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GetWET Geology The GetWET Observatory is situated in the Nunn Clay Loam soil that developed in Spring Creek alluvium. The well field is on the inside of a broad meander bend on the floodplain. The bedrock below the alluvium is Pierre Shale.
Click here for a summary diagram of the stratigraphy of the boreholes. Click here for the complete description of the cores recovered during the installation of the wells. |
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