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The geological and geomorphological structure of Buzăului Subcarpathians, a subunit of Curvature Subcarpathians, increases the apparition risk of natural hazards associated with distinct risk phenomena. The intensity, frequency and length result in a rapid modification of existent relief forms (morphography, morphometry and morphology) and the apparition of new ones, but also the accentuation of slope instability, with strong effects on road and touristic infrastructure. There are frequentdoaj:78f5c73784bb40efbf95df62ebd29949 fatcat:ouq55yhwoja4pjjkyhzrlvxeeu