LATEST NEWS
FROM Ol DOINYO LENGAI
December 2007 -
PRESENT
Link
to directory of news archives
I will post news about
Lengai here whenever it becomes available. The most recent news is at
the bottom of the page. If you have climbed Lengai or made photos from
the air please send me your observations and I will include them here.
Your contributions will be much appreciated by those who track the
activity and changes in the crater.
Photos on this page are
property of the individuals named and should not be used without
permission. Without the generosity of these contributers we would
not know what is happening at Lengai. Please respect their
rights.
December 2007: Roger Mitchell reports:"On the basis of
our investigations, Barry Dawson
and I have submitted a
paper to Mineralogical Magazine on the character of the ash erupted on
Sept 24th. This turned out to be a hybrid magma formed by the
assimilation of natrocarbonatite by a nephelinitic magma. The material
resulting from the desilication of nephelinite is a novel magma for
Lengai and the ash particles consists of:
nepheline+Na-melilite+combeite+ Na-Ca-phosphate-carbonate as major
phases - . Minor components are wollastoniteTi-andradite,
K-Fe-sulphide, Mn-magnetite. Very minor groundmass is high-P
gregoryite-like material plus nyerereite (< 5 %) Note primary cpx is
NOT present, hence this is NOT a melilitite or a nephelinite. Seems to
be an extreme variant of the 1966 ash."
December 2007: Joerg Keller and Jurgis Klaudius report: "Although
the
eruptive activity and changes of the crater morphology were
documented by photographs from the air and from the base of the
volcano, very
few visits to the summit are recorded in the whole period since Sept. 4th.
Access to the summit of Oldoinyo Lengai has become rather difficult
since the
paroxysm of early September. It appears that, to our knowledge, only
Tim Leach
from Ngare
Sero Mountain
Lodge/ Ngare Sero Lake Natron Camp could visit the summit with his
Maasai
guides and helpers in exploring a new route from the south or east. We
used
this route with the help of Tim’s Maasai guides Saringe, Tumba and
Lekoko. The route follows a
prominent steep ridge from the
east or slightly southeast ending at the
south-eastern edge of the south crater depression. The track is quite
strenuous
(to say the least!) and takes much longer than the old trail from the
west,
although being rather direct. However, with ongoing explosive activity,
the
south crater is the only safe arrival place.
The summit was reached
at 7 am on the 7th of December after seven hours of climbing. During
the stay
in the summit area for about 5 hours Jörg Keller collected fresh samples of black
lapilli, ash and bombs from the
active intra-crater cone. This material is
now
investigated to characterizethe new silicate magma involved and will
complement the observations of Roger Mitchell and Barry Dawson on the
ash blown
out on Sept 24th.
For
a possibly
easier descent, it was attempted to use
the old western route, but this idea had to be given up because the
very
cemented surface of the lapilli beds provides no grip on the steep
entrance
from above into the ascent chasm. Really dangerous! About
the
ongoing activity, Oldoinyo Lengai is sending
on and off its ash plumes high into the atmosphere. The intermittent explosive
activity during the period of our stay, with
ash plumes increasing in height to up to several thousand meters above
the
volcano alternating with periods with minor puffing or degassing, or
with
seemingly dormant phases, was obviously rather representative for the
three-month
period following the 4th September paroxysm. There are entire days when the volcano appears
calm, resuming then at
surprise with impressive explosions and ash plumes. So happened when
Jörg
Keller was just leaving the north crater towards the southern
depression (after
successful sampling in the ring plain around the new intra-crater
ash-and-cinder cone and on its slope). Given the
witnessed suddenness of the onset of
explosive activity this is a clear indication of the existing dangers
in the
summit area."

Onset of
the 7th December
ash eruption at 11:07 photographed by Joerg Keller from
crater rim
towards the
southern depression looking north.

7th December
ash eruption at 11:07 photographed by Joerg Keller from crater rim
towards the
southern depression
looking north.

The
ash-and-cinder cone within the north crater of Oldoinyo Lengai (Joerg
Keller)
Additional Information provided by Joerg Keller: "The climb is on an ever steepening and narrowing ridge separated by the
erosion rills that characzerize the southern sector. The whole thing is mostly on ashes (of the 1966/67
and of the recent eruption. No rock climbing but in the upper part quite exposed with walking on very narrow ridges.
Given the difficulties, I would imagine that in a group with mixed experience there is also the potential of individual failure.
The track is certainly also difficult for bringing equipment to the south crater depression. I must underline that the situation
of the mountain has completely changed. The south crater is a barren ashy landscape with the vegetation almost
completely destroyed. It would be possible in my view to camp there, but not too pleasant. As explained in my text,
I consider the north crater a dangerous place. It is blanketed with recent lapilli beds, and impressive strewn fields of
heavy bombs and blocks. With ongoing explosions it is certainly possible to select relatively safe directions, with calm
moments you will not know were a possible next shot is directed to."

