and soils. They also do not have the problem of acid wells. Therefore, it should be recognized that the acidity of Southeastern Connecticut's ground water is due to a combination of acid rain and the native rock and soil properties. Figure 2 is a picture taken in the Norwich area, at Exit 81 on Interstate 395. This outcrop shows the typical bedrock of the county. Figure 2 Typical Granitic Rock Outcrop in Norwich Conclusions and Recommendations

DOI link for and soils. They also do not have the problem of acid wells. Therefore, it should be recognized that the acidity of Southeastern Connecticut's ground water is due to a combination of acid rain and the native rock and soil properties. Figure 2 is a picture taken in the Norwich area, at Exit 81 on Interstate 395. This outcrop shows the typical bedrock of the county. Figure 2 Typical Granitic Rock Outcrop in Norwich Conclusions and Recommendations

and soils. They also do not have the problem of acid wells. Therefore, it should be recognized that the acidity of Southeastern Connecticut's ground water is due to a combination of acid rain and the native rock and soil properties. Figure 2 is a picture taken in the Norwich area, at Exit 81 on Interstate 395. This outcrop shows the typical bedrock of the county. Figure 2 Typical Granitic Rock Outcrop in Norwich Conclusions and Recommendations