Landslide RS survey includes the landslide recognition, the collection of the basic information, and the spatial analysis. With the Tiantaixiang landslide RS as an example, this paper illustrates the utilization of “special points” to determine the boundary and influence zone, movement characteristics and scale of the landslide. Landslide RS monitoring can be divided into direct RS monitoring and indirect RS monitoring. It is difficult to determine the exact time for large scale high velocity landslide movement, the scale of landslide movement is relatively small compared with the resolution of the satellite image, and as RS data are discontinuous and rather expensive,  they are not quite suitable for RS direct landslide monitoring. Indirect monitoring means monitoring the environmental change caused by landslide activities. The Yigong landslide RS serves as another example to illustrate RS monitoring of lake change, ecological destruction and new landslides caused by landslide dam burst.
Landslide RS evaluation means the evaluation of the stability, the prediction of the future activities, the detection of the affecting factors and the evaluation of the regional hazards caused by landslide development. Tiantaixiang and Qianjiangpin landslides and regional landslides in the Three Gorge area all serve as examples.