the challenge of natural hazards Flashcards
what are natural hazards?
natural hazards are natural events such as earthquakes that have the potential to do damage to humans and property
list 4 hazards
tectonic, atmospheric, biological, geomorphological
list the three things that affect hazard risk
vulnerability, capacity to cope, nature of hazard
vulnerability:
the larger the population exposed the greater risk
capacity to cope:
LICs (low encome countries) are particularly at risk as they do not have the money to protect themselves
nature of hazard:
the type, frequency and magnitude of a hazard affects the level of risk
what are the four layers of the earth from the outside to the inside?
crust, mantle, outer core, inner core
the crust:
varies in thickness(5-10km) beneath the ocean. made up of several large plates.
the inner and outer core:
hottest section (5000 degrees). mostly made of iron and nickel and is 4x denser than the crust. the inner layer is solid whereas the outer layer is liquid.
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
what is the crust split up into?
major fragments called tectonic plates
how many types of tectonic plates are there?
2- oceanic and continental
Oceanic tectonic plate:
thin 5-10km, dense so sinks under continential crust, young 70-100 million years old, basalt rock and continually renewed and destroyed.
Continental tectonic plate:
thick 20-200km, less dense, old 3.8 billion years old, granite and not destroyed.
How tectonic plates move?
these plates move due to convection currents in the mantle and where they meet tectonic activity (volcanoes and earthquakes) occur.
How are earthquakes caused?
Earthquakes are caused when two moving plates (convection currents) become locked causing friction to build up. from this stress, the pressure will eventually be released, triggering the plates to move into a new postion. this movement causes energy in the form of seismic waves, to travel from the focus towards the epicentre. as a result, the crust vibrates triggering an earthquake.