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The surficial geology of Fulton County, Ohio - insight into the Late Pleistocene-Early Holocene glaciated landscape of the Huron-Erie Lake Plain, Fulton County Ohio, USA
Table of Contents
Abstract
Acknowledgements
Table of Contents
List of Tables
List of Figures
1 Introduction
1.1 Introduction
1.2 Objective and Hypothesis
1.3 Structure of Thesis
2 Methodology
2.1 Overview
2.2 Ground Penetrating Radar
2.3 Electrical Resistivity
3 Surficial Geology of Fulton County, Ohio
3.1 Introduction
3.2 Study Area
3.2.1 The Defiance Moraine
3.3 Results
3.3.1 Alluvial Terrain
3.3.2 Eolian Terrain
3.3.3 Glacial Terrain
3.3.4 Glacial Fluvial Terrain
3.3.5 Glacial LacustrineTerrain
3.4 Discussion
3.4.1 Interpretation and Correlation of OSL Ages to Climatic Events
3.4.2 Clast Analysis
3.4.3 OSL Sample Six and the Defiance Moraine
3.4.4 Correlation of Early and Late Woodfordian Till
3.5 Conclusions
4 Ice-Walled Lake Plains
4.1 Introduction
4.2 Study Area
4.3 Background
4.4 Results
4.5 Discussion
4.5.1 Sediment Architecture and Previous Models
4.6 Conclusions
5 Lake Maumee
5.1 Introduction
5.2 Study Area
5.3 Background
5.4 Results
5.5 Discussion
5.5.1 Morphology
5.5.2 Elevation
5.5.3 Sediment Architecture
5.5.4 Timing of Winameg Ridge
5.5.5 Previous Models and Draining of Lake Maumee at Fort Wayne, IN .
5.6 Conclusions
6 Summary, Conclusions, and Future Work
6.1 Summary
6.2 Future Work
6.2.1 The Timing of Events
6.2.2 Elevation and Surficial Mapping
References
Appendices
A. Particle-Size Distribution of Sediment
B. Dipole-Dipole Profiles
C. Schlumberger Soundings
D. Ground Penetrating Radar Profiles Bài viết liên quan
