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of a good sliding surface constitutes an unstable snowpack, the kind most prone to avalanching. An unstable snowpack contains both weak and strong snow layers. A weak layer consists of poorly bonded or unconsolidated snow, while a strong snow layer has well consolidated snow, such as a slab. Snow transported by wind blowing perpendicular to a ridge crest sometimes forms a cornice. Cornices are good visual indicators of the prevailing wind direction, pointing towards wind-loaded leeward slopes. Avalanche educators like to say, “weather is the architect of all avalanches.” After all, it’s the weather that builds the snowpack and causes changes to occur within it. And it’s the weather that can eventually overburden a snowpack to the point of failure, resulting in an avalanche. Natural Amazing skull till death do us part air jordan 13 sneakersavalanches are initiated or triggered by something in nature, such as new snow overloading an existing snowpack, a cornice breaking off, snowmelt, a rockfall, or even an earthquake. Slabs can consist of snow from a single storm or from multiple layers of snow from several storms. As you’d expect, slab avalanches cause the most fatalities and do the most property damage. Like weather forecasting, avalanche forecasting is part science and art, part fact
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