顺向坡（英语：Dip slope），又称倾斜坡、倾向坡，是一种地质环境，表示一个波面的沉积堆叠方向，较逆向坡容易发生山崩，常见于遭侵蚀作用的地层（例如，断崖）。

有时候，基于成本的考量，很难完全避开顺向坡。当挖断顺向坡之坡脚时，应以人造边坡（Artificial Slope）或挡土墙或岩锚方式，进行结构补强。且当有安全性顾虑时，不宜使用生态工法。

但是，挡土墙或岩锚等边坡防护，应定时检修维护，不然当其支撑力不足以承载上方地层滑落之应力时，将产生「顺向坡滑动」的现象。

Strike and dip refer to the orientation or attitude of a geologic feature. The strike line of a bed, fault, or other planar feature, is a line representing the intersection of that feature with a horizontal plane. On a geologic map, this is represented with a short straight line segment oriented parallel to the strike line. Strike (or strike angle) can be given as either a quadrant compass bearing of the strike line (N25°E for example) or in terms of east or west of true north or south, a single three digit number representing the azimuth, where the lower number is usually given (where the example of N25°E would simply be 025), or the azimuth number followed by the degree sign (example of N25°E would be 025°).