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Licenses: Creative Commons Attribution 3.0 New Zealand Organisations: Hawke's Bay Regional Council

  • Wairoa River Bank Stability Offset Boundaries

    Hawke's Bay Regional Council
    In 2009 Tonkin & Taylor Ltd were engaged by Hawke’s Bay Regional Council to undertake a preliminary assessment of the bank stability over a 12km reach of the lower Wairoa River, extending from approximately 3km downstream to 9km upstream of the SH2 bridge in Wairoa town.The purpose of the study is to provide a preliminary assessment of the existing...
    Created 10 September 2022 Updated 3 February 2025
  • Hawke's Bay Flood Risk Areas

    Hawke's Bay Regional Council
    Much of the settled Hawke’s Bay region is low lying and built on river flood plains. This brings the risk of flooding, which is our most common natural hazard - a severe storm or flood happens every 10 years on average. Major storms affect wide areas and can be accompanied by strong winds, heavy rain or snowfall, thunder, lightning, and rough seas. They...
    Created 10 September 2022 Updated 3 February 2025
  • Hawke's Bay Minimum Safe Distance for Boats

    Hawke's Bay Regional Council
    Boat safe distance depth - generalised 50m
    Created 10 September 2022 Updated 3 February 2025
  • Earthquake Amplification

    Hawke's Bay Regional Council
    This dataset is a subset of data, prepared by the Institute of Geological and Nuclear Sciences for the Hawke's Bay Regional Council, designed to help the Council plan to reduce the adverse impacts of future earthquakes. This data set refers to polygons in Hawke's Bay within each of which the ground has been assigned a uniform class of response to seismic...
    Created 10 September 2022 Updated 3 February 2025
  • Hawke's Bay Coastal Inundation

    Hawke's Bay Regional Council
    The coastal inundation hazard is determined based on permanent and extreme inundation along the open coast for present day and for the years 2065 and 2120. Permanent inundation is defined as the result of a rise in sea level on the astronomic tidal processes, whereas extreme inundation is a result of storm effects in addition to the astronomic tide level...
    Created 10 September 2022 Updated 3 February 2025