斜坡上大规模的岩体重力蠕变是慢速滑坡的一种类型。在重力蠕变中,蠕变带可以延伸到地表以下100米左右。它是非常缓慢的向下和向外运动,一般不形成连续的破裂面,其蠕变速率大约为每年2厘米到每天20厘米的范围。在欧州、新西兰、伊朗、南美洲和美国等世界许多地方都调查和研究过这种斜坡上的大规模的岩石重力蠕变。大量实例表明,在不同地质背景条件下,其蠕变以不同的方式发生, Large-scale gravitational creep on slopes is a type of slow-moving landslide. In gravitational creep, the creep zone can extend to about 100 meters below the surface. It is very slow downward and outward movement, and generally does not form a continuous rupture surface, its creep rate is about 2 cm per year to 20 cm per day range. Massive rock gravity creep on such slopes has been investigated and studied in many parts of the world such as Europe, New Zealand, Iran, South America and the United States. A large number of examples show that under different geological conditions, creep occurs in different ways,