Poland is mostly a lowland country. About 90% of the country, especially its central and northern parts, lies at elevations less than 300 m above sea level. The remaining territory are highlands that lie at elevations of 300-612 m, and mountains that usually lie at elevations of up to 1,200 m, with the highest peak at 2,499 m. The division of Poland into hydrogeological regions is linked to the geographic division of Poland. The Hydrogeological Atlas of Poland (Paczynski, 1995) identifies three regions: lowland, highland, mountain. A newer and more detailed system of classification identifies 161 bodies of groundwater in Poland (Paczynski and Sadurski, 2007). Lowland parts of Poland were shaped by a Pleistocene ice cap. Therefore, the surface of the land is rich in glacial features and A summary of the current body of knowledge on springs in Poland is presented. The paper relates the location of springs to geological structure, spring discharge, use of particular springs as well as threats associated with local groundwater nitrate pollution. Other key points include the uneven distribution of springs across Poland as well as varying levels of understanding of springs in northern Poland and in certain mountain ranges. The paper ends with a recommendation to monitor more springs over longer periods of time with respect to discharge and water quality.