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Physical Sciences · Environmental Science

Landslides and related hazards
Research Guide

What is Landslides and related hazards?

Landslides and related hazards are the damaging processes and risks associated with the downslope movement of rock, soil, or debris—often triggered by rainfall, earthquakes, or hydrologic change—and their assessment, mapping, and management for risk reduction.

The research literature on landslides and related hazards spans hazard assessment, susceptibility mapping, and process-based understanding of slope failure and mass flows, including debris flows and rock-slope instabilities. This topic cluster contains 144,731 works (5-year growth rate: N/A). Core technical foundations include standardized landslide type classification, multi-scale hazard evaluation methods, and physically based descriptions of debris-flow behavior (Hungr et al., 2013; Guzzetti et al., 1999; Iverson, 1997).

Topic Hierarchy

100%
graph TD D["Physical Sciences"] F["Environmental Science"] S["Management, Monitoring, Policy and Law"] T["Landslides and related hazards"] D --> F F --> S S --> T style T fill:#DC5238,stroke:#c4452e,stroke-width:2px
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144.7K
Papers
N/A
5yr Growth
1.7M
Total Citations

Research Sub-Topics

Why It Matters

Landslide science directly supports public safety decisions such as zoning, infrastructure corridor planning, and early warning by linking failure mechanisms to mapped hazard and exposure. Guzzetti et al. (1999) in "Landslide hazard evaluation: a review of current techniques and their application in a multi-scale study, Central Italy" synthesized how landslide hazard evaluation methods can be applied across scales, which is central to producing actionable susceptibility and hazard maps for local planning versus regional screening. Standardized terminology and process distinctions in "The Varnes classification of landslide types, an update" (Hungr et al., 2013) matter operationally because emergency managers and engineers need consistent categories (e.g., falls, slides, flows) to choose monitoring strategies and mitigation designs appropriate to the expected kinematics and material. For flow-like hazards, Iverson (1997) in "The physics of debris flows" provided a physics-based framework for debris-flow behavior, supporting engineering design of protective structures and runout assessment where solid–fluid mixtures can rapidly threaten roads and settlements. Policy and funding signals in "National Landslide Preparedness Act and the Status of Landslide Risk Reduction" (2025) quantify U.S. federal support for implementation: $25 million annual funding for FY2021–FY2024 for the USGS to carry out NLHRP, plus $11 million for NSF landslide research grants and $1 million for NOAA, illustrating that landslide risk reduction is treated as an applied national capability rather than only an academic topic.

Reading Guide

Where to Start

Start with "The Varnes classification of landslide types, an update" (Hungr et al., 2013) because it provides the shared vocabulary and typology that most mapping, inventories, and hazard discussions assume.

Key Papers Explained

A practical pathway is classification → hazard evaluation → process mechanics. "The Varnes classification of landslide types, an update" (Hungr et al., 2013) standardizes what is being mapped and compared. "Landslide hazard evaluation: a review of current techniques and their application in a multi-scale study, Central Italy" (Guzzetti et al., 1999) then organizes how those mapped phenomena are translated into hazard evaluation across scales. For fast, flow-like hazards, "The physics of debris flows" (Iverson, 1997) provides the process mechanics that complement mapping-based approaches; for rock-slope problems, "A bonded-particle model for rock" (Potyondy and Cundall, 2004) and "The shear strength of rock joints in theory and practice" (Barton and Choubey, 1977) supply modeling and strength concepts often used to interpret instability in jointed rock.

Paper Timeline

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graph LR P0["The Physics of Glaciers
1969 · 3.4K cites"] P1["Kinetic theories for granular fl...
1984 · 3.0K cites"] P2["Equations for the soil-water cha...
1994 · 3.0K cites"] P3["Fluid flow through granular beds
1997 · 3.2K cites"] P4["A bonded-particle model for rock
2004 · 4.6K cites"] P5["Warming and Earlier Spring Incre...
2006 · 5.2K cites"] P6["The Varnes classification of lan...
2013 · 3.1K cites"] P0 --> P1 P1 --> P2 P2 --> P3 P3 --> P4 P4 --> P5 P5 --> P6 style P5 fill:#DC5238,stroke:#c4452e,stroke-width:2px
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Most-cited paper highlighted in red. Papers ordered chronologically.

Advanced Directions

Applied frontiers emphasized by the provided materials include institutionalization of landslide risk reduction and sustained monitoring capacity, reflected in "National Landslide Preparedness Act and the Status of Landslide Risk Reduction" (2025) and its multi-agency funding allocations ($25 million USGS NLHRP annually for FY2021–FY2024; $11 million NSF; $1 million NOAA). Research directions consistent with the top-cited foundations include tighter coupling of hydrologic state variables (Fredlund and Xing, 1994) with multi-scale hazard evaluation (Guzzetti et al., 1999) and more explicit links between rock-mass discontinuity strength (Barton and Choubey, 1977) and emergent failure in numerical rock models (Potyondy and Cundall, 2004).

