Hazardous Environments Flashcards
What is a hazard
An extreme event that threatens people, their property and settlements
When does a hazard become a disaster
When the hazard causes widespread destruction to property and human lives(death)
Risk
The probability of an event happening and the scale of its possible damage
Features of oceanic crust
-newer(less than 200 million years old
-denser(heavier)
-thinner(5km)
-can subduct
Features of continental crust
-older(1500million years old)
-less dense
-thick(30 km)
-cannot subduct
Ways tectonic plates move
-slab pull
-ridge push
-convection currents
Lithosphere
Top 100 km of the earth that makes up the earths tectonic plates
Asthenosphere
The rest of the upper part of the mantle that acts as a lubricant for the tectonic plates to move on
Trends in the distribution of earthquakes and volcanoes
-mostly correlate with plate boundaries
-volcanoes are three quarters around the pacific ring of fire which is a ring around the pacific
Volcanoes that aren’t on plate boundaries are called hotspot volcanoes
Features of constructive plate boundaries
-2 plates move apart, creating new crust in the middle as magma pushes its way up and solidifies
-creates effusive volcanoes and small earthquakes
Features of destructive plate boundaries
-two plates move towards each othee
-oceanic plate subducts underneath continental plate
-subducting plate melts because of high temps in the earth. Magma rises and is extruded at the surface, forming volcanoes
-creates powerful earthquakes and explosive volcanoes
Collision plate boundaries
-2 continental plates collide
–forced to buckle upwards
-causes powerful earthquakes and fold mountains. No volcanoes
Conservative plate boundaires
-2 plates slide past each other
-creates powerful earthquakes as pressure builds up between the plates then is suddenly released
How does a volcano form at a constructive boundary
-two plates move apart from each other
-magma rises to the surface at this weak spot and is extruded in eruptions
-this forms volcanoes when it solidifies to lava
-forms shield volcanoes
Characteristics of shield volcanoes
Short
Gently sloping
Composed of basaltic lava
Low viscosity
Effusive eruptions
destructive boundary volcano formation
-two tectonic plates converge together
-oceanic plate subducts underneath continental plate
-oceanic plate melts
-newly formed magma rises to the surface and is erupted
-forms a volcano over time as more material is erupted, cools and solidifies to lava
-forms strato volcanoes