Tectonics Flashcards
(21 cards)
7 major plates
- The Pacific
- The Eurasian.
- The African
- The American
- The Indo Australian
- The Nazca Plate
- The Antarctic plate.
Active volcano
– if they have erupted recently
Dormant volcano
resting – have not erupted recently
Extinct volcano
will not erupt again
Shield volcanoes
- Shield volcanoes have very runny lava (non-viscous); because of this they do not have
an ‘explosive’ eruption. - Lava spreads quickly across the landscape.
- With each eruption a new layer of rock is built on the previous one.
- Gradually a wide dome of rock is built up.
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* It is called a shield volcano because it looks like a curved shield lying on the ground (or
an upside down dinner plate).
* The slopes of a shield volcano are very gentle.
* The Hawaiian islands are a chain of shield volcanoes
Composite/strato volcanoes
- Composite volcanoes are the most common type of volcano.
- When you think of a volcano you are probably picturing the classic cone shape of the
composite volcano. - They are formed by hardened layers of lava and ash from successive eruptions.
- The lava is viscous (therefore thicker than with shield volcanos) and it cools and hardens
before spreading very far, therefore the volcanoes are steep sided. - The eruptions tend to be very violent, capable of producing deadly pyroclastic flows.
- Mount Vesuvius in Italy is an example of a Composite Volcano.
Volcanic Eruption Case Study Eyjafjallajökull Volcanic Eruption (2010)
Eyjafjallajökull is a moderately active volcano that had not erupted for 180 years before it came
to life in 2010.
There has been 18 years of volcanic unrest before the 2010 eruption. This activity had been
carefully monitored by satellite radar, GPS receivers and seismic monitoring.
Rather than one magma chamber filling up before the eruption, scientists believe two separate
sources of magma had been accumulating. The volcano erupted through the coming together of
these two types of magma. One type of magma was basalt and the other was silica-rich andesite.
On March 20 2010, Eyjafjallajökull began spewing molten lava in an uninhabited area of south
Iceland and on the 14th of April the volcano erupted again from the top crater. The second
eruption caused a massive glacial flood (800 people evacuated) and it threw up volcanic ash
several kilometres into the atmosphere. The ash plume led to air traffic disruption across NW europe
The Iceland Volcanic Observatory employs a range of methods to monitor volcanic activity so that
accurate predictions can be made:
- Gas sampling: changes in gas composition indicate the activity levels of magma
underground. - GPS technology: used to monitor any significant changes on the volcano so that the risk of
activity e.g. pyroclastic flows can be assessed. - Seismic monitoring: any minor earthquake activity is detected using seismographs and is
recorded. Rising blobs of magma can cause earthquake activity and so this may be a sign
of an eruption.
Magnitude
The strength of an earthquake
Focus
The point underground that shock waves travel out from
Epicentre
The point on the ground above the focus where the vibration is the greatest
Fault
a weak point in a tectonic plate where pressure within the crust is released
Earthquake Case Study: Turkey-Syria 2023 Causes
Cause of the earthquake:
- Transform/conservative plate boundary - Anatolian plate is sliding past the Arabian
plate. - Tension had been building up for a long time on the East Anatolian fault.
- Pressure was released and the plates slipped along a strike slip fault.
- Shockwaves were sent out causing severe shaking of the crust.
- The earthquake measured 7.8Mv.
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* As is the case with many earthquake events the mainshock was followed by many
aftershocks, including three above magnitude 6.0.
* Aftershocks represent minor re-adjustments along the portion of the fault that slipped at
the time of the mainshock.
Earthquake Case Study: Turkey-Syria 2023 Impacts:
- 47,000+ deaths across SE Turkey and NW Syria.
- 6500 buildings in Turkey collapsed across 10 cities, including a 2000 year old castle in the
city of Gaziantep. - Hundreds of thousands left homeless across SE Turkey and NW Syria.
- People left to fend for themselves with many camped out in makeshift shelters in
supermarket car parks, mosques, roadsides or amid the ruins, often desperate for food,
water and heat.
Structure of the earth Crust
A thin layer of solid rocks around the outside of the earth.
2 types of crust:
* Continental crust is crust made up of land is mainly composed of Granite.
* Oceanic crust is curst made up of oceans it is composed of Basalt.
* The earth’s crust is broken up into large slabs of rock called tectonic plates
Structure of the earth Mantle
- A layer of semi-molten (melted rock)
- The thickest layer.
- Heat currents called convection currents rise and fall in the mantle.
Structure of the earth Outer core
- A layer of molten (melted) rock.
- Average temperatures of 3000 degrees C.
- Composed of iron / nickel.
Structure of the earth Inner core
- The centre of the earth
- Temperature of about 2700 degrees C
- Described as a solid ball of iron and nickel
- It is in a solid state due to pressure from the other layers.
What are tectonic plates?
- Tectonic plates are sections of very thin crust.
- They float like rafts on the semi-molten material that makes up the earth’s mantle.
- These plates move on top of the mantle by a series of heat (convection) currents.
- The movement is very small at less than 1 cm per year, but it can result in volcanic
eruptions and earthquakes. - Earthquakes and volcanoes are found near plate boundaries. They can happen on the
seabed as well as on land.
Earthquake Management Earthquake Case Study: Turkey-Syria 2023 prediction
- Seismologists use GPS technology to analyse stress built up on faults. It had noted that
there was a lot of stress on the East Anatolian fault and that this could give way at any
time, including a large earthquake above magnitude 7.0.
Earthquake Management Earthquake Case Study: Turkey-Syria 2023 Prevention:
- Turkey introduced a seismic building code after a large earthquake in 1999. However,
many buildings pre-date the codes and some recent buildings have also not been built to
code due to corruption (developers paid money to officials and got a certificate saying the
building was safe) - People in SE Turkey paid an earthquake tax - this is meant to help with relief efforts;
however, the efforts were found to be poor with people complaining of a lack of
equipment, expertise and support to rescue those trapped under rubble. - Countries, such as the USA, deployed search and rescue personnel to Turkey (the US sent
150 specialists). - UN aid convoys were not permitted access to Syria to provide assistance until 3 days after
the earthquake. - The international community pledged aid to Turkey and Syria.