Papers at a Glance

# Paper Year Venue Citations Open Access
1 Warming and Earlier Spring Increase Western U.S. Forest Wildfi... 2006 Science 5.2K
2 A bonded-particle model for rock 2004 International Journal ... 4.6K
3 The Physics of Glaciers 1969 3.4K
4 Fluid flow through granular beds 1997 Process Safety and Env... 3.2K
5 The Varnes classification of landslide types, an update 2013 Landslides 3.1K
6 Equations for the soil-water characteristic curve 1994 Canadian Geotechnical ... 3.0K
7 Kinetic theories for granular flow: inelastic particles in Cou... 1984 Journal of Fluid Mecha... 3.0K
8 The physics of debris flows 1997 Reviews of Geophysics 2.9K
9 The shear strength of rock joints in theory and practice 1977 Rock Mechanics and Roc... 2.8K
10 Landslide hazard evaluation: a review of current techniques an... 1999 Geomorphology 2.6K

In the News

Code & Tools

Recent Preprints

Latest Developments

Recent research indicates that climate change is increasing the frequency and severity of destructive landslides, particularly in Alaska, due to more extreme atmospheric rivers (KTOO). Additionally, advancements in technologies such as remote sensing, AI, and digital modeling are transforming hazard detection, risk assessment, and understanding of landslide mechanisms, including submarine landslides and slow-to-fast sliding transitions (Nature, Scientific Reports, From observation to understanding).

Frequently Asked Questions

What are “landslides and related hazards” in research and practice?

Landslides and related hazards refer to slope failures and mass movements (including flow-like processes such as debris flows) and the associated risks that are assessed through mapping, classification, and hazard evaluation. "The Varnes classification of landslide types, an update" (Hungr et al., 2013) provides a widely cited framework for defining and distinguishing landslide types used in reporting and analysis.

How are landslide types classified in a way that supports hazard mapping and communication?

"The Varnes classification of landslide types, an update" (Hungr et al., 2013) updates a standardized classification that separates landslides by movement style and material, enabling consistent inventories and comparable susceptibility maps. A consistent classification reduces ambiguity when linking observed failures to triggering conditions and selecting mitigation approaches.

How do researchers evaluate landslide hazard across different spatial scales?

Guzzetti et al. (1999) in "Landslide hazard evaluation: a review of current techniques and their application in a multi-scale study, Central Italy" reviewed hazard evaluation techniques and demonstrated their use in a multi-scale setting. The key practical point is that methods and data requirements differ between local site assessment and regional screening, so scale must be explicit in study design and interpretation.

How are debris flows treated within “landslides and related hazards,” and what models guide understanding?

Iverson (1997) in "The physics of debris flows" treated debris flows as solid–fluid mixtures whose dynamics can be analyzed using theory and experiments, providing a basis for interpreting mobility and impacts. This framing helps distinguish debris-flow hazards from slower, slide-dominated failures when estimating runout and designing protections.

Which foundational mechanics papers are commonly used to model slope materials and failure processes?

Potyondy and Cundall (2004) in "A bonded-particle model for rock" provides a numerical approach for representing rock as bonded particles, supporting simulation of fracturing and rock-slope instability. Barton and Choubey (1977) in "The shear strength of rock joints in theory and practice" is frequently used to reason about joint-controlled rock mass behavior relevant to rockslides and rockfalls.

What is the current policy and funding context for landslide risk reduction in the United States?

"National Landslide Preparedness Act and the Status of Landslide Risk Reduction" (2025) reports annual funding for FY2021–FY2024 of $25 million for the USGS to carry out NLHRP, $11 million for NSF landslide research grants, and $1 million for NOAA. These figures indicate sustained, multi-agency investment in monitoring, preparedness, and applied research rather than one-off response spending.

Open Research Questions

  • ? How can the standardized movement-and-material distinctions in "The Varnes classification of landslide types, an update" (Hungr et al., 2013) be operationalized to improve cross-region comparability of landslide inventories used in susceptibility mapping?
  • ? What model structures best reconcile the process-based insights in "The physics of debris flows" (Iverson, 1997) with multi-scale hazard evaluation workflows described in "Landslide hazard evaluation: a review of current techniques and their application in a multi-scale study, Central Italy" (Guzzetti et al., 1999)?
  • ? How can bonded-particle approaches from "A bonded-particle model for rock" (Potyondy and Cundall, 2004) be validated against field-observed failure modes in jointed rock slopes characterized using "The shear strength of rock joints in theory and practice" (Barton and Choubey, 1977)?
  • ? Which hydromechanical parameterizations derived from "Equations for the soil-water characteristic curve" (Fredlund and Xing, 1994) most strongly control the timing and likelihood of rainfall-triggered slope failures in operational hazard assessments?
  • ? How should granular-flow theory from "Kinetic theories for granular flow: inelastic particles in Couette flow and slightly inelastic particles in a general flowfield" (Lun et al., 1984) be incorporated into debris-flow or dry granular runout modeling without overfitting beyond available observations?

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