Approximately 35 parallel, discontinuous glacial ridges occur in an area of about 100 km² in north-central Wisconsin. The ridges are located between about 6 and 15 km north (formerly up-ice) of the maximum extent of the Wisconsin Valley Lobe of the Laurentide Ice Sheet. The ridges are between 1 and 4 m high, up to 1 km long, and spaced between 30 and 80 m apart. They are typically asymmetrical with a steep proximal (ice-contact) slope and gentle distal slope. The ridges are composed primarily of subglacial till on their proximal sides and glacial debris-flow sediment on the distal sides. In some ridges the till and debris-flow sediment are underlain by sorted sediment that was deformed in the former direction of ice flow. We interpret the ridges to be recessional moraines that formed as the Wisconsin Valley Lobe wasted back from its maximum extent, with each ridge having formed by a sequence of (1) pushing of sorted ice-marginal sediment, (2) partial overriding by the glacier and deposition of subglacial till on the proximal side of the ridge, and (3) deposition of debrisflow sediment on the distal side of the ridge after the frozen till at the crest of the ridge melted. The moraines are similar to annual recessional moraines described at several modern glaciers, especially the northern margin of Myrdalsjkull, Iceland. Thus, we believe the ridges probably formed as a result of minor winter advances of the ice margin during deglaciation. Based on this assumption, we calculate the net rate of ice-surface lowering of the Wisconsin Valley Lobe during the period when the moraines formed. Various estimates of icesurface slope and rates of ice-margin retreat yield a wide range of values for ice-surface lowering (1.7-14.5 m/yr). Given that ablation rates must exceed those of ice-surface lowering, this range of values suggests relatively high summer temperatures along the margin of the Wisconsin Valley Lobe when it began retreating from its maximum extent. In addition, the formation of annual moraines indicates that the glacier toe was thin, the ice surface was clean, and the ice margin experienced relatively cold winters.