USGS Scientific Investigations Report 2018-5091: Characterization and Occurrence of Confined and Unconfined Aquifers in Quaternary Sediments in the Glaciated Conterminous United States

Figure 51A

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EXPLANATION

Probability of penetrating an

confined aquifer-material interval,

if present, in percent

Well count

≥10

6 to <10

3 to <6

0 to 20

>20 to 40

>40 to 60

>60 to 80

>80 to 100

Hydrogeologic terrane boundaries—Alphanumeric code indicates the

generalized complexity of the hydrogeologic framework in each terrane

Sediment thickness contrast

Major river

Maximum extent of glacial ice

Extent of Late Wisconsinan ice

Figure 51A. Probability of penetrating at least one aquifer-material interval in lithologic logs from selected confined and unconfined aquifers in North Dakota in the glaciated conterminous United States.

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