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Geology

Selected Works

Quaternary

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Articles 1 - 4 of 4

Full-Text Articles in Physical Sciences and Mathematics

Three-Dimensional Geological Model Of Quaternary Sediments In Walworth County, Wisconsin, Usa, Jodi Jau, Jason F. Thomason, David H. Malone, Eric Wade Peterson Jun 2016

Three-Dimensional Geological Model Of Quaternary Sediments In Walworth County, Wisconsin, Usa, Jodi Jau, Jason F. Thomason, David H. Malone, Eric Wade Peterson

Eric Wade Peterson

A three-dimensional (3D) geologic model was developed for Quaternary deposits in
southern Walworth County, WI using Petrel, a software package primarily designed for use in
the energy industry. The purpose of this research was to better delineate and characterize theshallow glacial deposits, which include multiple shallow sand and gravel aquifers. The 3D modelof Walworth County was constructed using datasets such as the U.S. Geological Survey 30 mdigital elevation model (DEM) of land surface, published maps of the regional surficial geology andbedrock topography, and a database of water-well records. Using 3D visualization and interpretationtools, more than 1400 lithostratigraphic picks were …

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Modeling The Sediment Fill Of The Uppertroy Pre-Glacial Bedrock Valley,Mchenry County, Llinois, Usa, Jodi Lau, Jason F. Thomason, David H. Malone, Eric Wade Peterson May 2016

Modeling The Sediment Fill Of The Uppertroy Pre-Glacial Bedrock Valley,Mchenry County, Llinois, Usa, Jodi Lau, Jason F. Thomason, David H. Malone, Eric Wade Peterson

Eric Wade Peterson

The Troy Bedrock Valley (TBV) and its tributary valleys are the principal pre-glacial drainage insouthern Wisconsin and northern Illinois, USA. This study focused on the headwaters of a tributarythat occurs in McHenry County, IL. Drilling, geophysical surveys, and the analysis of existinggeologic and water well data were used to determine the lithologic and geometric characteristicsof the sediments that fill the paleovalley. A 3D geologic model of these sediments was then developedin Petrel. More than 65 m of Quaternary sediments filled the paleovalley. The model domaincovers approximately 30 km2. The valley drains to the west and meanders, which is …

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Stratigraphy And Extent Of The Pearl-Ashmore Aquifer, Mchenry County, Il, Usa, Drew C. Carlock, David H. Malone, Jason F. Thomason, Eric Wade Peterson Dec 2015

Stratigraphy And Extent Of The Pearl-Ashmore Aquifer, Mchenry County, Il, Usa, Drew C. Carlock, David H. Malone, Jason F. Thomason, Eric Wade Peterson

Eric Wade Peterson

Quaternary glacial till, outwash, lake sediments, and loess compose the surficial deposits of McHenry County, Illinois. Much of the landscape of McHenry County were formed by at least three separate advances of the Harvard Sublobe of the Wisconsin Episode Lake Michigan Lobe, which was part of the Laurentide Ice Sheet. This project focuses on the delineation of the stratigraphy and extent of the Pearl-Ashmore Aquifer. The Pearl-Ashmore Aquifer is the combination of the proglacial outwash of the Wisconsin Episode Ashmore Tongue of the Henry Formation and the youngest outwash associated with the Illinois Episode, which is the Pearl Formation. A …

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Palaeotrophic Reconstruction And Climatic Forcing Of Mega-Lake Eyre In Late Quaternary Central Australia: A Review, Steve Webb Sep 2013

Palaeotrophic Reconstruction And Climatic Forcing Of Mega-Lake Eyre In Late Quaternary Central Australia: A Review, Steve Webb

Steve Webb

Extreme Quaternary climatic variation in Australia brought radical environmental changes to various parts of the continent. In this article, I discuss these changes in terms of mega-lake development in Central Australia, and in particular the southern Lake Eyre Basin (SLEB). The formation of these features, together with the fossil record of the region, throws light on the palaeoclimatic and palaeobiological relationships of megafauna and other animal groups, and the trophic development required to support them. Australian continental drying during the late Quaternary has been noted by many workers, but this process was punctuated by strong pluvial episodes of decreasing strength …

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