This photo by
Jurgis Klaudius shows the ridge which was used for the ascent. It is on
this
photograph one of the gray (ash coverd) sharp ridges, the most
prominent
and continuous
one pointing directly to the highest peak on this photo. It is
exactly the third gray ridge
from the left. The photo was taken by Jurgis on Dec 7, about
11:00.
December 2007:
A small group, including Jens Fissenebert of Moivaro - Lake Natron
Tented Camp & Campsite, visited the summit of Lengai on
Dec 25 by helicopter and
have
posted their photos at http://picasaweb.google.com/Moivaro.Lake.Natron.Camp/Lengai25thDecember
A few selected pictures from the site are shown below. Some of
them
reveal that the ash cone has now grown to cover nearly the entire
northern
two-thirds of the crater floor. It is now the only distinguishable vent
in the crater, having covered up all other cones, with the possible
exception of the tip of T49B which may be seen emerging from the cone
in some photos. (So far several
Lengai watchers have agreed that the new cone be designated T58
since that is the site of the former cone from which this eruption
began, however, this might change.) The northern and western
parts of the crater rim are no longer distinct, having been mostly
covered by the growing flank of
T58. Newly erupted ash and lapilli has filled in the flank area
below
the
former crater rim and down through the "Pearly Gates" through which the
former climbing route passed.
At great risk to their lives the visitors wandered around inside the
north crater and climbed to the edge of the active cone.
The following 6
photos are courtesy of Jens Fissenebert, Moivaro - Lake Natron
Tented Camp & Campsite

Lapilli and ash have deposited on the NW flank above the Pearly Gates,
making the climbing route impassible.

The slopes of the cinder cone have covered the NW and W crater rim.

The eruptive vent totally domonates the North crater.

The small spike on the far rim may be the remains of T49B.

View into the active vent

This could be the remains of T49B. Note the bombs littering the rim of
the cone.
December
2007: Raphael Wolf reports: " I climbed Ol
Doinyo Lengai on the 31st(new years eve) of Dec 2007. It
shook 3 times as my guide and I were
climbing." Below is a photo Raphael took looking into the vent of
the new cinder cone.

