Slow-moving slides may be triggered by cold temperatures
Slow-moving landslides, while not as dramatic as their faster-moving counterparts, can damage infrastructure and cause headaches for the communities they affect. Slow-moving slides are generally associated with rainfall or snowmelt, but a new study in Japan has shown that some of these slides may occur when a certain kind of clay is exposed to cold temperatures. In the January issue of EARTH Magazine, the link between ground temperature and slow slides is explored, including implications for the science of predicting similar landslides around the world.
These unique slides occur throughout Japan, but also in other areas that contain a special type of clay formed from the mixing of volcanic ash into sedimentary layers. The study area, in north-central Japan, has soils rich with this clay and has experienced hundreds of slow-moving slides over several decades. Most of the sliding is observed during the winter, but rain and snow appear to have little effect. Instead, the researchers suggest that this clay is the culprit: a sort of geologic glue that loosens its grip in cold temperatures.
Want to learn more about slow-moving landslides? Read more about this study in EARTH Magazine: http://www.earthmagazine.org/article/
Also in the January issue of EARTH Magazine
- One of the first studies to include observations from the deep seafloor of the Southern Ocean, shedding new light on the mechanisms that power the global conveyor belt.
- Travel to Australia, where fossil records have revealed unique characteristics of the extinct marsupial lion, setting it apart from most known predators.
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