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Sligo Bay
Cuan Shligigh

Overview

Sligo Bay is situated in Co. Sligo in the northwest of Ireland. Sligo Bay can be defined as an area east of a line made by the headlands at Aughris Head and Raghly Point. The distance between these two features is around 9 kilometres. Inside of these headlands are three smaller bays. These are Ballysadare Bay, Sligo Harbour and Drumcliff Bay. Two of these smaller bays, Ballysadare and Drumcliff, are partially separated from the outer bay by spit features with large areas of tidal flats that are exposed at low tide. Coney Island, Manguin’s Island and Oyster Island lie between Sligo Harbour and the outer bay. These intertidal areas are ideal habitats for shellfish whose abundance have supported humans inhabitation in the area since the Stone Age, evidenced by the large midden mounds which are found at various sites along the coast. These shells give Sligo its Irish name of Sligeach meaning ‘the place of shells’. INFOMAR surveys have also mapped the approaches to Sligo Bay.

Location of Sligo Bay in northwest Ireland.

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INFOMAR Survey History

Coverage from survey legs of Sligo Bay.(Click image for more detailed map).

Survey Coverage polygons can be downloaded as a shapefile from our Interactive Web Data Delivery System (IWDDS).

Select your area of interest. Vector datasets - Offshore - Offshore Shapefiles

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Shaded Relief

The 3D appearance is achieved using software called Fledermaus. By using some vertical exaggeration, artificial sun-shading (usually as if there is a light source in the nw 315°) and colouring the depths using various colour maps, it is possible to highlight the subtle relief of the seabed. This helps us to quickly understand the variation in depths.

MBES shaded relief overview image of the area mapped in Sligo Bay and approaches. (Click image for more detailed map)

Detailed MBES shaded relief image of rock outcrops on the seabed offshore of Raghly Point, Co. Sligo. (Click image for more detailed map)

Detailed MBES shaded relief image of rock outcrops and sediment scour marks on the seabed offshore of Aughris Head, Co. Sligo. (Click image for more detailed map)

Download a more detailed chart of the bathymetry of Sligo Bay here

Download Shaded Relief Bathymetry Geotiffs from our Interactive Web Data Delivery System (IWDDS)

Select your area of interest.Offshore Geotiffs - Bathymetry Shaded Relief Geotiffs.

Select your area of interest. Offshore Geotiffs - Lidar Shaded Relief Geotiffs.

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Backscatter

Multibeam Systems also collect additional information, including the strength of the acoustic signal (or return) from the seafloor. This is known as Backscatter. Differing seafloor types, such as mud, sand, gravel and rock will have different Backscatter values depending on the amount of energy they return to the sonar head. Rocky areas will typically have high returns while soft sediments like mud are more likely to absorb energy and have low Backscatter returns. These differing values are used to generate a grey-order image (i.e. dark for high returns, bright for low returns) of the seabed which can be used to examine the nature of the seafloor.

MBES backscatter image of the same area seen in shaded relief (above) off Raghly Point, Co. Sligo where varying the various shaded of grey represent the intensity of sound reflected from the seabed recorded by the multibeam sensors depending on hardness and other physical characteristics. The dark areas are rock outcrops and coarse sediments with fine sediments represented by light grey. (Click image for more detailed map).

Download a more detailed chart of the backscatter of Sligo Bay here

Download Backscatter Geotiffs from our Interactive Web Data Delivery System (IWDDS)

Select your area of interest.Offshore Geotiffs - Backscatter Geotiffs.

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Seabed Classification

The classification of the multibeam dataset from Sligo and Donegal Bays resulted in the creation of a 6 class classification divided into two types of rock, reflecting the different textures observed from rock outcrops in the bay. Three more classes divided the sediments into Fine Sand to Mud, sand and a sand veneer over rock. The final class displays areas of soft ground but showing high backscatter, possibly driven by biogenic content.

Seabed Classification Chart for Sligo and Donegal Bays (Click image for more detailed map).

Download a more detailed chart of the seabed classification of Sligo and Donegal Bays here

Further information about the classification process can be found in the Data Processing section.

You can download the Seabed Classification in ArcGIS GRID format data from IWDDS

(Data Type: ArcGIS GRIDS, Region: Offshore ArcGIS, Theme: Seabed Classification ArcGIS GRID

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LiDAR

LiDAR coverage in inner Sligo Bay from 2008 Tenix LADS survey. Interesting aspects include the sinuous tidal channels running through Ballysadare Bay in the south and also the navigation channel out of Sligo Harbour.

To view and navigate around the Lidar Sligo Bay dataset in Google Earth, click here

To view and navigate around the merged Donegal & Sligo Bay datasets in Google Earth, click here

To view additional datasets in Google Earth please click here

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Ground Truthing

A range of seabed sampling has been undertaken in Sligo Bay, both historically and under the INFOMAR project. These include grab samples, vibrocores and video footage. The locations of the grab samples have been mainly determined by the seabed classification made from the multibeam data.

Complete map of sampling locations of the northwest coast of Ireland including Sligo Bay and Approaches with a variety of sampling instruments. (Click image for more detailed map)

Sample locations can be downloaded as a shapefile from our Interactive Web Data Delivery System (IWDDS).

On the IWDDS Select your area of interest. Vector datasets - Offshore - Offshore Shapefiles

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Geology

Sligo Bay Geology


The rocks of Sligo Bay’s coastline are primarily composed of limestone and shale, with lesser exposures of mudstone and sandstone. Limestone is a carbonate rock that would have been formed many millions of years ago in a warm, shallow sea, whereas shale would originally have been formed from layers of mud in a deeper marine setting.

Onshore Bedrock Geology shapefiles can be downloaded from our Interactive Web Data Delivery System (IWDDS).

On the IWDDS Select your area of interest. Vector datasets - Onshore - Bedrock

Offshore Geology shapefiles can be downloaded from our Interactive Web Data Delivery System (IWDDS).

On the IWDDS Select your area of interest. Vector datasets - Offshore - Offshore Shapefiles

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Data Access

Full details outlining the process to gain access to datasets for the bay above or all INFOMAR data can be found in the INFOMAR | Data page of this website.

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Return to Survey Details Map

Follow these links to your area of interest on the INFOMAR website:

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