The Minnesota Geological Survey has released new guidance on how best to recognize the Coon Valley Member (Oneota Dolomite, Prairie du Chien Group) and how to differentiate it from the underlying Jordan Sandstone in southeastern Minnesota.
The intended audience is the water well drilling community, as there are rare situations where precise recognition of the Coon Valley Member is important for code compliance (per Minnesota Rules, Chapter 4725).
Generalized stratigraphic column describing the vertical location of the St. Peter Sandstone, members of the Prairie du Chien Group, and the Jordan Sandstone units in relation to one another. To the right are summarized descriptions of the common rock types associated with each unit.
An interval of drill core from Ramsey County that passes through the Coon Valley Member (Prairie du Chien Group) and Jordan Sandstone. Note how this single deposit of the Coon Valley Member is composed of a mixture of thinly bedded rock types (primarily dolostone and sandy dolostone in this example) while the Jordan Sandstone is entirely well sorted sandstone. Up is towards the left.
Questions?
For questions regarding the geology of the Coon Valley Member, please contact: