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在查明研究区滑坡地质灾害基本地质条件的基础上,对区内岩质崩塌地质灾害的发育特征进行了总结和分析,并对区内崩塌地质灾害的形成机制和发展趋势进行了分析。研究结果表明:研究区位于火焰山南麓,地势北高南低,地貌类型为构造剥蚀低山及河谷平原;研究区内共发育有崩塌地质灾害点29处,均为岩质崩塌;研究区内崩塌危岩体主要受坡体卸荷裂隙和风化裂隙控制,随着人类活动的不断加剧将对危岩体的影响日益加重。
On the basis of ascertaining the basic geological conditions of the landslide geological disasters in the study area, the development characteristics of the rock disasters geological disasters in the area are summarized and analyzed, and the formation mechanism and development trend of the disastrous geological disasters in the area are analyzed. The results show that: the study area is located in the south of Huoyan Mountain, the terrain is high in the north and low in the south, and the topography is of denuded lowland and plains. In the study area, there are 29 collapsible geological disasters in total, The rock mass with internal collapse is mainly controlled by the unloading cracks and the weathering cracks of the rock slope. With the continuous increase of human activities, the impact on the rock mass will be aggravated.