Highway Landslide Hazards in Indiana—Construction and Analysis of a Landslide Inventory Paper
Main Article Content
Abstract
Landslides are geologic hazards that occur throughout Indiana. Landslides are most prevalent in the southern half of the state, with two main landslide clusters in southeast and south-central Indiana. This paper discusses the construction of a landslide hazard geographic information system (GIS) data layer compiled from Indiana Department of Transportation (INDOT) sources. Landslide areas were identified using a digital elevation model (DEM) derived from light-compliant detection and ranging (LiDAR), a ground surface slope-angle map, and orthoimagery. These tools were used to map repaired and unrepaired landslide areas along highway infrastructure.
The study explores the relationship between landslide areas and various geological (bedrock, karst, and seismicity), climatic (rainfall), and anthropogenic (coal mining and land cover) factors. It finds that bedrock geology and the lack of a glacial cover are closely related to the occurrence of landslides. Areas with high landslide incidence closely relate to predominating shale bedrock formations and variable topography. Inclinometer data revealed that many landslides occur within the weathered bedrock zone where factors such as soil moisture and groundwater fluctuations play a role in landslide movement. The development of this study’s landslide inventory is anticipated to aid landslide susceptibility maps, risk assessments, and
emergency management within the state.
Downloads
Article Details
All content for Indiana Journal of Earth Sciences is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License (CC BY-NC 4.0; http://creativecommons.org/licenses/by-nc/4.0/), wherein the author retains copyright. As a service to the research community and as an outlet of its public mission, the IGWS commitment to true open access to scholarly information extends to authors, thus the Indiana Journal of Earth Sciences content is archived at the IGWS and the IU Open Scholar Works Archive.