| 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). |