Debris flow initiation in postglacial terrain: Insights from shallow landslide initiation models and geomorphic mapping in Southeast Alaska

• Published in: Earth surface processes and landforms Vol. 47; no. 6; pp. 1583 - 1598
• Main Authors: Patton, Annette I., Roering, Joshua J., Orland, Elijah
• Format: Journal Article
• Language: English
• Published: Bognor Regis Wiley Subscription Services, Inc 01-05-2022
• Subjects: Atmospheric models; Debris flow; Density; Detritus; Extreme weather; Geomorphology; Glacial deposits; Glacial sedimentation; Glacial soils; Glaciation; Glaciology; Harvesting; Hazard mitigation; Land use; Landscape; Landslides; Landslides & mudslides; Mapping; Modelling; Rain; Rainfall; Rivers; Soil; Tephra; Terrain; Timber inventory; Volcanic activity; Volcanic soils; United States > US; Alaska
• ISSN: 0197-9337; 1096-9837
• DOI: 10.1002/esp.5336

Debris flows pose persistent hazards and shape high‐relief landscapes in diverse physiographic settings, but predicting the spatiotemporal occurrence of debris flows in postglacial topography remains challenging. To evaluate the debris flow process in high‐relief postglacial terrain, we conducted a geomorphic investigation to characterize geologic, glacial, volcanic, and land use contributions to landslide initiation across Southeast Alaska. To evaluate controls on landslide (esp. debris flow) occurrence in Sitka, we used field observation, geomorphic mapping, landslide characteristics as documented in the Tongass National Forest inventory, and a novel application of the shallow landslide model SHALSTAB to postglacial terrain. A complex geomorphic history of glaciation and volcanic activity provides a template for spatially heterogeneous landslide occurrence. Landslide density across the region is highly variable, but debris flow density is high on south‐ or southeast‐facing hillslopes where volcanic tephra soils are present and/or where timber harvest has occurred since 1900. High landslide density along the western coast of Baranof and Kruzof islands coincides with deposition of glacial sediment and thick tephra and exposure to extreme rainfall from atmospheric rivers on south‐facing aspects but the relative contributions of these controls are unclear. Timber harvest has also been identified as an important control on landslide occurrence in the region. Focusing on a subset of geo‐referenced landslides near Sitka, we used the SHALSTAB shallow landslide initiation model, which has been frequently applied in non‐glacial terrain, to identify areas of high landslide potential in steep, convergent terrain. In a validation against mapped landslide polygons, the model significantly outperformed random guessing, with area under the curve (AUC) = 0.709 on a performance classification curve of true positives vs. false positives. This successful application of SHALSTAB demonstrates practical utility for hazards analysis in postglacial landscapes to mitigate risk to people and infrastructure.
We conducted a geomorphic investigation to characterize the geomorphic histories that influence landslide initiation in postglacial terrain. Near Sitka, Southeast Alaska, we found that debris flow density is greatest on south‐ or southeast‐facing hillslopes where volcanic soils overlie till, where timber harvest has occurred since 1900, and where slope angle and contributing area are large. We also find that the topographic landslide susceptibility model SHALSTAB successfully predicts landslide‐prone areas in a postglacial landscape.