Debris-Flow Hazards within the Appalachian Mountains of the Eastern United States

Gerald F. Wieczorek; Benjamin A. Morgan

doi:10.3133/fs20083070

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Debris-Flow Hazards within the Appalachian Mountains of the Eastern United States

Gerald F. Wieczorek·Benjamin A. Morgan

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Abstract

Tropical storms, including hurricanes, often inflict major damage to property and disrupt the lives of people living in coastal areas of the Eastern United States. These storms also are capable of generating catastrophic landslides within the steep slopes of the Appalachian Mountains. Heavy rainfall from hurricanes, cloudbursts, and thunderstorms can generate rapidly moving debris flows that are among the most dangerous and damaging type of landslides. This fact sheet explores the nature and occurrence of debris flows in the central and southern Appalachian Mountains, which extend from central Pennsylvania to northern Alabama.

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Source-reported bounding extent: 34° to 43° latitude; -86° to -72° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeX RIS

Gerald F. Wieczorek, Benjamin A. Morgan. 2008. Debris-Flow Hazards within the Appalachian Mountains of the Eastern United States. https://doi.org/10.3133/fs20083070

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