Photo courtesy Raphael Wolf
January 2008: Vegard Laukhammer reports: We were
four people that were only 50metres
from the top when it erupted this Monday (January 14).
We barely survived. Luckily the lava never came towards us so we
only
had to get out of the shower of stones. His email included
reference to a website, http://www.vgb.no/14423/perma/280695.
A translation of the text from Norwegian to English has been
provided courtesy of Sven Dahlgren,
a
member of the Lengai 2002 expedition. (Editor's note: There is
serious doubt that there
was actually any flowing lava involved in the eruption; evidently the
guide feared lava but did not actually see any lava.) The translation
is as follows:
" We are
still somewhat shaky after the extreme experience yesterday. After a
fantastic
excursion in the weekend, where we visited a Masai village on Friday
evening
and were on a spectacular safari at Ngorongoro Saturday, we were ready
to climb
the volcano Oldoinyo Lengai the night between Sunday and Monday. The walk
took us to nearly 2700 m a.s.l. and was very strenuous with 6 hours
walk from
midnight. The last two hundred meters we were climbing straight up like
monkeys.
According
to Vegar’s watch we were at the summit at 06:52. The visibility was so
poor and
there were so much smoke that we decided to try to climb down again
after 10
minutes. And LUCKY LUCKILY for that…. About 10
minutes later (07:15), when we had been able to climb about 50 meters
down from
the summit, a thundering, ear-breaking sound came from the volcano. A
large
shower of rocks (many the size of a football) were thrown out from the
volcano
directly towards us 4 on the top. Our local guide yelled what we all
already
felt – today we’re gonna die….!We
rushed
down the mountain slope (we just had
been afraid to climb up). We were running, falling and rolling down
within a
big cloud of dust, rocks and ash from the volcano. Vegar and
I, and our guide, managed in one or another way to fight us to the
right and
out of the main cloud. And we continued with some crazy stunts down the
mountain slope in cracks and crevasses, when our guide is shouting: The
lava is
coming, the lava is coming!!
With all
the power we managed we rushed down for about one hour, the same
distance we
had spent 6 hours climbing up… In one or another miraculous way we were
not injured (although Vegard got some significant
scratches and cuts, both our butts are fairly well-scrubbed, and we are
totally
beaten up). BUT ALIVE!! Totally we
were 10 persons on the mountain (the others did not reach the summit
and were a
bit lower down than us, though they were directly down-slope from the
eruption.
We were absolutely certain they had perished. Being
afraid of new eruptions, and with a guide preliminarily blinded by the
sulfuric
dust, we spent more than an hour to maneuver ourselves out of a
labyrinth of
old deep lava crevasses and back to the car that was parked at the foot
of the
mountain.
Totally
exhausted we could with great satisfaction see that one after the other
appeared in safety, and we could finally permit ourselves to react on
the
incident.
The last
man that was among us on the mountain, had injured
both his ankles after a long and dangerous rush down some old lava
crevasses
(the lava was luckily limited, and to the other side) and he had to be
helped
down the last distance by our brave chauffeur
January 2008: Jens
Fissenebert of Moivaro - Lake Natron
Tented Camp & Campsite has reported that the groups on the 14th
January (see report of Vegard Laukhammer above) all went up the
old west route through the pearly gates. This explains why the
guide feared that lava might flow down on them from above. This
experience shows that the old climbing route is far too dangerous to
use now!
Jens also reports: "As we've been up on the
25th
Dec., the
south crater was filled with ash, but you couldn't see any stone
impacts. On the
4th Jan. the helicopter group reported that it (the South Crater)
was
looking like after a bomb hail.
That's
why I'm worried even to climb up the new route and also to camp there."
January 2008: Paul Johns reports "We were the ones that
took Jens
up the volcano on Dec 25th. On Jan 6. we landed in the south
crater
and walked to the peak. The volcano
erupted on our flight to the crater and again 15 minutes after we left,
I guess
we were lucky. Once we landed we could see the size of the rocks that
were
being thrown into the south crater, we estimated that these rocks were
less
than 12 hours old, as the soil was still damp and freshly
disturbed."

Impact site in the South Crater of a block (or possibly a bomb) ejected
from the ash and cinder cone (T58) in the
North Crater. Photo made Jan 4, 2008. Photo courtesy Paul
Johns.
January 2008:
Tom
Pfeiffer of Volcano Discovery has
posted an extremely informative report of a 17-21 January expedition at
http://www.volcanodiscovery.com/volcano-tours/lengai/activity_report/17-21jan08.html
It is clear from this photo
of the impact site and from Tom's report
that visiting the summit area of Lengai is now extremely dangerous!
January 2008: On the 19th of
January,
led by the Maasai guide William,
Bernhard Donth (Saarbruecken) and Thomas
Schulmeister (Berlin) climbed Oldoinyo Lengai from the old route
(NW flank
above the Pearly Gates). "During ascent there was occasionally rain of
fine grey
ashes and small white pebbles into the route.
About 200 m under the top plateau we heard (but did not see) the
sound
of nearby flowing lava (?) known from the former hornitos. Our driver reported at the same time from the
parking place by radiophone that there is a small flow of black lava to
be seen
on the left of the Pearly Gates wall. This observation could not be
verified up
to now. After eight hours climbing at 01:40 p.m. the active crater
floor was
reached. There was no fresh lava to be
seen inside and outside of the active main crater. Permanently there
were small
ash jets from the active crater. While
the eastern part of the plateau is covered by smaller and larger
stones, the
west side consists of much smaller particles. While
the way up is passable if an ice pick or
geological hammer is used, the way down seems to be impossible without
using
further alpine equipment. Therefore we crossed the plateau and went to
the
south crater. For the way down the new route, beginning at the far
southeast
edge of the inactive south crater, was used. At the summit ridge we saw
the
Volcano Discovery team of Tom Pfeiffer, which camp in the south crater.
We did
not visit the top of the summit ridge because of the late hour. The new
way
down is steep and sandy but short and quite sure (less than 3
hours)." Some first pictures can be seen
at http://www.schulmeister.org/Lengai08
(ED NOTE: Many of these photos are panoramas and are extremely
informative about the changes to the crater during this eruption.)
January 2008 :Phil Benham sent photos of their January 18 visit with Nature Discovery during which they
camped on top for two nights. He forwarded several photos, one
of which is shown below: A large number of additional excellant,
detailed photos of the activity and summit area are posted at http://www.kodakgallery.com/I.jsp?c=86ee2wd.cdr2yfqp&x=0&y=d8d01o

