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      • Landslide hazard maps indicate the possibility of landslides occurring throughout a given area. An ideal landslide hazard map shows not only the chances that a landslide might form at a particular place, but also the chance that it might travel downslope a given distance.
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  2. These maps might be as simple as a map that uses the locations of old landslides to indicate potential instability, or as complex as a map incorporating probabilities based on variables such as rainfall, slope angle, soil type, and levels of earthquake shaking.

  3. Landslide hazard maps indicate the possibility of landslides occurring throughout a given area. An ideal landslide hazard map shows not only the chances that a landslide may form at a particular place, but also the chance that it may travel downslope a given distance.

  4. Jan 24, 2024 · Regional mapping of actively deforming landslides, including measurements of landslide velocity, is integral for hazard assessments in paraglacial environments. These inventories are also critical for describing the potential impacts that the warming effects of climate change have on slope instability in mountainous and cryospheric terrain.

  5. A Landslide is the movement of a mass of rock, debris, or earth down a slope. In the National Risk Index, a Landslide Risk Index score and rating represent a community's relative risk for Landslides when compared to the rest of the United States.

    • Determining Acceptable Risk
    • Hazard Assessment of Landslides
    • Factors Associated with Landslide Activity
    • Compensating For Insufficient Data: The Isopleth Map

    Figure 10-1 DEVELOPMENT PLANNING STUDY AND LANDSLIDE HAZARD ASSESSMENT ACTIVITIES The areal extent and variety of development activities being considered make determining the landslide susceptibility based on all existing landslides, regardless of type, an appropriate approach (DeGraff, 1982). A simple inventory of past landslides, along with data ...

    Three principles guide landslide hazard assessment. First, landslides in the future will most likely occur under geomorphic, geologic, and topographic conditions that have produced past and present landslides. Second, the underlying conditions and processes which cause landslides are understood. Third, the relative importance of conditions and proc...

    b. Bedrock

    The map overlays used to determine areas of bedrock, slope steepness, and hydrologic factor present in the entire study area can now be revised to make the hazard zonation map. Figure 10-12 shows the original maps redrawn into hazard zones. Combinations with extreme hazard are redrawn and relabeled as extreme hazard zones. Redrawing and relabeling for combinations representing other hazard zones produces a completed hazard zonation map displaying four levels of relative hazard. The empirical...

    The objective is to minimize the value of W. In other words, find the smallest W values that can be computed for three groups of the proportional values. This applies the principle of least squares, a common statistical approach, to this one-dimensional problem through minimizing the sum of squared deviations about the around means. Step 3:The boun...

  6. Landslide Map: This map shows the distribution of relative landslide incidence and susceptibility across the conterminous United States. Red areas have the highest rates of landslide incidence. Pink areas have high rates of landslide incidence and susceptibility. Map by the United States Geological Survey. Enlarge Image. Table of Contents.

  7. The Global Landslide Hazard Map presents a qualitative representation of global landslide hazard at a global scale. It is the combination of the The Global Landslide Hazard Map: Median Annual Rainfall-Triggered Landslide Hazard (1980-2018) and The Global Landslide Hazard Map: Earthquake-Triggered Landslide Hazard which has then been simplified ...

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