part of Java, the situation
was even more severe. At Solo and Rembang some reported small and
continuous earthquakes, and the explosions were tremendous,
booming frequently through the 11th with such violence as to shake
the houses noticeably. And still the might of the detonations only
increased, and the . Once again the priests sang with joy that
liberation was at hand, and even some of the Europeans now felt
fear and concern. What was happening? None of the suspected
volcanoes were known to be in eruption, and yet almost 2,500 miles
of island chain was being rocked by cataclysmic quakes. Not a few
must have contemplated the fate of Pompeii and
Herculaneum---buried by Vesuvius in AD. 79 – but there was little
anyone could do but wait. These were the conditions on Java and
neighboring islands as dusk approached on April 10. But for those
living on the peninsula upon which Tambora stood, matters would
grow much worse this night. For in the late afternoon of the 10th
Mt. Tambora in fact entered paroxysmal eruption and would inflict
a devastation that would leave precious few survivors to tell the
tale.
Itinerary Tambora Trekking
Tours
TAMBORA TREKKING ADVENTURE 4Days / 3Nights
Day 1 ARRIVAL BIMA - TRANSFERRED TO PANCASILA VILLAGE (L.D)
Arrival at Bima Airport from Denpasar, meeting service and
having lucheon at
local restaurant enroute, transferred directly to Pancasila
Village. dinner and
one night stay at native house. Get rest.
Day 2 TAMBORA TREKKING - OVERNIGHT AT RIM (B.L.D)
After breakfast at native house, start trekking Tambora to the
Rim.
Arrival at Rim and stand a tent and preparing for dinner and get
rest.
Luncheon enroute.
Day 3 RIM - SUMMIT - DESCENT TO PANCASILA VILLAGE (B.L.D)
After breakfast at Rim, continue ascending to the Summit of
Tambora.
Taking picture on the summit and descend back to Pancasila.
Luncheon
enroute. Arrival at Pancasila and having dinner at native house
and drive
back to Bima. Overnight at hotel in Bima.
Day 4 BIMA - TRANSFERRED TO AIRPORT (B)
After breakfast at Hotel, around 10.00am check out hotel and
transferred
for your flight back to next destination at 12.50. End of
Service.
Including In Price:
+ 1 night accommodation at Bima Hotel
+ Trekking tour guide
+ Trekking Gear (Sleeping bag, tent, matras, cooking gear)
+ Meals & Fresh Water
+ Porters
+ Return Transfers Airport - Tambora - Bima - Airport
+ 1 ngiht native house room at Pancasila Village
Excluding In Price:
- Air tickets
- Air port taxes
- Nature expenses
Personal Packs:
Sun block lotion,
hat / cap.
Sun glasses
Camera, Handycam,extra roll film for manual camera of fully
charged battery for digital other batteries.
Small towel
4/6 pcs of T-shirt.
Long trek pants/wind proof
Jacket and rain coat
4 pcs of short
Trek stick/lekki
Torch / flash light
For Reservation and Price
Please contact Us by email : lomboktrekking@gmail.com
Untuk Itenereary Tambora
Trekking di larang keras meng copy paste tanpa se Ijin dari P.T
Lombok Trekking Travel Service
Route
to Mount Tambora Peak
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Route |
Duration |
What We'll Found There |
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Pancasila Village -
Pos I |
1 Hours |
At Pos I, there are
basecamp and spring water |
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Pos I - Pos II |
1 Hour |
Pos II, there we'll
found a small river |
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Pos II - Pos III
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3 Hours |
Accross tropical
forest straight to Pos II, there we'll found spring water |
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Pos III - Pos IV |
1 Hour |
Tropical Forest |
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Pos IV - Pos V |
30 mints |
Tropical Forest |
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Pos V - Crater Rim |
2 Hours |
Accros tropical
forest to Edelweis vegetation and desert. |
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Crater Rim - Peak |
1,5 Hours |
Accross desert |
For complete
information for Mount Tambora Trekking, please feel free to
contact us |
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