Landslide deposits often exhibit surface features, such as transverse ridges and X-shaped conjugate troughs, whose physical formation origins are not well understood. To study the deposit morphology, laboratory studies typically focus on the simplest landslide geometry: an inclined plane accelerating the sliding mass immediately followed by its deceleration on a horizontal plane. However, existing experiments have been conducted only for a limited range of the slope angleθ. Here, we study the effect ofθon the kinematics and deposit morphology of laboratory landslides along a low-friction base, measured using an advanced 3D scanner. At lowθ(30°–35°), we find transverse ridges formed by overthrusting on the landslide deposits. At moderateθ(40°–55°), conjugate troughs form. A Mohr–Coulomb failure model predicts the angle enclosed by the X-shaped troughs as 90° −φ, withφthe internal friction angle, in agreement with our experiments and a natural landslide. This supports the speculation that conjugate troughs form due to failure associated with a triaxial shear stress. At highθ(60°–85°), a double-upheaval morphology forms because the rear of the sliding mass impacts the front during the transition from the slope to the horizontal plane. The overall surface area of the landslides increases during their downslope motion and then decreases during their runout.