A water draining foot mat having a base with a plurality of upward extending projections where the upper draining surface of the base is sloped to facilitate the draining of water from the mat and the tops of the projections form a support for people to step on. The projections are sufficiently spaced apart to permit the majority of snow impinging the mat to contact the base where it can melt with the assistance of sunlight or salt so that the resulting water flows off the mat. The mat optionally includes water retaining walls with one or more water exits so that the walls in conjunction with the slope of the upper surface of the base cause water impinging on the mat to flow towards the water exits and off the mat.