Year 10 Natural Hazards and Tectonic Theory 1A Flashcards
natural hazard
natural event that has potential to cause damage or destruction or death
earthquake
a sudden violent movement in the Earth’s crust
tectonic hazards
caused by movement of tectonic plates
weather hazards
tropical storms, drought, floods
molten
hoy, liquid and melted rock
magma
molten rock when it’s underground
lava
molten rock when it’s over the ground
Why is urbanisation affecting hazard risk?
high population density means more people in area so more are affected
Why is poverty affecting hazard risk?
low development means weak buildings and less medical care so less help and more deaths
Why is climate change affecting hazard risk?
higher temperature means more things like tropical storms so more are affected
Why is farming affecting hazard risk?
low lying land is more at risk to flooding
What is the inner core?
solid made or iron and nickel and is 5000°C and under high pressure
What is the outer core?
liquid made of iron and nickel
What is the mantle?
semi molten rock that is 3800°C
What is continental crust?
thick (20-200km) and less dense, made of granite, old (3.8 billion years old)
What is the crust?
surface layer of the Earth and there are two types, oceanic and continental
What is oceanic crust?
thin (5-10km) and more dense, made of basalt, young (200 million years old)
tectonic plate
section/segment of crust
plate margins
where plates meet
constructive plate margin
two plates moving away from each other so rising magma fills the gap
destructive plate margin
two plates moving towards each other and the oceanic crust is subducted under the continental crust
conservative plate margin
two tectonic plates slide past each other or side by side at different speeds
convection
convection currents occur by magma being heated by the core so it rises and when it hits the crust it splits in two opposite directions pushing crust apart and moving the plates
ride push
molten magma rises in the gap created between a conservative plate margin and cools to form new land which pushes the original plates further apart
slab pull
oceanic crust is subducted at destructive plate margins and gravity causes the plate to sink so it pulls the rest of the plate along causing the entire plate to move
What does VEI stand for and what does it do?
Volcanic Explosivity Index, shows magnitude of volcano (1=low, 8=high)
What is composite volcanoes?
cone shaped volcano that occur at destructive plate margins
What is shield volcanoes?
flat like a shield and occur at constructive plate margins
What is high viscosity?
thick lava from violent eruptions e.g. composite volcanoes
What is low viscosity?
thin, runny lava from less violent eruptions e.g. shield volcanoes
earthquake focus
point under ground where an earthquake starts
epicentre
point on Earth’s surface directly above the earthquake focus
Richter scale
used to decide the magnitude of earthquakes
seismic wave
waves of energy that travel through the earths layers
seismometer
equipment used to measure and record earthquakes
plate movement at constructive plate margin
two plates move away from each other
earthquakes at constructive plate margin
sometimes occur at constructive plate margins, two plates are pushed apart so pressure builds up within the rocks and that pressure releases vibrations which can cause small earthquakes
volcano formation at constructive plate margin
as the two plates move away magma rises to fill the gap which form volcanoes
volcano type at constructive plate margin
creates shield volcanoes which are wide, flat and shield shaped
VEI at constructive plate margin
low VEI due to not very violent eruptions and has thin, runny lava (low viscosity) that spreads over large distances
volcano example at constructive plate margin
Mount Nyiragongo, Democratic Republic of the Congo, Africa
plate movement at destructive plate margin
two plates move towards from each other
earthquakes at destructive plate margin
pressure and friction builds up within the rocks and eventually the plates slip suddenly to new position and this sudden movement causes vibrations that are felt as earthquakes
volcano formation at destructive plate margin
as the two plates move towards the oceanic plate slips under the continental plate causing immense heat and pressure so the oceanic plate melts and sinks, turning into magma which then rises through cracks to surface and forms volcano
volcano type at destructive plate margin
creates composite volcanoes which are high, steep and cone shaped
VEI at destructive plate margin
high VEI due to violent eruptions and has thick lava (high viscosity) that explodes into clouds of thick ash
volcano example at destructive plate margin
Mount Sakurajima, Japan, Asia
plate movement at conservative plate margin
two tectonic plates slide past each other