Monday, February 16, 2009

Seismic frescoes - possibly the oddest earthquake induced landslide story of all time?

There is little doubt that the Wenchuan (Sichuan) earthquake in May generated a huge number of shallow rock slides. A very odd story has now appeared in the Chinese media in which it is observed that the rock slide scars appear to form frescoes (wall-mounted murals) on the mountain sides. So, in the words of the People's Daily Online "Although the massive Wenchuan Earthquake caused tremendous damage, it has also brought new natural wonders - a large number of seismic frescoes that were formed on cliffs from Yingxiu to Luobuzhai by landslides during the earthquake."

So what do these seismic frescoes look like? This one apparently resembles "waving reeds" (images courtesy of People's Daily Online):

This one is I think meant to be a cockerell crowing (the caption in the original article is a little bizarre):

And finally, this one is apparently "a girl playing the violin" (I am struggling to see this one, I must admit).



The article implies that there are many more, consisting of "human figures, animals, plants, as well as legends of ghosts and monsters. The majority of the frescoes depict various kinds of human figures."

The article finishes by noting that this phenomenon could be developed for tourism, although I suspect that the combination of enlargement of the scars during rains and revegetation during the rest of the year may render this difficult. I have never heard of landslide scars being interpreted in this way - landslide scars as art!

Tuesday, February 10, 2009

Landslide on the Mahakali River on the Nepal / India border

Thanks to both David Hopkins and Ripendra for drawing my attention to a landslide on Friday on the Mahakali River on the border between Nepal and India. Although it has occurred in a remote area, it is interesting because the landslide appears to have partially blocked a fairly large river coming down from the high Himalayas.

The landslide occurred in the Chautuldhar (Chetalkot) area of Rephalikot, close to Tawaghat in Dharchula, right on the border of Nepal (to the east) and India (to the west) (see Google Earth image below - click on the image for a better view).

The reports suggest that cracks were first seen on Thursday, which led to a large scale failure on Friday. The location is shown on the Google Earth perspective view below (the actual location of the landslide appears to be in a small area of low resolution imagery):


Reports suggest that the river is flowing through a gap of just 2.5 metres, which has created a barrier lake that is threatening a number of villages upstream. The main road is blocked and may take as much as a month to reopen, and there is a threat of further landslides.

An interesting dimension to this is the proximity of the Dhualiganga I hydroelectic scheme. I have annotated the diagram above to show the location of the dam and the power house. This is a run of the river scheme in which the Dhauliganga River has been dammed with a 56 m high concrete faced rock fill dam to create a head of water. The water is then passed through a tunnel beneath the mountain to the powerhouse, where turbines are located. The project was completed in October 2005. Some newspapers are speculating that the landslides may have been associated with the construction of the tunnels as the failure occurred in the dry season with no obvious trigger. However, the tunnel is 6 km from the landslide site, so this is not likely. However, if a large lake were to form at the landslide site, and then was to be released rapidly, then the powerhouse would be threatened. It is not clear to me whether this is a possibility, but given that the river is now reportedly flowing again I suspect the chances at present are low.

As an aside, the dam site itself appears to be quite interesting from a slopes perspective:

Monday, February 9, 2009

Australian wildfires and risks of increased erosion rates

ResearchBlogging.org(Updated 10th Feb to include latest casualty numbers)

The extraordinary wildfires in Australia are dominating the headlines in the UK, half a world away. Wildfires are quite common events, but the number of fatalities that this particular episode has caused is really quite unusual. Below in Figure 1 I have plotted the recorded worldwide recorded number of deaths from wildfires for the period since 1980, using data from the CRED EM-DAT database . I have added the (updated to) 173 reported deaths from this event so far as an extra column, although note that reports suggest that this total may rise substantially:

Figure 1: Global numbers of reported fatalities from widlfires, based upon the CRED EM-DAT database. The 2009 value is the reported number of deaths from the Austrlian wildfires.

The average annual global total number of deaths is 59.5 fatalities per annum. Care is needed in the interpretation of the above as CRED only record events that kill ten or more people, thus these values consistently underestimate the true toll, but nonetheless the unusual impact of these events is clear.

In the context of this blog it is also interesting to think through the likely long term impact of these fires in terms of erosion and landslides. A recent paper by Smith and Dragovitch (2008) looked at the long term consequences of wildfires in SE. Australia. These two researchers have published extensively on sediment production and erosion in Australia, so have a strong pedigree.

The study focused on a fire that occurred in January 2003 during a drought in the Snowy Mountains near to Thredbo (Fig. 2), a sub-alpine environment. The study used erosion pins to monitor surface level change on both burnt and unburnt hillslopes over a period of 795 days after the fire.


