EOY TECTONICS PAPER 1 Flashcards
what are the two types of volcanoes
shield and composite
which plate boundary does not create volcanoes?
conservative
what kind of volcanoes do divergent plate boundaries cause and how and describe this volcano
Shield. As plates move apart, magma rises through the gap. The magma is balsat and hot and runny. it forms fluid lava flows and shallow sided volcanoes.
basic lava, which is non-acidic and very runny
gentle sides as the lava flows for long distances before it solidifies
no layers, as the volcano just consists of lava
less violent eruptions
shorter periods between eruptions
what kind of volcanoes do convergent plate boundaries cause and how and describe this volcano
composite. As the plates push together, oceanic plate is subducted. As it sinks, it melts and creates magma called andesite. Sea water is dragged down with it. This makes the magma less dense so it rises in plumes (or ‘blobs’) upwards through the continental crust. The water erupts as steam, making volcanoes very explosive. Volcanic ash and ‘bombs’ are blasted up and outwards as pyroclasts.
only between oceanic and continental … not anything else
Andesitic magma, which is lower in temperature, has more silica and a lot of dissolved gases and is more likely to explode when it reaches the surface.
Acidic lava, which is very viscous (sticky).
Steep sides as the lava doesn’t flow very far before it solidifies.
Alternate layers of ash and lava. For this reason, they’re also known as stratovolcanoes. Strato means layers.
Violent eruptions.
Longer periods between eruptions.
Why are composite volcanoes more explosive than shield volcanoes?
Andesitic magma, which is lower in temperature, has more silica and a lot of dissolved gases and is more likely to explode when it reaches the surface. Acidic lava, which is very viscous (sticky). Steep sides as the lava doesn’t flow very far before it solidifies.
On the other hand, shield volcanoes are found at constructive plate boundaries and hotspots. Composite cone volcanoes are made of hardened layers of ash and lava, and have a steep, cone-like shape. Its lava has high levels of silica and a high viscosity which makes eruptions highly destructive.
Volcanic eruptions are unpredictable. However, scientists can monitor volcanoes to estimate when they are likely to erupt. Scientists can use a variety of techniques to do this, such as
seismometers - used to measure earthquakes occurring near an eruption
tiltmeters and GPS satellites – these devices monitor any changes in landscape. Volcanoes tend to swell near an eruption
monitoring gases escaping from a volcano using robots called Spiders – often there is an increased release of sulphur dioxide near an eruption
measuring temperature - volcanoes become hotter when magma starts to rise through the main vent
looking at the past history of eruptions - scientists can identify patterns of activity
talk about volcanoes on plumes
Hotspots are areas of volcanic activity that are not related to plate boundaries hot magma plumes from the mantle rise and going through weaker parts of the crust
This can create volcanoes in Ireland the plume stays in the same place but the plates continue to move which sometimes causes a chain of islands such as hawaii
what is an earthquake
a sudden release of energy
the power of an earthquake (how much the ground shakes) is known as the earthquakes what?
magnitude
what does a seismometer measure for an earthquake
its magnitue
how earthquake happens at a convergent boundary
tension builds up when one plate gets stuck as it’s moving down past the other into the mantleThe place eventually jerk past each other sending out shock waves (vibrations) these vibrations are the earthquake
how earthquake happens at a divergent boundary
tension builds along cracks within the plates as they move away from each otherThe place eventually jerk past each other sending out shock waves (vibrations) these vibrations are the earthquake
how earthquake happens at a conservative boundary
tension builds up when plates that are grinding past each other get stuckThe place eventually jerk past each other sending out shock waves (vibrations) these vibrations are the earthquake
what is the focus of an earthquake
the point in the earth where the earthquake starts. This can be the earth’s surface or anywhere up to 700 km below the surface.
what are shallow-focus earthquakes caused by
Tectonic plates moving at or near the surface they have a Focus between 0 KM and 70 km below the earth’s surface