P A P U A Listening to volcanoes For further 4177 contact: Nobody can stop a volcanic eruption. But what volcanologists (scientists who study volcanoes) try to do is ‘listen to’ the volcanoes with instruments in much the same way as a doctor listens to a patient with a stethoscope. Assistant Director (Volcanology) Rabaul Volcanological Observatory P.O. Box 386 Rabaul East New Britain Province ΗΗΗΗΗΗΗΗΙΗΗΒΗΗΗΗΗΗΗΗΗΗίΗΗΗΗ They then may be able to alert people to any increased restlessness and danger from the volcano. Government authorities will initiate evacuation plans if an eruption is thought to be likely . Telephone: 9821699 Facsimile: 9821004 ... .. ' :···'.·.:·-··" ···'·"··-"···: ·······.- , The instruments that volcanologists use include: • Earthquake recorders (seismographs) that detect earthquake ‘waves’ coming from rock movements deep inside the volcano. receiving reports from observers. I Surveying >,· % V .. ■ · •f · ■·.:· liri r .> - .-v fi • Surveying instruments that measure uplift, tilt, and sideways movement of the ground. ran • Thermometers that measure changes in the surface temperature of the volcano, and gas sampling apparatus. RVO was established in 1940. It was destroyed in the Second World War, and re established in 1950. It has been part of the Geological Survey of Papua New Guinea (Department of Mining and Petroleum) since 1973 when PNG achieved selfgovernment. This leaflet was produced by the Papua N e w Guinea - Australia Volcanological Sen/ice Support Project which is funded by the Australian International Development Assistance Bureau (AusAID). For further information contact: Executive Director, Australian Geological Survey O rganisation, GPO Box 378, Canberra, A C T 2601, Australia. I I I Gas sampling 'AusAID Dangerous volcanoes of Papua New Guinea P A P U A N E W G U I N E A _____________________________________________________________________________ I II I Ο II N I jt I LIVING ON VOLCANOES CAN BE HAZARDOUS P apua New Guinea has many active volcanoes. Θ Volcanic cloud Θ Hot pyroclastic flow down valley O Lava flow bulldozing houses in valley Lava erupted Fourteen of them - probably as many as 150 years. Many other ‘dormant’ volcanoes may become active in the All of these PNG volcanoes are a danger to people living on and near them especially at Rabaul, and on Manam, Karkar, Ulawun, and Lamington. 1. Pyroclastic flow: Gas-rich ‘avalanches’ of hot ash and pumice flow down the side of the volcano at speeds of 100-200 kilometres an hour (Lamington 1951, Manam1996) 2, Ash fall: Gas-rich lava explodes below the volcano crater and fires out ____ ash upwards at high speed, sometimes to a great height (20-30 kilometres) - the wind spreads the volcanic cloud and fine ash covers the surrounding area (Vulcan 1994). Rabaul Ulawun Ritter Lamington / \ A ctive volcano 4 0 0 kilom etres Volcanoes o f Papua New Guinea. M any other active volcanoes are under the sea and are not shown here. Heavy ash fa ll from the 1994 eruption at Rabaul caused the roofs o f buildings to collapse and vehicles to be buried in the central business district o f the town. There can be different types of eruption from the same volcano at different times. future. lam *M an am P * . Karkar Θ Tsunamis (large sea wave) There are many different types of volcanic eruption. Three are illustrated here. 17 - have been in eruption in the last £ \O th e r young volcano O Ash fall collapses roofs 24/ 09/382 3. Lava flow: Lava (rock that has become hot and molten) is squeezed out at the surface and flows down the side of the volcano (Tavurvur 1994, 1996) Lava from deep within the earth A blast from the eruption at Lamington in 1951 devastated the northern side o f the volcano. A jeep has been hurled up onto tree stumps. LIVING MORE SAFELY ON VOLCANOES Manam: 1996: 12 people w e re killed when pyroclastic flow s moved dow n a va lle y to th e sea. Rabaul: A huge eruption fo rm e d part of R abaul H a rbo u r about 1400 ye a rs ago. It p roduced a thick ash layer over m ost of th e surro u n ding area. 1937: Eruptions at Vulcan and Tavurvur volcanoes killed 500 people and destroyed gardens and plantations. long Island: Karkar: 1951: a m ajor e ru p tio n killed 3000 people and d e stro ye d a g o ve rn m en t station. 1990: six people w e re killed by vo lc a n ic gas on T avurvur volcano. 1994: e ru ptions at Tavurvur and Vulcan killed five people a nd ca u se d se riou s dam age to m uch of R abaul tow nship - 100,000 people w ere eva cu ate d and property dam age w as estim ated to be 2 80 m illion kina. 1979: an eruption d estroyed rain fo re st and killed tw o Rabaul V olcanological O bservatory v o lca n olog ists large-scale evacuation plans w e re prepared. Bitter Island: 1888: th e volcano collapsed into the sea and ca u se d large sea w aves (tsunam is) that w ashed o ve r coastal villages in D a m pie r Strait killing m any people. A m a jo r eruption a b out 300 ye a rs ago ca u se d a ‘tim e of darkness’ and the destruction o f crop s in the H ighlands of PNG . Ulawun: This large, frequently active volcano could co llapse and produce sea w aves (tsunamis) along the co a stlin e of the B ism a rck Sea. Bam: 1954-60: T h e island population w a s e vacuated to th e m ainland fo r an extended period - deaths on the m ainla n d w ere attributed to d iet c h a n ge s a nd severe ‘h o m e sickn e ss’. O Airstrip O Volcano observatory with modern equipment O People living in safest