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Introduction

Volcanic Hazards

Scientists

Emergency Managers

The Media

Appendices
Volcanic Terminology Page 30
Volcanic Terminology Page 31
Tips for Interviewees Page 32
Resource Guide Page 33
Volcano Observatories & Directors Page 34
Related Reading Page 35
Internet Resources & Volcano Alert Levels Page 36
Example press release Page 37
Communication During Volcanic Emergencies
An Operations Manual for the Caribbean

ANDESITE - A type of pale volcanic rock, very common in the Caribbean. ASH - Particles of magma less than 2 mm across. Volcanic ash is produced during explosive eruptions. It may be formed either from a disrupted spray of liquid magma ejected from a volcanic vent, or from the pulverisation of preexisting rock that may have blocked the vent during a period of quiescence.

BOMB - Rounded volcanic fragment larger than 64 mm across ejected from a volcano during an explosion. During flight through the air, bombs may develop distinctive torpedo or spindle shapes.

BOULDER - Generic term for rounded rock fragments, not necessarily volcanic, more than 256 mm across.

CALDERA - A giant volcanic crater (notionally larger than 1 km across) formed by collapse or explosion, collapse being more important among larger calderas. The name comes from the Caldera Taburiente on La Palma in the Canary Islands.

CINDER - Generic term for coarse volcanic ash and lapilli.

COLUMN COLLAPSE - During moderate to large explosive eruptions an enormous amount of ash and coarser debris is ejected from the vent to form an eruption column that can rise to tens of kilometres. When the mass of the debris is too heavy it begins to fall back to Earth - a condition known as column collapse. Commonly the collapsed material pours off down the flanks in the form of pyroclastic flows.

CONE - Conical constructs built up by the accumulation of material around a vent. They may consist of tephra or a mixture of tephra and lava flows. Cones may be the result of a single eruption or the product of many eruptive episodes.

CRATER - A pit or depression, typically located around a vent. Craters may be formed during construction of an enclosing cone, by the excavation of rock during volcanic explosions, or by the collapse of ground left without support after magma has been erupted. Craters wider than about 1 km are
normally termed calderas.

DACITE - Type of volcanic rock, typical of volcanic domes like those of Monserrat. Very common throughout the Caribbean.

DYKE - Vertical fractures filled with solidified magma. When magma stops flowing through a fissure on the ground it solidifies to form a 'wall' of volcanic rock that may be exposed by future erosion. Similar features lying almost horizontally are termed sills.

ELECTRONIC DISTANCE METER (EDM) - A surveying instrument that is used in volcanology to measure very precisely the distances between benchmarks in a ground deformation monitoring network. A beam of infrared, laser, or microwave radiation generated by the instrument - mounted on a tripod positioned over one benchmark - is bounced back by a reflector mounted on a second tripod mounted above another benchmark, and the distance determined to within a centimetre or two over distances of several kilometres.

ERUPTION COLUMN - During explosive eruptions, ash and debris ejected from the vent forms a vertical jet that may reach tens of kilometres in height. Because it is hotter than the surrounding atmosphere, an eruption column rises due to buoyancy.

FISSURE - A surface fracture. Often the surface expressions of dykes, fssures may also open near the rims of unstable slopes, including craters.

FORECAST - A statement describing the expected behaviour of a volcano.

FUMAROLE - Fissure or vent in the surface formed by the escape of volcanic gases and heated groundwater.

FUMAROLE FIELD - Fumarole fields are formed in active volcanic areas where the crust is hot at very shallow depths and where there is a ready supply of water in the form of precipitation. Rainwater or groundwater, is heated underground and changed to steam by the hot rock beneath, and makes its way back to the surface through cracks and fissures. This process give the name to many of the volcanoes of the Antilles as fumarole fields are called "soufriere" in french.
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