2 relatively strong earthquakes in the border area in between Tanzania and Kenya
Last update: June 3, 2013 at 10:44 am by By Ashish Khanal
Update 10:48 UTC : The video below gives a good impression of the strange crater of the Ol Doinyo Lengai volcano.
Update 10:26 UTC : We invite Tanzanian and/or Kenyan people with a view on Ol Doinyo Lengai volcano, to tell us that the volcano did not show sgns of additional activity as we see both earthquakes very close to the volcano. The second one has an epicenter on the slopes o the volcano !
Ol Doinyo Lengai volcano – Image courtesy and copyright SteveAxford
Only 1 reported earthquake by the seismological agencies, but in fact people are reporting 2 quakes being felt in Nairobi.
The earthquake struck in the Lake Natron area.
As depth is given 10 km which corresponds internationally as “we are not sure at all”.
Please keep also in mind that there is always an error margin in pointing the location of the epicenter. All this to tell that this earthquake will be probably tectonic but there is always a chance that the quake can be linked to the nearby volcano.
Seismogram image courtesy Geofon, Germany
174 km SW of Nairobi, Kenya / pop: 2,750,547 / local time: 06:24:45.4 2013-06-03
107 km NW of Arusha, Tanzania / pop: 341,136 / local time: 06:24:45.4 2013-06-03
73 km W of Longido, Tanzania / pop: 9,403 / local time: 06:24:45.4 2013-06-03
Most important Earthquake Data:
Magnitude : 4.6
Local Time (conversion only below land) : 2013-06-03 06:24:45
Kerinci volcano, Sumatra, Indonesia (AV – June 2 – 14:41 UTC)
2 great twitter sites to follow up activity and images of Gunung Kerinci : @Infoseismic and @padangekspres
The image below is a twitter image of the ash cloud earlier today :
Twitter Image courtesy @ Padangekspres
Kerinci volcano, Sumatra, Indonesia (AV – June 2 – 12:15 UTC)
The Indonesian press reports that some villagers living on the slopes and at the base of the Kerinci volcano (alert level Waspada or 2 on a scale of 4) have fled their houses due to a number of “atomic bomb” black smoke eruptions. The atomic bomb description has to be regarded as a mushroom kind of smoke column. This kind of explosions are very similar than those happening in September 9/2007.
Villagers are fearing that their crops will be lost as soon after the eruption black ash was falling out of the sky. To make it even worse, it started to rain shortly thereafter making the ash even more dangerous for crops. Villagers also told the reporters that they felt strong vibrations.
We expect that CVGHM will increase the alert level from Waspada to Siaga (3 on a scale of 4) very soon.
The volcano was in Waspada status since 2007!
Mount Kerinci is the highest volcano in Indonesia.The summit towers 3805 m above sea level.
No change in activity
The Government of the Argentine province of Neuquén (Argentina side of the border) ordered by decree a “high alert” for the town of Caviahue and surrounding areas that could be affected by the possible eruption of Copahue, the government said. 800 people will be asked to evacuate at the Argentina side of the border. The evacuated people will be lodged in hotels at approx. 70 km from Caviahue.
The Argentina side of the border and more specifically Caviahue will probably get the big ash shower when Copahue would erupt ast Easterly winds are the main wind direction in the Andes.
The village of Caviahue, east of the Copahue volcano – Image courtesy a60
Webcam COPAHUE to follow the events – Sernageomin1
Nothing to see at the moment of writing because of very bad weather.
The evacuation of the 400 families living under treat of lahars (hot mud flows – in part generated by melting snow) and pyroclastic flows (extremely hot ash avalanches that burn everything on their way) is being effectuated orderly.
Nothing special going on so far and nothing serious expected as far as VAAC Buenos Aires is reporting. (NO VA EXP (text on map) is of course NO Volcanic Ash expected). This map is a precision of 19:30 UTC on May 28 (today).
