The State of Wisconsin is located in an unusually water-rich portion of the world in the
western part of the Great Lakes region of North America. This article presents an overview of …

Abstract The midcontinent of North America contains some of the thickest and most
extensive last-glacial loess deposits in the world, known as Peoria Loess. Peoria Loess of …

The erodent layer hypothesis (ELH) proposes that drumlinization leaves no substantial
stratigraphic record because it is primarily an erosional process that cuts an unconformity …

Global glaciations have varied in size and magnitude since the Early–Middle Pleistocene
transition (~ 773 ka), despite the apparent regular and high-amplitude 100 ka pacing of …

In a recent INQUA project the extent of Pleistocene glaciations has been digitally mapped
and the chronology of events reviewed. The onset of the present Ice Age in both …

Accurately measuring river meander migration over time is critical for sediment budgets and
understanding how rivers respond to changes in hydrology or sediment supply. However …

Excessive loading of fine sediment is a prominent cause of river impairment, not only due to
direct effects on biota and habitat but because sediment is often laden with excess nutrients …

We present the first study of the distribution, genesis and paleoenvironmental significance of
late Pleistocene loess in northeastern Wisconsin and adjacent parts of Michigan's Upper …

A machine learning methodology for processing and visualizing high‐resolution LiDAR
digital data is used to map drumlins and mega‐scale glacial lineations (MSGLs) on the bed …

Abstract Early, Middle, and Late Pleistocene till units are exposed in Wisconsin, some of
which are intensely weathered and possess reversed remanent magnetization. Late …