The massive glaze deposit from January-February 2014 on the Republic of Moldova’s territory. The glaze is a deposit of ice, smooth and compact, generally transparent formed by freezing of supercooled raindrops on objects the surface temperature of which is below or slightly above 0°C. The territory of the Republic of Moldova, situated at the intersection of warm and cold air fronts, is vulnerable to complex ice deposits, including glaze. One of the recent records was in January-February 2014 when in some South-East areas of the country the glaze was reached the dimensions more than 20 mm in diameter (Chişinău and Tiraspol meteorological stations). In this case study another fact registered is that the duration of glaze maintenance on some objects exposed favorable to advection was 377 hours in Chişinău, 353 in Corneşti (Ungheni district), and the maximum recorded value in Ştefan-Vodă-423 hours. In conclusions, there are presented some recomended activities regarding reducing negative consequences of glaze deposit, specifically for the Republic of Moldova.