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Appendix 3: Glossary
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A mata |
A hole or depression. |
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Andesite |
A generally grey volcanic rock containing 53 up to less than 62 per cent silica (SiO2) and forming a chemical series with basalt, dacite and rhyolite. |
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Ash |
Pieces of generally glassy volcanic rock less than 4 millimetres in diameter. |
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Ash fall |
A term commonly used to distinguish the gravitational fall of particles from eruption clouds, from the deposits of pyroclastic flows. |
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Basalt |
A dark volcanic rock containing less than 53 per cent silica (SiO2) and forming a chemical series with andesite, dacite and rhyolite. |
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Caldera |
Large generally elliptical or sub-circular surface depressions at least 1–2 kilometres wide, formed by the collapse of the roofs of magma reservoirs. |
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Crater |
The small depressions commonly seen on volcanoes, especially at their summits, and which are generally less than 1–2 kilometres in diameter (see also caldera). |
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Dacite |
A generally light-greyish volcanic rock containing 62 up to less than 70 per cent silica (SiO2) and forming a chemical series with basalt, andesite and rhyolite. |
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Doctor-boi |
New Guinean medical assistant. |
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Dukduk |
Masked ritual figure; secret society. |
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Geothermal |
Relating to or produced by the internal heat of the earth, whether magmatic or produced by radioactivity. |
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Guria |
Earthquake. |
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Hydrovolcanic eruption |
Explosions caused by magma encountering subsurface water and producing intense fracturing and expulsion of fragmented rocks. |
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Ignimbrite |
A pumice-rich deposit or rock commonly of dacitic or rhyolitic composition produced by deposition from a pyroclastic flow. |
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Intrusion |
Rocks representing magmas that have filled and solidified in fissures, cracks, faults and other spaces beneath volcanoes but which have not erupted from them. |
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Kaia |
Refers to different spirits that appear most commonly as giant snakes called valvalir or kaliku. |
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Kina |
PNG national currency. |
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Kuanua |
Tolai language. |
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Landeshauptmann |
Administrator. |
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Lava flow |
A ground-hugging stream of erupted magma and rock, commonly referred to simply as ‘lava’ and clearly distinguishable from pyroclastic flows. |
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Magma |
Subsurface materials in the earth’s crust and upper mantle that have become molten and that either erupt from volcanoes or form intrusions beneath them. Most magmas are technically alumina-silicate liquid and most contain at least some pre-eruption crystals. |
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Matamatanai |
Commemorative ceremony. |
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Nuées ardente |
The term means ‘glowing cloud’ and was introduced for the block-and-ash type pyroclastic flows observed at Mount Pelée on 8 May 1902. |
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Patuana |
Older people. |
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Peléean eruption |
The name derives from the explosive eruptions at Mount Pelée in 1902 when nuées ardentes were first described and named. Both terms are no longer volcanologically fashionable. |
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Phreato |
A widely used prefix that corresponds commonly to the early ‘hydroexplosive’ phase that precedes some magmatic eruptions. |
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Plinian eruption |
Paroxysmal ejections of large volumes of pyroclastic materials, at times accompanied by caldera formation. The eruptions form high-rising eruption columns and clouds. Large-volume pyroclastic flows may develop when the column collapses, including ignimbrites if pumice is abundant in the flows. |
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Pumice |
Pieces of highly frothed volcanic rock commonly of dacitic or rhyolitic composition and which can float on water. |
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Pyroclastic |
Literally meaning ‘fire broken’ and applied to fresh magma or hot volcanic rocks that have been broken up during volcanic explosions. |
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Pyroclastic flow |
Fast-flowing hot emulsions or ‘avalanches’ of pumice, volcanic ash, dust, blocks and entrained air, which tend to follow the floors of valleys during their emplacement. |
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Ra-baul |
The mangroves. |
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Scoria |
A pyroclastic rock in fragments containing abundant round, bubble-like cavities (vesicles). Scoria is commonly basaltic or andesitic and ranges in colour from black or dark grey to deep rust-reddish depending on its state of oxidation. It is not pumiceous. |
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Strombolian eruption |
Weak to violent ejection of pasty blebs of fluid lava, accompanied by spherical to fusiform ‘bombs’, cinders and ash. The activity can be spectacularly incandescent at night-time. Lava flows may be formed. |
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Subduction |
The process whereby a tectonic plate is thrust under an adjoining plate and descends deep into the earth’s interior. |
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Surge |
Laterally propelled eruption clouds caused typically by the interaction of magma with lake water or in shallow-water coastal areas (see hydrovolcanic eruptions). They flow across the water surface away from the vent and the base of the main eruption cloud or column. |
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Tabu |
Shell money. |
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Tephra |
A commonly used synonym for pyroclastic materials or pyroclastic rocks in general. The term was used originally by Aristotle. |
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Tinata tuna |
Our own language. |
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Tomography (seismic) |
Mapping features beneath the earth’s surface using the measured velocities of earthquakes. |
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Tsunami |
A Japanese term referring to a long, high sea wave caused by an earthquake or some other disturbance such as a volcano collapsing into the sea. Tsunamis increase their heights where approaching coastlines and can be hazardous. |
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Tubuan |
Masked ritual figure; secret society. |
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Vulcanian eruption |
Violent ejections of solid or viscous hot volcanic fragments, at times in cauliflower- or mushroom-shaped clouds. Pyroclastic flows can take place, but lava flows are typically absent. |
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Vunatarai |
Matrilineal descent lines. |
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