Photo courtesy Phil Benham
January 2008: Thomas
Holden
of Nature Discovery (A safari
company in Tanzania)
has reported on a new
climbing route up Lengai. He writes: “Here's the latest news on the
re-opening
of Oldonyo Lengai on a new route from the SE: On the 18th of January,
led by
guides of Ngare Sero Natron Camp (with many thanks to Tim Leach of Lake
Natron
Ngare Sero Camp), we climbed Lengai from a new route on the South East,
a mere
1 hour drive from Ngare Sero village to reach the starting point. We
found this
route a vast improvement over the old route (and also the other
southern routes
we recently attempted) and although a steep alpine adventure style
trail, the
route follows an unbroken ridge ascending without any big drops or
exposed
sections of scrambling. Most importantly, this route crests the summit
area at
the far southeast edge of the inactive south crater, with the summit
ridge to
the north acting as a buffer to the active north crater. From the south
crater
we continued to the summit ridge counter-clockwise to the west, to view
the
active crater from the top of the summit ridge. We did not descend to
the
active crater floor, as any significant eruption while down there could
certainly spell big trouble."
In a later email Thomas adds this about the new climbing route: "The old route,
near the top was steeper and more difficult than any part of this new
route.
The new route does not have any sections like that, nor does it have
any
chasms, holes, or drop-offs which one could potentially fall into. The
only difficult
thing about it is that it’s a new route, and we need to ‘wear it in’,
as in-
dig a few more footsteps and make a few switchbacks on the steeper
sections, to
make it easier to keep footing.
"

New SE ascent route. Photo courtesy Thomas Holden
February 2008: Michael
Dalton-Smith reported in a
Feb 4 email:
“I'm in Tanzania
and in view of Lengai. The
mountain is very active, and I have seen several eruptions. There was a
fairly
big one yesturday at 12:00 pm with a cloud that rose about 3000ft above
the summit.
Activity was present all day with a stop around 4pm, and then renewed
activity
with ash rising 1000-1500ft above the crater. It was clear this was
small
effusive eruptions of ash. This morning atsunrise (6am) however there
was a
larger eruption with the ash rising about 4500ft. It was a fairly dense
cloud
that flattened out at the top. I am currently in the Gol mountains just
east of
Sanjan gorge, and the camp manger of asilia said there was a several
large
explosive eruptions 3 days ago. Two bangs could be heard in the morning
and the
evening. it was too hazy for photos. An interesting note, the guy here
says
that the position of the ash column has moved further north in the
crater maybe
suggesting that new vent has opened closer to the edge of the crater
floor on
the north side.”
February 2008: Michael
Dalton-Smith reported
in a Feb 6 email: "Opted out of
the climb, eruptions have been too strong, we drove past Lengai today
and it was
having some of the biggest eruptions in a long time. Active
continuely from
sunrise to about 2pm."

Lengai erupting on Feb 6. Photo courtesy Michael Dalton-Smith
February
2008: Michel Picard was
flying
from Seronera to Arusha on Feb 12 and photographed a dark ash cloud
above
Lengai.

Photo courtesy Michel Picard
February 2008: Gerrit Jan
Plaisier and Rob Alakopsa
of KLM Royal Dutch Airlines
forwarded photos of Lengai made at 0755 UTC on Feb
15 by a MartinAir flightcrew. Plume
is estimated to rise to 36,000 ft.

Photo courtesy Martinair flight crew
February
2008: Nigel D’Aubrey sent the following
photo that he made while on El
Al flight 512 from Johannesburg to Tel Aviv on Feb 20.

Photo courtesy Nigel D'Aubrey
February
2008: Jurgis Klaudius, who has studied Lengai
for a number of years, writes a safety warning from
Freiberg, Germany: "I have to
propose that the whole upper cone area shall be a "no go". I have
experienced
the sudden onset of the explosive eruptions, which appear without any
kind of warning.
and those I have seen are minor "puffs" compared to the event,
recorded by the picture of the aircrew. it seems that the intensity of
the
eruptions is highly variable, therefore their impact is not
predictable! if an
eruption like this occurs during a stay at the summit area, there is
hardly a
chance to survive!"
February 2008: Claude
Humbert writes:”I was part of a party of 11 people, mostly
French (one
Spanish), we attempted to climb on the southern side on February 24,
2008,
starting at 3 AM. About halfway from the summit, the person in
charge of
the group decided to stop and start climbing down.” Claude sent
the following photo of lightening in the ash plume. Additional
photos of the same visit were forwarded by Evelyne Pradal. A report will
be sent later.

