Surficial Geology of the Fulton Quadrangle

Author

Avery Merkley, University of Northern IowaFollow
Starr Claussen, University of Northern IowaFollow
Sage Cappi, University of Northern Iowa
Chad Heinzel, University of Northern IowaFollow

Location

ScholarSpace, Rod Library, University of Northern Iowa

Presentation Type

Open Access Poster Presentation

Document Type

poster

Abstract

• The Fulton 7.5’ Quadrangle lies within a geographic region known as the East-Central Iowa Drift Plain.
• The East-Central Iowa Drift Plain is characterized by glacial deposits that occurred over 1.8 million years ago. These glacial deposits are part of what makes up the loose soil material, which overlays a bedrock surface that is about 360-485 million years old.
• This area experiences significant change in elevation from the highest points to the lowest points in the Quadrangle.

Start Date

28-7-2023 11:00 AM

End Date

28-7-2023 1:30 PM

Event Host

Summer Undergraduate Research Program, University of Northern Iowa

Faculty Advisor

Chad Heinzel

Department

Department of Earth and Environmental Sciences

Copyright

©2023 Avery Merkley, Starr Claussen, Sage Cappi and Chad Heinzel

Creative Commons License

This work is licensed under a Creative Commons Attribution 4.0 International License.

File Format

application/pdf

Recommended Citation

Merkley, Avery; Claussen, Starr; Cappi, Sage; and Heinzel, Chad, "Surficial Geology of the Fulton Quadrangle" (2023). Summer Undergraduate Research Program (SURP) Symposium. 1.
https://scholarworks.uni.edu/surp/2023/all/1