A peatland with roughly parallel narrow ridges of peat dominated by fenland vegetation interspersed with slight depressions, many of which contain shallow pools
A peatland with roughly parallel narrow ridges of peat dominated by fenland vegetation interspersed with slight depressions, many of which contain shallow pools.
A long narrow area of pack ice, about 1 km or less in width, usually composed of small fragments detached from the main mass of ice, and run together under the influence of wind or current.
Sea ice terminology. Describes a long narrow area of pack/drift ice, about one (1) km or less in width, usually composed of small fragments detached from the main mass of ice, which run together under
the influence of wind, swell or current.
A long narrow area of pack ice, about 1 kilometer (0.6 mile) or less in width, usually composed of small fragments detatched from the main mass of ice, and run together under the influence of wind or
current.
A long narrow zone of floating ice, about 1 km or less in width, usually composed of small fragments detached from the main mass of ice, and run together under the influence of wind, swell or current.
Long narrow area of pack ice, about 0.5 n mi (1 km) or less in width, usually composed of small fragments detached from the main mass of ice, and run together under the influence of wind, swell, or cu
rrent.
The term is applied for characterizing irregularities of the total and partial concentration in a delineated zone when it is impossible to depict the position of strips and patches on the ice chart as
separate zones.
Strombolian Eruptions are characterised by huge clots of molten lava bursting from the summit crater to form luminous arcs through the sky. Collecting on the flanks of the cone, lava clots combine to
stream down the slopes in molten rivulets. The explosions are driven by bursts of gas slugs that rise faster than surrounding magma