Natural Hazards in Iron, Utah

This study examines natural hazards that may impact future housing development in a 1-square-mile area located in Iron, Utah. The goal is to identify potential geologic risks and inform residents and developers about land safety. We focus on analyzing geological materials, seismic history, and topographic features. The site’s geology includes alluvium, which may pose construction risks. For example, the loose alluvium could lead to mudslides. We also reviewed seismic hazards by examining the region’s earthquake history. Since 1902, the area has experienced only regional earthquakes, with an average magnitude of 3.0 and a maximum magnitude of 6.3. This frequency and intensity suggest the area may experience seismic hazards. Topographic features could also pose additional risks. These could exacerbate problems like mass movements and flooding. By identifying geological, seismic, and topographic hazards, this research provides valuable insights to guide development decisions. We recommend implementing strategies like implementing protections against mass movement to mitigate these risks and ensure safer living environments for future residents. Understanding these hazards is essential for creating sustainable, safe housing developments in Iron, Utah.

Publication Details

Journal
ScholarSpace - JCCC (Johnson County Community College)
Published
2025-05-01
Primary Topic
Landslides and related hazards
Type
article
Field-Weighted Citation Impact
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article

Natural Hazards in Iron, Utah

ScholarSpace - JCCC (Johnson County Community College)
Landslides and related hazards
article

Natural Hazards in Iron, Utah

article en

Abstract

This study examines natural hazards that may impact future housing development in a 1-square-mile area located in Iron, Utah. The goal is to identify potential geologic risks and inform residents and developers about land safety. We focus on analyzing geological materials, seismic history, and topographic features. The site’s geology includes alluvium, which may pose construction risks. For example, the loose alluvium could lead to mudslides. We also reviewed seismic hazards by examining the region’s earthquake history. Since 1902, the area has experienced only regional earthquakes, with an average magnitude of 3.0 and a maximum magnitude of 6.3. This frequency and intensity suggest the area may experience seismic hazards. Topographic features could also pose additional risks. These could exacerbate problems like mass movements and flooding. By identifying geological, seismic, and topographic hazards, this research provides valuable insights to guide development decisions. We recommend implementing strategies like implementing protections against mass movement to mitigate these risks and ensure safer living environments for future residents. Understanding these hazards is essential for creating sustainable, safe housing developments in Iron, Utah.

ScholarSpace - JCCC (Johnson County Community College)
Sustainable cities and communities
Openalex Percentile: Top 40%
Landslides and related hazards
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