A look at volcano risk for young students. Produced by the MED-SUV project

and dt their thei heir risks risk r isk ks A look at volcano risk for young students. Produced by the MED-SUV project. Volcano Shapes: place (on Ea...
Author: Cynthia Garrett
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and dt their thei heir risks risk r isk ks

A look at volcano risk for young students. Produced by the MED-SUV project.

Volcano Shapes: place (on Earth and OTHER PLANETS) where magma comes to the surface. This event is called a volcanic eruption.

Different types of volcanoes have ave ption various shapes due to the eruption type and the nature of magma theyy erupt. The most famous shape is a ve cone. Cones form when eruptive natingg material accumulates as alternating deposits of lava flows, rock fragments or volcanic ash.

Piton de la Fournaise Shield volcano W S

E

N

SAINTE-ANNE SAINTE-rose

Etna and Vesuvius (Italy); Pitonn de laa Fournaise (La Réunion Island, ain) France); Teide (Canary Islands, Spain) ped and Colima (Mexico) are cone shaped volcanoes. But cones are not the volcanoes he only or possible shape of volcanoes. For sions. example, calderas are depressions.

10 km

Etna Strato volcano

E N

Volcano Shapes

A volcano is a

W

S

Catania

A caldera forms during a highly explosive eruption as the volcano collapses. The eruptive activity gen generally continues after the col collapse creating multiple eruptive cen en centers within a caldera. The Ca Cam Campi Flegrei in Italy, Furnas and A Agu Agua de Pau Azores Islands (At (Atlantic Ocean, Portugal) are exa examples of calderas.

Phlegrean fields

110 0 km

caldera volcano

E

Vesuvius

S

N

Naples

W

S

SRATO volcano

E pompei

10 0 km m

N

solfatara

W

Pozzuoli Mt nuovo

Bagnoli

10 km

Volcanic hazards: Volcanoes present potential threats to people and property.

-> Lava flows are extremely hot and can burn everything in their path. Even after lava cools in massive rock, the land covered by the flow cannot be used for years. If you see a lava flow, do not go near it! It may flow slowly and regularly but it is hot, releases dangerous gases and can explode. After the the eruption has ended, do not walk on lava flows; they remain hot for years.

bombs (Tephra fall)

ash or tephra fall

(see zoom below)

Volcanic hazards

-> Volcanic gases: in addition to lava, volcanoes may release gases into the atmosphere. These gases can be dangerous to your health, even if you cannot smell anything.

fumaroles (Volcanic gases)

-> Ash or tephra fall: small fragments (pieces of magma) from volcanic eruptions are projected into the air and drop like rain over lava flow large areas. Fine ash can cause health problems if inhaled. Heavy ash falls may also cause roofs to collapse. -> Pyroclastic flows: these are mixtures of hot gases and volcanic material (ash and rocks) that move downhill very fast. It is a very dangerous phenomenon! -> Lahar: this Javanese word refers to a mixture of water and volcanic material. Lahars usually occur near a river or when it is raining a lot. These mudflows can bury large areas under meters of debris. -> Debris avalanches or volcanic landslides: during an eruption, part of the volcano may collapse and cause landslides.

pyroclastic flow

debris avalanche (landslide) lahar (mud) flow

(see zoom below)

earthquake

-> Earthquakes: earthquakes often accompany volcanic activity. People need to be prepared for them too. tephra (ash) fall

lahar (mud) flow

Monitoring

Timescale

Fortunately, most of the time, monitoring help us anticipate eruptions and prepare for evacuation. Scientists have several types of monitoring systems and observation tools available. They can use ground-based systems (tiltmeters, GPS, cameras, seismometers, etc…); airborne systems (visual and thermal imaging, gas measurements) and space systems (radar, optical and infrared imagery) to monitor gas emissions, surface deformation, or earthquakes.

Eruptions can last a few hours to several years. Between eruptions, volcanoes can remain quiet for several hundred of years. For this reason, even a volcano that has never erupted in living memory may be a threat. arctic ocean

AgUa de paU and furnas

(Portugal)

phlegrean fields, vesuvius and etna

teide

(Spain)

Colima

(Mexico)

indian ocean

pacific ocean

atlantic ocean

piton de la fournaise

(La réunion Island)

Thermal imaging

Eruptive history of some volcanoes of interest in the MED-SUV project: phlegrean fields

Satellite

Airborne observation etna

Cameras Gas measurement

vesuvius

piton de la fournaise

Ground motion sensors

Agua de pau

GPS

furnas

Tiltmeter Ground observation

Colima

TEIDE -4000

-3000

-2000 (years)

= Eruption or a period of multiple eruptions = Example of major eruptions

-1000

Today

monitoring

Timescale

(Italy)

If you live in or visit a volcanic area: Prepare by examining the community’s emergency plan, if there is one, together with your family. Contact the mayor’s office for details. In the event of an eruption, stay informed and follow only official instructions issued by civil protection authorities. Prepare a kit. It should contain at least the following items: a flashlight and extra batteries, a first aid kit and its manual, emergency food and water, respiratory (breathing) protection, eye protection (goggles), a manual can opener, essential medications, sturdy shoes, and a batterypowered radio. For more information, refer to official civil protection information.

http://med-suv.eu/ This material is produced by the MED-SUV project for children and young students. It does not in any case replace official civil protection and government messages. This brochure has received funding from the European Community's Seventh Framework Programme [FP7/2007-2013] under the MED-SUV project: grant agreement n° 308665. 2015 - Design: Kalankaa - Illustrations: graphisme-medical.fr Pictures: © Tanguy de Saint Cyr / Fotolia; © Audrey Baills; © INGV