Gravity erosion, also known as mass wasting, doesn't actually *form* land features in the same way that wind or water erosion does. Instead, gravity erosion is the process of moving existing materials downhill. This means it plays a crucial role in shaping and modifying existing landforms.

Here are some land features that are modified by gravity erosion:

* Slopes: Gravity erosion constantly works to steepen slopes, especially after events like heavy rainfall or earthquakes. This can lead to landslides and other forms of mass wasting.

* Valleys: Gravity erosion contributes to the widening and deepening of valleys through processes like rockfalls, debris flows, and soil creep.

* Canyons: While canyons are primarily formed by water erosion, gravity erosion plays a role in shaping their sides, contributing to the formation of cliffs and talus slopes.

* Hills: Gravity erosion can gradually erode hills, leading to their flattening over time.

Here are some land features that are directly formed by gravity erosion:

* Talus slopes: These are accumulations of rock debris at the base of cliffs or steep slopes, created by rockfalls and other forms of mass wasting.

* Landslide scars: These are the depressions left behind after a landslide, which can be quite significant in size and shape.

* Debris flows: These are rapid movements of water-saturated sediment, which can carve channels and deposit large amounts of material at lower elevations.

* Soil creep: This is a very slow, gradual movement of soil downslope, which can contribute to the tilting of trees, fences, and other structures.

It's important to remember that gravity erosion often works in conjunction with other erosional forces, such as water, wind, and ice. This makes it difficult to isolate the specific features formed solely by gravity, but its impact on shaping the Earth's landscape is undeniable.