the previous record holder, Mount Rainier, Washington, which during the 1971–1972 season received of snow. Highest seasonal average annual snowfall – The world record for the highest average annual snowfall is , measured in Sukayu Onsen, Japan for the period of 1981–2010. Largest snowflake – According to Guinness World Records, the world's largest snowflake fell in January 1887 outside present-day Miles City, Montana. It measured in diameter. The cities (more than 100,000 inhabitants) with the highest annual snowfall are Aomori (792 cm), Sapporo (485 cm) and Toyama (363 cm) in Japan, followed by St. John's (332 cm) and Quebec City (315 cm) in Canada. Metamorphism According to the International Association of Cryospheric Sciences, snow metamorphism is "the transformation that the snow undergoes in the period from deposition to either melting or passage to glacial ice". Starting as a powdery deposition, snow becomes more granular when it begins to compact under its own weight, be blown by the wind, sinter particles together and commence the cycle of melting and refreezing. Water vapor plays a role as it deposits ice crystals, known as hoar frost, during cold, still conditions. During this transition, snow "is a highly porous, sintered material made up of a continuous ice structure and a continuously connected pore space, forming together the snow microstructure". Almost always near its melting temperature, a snowpack is continually transforming these properties wherein all three phases of water may coexist, including liquid water partially filling the pore space. After deposition, snow progresses on one of two paths that determine its fate, either by ablation (mostly by melting) from a snow fall or seasonal snowpack, or by transitioning from firn (multi-year snow) into glacier ice. Seasonal Over the course of time, a snowpack may settle under its own weight until its density is approximately 30% of water. Increases in density above this initial compression occur primarily by melting and refreezing, caused by temperatures above freezing or by direct solar radiation. In colder climates, snow lies on the ground all winter. By late spring, snow densities typically reach a maximum of 50% of water. Snow that persists into summer evolves into névé, granular snow, which has been partially melted, refrozen and compacted. Névé has a minimum density of , which is roughly half of the density of liquid water. Firn Firn is snow that has persisted for multiple years and has been recrystallized into a substance