Photo courtesy Claude Humbert

Lengai seen from Engare Sero camp area. Photo courtesy Evelyne Pradal.
February
2008: Michael
Dalton-Smith reported
in a Feb 27 email: "It seems
as
if
Lengai's eruptions are getting stronger. My business
partner is still in Gol, and said yesterday
that Lengai blew 4 times the height of
the pictures I sent you. (See second photo above.) He said it was
a massive cloud and came with a bang. You may be
interested to know, we asked the Masai from the village
closest to Lengai if they would evacuate or
if they were scared of the volcano, and
they replied that if the volcano were to blow and kill
them all it would be the wish of their
god Lengai. I think it is a very heightened spiritual time there right
now. The
village closest all seem to be full of Masai."
February 2008: Dave Rhys
writes: “I just returned from Tanzania
where we witnessed distantly from the Serengeti Plain and Ngorongoro
Crater three eruptions of Oldoinyo Lengai on February 27-28,
and
later by plane leaving to London
on Feb. 29. The single ash plumes rose rapidly each time but were
not followed
by any continuous eruption, and were dispersed rapidly afterward on Feb
27-28
by strongly northerly winds which dispersed the ash clouds
southward. Thin
ash coatings on plant leaves were observed around the rim of
Ngorongoro
crater the next day distant to roads which may have provided dust, and
on
surfaces which were previously clean the day before.”

Photo courtesy Dave Rhys.
March 2008: Max
Voigt made the following photograph while on a Nairobi to
Johannesburg flight on March 1.

Photo courtesy Max Voigt.
February-March 2008: Ben
Wilhelmi sent the following photos he made in late February and on
March 1 and 2.

Photo courtesy Ben Wilhelmi.

Photo
courtesy Ben Wilhelmi.

In this view it seems that the tops of two old hornitos appear at the
lower right rim of the
ash cone. Photo courtest Ben Wilhelmi.
March 2008:The
following pictures by Tony
Drummond-Murray from 3 - 5 March are of
possibly the strongest eruption ever photographed at Lengai! This shows
the extreme
danger present on even the
lower slopes of the mountain. The second picture appears to show
a pyroclastic flow
from a collapsing ash column, or
if not that, a debris avalanche from collapse of part of the crater rim
or the new cinder cone.
Tony writes:: “My Wife and I have just returned from Lake Natron
Area (early March 08), and were prevented from scaling the mountain by
several massive erruptions that seem to be larger than any shown on
your, or other sites. The volcano, and immediate environs, is
definately NOT a place to be!
We saw several substantial emissions, each of which started "after
breakfast", with a very quiet run up. There were several massive
ground strikes of lightning from the thinner sections of the
cloud to ground (the lower slopes of the mountain), certainly on
05/03/08. I was of the opinion that these were comparable in length
with the actual height of the mountain itself. We thought there were
strikes within the cloud too, but these may have been ground
strikes that we did not actually witness. Sadly on the 05/03/08 date,
there was light cloud present before the eruption, and this
restricted views of the cone. I would not have thought that it was of
sufficient size/density to have contributed to the lightning that we
saw.
I did try, with binoculars from the Camp Site, to see if there was any
"red glow" to be seen at night (04/03 & 05/03). I was unable
to detect any, but suspect the high density of the cloud would
prevent any visible light escaping the inner cone.
The whole of the valley between Oldonyo Lengai and the Escarpment
itself was covered with a highly visible layer of light ash after the
eruption on 04/03, a process that was doubtless repeated on 05/03
too. We understand too that the local Villagers, certainly within the
dusted area, were being evacuated, as their animals could not eat.
We did hear some thunderlike noises at the camp site on 3 Feb. We took
this to be the sound of the eruptions, but this was our first
experience of the volcano, and it might have been thunder, but I saw no
lightning at this time.
On the 5th, the plume appeared larger, even, than on the 4th. From
our vantage point, and we had driven out of the Camp Site and
turned generally "left" towards the top of the Lake (perhaps a
mile or so from the Site), the peak of the plume appeared to
stretch from the summit to VERTICALLY overhead, as well as being
distributed downwind towards the Escarpment."

Photo courtesy Tony Drummond-Murray

Photo courtesy Tony Drummond-Murray

Photo courtesy Tony Drummond-Murray

Photo courtesy Tony Drummond-Murray

Photo courtesy Tony Drummond-Murray
March 2008: Pilot
Ben Wilhelmi sent the following photo made 10h10 on March
5. Estinated plume height 50,000 ft.