The eruption that started last week at Pavlof, at the far western end of the Alaska Peninsula, is still going strong. AVO says that the lava flows and fountains are continuing, with steam-and-ash plumes reported to be reaching in 5-6 km (low 20,000s feet). However, they did note that the plume doesn’t seem to be very ash rich as much of the volcanic material is staying closer to the summit of the volcano — but that didn’t stop some ash dusting towns as far away as Sand Point, 88 km (55 miles) to the east. Some images of the eruption (see above) clearly show the white plume that is likely mostly derived from melting snow and the dark grey plume made of volcanic ash and tephra. The activity is still producing small pyroclastic flows from snow-lava interactions and lahars further downslope as the volcanic debris mixes with melted snow/ice — be sure to check out the image of Pavlof taken May 16 over on the NASA Earth Observatory showing all these features. The seismicity (volcanic tremor) at Pavlof is almost constant, so there don’t seem to be many signs that the eruption is nearing an end — the current level of activity is likely the new normal at Pavlof for the time being, with some potential for explosions that might produce plumes reaching 9 km.
Late afternoon, going into sunset , May 18, 2013 (100UTC May 19, 2013) … several plumes appeared in central west Mexico — quickly followed by large prominent columns (steam or smoke?) produced near the Texas border.
Location .. somewhere very close to:
29°12’52.46″N , 102° 1’15.06″W
If you look at the area on Google earth, you will quickly come to see
1) It is a desert
2) There are several very old (dormant) volcanoes at this location
Interesting press release from CVO this evening. While they’re playing this down, it is interesting that there are (and have been) many more earthquakes than they mention in the report (for days now!)! The events plot beneath the most recent vent area,…not where geothermal exploration this past year had triggered earlier activity on the western flank of the volcano. I had been watching these events, but obviously not closely enough!!! I’m sure the deep low-frequency event within the shallower activity got their attention. This is a rhyolitic volcano (so there are few analogs to precursory activity) and the seismicity at Chaiten and more recently at Cordon Caulle began at around 8 km depth!!
Maybe nothing,…maybe something!!! Definitely the most interesting seismicity in the Cascades for a long while!!!
Earthquakes at Newberry, April 08-12 – April 12, 2013
Between 04/08 – 04/12, five earthquakes were located within or along the margins of the Newberry caldera by the Pacific Northwest Seismic Network (PNSN, http://www.pnsn.org). The first two occurred at 04:19 & 04:20 PDT on 04/08 and were followed over the next 20 minutes by eight smaller (and therefore unlocatable) earthquakes. Three days later at 5:01 PDT a “low-frequency event”, so-called because it lacks higher-frequency waves that are commonly observed in regular earthquakes, occurred at a depth of ~8 km. Finally on 04/12 two additional earthquakes occurred at 02:28 and 04:06 PDT. The largest of these five events was a M 1.2. These five events appear as orange or red (two most recent) circles in the below map-view plot.
Newberry earthquakes, 2011 – 2013
Map showing earthquakes located within the Newberry caldera from 2011 – 2013. Earthquakes from April 08-12, 2013, are colored orange or red (for April 12 events).
Although these five events are nothing to get excited about, they are noteworthy because only six other earthquakes have been located within or along the margins of the Newberry caldera since the Newberry seismic network was expanded from one to nine seismic stations in the summer of 2011 (none of these events would have been detected prior to 2011). In addition, the 04/11 event is the first low-frequency event ever recorded in the Newberry area. Low-frequency events are not unusual at volcanoes, and when observed are commonly thought to reflect movement of fluid (water, gas, or other) through cracks. Given that there are active hot springs within the caldera, the occasional occurrence of such events should not be surprising. An unusual feature of this low-frequency event is its depth (8 km). Since the 1980s, such “deep low-frequency events” have been seen intermittently at Mount Baker (31), Glacier Peak (9), Mount Rainier (9), and Mount St. Helens (9). At these other volcanoes the deep low-frequency events occur as part of background seismicity and have not been associated with eruptions or unrest at the surface (for more information about these type of events in the Cascades, see Nichols et al. (2011)**). Although intriguing from a volcanological perspective, these events are again nothing to get excited about.
