A method of forecasting associated with these phenomena is known as the Rutschblock test.
A method of forecasting associated with these phenomena is known as the Rutschblock test. These phenomena can be caused by the rapid diffusion of warm air from the ground, which creates unstable layers of depth hoar. One type of this phenomenon is facilitated by the presence of a lubricating layer, and a majority of deaths are caused by the slab type. Most of them occur on slopes between thirty and forty-five degrees and their speeds can reach over two hundred miles per hour. FTP name these phenomena in which large masses of snow rapidly slide down a mountain.
A method of forecasting associated with these phenomena is known as the Rutschblock test.
{avalanche}s