This document discusses river landforms in the upper course of a river. It begins by explaining that river landforms are shaped by the geology of an area and river processes. The dominant process in the upper course is erosion, which cuts down vertically to form a V-shaped valley. One landform discussed is interlocking spurs, which are areas of resistant rock that the river bends and winds around, leaving protruding areas of hard rock between indentations eroded into softer rock. Another landform is waterfalls and gorges, which form where there are bands of hard and soft rock. Waterfalls erode upstream over time, deepening plunge pools and forming steep rock walls of a gorge as the waterfall retreats