Cone-shaped structure with a central vent or pipe that links the Earth’s interior to the surface.
How is a volcano formed?
When there is a weakness in the Earth’s crust where magma can escape from the mantle
Another word for molten rock is
Magma
What is lava
When magma reaches the earth‘s surface
Volcanos and Earthquakes are found near the boundaries of continental plates. When one plate slides beneath another magma can reach the surface.
Where are volcanoes found
in hot and cold regions.
Can volcanoes be found in sea?
Yes, on the seabed.
Cone-shaped structure
The visiblepartofthevolcanothat we see above ground. Formedbytheaccumulationofmagma, ash, and rockdebrisexpelled by the volcanoduringeruptions.
Magma chamber
A large pool of molten rock that feeds the volcano with magma, located several kilometers beneath the volcano's surface.
Central vent or pipe
The openingthroughwhichmagma,ash, andvolcanicgasesescapefromtheEarth'sinterior to the surface,connecting to a magmachamber located beneath the volcano.
Lava flows
Solidified streams of molten rock that flowdown the slopes of the volcanoduring an eruption.
How does a volcano look
A cone-shaped structure with a vent/pipe
Archipelagoes
volcanoes that form chains of islands
Tephra
Solid materials/ bombs ejected from volcano
Tuff
Ash and dust
Lapilli
Small rock fragments
Lahar
Volcanic ash and water moving downhill/mudflow
Types of volcanic material
Ash
Cinders
Debris
Minor vent
Cone
Major vent
New crater
Rim
Subsidiary
Minor vent
Vent eruption
Blown off by
Shield volcanoes
Formed from basic lava
Non-violent, as volcanic gases escape quite easily from the vent
Sides of the cone are gentle and consist of ash and cinder
Shield volcanoes
Mauna Loa
Mauna Kea
Strombolian volcanoes
Produce ash, cinders and volcanic bombs which are hurled into the air
Acidic lava forms steep-sided cone-shaped volcanoes
Red-hot ash and gas, known as nuee ardente, pour from the vent, destroying everything in their path
Strombolian volcanoes
Paricutín
Smaller types in Nevis
Composite cones
Flat-based steep-sided cones consisting of alternate thick layers of ash and cinders and viscous lava
Lava often escapes from the sides of the cone, building up small cones or conelets
Composite cones
Fujiyama
Caldera formation
1. Central part of the crater of a composite cone is blown away by an explosion
2. Top of the volcano slowly subsides into the underlying magma chamber
3. Circular depression or crater known as a caldera is formed in the remains of the volcano
Magma
Molten rock in a semi-liquified state deep inside the Earth
Lava
Molten rock on the Earth's surface
Basic/fluid lava
Builds up gentle-sided cones
Thin and runny, flowing for several kilometres before solidifying
Acidic lava
Cools quickly around the vent
Forms steep-sided cones
Acidic lava
Mount Soufrière in St Vincent
Crater lakes
Gran Étang and Lake Antoine in Grenada
Volcanic plug or neck formation
1. Vent of a volcano becomes blocked with thick, viscous lava
2. Cone is gradually eroded away
3. Plug or neck stands as a pinnacle in the vent or pipe
Volcanic plugs or necks
Gros Piton and Petit Piton in St Lucia
The Pitons, St Lucia
Volcanic plugs or necks
Gros Piton (800 m)
Petit Piton (710 m)
Both peaks can be climbed
Volcanic tourist attractions
Hot or thermal springs at Bath, St Thomas and Milk River, Jamaica
Spas developed around the springs
Famous for medicinal properties
Volcanic features
Fumaroles or solfataras in the Valley of Ten Thousand Smokes in Alaska, Valley of Desolation in Dominica, and Sulphur Springs at Soufrière in St Lucia
Geysers in Yellowstone National Park, USA, including Old Faithful
Vulcanologist
A person who studies volcanoes, watching, recording and interpreting their activity
What vulcanologists look out for
Likelihood of eruptions can be predicted with seismographs, tiltmeters, gas emissions, and bulges in the Earth's surface