Photo courtesy Ben Wilhelmi
March 2008:
Ben Wilhelmi sent the following photos made 11 and 12
March.

Strong ash eruption seen from the east. Photo courtesy Ben
Wilhelmi

This March 12 photo shows that the powerful eruptions of March 3-5 did
not significantly alter
the ash cone or crater rim. Large amounts of ash and cinders have
piled up against the
northward facing ridge below the summit. Photo courtesy Ben
Wilhelmi

This image shows that the east, north, and west flanks of the ash ash
cone have buried the
original crater rim. Oversteepening of the cone flank has in
places resulted in small landslides
which can be seen as dark material covering the lighter areas of older
weathered carbonatite
just below the cone. Photo courtesy Ben
Wilhelmi.

View of the south crater from the east shows an ash and cinder layer so
deep that previously
prominent erosion gullies are becoming indistinct. It appears
that all vegetation has either died
or been buried under ash. Photo courtesy Ben
Wilhelmi
March 2008: Kent Richter
made the following photo while camped at Thomson Serengeti Nyumba at Robanda on 16
March.

Photo courtesy Kent Richter
March 2008: Thomas Unterweissacher
made photos of the eruption on March 16 from the summit of Mt Meru.

Photo courtesy Thomas Unterweissacher
March 2008: Ben
Wilhelmi sent the following photos made on 18 March at 1530 local
time.

Photo
courtesy Ben
Wilhelmi.

Photo
courtesy Ben
Wilhelmi.

Photo
courtesy Ben
Wilhelmi.

Photo
courtesy Ben
Wilhelmi.

March 2008: Ben
Wilhelmi sent the following photos (0930 March 22) looking
straight down into the crater. He reports that as of March 22 there
have been no reports of activity for three days, and that a smell of
hydrogen sulfide is back after not having been present for a long time.

Photo
courtesy Ben
Wilhelmi.

Photo
courtesy Ben
Wilhelmi.
March 2008: Thomas Holden
reports that as of March 29, there has been no activity at Lengai for
10 days.
March 2008: Paul Westerman reports: "I summited Ol Doinyo Lengai on
3/25 (pictures attached) around
11am with a friend from Arusha and a local maasai guide. Walked
to the
top of the ash cone and heard the tremendous roar. No
sulphur smell
but some heat. The next day 3/26 we observed some smoke
and ash
fall (on the downwind side) starting around 9:30am while we
were at the shore of Lake
Natron."

Photo courtesy Paul Westerman
April 2008: Chris Daborn of Tropical
Veterinary Services Ltd reports on April 2: " Lengai has of
late quietened down significantly - first in changing ash colour
from a "salty" white to a more inert black and now with much
smaller eruptions that barely extend above the
mountain. We have heavy rains on at present which makes
movement in the area difficult - but are also washing ash residue away.
April 2008: Jurgis Klaudius
reports:" I just checked modis data and found that there was a thermal
anomaly
in the north crater on 3rd of April indicating that the eruptions are
still
going on."
April 2008: Ben Wilhelmi flew over
Lengai on 7 and 8 April and sent many photos of the crater and the
flanks of Lengai. The flanks show newly formed erosion gullies in
the recently deposited ash. Lengai was inactive on the 7th but
erupted on the 8th.

Crater on April 7. Photo courtesy Ben Wilhelmi.

This is cropped from an image of the flank and shows an
unusual feature resembling a lava flow from a flank vent,
but is more likely the track of a bomb tumbling down the flank
or some other disturbance to the surface. Photo courtesy
Ben Wilhelmi.

