Mid-February 2014 North American winter storm of further-north Georgia received unusually heavy snows. Precipitation started as light rain late on the 10th, with significant snow by the following morning while still above freezing, turning back to light rain before ending by mid-day. More light rain began after midnight, changing to snow as temperatures fell, then to sleet, freezing rain, back to sleet again before another significant snow by the morning of the 13th. Areas north of the city generally got mostly snow and sleet, while a large swath from the south metro area eastward got the heaviest ice accumulations, though a dry slot at mid-day proved
Hail smaller area, on transport and infrastructure. Accumulated hail can also cause flooding by blocking drains, and hail can be carried in the floodwater, turning into a snow-like slush which is deposited at lower elevations. On somewhat rare occasions, a thunderstorm can become stationary or nearly so while prolifically producing hail and significant depths of accumulation do occur; this tends to happen in mountainous areas, such as the July 29, 2010 case of a foot of hail accumulation in Boulder County, Colorado. On June 5, 2015, hail up to four feet deep fell on one city block in Denver, Colorado. The