** Nichols, M. L., S. D. Malone, S. C. Moran, W. A. Thelen, and J. E. Vidale (2011), Deep long-period earthquakes beneath Washington and Oregon volcanoes, Journal of Volcanology and Geothermal Research, 200(3-4), 116-128.
The forested dacite domes of Cerro Machín, nested within an older caldera. Pyroclastic flow deposits from Machín have been traced upwards of 40 kilometers from their source at the volcano. Image: INGEOMINAS, taken November 16, 2011.
I like to keep close tabs on the volcanoes in Colombia — with half of my family living in the country, it seems only appropriate. Some of my first volcanic memories are of seeing firsthand some of the lahar deposits at Nevado del Ruiz from the 1985 eruption. Now, at that time, only two Colombian volcanoes really made any noise: Galeras in the south near Pasto and the aforementioned Ruiz in central Colombia. Nowadays, thanks to increased monitoring on Colombian volcanoes by INGEOMINAS, we know a lot more about the restless nature of the volcanoes of the South American country. Five volcanoes are now on elevated alert status, meaning that they show some level of activity that could lead to an eruption: Ruiz, Galeras, Cumbal, Sotará, Huila and Machín.
Over the past week, Cerro Machín, a dacite dome complex to the to the south Ruiz near Ibagué, has been feeling some increased seismicity. The INGEOMINAS special bulletin details a M2.9 earthquake that occurred at a depth of ~4.7 km beneath the volcano that was felt by local residents. This was part of a swarm that produced over 210 earthquakes in a few hours on February 10 — all within 2 and 5 km depth, but all very small. Now, before you need to get too nervous about this activity, INGEOMINAS rightly points out that these swarms have occurred before at Machin and that sensitive new seismometers are likely to notice this type of activity that might not have been noticed in the past. Not a lot to see, but in the small chance that Machín does get more active, the Observatorio Manizales has a webcam pointed at the volcano. Machín’s last known eruption was over 800 years ago.
Right now, the most active volcano in Colombia is still Nevado del Ruiz. The volcano is still experiencing elevated seismicity, along with a ~950 meter steam plume that occasionally has minor ash as well — which can be seen via webcam, weather permitting.
The submarine eruption at El Hierro continued into 2011. Image: INVOLCAN
2012, for all the hype about apocalypse, was a volcanically-quiet year. No Eyjafjallajökulls, no Puyehue-Cordon Caulles, no Pinatubos. Sure, we had some notable eruptions, but most were small-to-moderate events that, many times, won’t even end up getting preserved in the geologic record. However, that didn’t stop me from posting way too much! No, really, it was still a great year for Eruptions, with decidedly more posts about the science of volcanoes when the actual volcanic events were low. Here is the 2012 Volcanic Year in Review!
I also tackled a topic that came up repeatedly during the year – the missing eruptions in the ice cap record. Namely, the ice cores suggest a large eruption in 1258 AD, but no source has been definitively identified (although inroads have been made). Another mysterious caldera eruption, the Kuwae caldera eruption in the 1450s, was also examined about whether it actually occurred.
Both Popocatépetl and Nevado del Ruiz kept on producing small eruptions as we headed into June, while Cleveland in Alaska had a explosive eruption, likely due to collapse of the dome that had been growing in the crater since earlier in the spring. We also saw the alert status raised at El Hierro in the Canary Islands for the first time in months after an intense seismic swarm occurred — but this swarm didn’t lead to any new eruption.
With all the excitement of the US Presidential election in early November, I looked at the perception of probability versus prognostication when it comes to volcanic mitigation. If you’re looking for a volcano movie to watch, I finally wrote up my guide to volcanic cinema and I described what a SHRIMP-RG is and how I use it in my research.
