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    "en": "Sediment Rock Avalanche"
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    "en": "Rock avalanches are a translational form of mass movement where the transported material is dry rock that is fragmented before or during slope failure. They are rapid with long runouts and large volumes and often involve the entrainment of slope material, commonly therefore, giving rise to debris slides or flows. The motion of rock avalanches is massive such that the bulk of the rock fragments move together as a largely coherent mass (adapted from Collins, 2014 and USGS, no date). <br /> <p>Collins, G.S., 2014. <a href=\"https://doi.org/10.1007/978-1-4614-9213-9_321-1\">Rock avalanche. In: Encyclopedia of Planetary Landforms. Springer</a>. Accessed 15 October 2020.</p>"
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      "Volcanos and earthquakes are commons triggers for rock avalanches. They can occur in all rock types but are associated with rock that is more competent. Large rock avalanches are hypermobile and exhibit more movement than predicted from frictional models incorporating air entrainment, pore pressures or fine bed layers (Hungr et al., 2001, 2014)."
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