Former interlocking spurs may be cut off by the glacier as it flows downhill, leaving truncated spurs and steep valley sides.
The width and shape of the resulting glacial trough will depend on the nature of the rock type and the intensity and weight of the glacial and its erosion.
An example of a glacial valley is Glencoe.
The valley becomes wider and straighter, often with a misfit stream which no longer fits the valley floor.