NE SE NE sec. Discharge is west to run in right foreground. The spring pool is about 50 ft in diameter and in a natural wooded setting in the headwater area of Shady Brook, which drains to Lake Panasoffkee. The surrounding land is fairly flat with numerous closed depressions and some nearby swampland. Land surface is sandy with limestone bedrock near the surface and fragments scattered on the surface.
Bedrock is overlain by clay and sandy clay layers.
Discharge apparently is from solution channel or cavern openings in the limestone below the ledge. The water had a dark brown tannin color, and although the water was not turbid, the color reduced visibility to only a few feet of depth. The color suggests a shallow source closely associated with surface runoff. The owner reports that the degree of color varies considerably, on occasion being nearly colorless, but that it generally has appreciable color. About 10 ft S. of the main spring is a spring that is about 30 ft in diameter and that had a measured depth of 30.1 ft on July 26, 1946.