Challenges of Natural hazards KO Flashcards
The Crust
Varies in thickness (5-10km) beneath the ocean. Made up of several large plates
The Mantle
Widest layer (2900km thick). The heat and pressure means the rock is in a liquid state that is in a state of convection
The inner and outer core
Hottest section (5000 degrees). Mostly made of iron and nickel and is 4x denser than the crust. Inner section is solid whereas outer layer is liquid
Ash cloud
Small pieces of pulverised rock and glass which are thrown into the atmosphere
Gas
Sulphur dioxide, water vapour and carbon dioxide come out of the volcano
Lahar
A volcanic mudflow which usually runs down a valley side on the volcano
Pyroclastic flow
A fast moving current of super-heated gas and ash (1000oC). They travel at 450mph
Volcanic bomb
A thick (viscous) lava fragment that is ejected from the volcano
Warning signs of earthquakes
. Small earthquakes are caused as magma rises up
. Temperature around the volcano rises as activity increases
. When a volcano is close to erupting, it releases gases
Monitoring techniques (Earthquakes)
. Seismometer’s are used to detect earthquakes
. Thermal imaging and satellite cameras can be used to detect heat around a volcano
. Gas samples may be taken and chemical sensors used to measure Sulphur levels
Preparation for volcanic eruptions
. Creating an exclusion zone around the volcano
. Being ready and able to evacuate residents
. Having an emergency supply of basic provisions, such as food
. Trained emergency services and a good communication system
Predicting earthquakes
.Satellite surveying (tracks changes in the earth’s surface)
.Laser reflector (surveys movement across fault lines)
.Radon gas sensor (radon gas is released when plates move so this finds that)
.Seismometer
.Water table level (water levels fluctuate before an earthquake).
.Scientists also use seismic records to predict when the next event will occur.
Protection against earthquakes
. Building earthquake-resistant buildings
. Raising public awareness
. Improving earthquake prediction
Convection currents
. Radioactive decay of some of the elements in the core and mantle generate a lot of heat
. When lower parts of the mantle molten rock (Magma) heat up they become less dense and slowly rise
. As they move towards the top they cool down, become more dense and slowly sink
. These circular movements of semi-molten rock are convection currents
. Convection currents create drag on the base of the tectonic plates and this causes them to move
Causes of Nepal Earthquake
. On a destructive plate margin, involving the Indo-Australian & Eurasian plates.
. Magnitude 7.9 earthquake
. About 50 miles from the capital Kathmandu
. Very shallow focus of 15km deep
Effects of the Nepal Earthquake
9000 people died , 20,000 injured. 8 million people affected
250,000 homes collapsed or were damaged. 3 Million left homeless.
Landslides and avalanches caused flooding and further deaths
Management / response to Nepal Earthquake
Individuals tried to recover people.
Many countries responded with appeals or rescue teams.
Heavily relied on international aid.
98% of rubble remained after 6 months.
Destructive plate margin
When the denser plate subducts beneath the other, friction causes it to melt and become molten magma. The magma forces its ways up to the surface to form a volcano. This margin is also responsible for devastating earthquakes
Constructive plate margin
Here two plates are moving apart causing new magma to reach the surface through the gap. Volcanoes formed along this crack cause a submarine mountain range such as those in the Mid Atlantic Ridge
Conservative plate margin
A conservative plate boundary occurs where plates slide past each other in opposite directions, or in the same direction but at different speeds. This is responsible for earthquakes such as the ones happening along the San Andreas Fault, USA
Causes of Earthquakes
. Earthquakes are caused when two plates
become locked causing friction to build up. . From this stress, the pressure will eventually be released, triggering the plates to move into a new position.
. This movement causes energy in the form of seismic waves, to travel from the focus towards the epicenter.
. As a result, the crust vibrates triggering an earthquake
What is the Epicenter
The point directly above the focus, where the seismic waves reach first, is called the EPICENTRE
What are Seismic waves
SEISMIC WAVES (energy waves) travel out from the focus
What is the Focus
The point at which pressure is released is called the FOCUS
Causes of the Chile earthquake
The Nazca plate and South American plate move towards each other on a destructive plate margin
The magnitude 8.8 earthquake struck just off the coast of Chile, It was followed by a series of smaller aftershocks
Effects of the Chile earthquake
500 deaths, 12,000 injured.
800,000 people affected.
220,000 homes, 4500 schools destroyed.
Port of Talcahuanao and Santiago airport badly damaged.
Landslides cut communities off for days
Management / responses to the Chile earthquakes
Emergency services acted swiftly
International help was sent quickly.
Temporary repairs were made to important highways within 24 hours
Power and water restored to 90% of homes within 10 days