Geotimes
Untitled Document

Geophenomena

Landslides bury Guatemala
Quake sets off landslides in Kashmir

Landslides bury Guatemala

As Hurricane Stan moved across Central America in early October, the storm brought torrential rainfall into an already saturated region. Ultimately, the storm triggered landslides of all sizes across the country, which had only recently recovered from the effects of Hurricane Mitch, seven years ago.

Heavy rains during hurricanes and tropical storms trigger devastating debris flows and landslides in Guatemala, such as this one shown in 2000, two years after Hurricane Mitch hit. This year, Hurricane Stan buried villages in mudslides and sent smaller debris flows coursing down rivers into settlements. Courtesy of Bob Bucknam, USGS.


One of the most horrifying accounts came from a small Mayan village on the flanks of Volcano Atitlán, on the shores of a lake of the same name. A slurry of fluid mud buried Panabaj on Oct. 5. More than 500 people were killed — most likely buried alive — trapped in their houses or unable to outrun the flow. (Debris flows can move at speeds of 50 kilometers per hour, or 30 to 35 miles per hour.) A week after the landslide, the remaining residents of the village decided to turn it into a memorial, according to The New York Times.

Such debris flows are lethal, says Anthony Crone of the U.S. Geological Survey (USGS), who worked in the region after Hurricane Mitch, “and once they stop flowing, they set up like concrete.” Carrying large blocks of rock and tremendous amounts of debris, “they flow very quickly and [over] long distances,” with “a lot of power.”

In addition to the mudflow that buried Panabaj, many small landslides occurred to the north and northeast of Lake Atitlán, Crone says from his examination of high-resolution satellite images of Volcano Atitlán and its flanks, taken within days of the landslides. These debris flows appeared to be less dense and less fluid than mudslides, though Crone says such labels are speculative until geologists can get on the ground. Geologists from USGS have not yet visited the sites, as they generally must be invited by a local government and sponsored by the U.S. Agency for International Development or other relief organizations.

Crone compares the area surrounding the volcano’s flanks to a dangerous layer cake of loosely packed volcanic sands, topped by soils that develop into impermeable clay layers covered in vegetation. As more volcanic episodes occur, they top the clay soils with loose volcanic sand again, and the buried clay soils act as a barrier to water percolating down through those upper layers. During storms, the water gathers in a pond trapped above the clay soil.

Thus, when Hurricane Stan hit, the already wet steep hillslides may have been primed to fail, Crone says: The trapped water probably lubricated the volcanic deposits perched on the hillslopes. He describes the areas that failed as very steep, with highly eroded river valleys that channeled some of the landslides.

In many of the region’s small towns and villages, people tend to build in the potential path of landslides, says Manolo Barrillas, currently a graduate student at the Colorado School of Mines in Golden, Colo., who has worked in the area. “Most of the people are very poor,” Barillas says, and live without water infrastructure or land-use planning. “Many of those people live in a very high risk area.”

According to CONRED, Guatemala’s disaster management division, the two largest mudflows killed almost 1,000 people between them (hundreds of people were reportedly still missing, weeks later). Smaller mudflows also occurred around western and central Guatemala, bordering Mexico, Barillas says.

Several years ago, after Hurricane Mitch, “abnormally heavy rains, possibly associated with El Niño and La Niña, caused a big mudflow,” Barillas says, so at least some people living on Atitlán’s flanks were probably aware of landslide risks in addition to volcanic risks. Still, some mayors claimed that they did not receive evacuation alerts for this storm, he says.

Towns and farms, in a region where volcanic soils are perfect for coffee and other crops, are sometimes far enough apart that communication about past hazards can be difficult, says Janelle Haapala, a graduate student at Michigan Tech and lead author of a USGS landslide hazards map for Guatemala, to be released early next year. So far, says Jim Vallance of the USGS Cascades Volcano Observatory, a co-author of the map, the slope failures that occurred after Hurricane Stan seem to have substantiated their findings.

Hurricane Mitch affected the eastern part of Guatemala in 1998, devastating parts of Honduras, Nicaragua and El Salvador as well, whereas Hurricane Stan hit the Yucatan Peninsula directly and then traveled into western Guatemala. Soon after, the last tropical storms of this season, Alpha and Beta, caused widespread flooding in Honduras and Nicaragua, but no landslides were reported.

Naomi Lubick


Quake sets off landslides in Kashmir

The region of Kashmir, shared by India and Pakistan, remains devastated by an earthquake that struck on Oct. 8, causing several landslides. A dozen major aftershocks shook the region, including a magnitude-6.2 event two hours after the main magnitude-7.6 earthquake.

Pakistan’s government reports that more than 74,000 people have died in collapsing buildings and landslides that were focused by tight canyons and steep rivers in the region. Rescue workers could not reach some areas for days, mostly in Pakistan’s remote mountains, as roads to extremely remote villages affected by the earthquake were impassable. In November, people continued to take shelter in tents or with any remaining materials they could find, according to The New York Times.

Edwin Harp, a landslide specialist at the U.S. Geological Survey in Golden, Colo., says that images from privately owned satellites showed “so many [landslides] coalescing along the river valleys,” that there are probably thousands of landslides, both large and small, in the area. “For an earthquake this large, that’s kind of surprising,” Harp says. One very large landslide — 2 kilometers long by about 1.5 kilometers wide — seems to have blocked the drainages of two rivers that come together, he says, which is a concern: The possibility that lakes could form behind the new natural dam could also eventually lead to its failure.

Northern Pakistan’s communities tend to form in narrow, steep canyons, which make perfect funnels for landslides, according to Brian Tucker of GeoHazards International in Palo Alto, Calif. The location of these traditionally mud-built structures, in a region with a lot of seismic activity, makes for a deadly combination, he says. “It is not a trivial problem” to solve.

Naomi Lubick

For initial coverage of the Kashmir earthquake, visit the Geotimes Web Extra archive.

Back to top

Untitled Document


Geotimes Home | AGI Home | Information Services | Geoscience Education | Public Policy | Programs | Publications | Careers

© 2014 American Geological Institute. All rights reserved. Any copying, redistribution or retransmission of any of the contents of this service without the express written consent of the American Geological Institute is expressly prohibited. For all electronic copyright requests, visit: http://www.copyright.com/ccc/do/showConfigurator?WT.mc_id=PubLink