This storm became impressive as it moved into the Ohio Valley during the 13th. However, as additional energy moved into the eastern part of the country, a new area of low pressure developed near the North Carolina coast late on the 13th. This allowed mainly light snow to overspread the region from south to north during the early morning hours of the 13th. Low pressure developed in the southern Plains on Monday the 12th as a cold front pushed southward across the Northeast. By Tuesday the 13th, the storm moved eastward across the lower Mississippi Valley while the cold front became stationary in the Carolinas. On the night of the 13th, the primary low moved into the far eastern Ohio Valley while a secondary low developed on the stalled front in the Carolinas. During the day on Wednesday the 14th, this secondary low strengthened rapidly and moved northeastward along the mid-Atlantic and New England coasts while the primary low dissipated in the central Appalachians. By Thursday the 15th, the storm had moved into eastern Canada.