Figure 2: Google Earth perspective image of the area around Thredbo, the location of the study reported by Smith and Dragovich (2008)

The study showed that after the fire the areas that had been burnt suffered a net loss of soil representing an average of 3.8 mm of material, with the most intense erosion occurring on the lower slopes (Fig. 3). On the other hand, the unburnt areas saw a net accumulation of soil of an average of 2.6 mm, again with the greatest accumulation at the lower slopes.

Figure 3: Mean net soil loss and gain for burnt and unburnt areas as reported by Smith and Dragovich (2008).

Thus, the burnt areas clearly suffered a net loss of material in the aftermath of the fires. The study showed that this loss of soil declined with time after the fire, with a slight increase again during snow melt, presumably as vegetation re-established. However, these values are perhaps surprisingly low compared with those recorded in other environments, especially in N. America, given the steep slope angles seen in Figure 2. Interestingly, Shakesby et al. (2007), who studied post-fire erosion in Eucalyptus forests in SE. Australia, came to similar conclusions, stating that "except under extreme post-fire rainfall conditions, present-day wildfires affecting south-east Australia seem to be less potent in geomorphological terms than might be expected given the severity and frequency of the wildfires". They attribute this to the rapid rate of plant growth in the aftermath of fires plus the resistance of the soil to erosion.

The conclusion is therefore that although the fires have devastated vast areas, and made thousands homeless, there should not be a serious increase in erosion in the burnt areas. This will help greatly in the post-fire recovery of the burnt areas.

References:
H SMITH, D DRAGOVICH (2008). Post-fire hillslope erosion response in a sub-alpine environment, south-eastern Australia CATENA, 73 (3), 274-285 DOI: 10.1016/j.catena.2007.11.003

R SHAKESBY, P WALLBRINK, S DOERR, P ENGLISH, C CHAFER, G HUMPHREYS, W BLAKE, K TOMKINS (2007). Distinctiveness of wildfire effects on soil erosion in south-east Australian eucalypt forests assessed in a global context Forest Ecology and Management, 238 (1-3), 347-364 DOI: 10.1016/j.foreco.2006.10.029

Friday, February 6, 2009

Name the landslide 3

Time for a bit of Friday fun, that is Name the Landslide round 3. This one has been set be Peter Weisinger, winner of round 1. The challenge is, as ever, to identify the landslide shown in the Google Earth images below and to provide a brief description, suing the comments below. Do feel free to use the comments section to work towards a team solution.

Peter has very kindly provided two perspectives:


Over to you...

Dave

Another landslide video - car hit by landslide in Japan

There has been an extraordinary flurry of landslide videos of late (e.g. here) presumably reflecting both the high occurrence of landslide events and the ubiquity video sharing sites. Another has appeared this morning - this time from Japan. The video should be embedded below or can be viewed here.

Watch more LiveLeak videos on AOL Video



I guess this is not as spectacular as for example this one, this one and this one, but is interesting nonetheless. The occupants of the car were lucky that the slide did not engulf the car or push it off the road. One interesting aspect is the way that the car was bulldozed rather than being buried, which is a useful observation when we think about the rescue of survivors.

Does anyone know where in Japan this happened? The date on the video appears to be 31st January.

Tuesday, February 3, 2009

Virtual field trip - the Marcus landslide in Arizona

The Arizona Geological Survey have created a rather nice virtual field trip and very useful virtual field trip about the Marcus landslide in Arizona. It is available here:

http://www.azgs.az.gov/MarcusLandslide_2008.shtml

The slide is a 500,000 year old rock slide that has has a length of about 2 km from scarp crown to deposit toe (see Google Earth image below) and a deposit volume of about 5.25 million cubic metres. The elevation difference is about 500 m.


Two minor criticisms from me, though:
  1. The site does not give the lat/long of its location, which makes looking at it on Google Earth rather more difficult than it ought to be. The location of the crown is: 33°40'47.27"N, 111°48'1.31"W. The deposit extends almost due east from this point;
  2. The site states that "Poised for collapse, a heavy rain, a bolt of lightning, or an earthquake could have spontaneously triggered". It is highly unlikely that lightning would trigger failure.
Finally, there is a paper in Geomorphology describing the landslide in more detail, including its dynamics, failure and age. It is available for downloading as a pdf here. There reference is:

Douglass, J., Dorn, R.I. and Gootee, B.F., 2004. A large landslide on the urban fringe of metropolitan Phoenix, Arizona. Geomorphology, 65, 321-336. doi:10.1016/j.geomorph.2004.09.022

Sunday, February 1, 2009

(updated) Name the landslide 2

Updated with a hint below

The winner of the Name the Landslide 1 hasn't yet been able to suggest round 2 (the invite is still open), but in the meantime here is one to think about. As before, the challenge is to name the landslide as shown on Google Earth and to briefly describe the main movement event. Trickier this time...

Please post your suggestions in the comments section.

Hint: the landslide was triggered in 1999, along with about 22,000 others.