The surficial geology in its vicinity consists of Wisconsinan Till, a lake, and some alluvium in the lower reaches.

It flows south for several tenths of a mile and enters Jones Lake, where it receives two unnamed tributaries from the right.

From the southern end of Jones Lake, the creek flows south-southeast for a few miles, receiving two unnamed tributaries from the left and two from the right and entering a valley.

[6] In the upper reaches, the surficial geology alongside the creek consists entirely of Wisconsinan Till, except for Jones Lake.

[2] The mouth of the creek is in the United States Geological Survey quadrangle of Hop Bottom.