Eruption on April 8.
April 2008: Recent reports from
Ben Wilhelmi and Michael Dalton-Smith indicate that
Lengai has shown little activity during early April, although
visibility has been hampered by atmospheric clouds on several occasions. Photos from the air by Ben Wilhelmi showed no activity on
April 11.
April 2008: Matthieu Kervyn reports
that MODIS data has indicated a significant hotspot on Lengai on April
17, showing that activity, although intermittent, is continuing.
MODIS also detected the eruption of April 8 shown in above photos.
May 2008: Chris Weber of Vulkan Expeditionen
International and
Marc Szeglat visited Lengai on 14-16 May. Chris reports: "Only minor
ash eruptions were reported by local Masai after the last noteable
eruptions on
8 April and 17 April 2008. Some of the evacuated local Masai had
returned back
to their settlements, but part of the livestock had not returned from
evacuation
sites yet midd of May 2008. The volcanic fall-out of pyroclastics was
still
visible around the volcano. Due to a heavy rain period (season)
vegetation
damage was not as severe, as it could have turned out by this strong
explosive
eruption period of O. Lengai (BGVN 33:2). Up to around 1000 m altitude
the
vegetation, mostly “Elephant grass”, normal grass and some Akazia
trees, were
undamaged around the volcano, except for the western sides where severe
damage
of the vegetation occurred as far as 10 kilometers away from the
summit. Some
lahars had happened on the north and northeast of the volcano’s
outruns. The
elderly Masai reported, that in compare to their visible observations,
the
recent eruption period was stronger than the 1966/1967 explosive
event. The former
common trekking route (track) up O. Lengai is not recommended so far,
because
of rockfall hazards and bad hiking conditions. We used a very steep
route on
the SE side (named “simba route”) of the volcano to climb up. From
about 1000 m
altitude volcanic ash-layers were clearly visible on the ground, but
new grass
had already grown since the eruption. At approximately 1500 m on the
SE-
volcano flank, all vegetation started to be covered (or being
destroyed) by
volcanic pyroclastics (“ash fall out”). From about 2500 m, additional
impacts
of volcanic bombs were visible. The volcano’s inactive south crater was
the
location of our camp site. All vegetation was wiped out and volcanic
bomb
impacts from the last explosive events on April 2008 were quite
impressive to
study. The active
north crater of O. Lengai had a new morphology. The diameter of the
crater from N to S was 300 m
and from
E to W 283 m. The crater floor was at approx. 2740 m altitude,
accordingly 130
m deep seen form the west crater rim. Two vents
were
located as c1 and c2 inside the crater and obviously not at older
hornito
locations. Both vents were
dergassing
with strong pressure and quite noisy. On 15 May a period of powder ash
eruption
started until midday. This happened again on 16 May,
unknown which
vent was responsible for this. After our descent we visited an
abandoned Masai
boma on the west side of O. Lengai. The “ash fall” forced
the local
family Lesele to flee from their home only a few kilometers away form
the
summit of O. Lengai."

Photo courtesy Chris Weber

Photo courtesy Chris Weber

Photo courtesy Chris Weber
June 2008: A fly-over by Ben Wilhelmi shows an ash eruption
on June 8. Photos made by Ben on 1, 3, 10 and 12 June show no
activity.

June 8, 2008. Photo courtesy Ben Wilhelmi
June 2008: The photo
below by Fred Belton shows an
ash-poor plume above Lengai at about 3 PM on June 12.

Photo by Fred Belton
June 2008: Fred Belton and Paul Hloben climbed Lengai on June
18 with Masaai guide Peter and
other Tanzanians Paul Mongi
and Mweena Hosa, and spent
about 1 hour on the rim of the active cinder cone. Mineral
samples were collected by Belton. Details of their visit may be
seen on the 2008 Expedition slide show page. (under construction)
On June 17 a group of local Masaai from Engare Sero village climbed
Lengai via the western route through the Pearly Gates, which has been
closed to climbers for several months due to dangerous activity.
The climbers of June 18, led by the Maasai guide Peter, followed the footprints
of the Maasai group from the previous day. The ascent route is
the same as before except that the entire route is now covered by thick
ash deposits. The powdery ash has actually decreased the
difficulty of the descent and in some places it is nearly possible to
run down the mountain. However, climbers should be aware that the
route is subject to danger from above should there be a significant
eruption from the cinder cone.
The alternative route that approaches Lengai from the NE via a dry
river bed and grassy track off the Engare Sero-Engaruka road and
terminates in the south crater is steep and dangerous. Most climbers
attempting this route recently have turned back without reaching the
summit. However, some groups such as Chris Weber's team have
successfully reached the summit via this route. (See above
report.) We do not recommend it.
The new active cone covers the former crater floor entirely except for
a region just north of the summit. The west, north and east sides of
the former crater are now about 30m higher than before and enclose a
deep pit crater with a couple of small vents visible in the
bottom. To the south, the rim of the new cone rests on the crater
floor. To the east and west the new cone merges with and covers
up the old rim at the points where it intersects the arc formed by the
summit ridge. Thus there is now a section of the former crater
floor which is bounded to the north by the new cone's southern rim and
to the east, south and west by the original curving summit ridge.
This is much like the morphology of the crater after the 1966-67
eruption when there was a similar pit crater to the north and a
"southern depression" below the summit, although this pit crater
appears larger than the one from '66-'67, and the current "southern
depression" appears smaller than the one formed in the sixties.
During the visit from approximately 9:20 -10:20 AM the pit crater
frequently emitted an ash-poor plume from somewhere in the SW part of
its floor. Climbers on the rim experienced light ashfall.
Loud rumbling was continuous and occasional sounds of gas jetting and
rockfall were heard amid other noises that are not easily
described. Occasionally there was a sloshing/hissing noise
resembling the sound of "lava at depth" often heard at Lengai in
the past, but there was no evidence of any lava in the crater.
The summit and south crater were not visited due to lack of time and
poor visibility due to increasing atmospheric clouds around the summit.
For more information on this climb, see the 2008 expedition
slide show.

