On 1 July 2025, NIWA merged with GNS Science to become Earth Sciences New Zealand.

Coasts

NIWA aims to provide the knowledge needed for the sound environmental management of our marine resources.

  • LakeSPI diver

    How LakeSPI works

    LakeSPI (Lake Submerged Plant Indicators) is based on the principle that New Zealand lakes can be characterised by the composition of native and invasive plants growing in them, and the depths to which these plants grow.
  • Journey Across an Underwater Landscape

  • Sediments and mangroves

    Research Project
    Mangrove forests, which are important parts of estuarine ecosystems in a number of ways, are sensitive to changing sea level.
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    New Zealand Coastal Society Annual Conference: ‘Making Waves, 20 years and beyond’

    News article
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    How prepared are we for a major marine earthquake?

    News article
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    DTIS - Deep Towed Imaging System

    DTIS is a camera system designed and built by NIWA staff, which is used to take pictures and video of deep sea biodiversity and seafloor habitats at depths of up to 6km.
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    Category H - Drowned valleys, rias or fjords

    Deep (10s of metres), narrow, elongated basins which are largely subtidal - the estuary bed is still below water at low tide.
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    Category G - Fjords or sounds

    Very deep (up to 100s of metres), narrow, elongated basins which are largely subtidal.
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    Category F - Barrier enclosed lagoons or drowned valleys

    Similar in some respects to Category E estuaries, these have shallow basins and narrow mouths, usually formed by a spit or sand barrier. However, Category F estuaries have complex shorelines and numerous arms leading off a main basin.
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    Category E - Tidal lagoons or barrier enclosed lagoons

    Shallow, circular to slightly elongated basins with simple shorelines and extensive intertidal area.
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    Category D - Coastal embayments

    Shallow, circular or slightly elongated basins with simple shorelines and wide entrances that are open to the ocean.
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    Category C - Tidal river lagoons

    These occur where the mouth of a main river channel connects to shallow lagoons.