areas O Evacuation routes are established and officials have evacuation plans Θ Wharfs PAPUA NEW GUINEA - AUSTRALIA VOLCANOLOGICAL SERVICE SUPPORT (VSS) PROJECT V olcan ic eruptions cause much destruction in Papua New Guinea. They can have a disastrous impact on human lives, property, agricultural lands, and community infrastructure such as roads, houses, hospitals, and schools. Economic development is set back and poverty increases. Yet the rich soils of volcanic areas attract people and agricultural development. A volcanic eruption from Tavurvur in September 1994 produced ash that destroyed much of Rabaul town including the central business district. The Rabaul Volcanological Observatory (RVO) is responsible for monitoring dangerous volcanoes throughout Papua New Guinea. RVO is part of the Geological Survey of Papua New Guinea. The governments of Papua New Guinea and Australia in 1995 agreed to participate jointly in a Papua New Guinea - Australia Volcanological Service Support Project which will continue through until the end of 1999. The Australian contribution to the VSS Project is being funded by the Australian Agency for International Development (AusAID). VSS Project Goal: Reduction of the impact of volcanic hazards on Papua New Guinea communities Attention is being directed particularly to upgrading the monitoring equipment at the five ‘high-risk’ volcanoes of Rabaul, Manam, Karkar, Ulawun, and Lamington. These are all active volcanoes where there are significant numbers of people who are at risk to future volcanic eruptions. The volcanoes will be equipped with new instruments to measure earthquakes as well as the tilting and uplift of the ground surface of the volcanoes.. Project work on the five volcanoes will be undertaken by RVO staff and Volcanologists must obtain information about active volcanoes by studying them in the field using the best possible sampling and monitoring equipment. by scientists from Australia, mainly from the Australian Geological Survey Organisation. For further information contact: MrB-Taiai Assistant Director (Vulcanulogy) Rabaul Volcanological observatory P.O. Box 386 Rabaul East New Britain Province Papua New Guinea Telephone: 16751982-1699 Facsimile: 16751982-1004 Dr R.W. Johnson Chief Research Scientist Australian Geological Survey Organisation GPOBox 378 Canberra ACT 2601 Australia The VSS Project includes a wide range of activities. For example, RVO staff will receive training in the use of computer systems for mapping volcanic hazards on the five high-risk volcanoes. Telephone: 16116-2499377 Facsimile: (6116-2499986 'AusAID LOOKING INSIDE RABAUL VOLCANO f t scientific survey of the Earthquake northeastern Gazelle Peninsula area will be carried out in 1997 in order to produce pictures, or ‘im ages’, of the deep interior of Rabaul volcano. It is to help the Rabaul Volcanological Observatory (RVO) understand how Rabaul volcano ‘w orks’. The survey is known as RELACS which stands for ‘Rabaul Earthquake Locations And Crustal Structure’, and is a part of the AusAID-funded PNGA ustral ia Volcanological Service S upport Project. Medical doctors in hospitals use X-rays and ‘CAT scan’ equipment RELACS will be carried out by to produce images of ‘slices’ scientists from RVO, the Australian through the human body - without Geological Survey Organisation, doing any harm to their patients! the Australian National University, and the University of Hokkaido (Japan). The survey involves The pictures they obtain help the doctors locate those parts of the detecting natural earthquake inside of the patient’s body that ‘waves’ that pass through the deep may require medical attention. parts of the volcano and measuring ‘CAT’ stands for Computer them at a large number of seism ic Assisted Tomography. recorders which are placed on land and on the sea floor. ‘Seismic tomography’ is the Small explosive charges will be let scientific name used to describe off in the deep sea and in drill holes investigations such as the on land, and their waves recorded RELACS survey at Rabaul. in order to improve the survey Seismic tomography at volcanoes results. These explosions are much sm aller than those felt com m only is similar to a CAT scan, except by people in the Rabaul area from that earthquake and explosion earthquakes. waves are used (rather than Xrays) and the ‘patient’ is a dangerous volcano. The white circles and cun/es are earthquake waves passing through the deep interior of a volcano. The waves are bent when they pass through lava and hot rock deep below the surface (green and red area beneath the volcano). This ‘bending’ o f the waves can be measured at seismic recorders and then the position and shape of the deep bodies of lava mapped out. m ore than 50 recorders will b deep water on the The4and recofders Landowners will be ad^ed to ensure the1safety of the i j j hopes that everyone in tl community will help by , | ί -Kept s a f e t y being Timing Antenna [Satellite) nearby, and by conti 3 | staff if they have an: Layer of dirt over plastic about a site. Recording Box for further information contact: Assistant Director (Volcanology! Rabaul Volcanological Observatory P.O. Box 386 Rabaul East New Britain Province Telephone: 982-1699 Facsimile: 982-1004 Example of a seismic recorder to be used during the RELACS survey. Inset: how the recorder will look when set up for measurements. ,\C A 1 "AusAID
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