Hard (immobile) |
Immobile hard substratum e.g. solid rock, concrete but inc. soft rocks , such as chalk . |
Artificial (man-made) |
Man-made structures e.g. of metal, wood or concrete. |
Bedrock |
Any stable hard substratum, not separated into boulders or smaller sediment units. Includes soft rock-types such as chalk, peat and clay (Hiscock et al., 1999). |
Large to very large boulders |
Boulders >512 mm; likely to be stable (Hiscock, 1996). |
Small boulders |
256 - 512 mm. May be unstable. |
Hard (mobile) |
Mobile hard substratum, e.g. cobles, pebbles that are regularly moved by wave action |
Cobbles |
64-256 mm. May be rounded to flat. Substrata that are predominantly cobbles. |
Pebbles |
16-64 mm. May be rounded to flat. Substrata that are predominantly pebbles. |
Sediment (soft) |
Particulate solid material accumulated by natural processes (from Baretta-Bekker et al., 1992) |
Coarse sediment |
Gravel, sandy gravel and gravelly sand ( Long, 2006) |
Gravel or shingle |
4 -16 mm. Clean stone or shell gravel including dead maerl. >80% gravel. |
Sandy gravel |
50 -80% gravel, 20 -50% sand. |
Gravelly sand |
50 -80% sand, 20 -80% gravel. |
Sand and muddy sand |
Fine to coarse sands and muddy sands (Long, 2006) |
Sand |
0.063 - 4 mm. >80 % sand |
Coarse clean sand |
0.5 - 4 mm. >80 % sand. |
Medium clean sand |
0.25-1mm > 80 % sand. |
Fine clean sand |
0.063 - 0.5 mm. >80 % sand. |
Sandy mud |
50 - 80 % mud, 20 - 50 % sand |
Mud and muddy sand |
Muds and sandy mud (Long, 2006). |
Muddy sand |
50 - 80 % sand, 20 - 50 % mud. |
Mud |
<0.063 mm (silt / clay fraction). >80% mud. |
Mixed |
Mixtures of sediment types, composed of pebbles, gravel, sand or mud. This category includes muddy gravels, muddy sandy gravels, gravelly muds, and muddy gravelly sands. |
Muddy gravel |
50 - 80 % gravel, 20 - 50 % mud. |
Gravelly mud |
50 -80% mud, 20 -50% gravel. |
Muddy sandy gravel |
50 -80% gravel, 20 -50% mud and sand |
Muddy gravelly sand |
50 -80% sand, 20 -50% mud and sand |
Sandy gravelly mud |
50 -80% sand, 20 -50% mud and sand |
Biogenic reef |
An elevated structure on the seabed built by calcareous or other concretion-forming organisms, or by chemical precipitation (Hiscock, 1996) e.g. reefs of Modiolus modiolus or Sabellaria alveolata. |
Burrow dwellers |
Occupies or shares space in burrow constructed by other organisms. |
Caves |
A large hollow in the side of a vertical rock face or cliff. |
Crevices or fissures |
Narrow openings (Thompson, 1995) |
Macroalgae |
Macroalgae surfaces, such as the fronds of kelps or fucoids. |
Maerl |
Calcareous nodules (rhodoliths) of maerl that may build up to form maerl beds |
Seagrass |
Habitat associated with seagrass bed communities. |
Strandline |
A line on the shore of composting debris deposited by a receding tide; commonly used to denote the line of debris at the level of extreme high water (Lincoln et al., 1998). |
Salt marsh |
A flat, poorly drained coastal swamp inundated by most high tides (Lincoln et al., 1998). |
Overhangs |
An overhanging part of a rock formation (Thompson, 1995). |
Other species |
The surface of other species, e.g. shells or carapace. |
Peat (fossilized) |
A pure organic soil, the result of plant material accumulating in waterlogged conditions (from Fitter & Manuel, 1986). Fossilized peat may also be exposed and provide a unique substratum in the intertidal. |
Rockpools |
A pool of water among rocks left behind by the ebbing tide |
Under boulders |
Habitat associated with the underside of boulders. |
Wrecks |
Remains of sunken vessels (boats and ships). |