In layman's terms it is an elongated hill that runs north-south with the grade varying from 3 to 10 percent typically and sometimes upwards of 50 percent. They were created by the advance of glaciers from the last ice age. In more extreme situations here the glaciers dug and mounded enough to form the Finger Lakes with the melt water. Right where I am some of the more favorable soil types for farming have occurred on the drumlins but is not always necessarily true for every drumlin. The drumlins where I am at are known for artesian springs. This describes them to some degree here in Western NY but there are other examples here in the US and they probably have some different features.
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