After nearly five Earth years on Mars, the Mutch Memorial Station (Viking Lander 1) finally witnessed a local dust storm that eroded trenches, conical piles, and other disturbed surfaces in the sample field and near the lander. The event, called the Dust Storm of Sol 1742, occurred late in the third winter of lander observations between Sols 1728 and 1757. Analyses of tiny new wind tails and movement of materials indicate that the eroding winds were variable but more northeasterly than those that had perviously shaped the surface. Pebbly residues and movement of 4--5 mm clods suggest drag velocities as friction speeds of the winds were about 2.2--4.0 m/s. Wind speeds at the height of the meteorology boom (1.6 m) were probably about 40--50 m/s. Much of the observed erosion could have occurred in a few to several tens of seconds but somewhat longer times are suggested by analogy with the erosion of terrestrial soils. Most of the erosion occurred where preexistig equilibrium conditions of surface configurations and surface material properties had been altered by the lander during landing and during surface-sampler activities, but thin layers of bright fine-grained dust were also removed and redistributed. Surfaces where preexisting equilibrium conditions were unaltered appeared to be uneroded.