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怀化市地处湘西南,雪峰山贯穿全境,山峦叠嶂、沟谷纵横,地质构造复杂,地质环境脆弱,崩塌、滑坡等坡面地质灾害频繁发生。活动断裂纵横交错是孕育怀化市坡面地质灾害的地质构造基础,强烈风化与疏松地表是其物质来源,降水与径流量丰沛是其动力条件,暴雨、洪水是其诱发因素。人类活动,如水利水电工程建设、矿产资源开发工程、边坡开挖、乱采滥伐森林植被,增加了地质环境的压力,破坏了生态平衡,成为重要的致灾因子。怀化市崩塌、滑坡类型上以白垩系红层中的风化残坡积层中的土质类居多;时间上在过去15年呈波浪状上升态势,以2001年、2004年尤为严重;空间上主要集中沅水及其支流两岸谷坡地带和中低山丘陵区的100～450 m斜坡陡峭段。
Huaihua City is located in southwestern Hunan, Xuefeng Mountain runs through the whole territory, overlapping mountains, valleys, geological structure is complex, the geological environment is fragile, landslides and other slope geological disasters occur frequently. The criss-crossing of active faults is the geological tectonic foundation that geohaged the geological disasters on the slope of Huaihua. The strong weathered and loose surface is its material source. The heavy rainfall and runoff are its dynamic conditions. Rainstorm and flood are the inducing factors. Human activities, such as construction of water conservancy and hydropower projects, mineral resources development projects, excavation of slopes, indiscriminate deforestation and deforestation, increase the pressure on the geological environment and undermine the ecological balance, becoming an important disaster-causing factor. Huaihua City, the collapse of the landslide type in the Cretaceous red layer of the weathered residual slope in the accumulation of many soil types; time in the past 15 years showed a wave-like upward trend in 2001 and 2004 is particularly serious; mainly in space Yuanshui and its tributaries valley slopes and hilly areas in the hilly 100 ~ 450 m slope steep sections.