So, there you have it. The Volcanic Year in Review … and hopefully 2013 will bring us more volcanic excitement.
Erik Klemetti is an assistant professor of Geosciences at Denison University. His passion in geology is volcanoes, and he has studied them all over the world. You can follow Erik on Twitter, where you’ll get volcano news and the occasional baseball comment.
The Santiaguito dome on Santa Maria in Guatemala, showing a diffuse ash plume and a possible pyroclastic flow in the foreground. Image: Webcam capture on November 29, 2012 / INSIVUMEH.
You can see some of this activity on the INSIVUMEH webcam for the Santiaguito dome complex — even in the image from today, an ash plume as possible small pyroclastic flows are visible (see above).
New Zealand’s Mount Tongariro volcano erupted for the second time this year on Wednesday (Nov. 21), sending a plume of ash 2.5 miles (4 kilometers) skyward and raising the odds that another eruption is imminent.
Tongariro, one of three active volcanoes that stand over Tongariro National Park in the heart of New Zealand’s North Island, lay dormant for more than a century before blowing open its Te Maari crater in August.
That eruption was augured by an increase in seismic activity, but Wednesday’s eruption came without any warning, said volcanologist Tony Hurst, who spoke to Radio New Zealand.
A view of Mount Tongariro just after it erupted on Wednesday (Nov. 21).
CREDIT: Via Stuff.co.nz | Lomi Schaumkel/Tamatea Intermediate School
New Zealand’s Mount Tongariro volcano erupted for the second time this year on Wednesday (Nov. 21), sending a plume of ash 2.5 miles (4 kilometers) skyward and raising the odds that another eruption is imminent.
Tongariro, one of three active volcanoes that stand over Tongariro National Park in the heart of New Zealand’s North Island, lay dormant for more than a century before blowing open its Te Maari crater in August.
That eruption was augured by an increase in seismic activity, but Wednesday’s eruption came without any warning, said volcanologist Tony Hurst, who spoke to Radio New Zealand.
There were hikers in the area at the time of the eruption, including a group of schoolchildren, but no injuries have been reported. Hurst said the eruption was relatively non-threatening because it didn’t eject many rocks, suggesting it may have originated from the same vent that had been mostly cleared out by the August eruption, which rained rocks on a hiker’s shelter a mile (1.5 km) away from the crater.
Middle school teacher Paul Lowes was hiking on Tongariro with his class when Wednesday’s 5-minute eruption began, at about 1:25 p.m. local time.
“We were sitting there celebrating with the kids, the achievement of them getting up there, and next thing, one of them pointed out, ‘Look what’s happening.’ I turned around and there [the volcano] was, just starting to blow,” Lowes told Stuff.co.nz. “We stopped in a bit of awe of it to start with, and didn’t realize what was actually happening. And as it was getting bigger, then it was sort of, ‘Right-o, it’s time to move everyone out of here.'”
Scientists had no reason to expect the eruption, but one no-warning eruption serves as a warning for the next. That’s because, historically, the Te Maari crater has had a tendency to break a silence and keep talking.
“In 1892 and 1896, it sort of had eruptive periods that went on for months with a number of different events,” Hurst told Radio New Zealand. “Having [now had] two events, it could well have more than two in this sequence. There’s an enhanced risk at the moment, certainly.”
But Tongariro is not the only potential loose cannon in the park right now. Last week, GNS Science, an official monitoring body in New Zealand and Hurst’s employer, issued a warning that Mount Ruapehu, a neighboring volcano, is showing signs that it may erupt in the coming weeks or months.
Tongariro National Park served as the backdrop of numerous scenes in the “Lord of the Rings” film trilogy, standing in for the fictional land of Mordor.
The park’s third active volcano, Mount Nguaruhoe, featured as the movies’ Mount Doom in long shots. That volcano last erupted in 1975.