Landslide Hazard level: Very low ?

In the area you have selected landslide susceptibility is classified as very low according to the information that is currently available. This means that this area has rainfall patterns, terrain slope, geology, soil, land cover and (potentially) earthquakes that make localized landslides a rare hazard phenomenon. Based on this information, planning decisions such as project siting, project design, and construction methods, may want to consider the potential for landslides. Further detailed information should be obtained to better understand the level of landslide susceptibility in your project area.

Recommendations

• GOVERNMENT EXPERTISE: Contact the governmental organizations responsible for management of landslides in the project country (e.g. ministry of environment, national geological survey and/or local authorities) to obtain more detailed information on areas previously affected by landslides and areas considered to be highly susceptible. More information
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  Responsibility for landslide management is undertaken by a range of organisations, with significant variations between jurisdictions. It is important to identify the key organisations to contact.

  In many cases, national or state geological surveys maintain databases of landslides, which can include maps of known landslides, case studies of significant landslide events and a timeline of when major landslides have occurred. This provides important information about the local conditions (such as slope angle, geological materials and land use) in which landslides have occurred. This information can be used to see whether sites with similar conditions to those at the project site have suffered from landslides, or whether the project site (and its adjacent slopes) may have been subject to instability in the past.

  The data can also be used to consider the conditions under which landslides have been triggered. For example, what is the level of rainfall intensity and duration that led to landslides, and/or what was the nature of earthquake shaking that led to landslides occurring? In such cases, determine how large the landslides were, and examine how far they travelled.

  It is important to note that many such datasets are not complete because of the complex nature of collecting, curating and portraying landslide information. Thus, the absence of known landslides in similar conditions to those at the sites under consideration does not necessarily indicate that the sites will not be subject to landslides.

  More detailed information is often held by local government organisations. The format of these data can be variable – in some cases a detailed map of landslides might be available, whilst in others there might be a portfolio of case studies. This can provide insight into the problems that might be encountered at the sites under consideration, and of the processes that lead to landslides occurring.

  National and local government officials in planning and/or engineering departments, often have strong knowledge of specific local or site conditions (for example the types of materials and or slope gradients) that have been associated with landslide problems in the past. Seek their insight and advice where possible.

  However, every site is different, such that landslides can occur in areas that have not be prone to instability before. Thus, remember that this type of desk study does not remove the need to understand the likelihood of slope instability at a particular site.

  Weblinks: The USGS provide useful information on signs that might indicate that instability is developing: http://landslides.usgs.gov/learn/prepare.php

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• REGULATIONS: Ensure that the project obeys existing (if any) landslide zoning regulations. More information
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  Landslide zoning can be undertaken by a range of institutions, including national government, state level authorities and local governments, as well as private organisations. Determine which authority, if any, is responsible for landslide zonation in your area. In general the local planning department will be aware of the relevant regulations, although they may not undertake the zonation itself.

  Landslide zoning can be enshrined within legislation or it can be advisory. It is important to determine which is the case. Seek professional advice if necessary, and ensure that where zonation is prescriptive the recommendations are implemented.

  Landslide zoning most commonly takes into consideration slope angle and the type of material present. Other key factors can include the elevation of the site; its vegetation; previous land use; and its proximity to a slope. In some cases, zonation may include experience from previous events that, for example, has indicated that landslides can have a high degree of mobility.

  Remember that a site does not have to lie on a slope to be affected by a landslide. In many cases buildings on the valley floor are affected by landslides from adjacent slopes.

  In some cases it may be appropriate to undertake a landslide zonation for the project. If so, seek advice as to the most appropriate methodology to follow. Data for the zonation can be obtained from the local authority, geological survey, mapping agencies, satellite data providers, etc.

  Remember that a landslide zonation is not foolproof, and in particular may not take into consideration local site conditions. It does not remove the need for proper site investigation.

  Weblinks: Organization of American States guidance on landslide hazard zonation: http://www.oas.org/dsd/publications/unit/oea66e/ch10.htm

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