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Bench: a flat section in steep terrain.  Characteristically narrow, flat or gently sloping with steep or vertical slopes on either side.  A bench can be formed by various geological processes.  Natural erosion of a landscape often results in a bench being formed out of a hard strip of rock edged by softer, sedimentary rock.  The softer rock erodes over time, leaving a narrow strip of rock resulting in a bench.  Coastal benches form out of continuous wave erosion of a coastline.  

Whistler & Garibaldi Park

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Cutting away at a coastline can result in vertical cliffs dozens or hundreds of metres high with a distinct bench form.  Often a bench takes the form of a long, flat top ridge.  Panorama Ridge in Garibaldi Provincial Park is an excellent example of a bench.  The Musical Bumps trail on Whistler Mountain is another good example of bench formations.  Each "bump" along the Musical Bumps trail is effectively a bench.  Russet Lake in Garibaldi Provincial Park has a prominent bench adjacent to it.  The bench separates Russet Lake and Adit Lakes.  Adit Lakes are two idyllic little tarns in a hidden valley separated from the much busier Russet Lake valley by this bench.  Towering above Russet Lake is The Fissile, which is visible from Whistler Village in several places.  Easy to spot on a clear day if you look up the valley between Whistler Mountain and Blackcomb Mountain, The Fissile is the symmetrical mountain peak in between.  The image below is the bench that separates Russet Lake and Adit Lakes and The Fissile in the next image at the far left.