Summit of Lengai behind new crater rim. Photo by Fred Belton

Small ash eruption on June 18. Photo by Fred Belton
June 2008: Ben Wilhelmi photographed
4 of the 5 climbers on his June 18 flyover.

Note the 4 climbers just below the crater rim. Photo courtesy Ben
Wilhelmi
June 2008: Photos by Ben
Wilhelmi made on June 19 show no activity, but on June 30 he
photographed gray plumes emerging from the crater.
July 2008: On July 1, Ben Wilhelmi made photographs and
noted a small collapse of the south part of the new crater rim.

On July 1 there appears to be a small crater rim collapse on the south
(upper right) crater rim. Photo courtesy Ben Wilhelmi.

Ben overexposed this photo to reveal details of the inner crater.
Photo
courtesy Ben Wilhelmi.

View of the south crater floor showing numerous bomb or block impact
craters. Photo courtesy Ben Wilhelmi.
July 2008: Ben Wilhelmi forwarded
photos he made during flyovers on July
3, 14, 18, 23, and 25, all of which showed no changes and either
no activity at all or very light smoking of the crater. A photo
taken on July 18, posted below, shows white smoke emerging from a
small area on the NE part of the former crater rim. at the place where
the new crater wall has merged with it.

Photo courtesy Ben Wilhelmi
July 2008: Thomas Holden reports:
"On 27 July a guide witnessed
a "small eruption." (No details given.) "The guide gathered
samples in a Maasai shuka which was burned and melted because he
collected the materials when they were still hot."
August 2008: Ben Wilhelmi forwarded
the following message from Remi Kahane
about a climb on 3 August: "Severin
Polreich and Remi Kahane
(Arusha), guides Godson
(Arusha) and Juma (Maasai from
Lake Natron village office) went on the old route (NE) to the top of
the vulcano. Jens from Moivaro
Lake Natron camp site informed us that this old route had been used
recently and successfully, and that the vulcano was quiet since 1 July,
but still active and then dangerous. He also advised us to hire a local guide
at the village, since a recent regulation from the village authority
makes it an obligation. Fee is 100 $ and guide is not a professional.
He knows the way. We spent 15
minutes at the rim of the crater (10 a.m.) and could hear very clearly
strong and constant rambling of the vulcano, no smoke from the crater
however. Fumeroles on the external rim were present, and sulfur odor
was strong."
August 2008: Ben Wilhelmi sent
photos from Aug 8 and reported
that the mountain was quite. He photographed some climbers standing on
the crater rim. Ben also sent photos of Lengai made on Aug 23 which revealed no activity.
Sept 2008: Hervé Loubieres and Françoise
Vignes of Toulouse
report: “We
climbed to
the top on 2008 September 1st through the NW route with
Shiro,
our Maasaï guide. This climbing route was hard, walking on ashes
deposits, and long (7 hours) but without any difficulties.
We
reached the Crater summit at 7:00am. While climbing we heard the
roar of
the volcano activity before passing through the Pearly Gates. There
were white
fumerolles on the external rim of the crater (picture
SouthFaceFinalClimb). No
sulfur smell. Inside
the crater on the South rim (picture SouthCraterRim) there were also
fumerolles. And in the crater
floor there were 2 active vents erupting black
lava (picture CraterFloorVent), one of them was bigger with a diameter
around
10 meters and a permanent activity. After
having walked around the crater and a too short rest, we went down at
8:10 am
by the same way, very exhausting due to the heat and to the ashes dust."

Erupting spatter cone within the pit crater of Lengai on Sept 1,
2008. Photo courtesy
Hervé
Loubieres and Françoise
Vignes
Sept 2008: Ben Wilhlmi sent
photos he made of Lengai from a
distance on Sept 3. No
plume was visible.
Oct 2008: Jens
Fissenebert of Moivaro - Lake Natron
Tented Camp & Campsite reported
a small eruption on Oct 1
beginning at 1:45 PM. Details are not yet known.