Unit 3 - Tectonic hazards Flashcards
(143 cards)
What’s the Earths structure?
Inner core, outer core, mantle and crust.
Characteristics of the core?
- iron and nickel at 6200*c
- inner core is 1250km thick
- outer core is 2200km thick
Characteristics of the mantle?
- rich in silicate rocks
- 2900km thick, 1000*c
- rocks are semi molten
What is the asthenosphere?
- apart of the mantle, 80-200km
- solid, but rocks can deform under pressure
What are the 2 types of crust?
- oceanic crust (6-10km)
- continental crust (70km)
What is the lithosphere?
The rigid outer layer of the Earth consisting of the crust and solid outermost layer of the upper mantle.
What is the Moho Discontinuity?
The boundary between the crust and the mantle.
What are the 3 types of plate boundary?
-converging/destructive
-diverging/constructive
-transform/conservative
Movement of converging boundaries?
Pulling together, causing push mountains (South america)
Movement of diverging boundaries?
Pulling apart, creating new land (Iceland)
Movement of conservative boundaries?
Moving next to each other (san andreas fault)
What is the theory of convection currents?
- heat is moved towards the crust by circuling convection currents
- spread out the surface, like a conveyer belt
- the plates move on the asthensphere
What data is against convection currents?
modern scientific technologies have been unable to identify any convection cells in the mantle that would be strong enough to move plates.
What is ridge push?
-molten magma rises at a midocean ridge divergent boundary
- rocks are heated, expand and rise above the seafloor, forming a slope away from the ridge
- as rock cools, it becomes denser, causing it to slide down the pkates, exerting a force
- the gravitational sliding is the active driving force
What is slab pull?
-at the convergent plate boundaries, one plate is denser than another
- the denser plates subducts under the less dense plate
- the subducting plate is colder and heavier than the mantle, so it continues to sink, pulling the rest of the plate with it.
What happens to the plates at diverging plate boundaries at oceanic plates?
- diverging plates under oceans driven by slab pull, bring magma to the surface to form a ridge
- can form volcanoes and new islands
What happens to the plates at diverging plate boundaries at continental plates?
- mountain ridges are found at the plate margins as hot magma forces the crust to bulge
- parallel faults are found, forming rift valleys
What happens to the plates at converging plate boundaries at oceanic plates?
-the colder, denser plate will subduct beneath the other, forming an ocean trench
- some magma may be able to rise, forming island arcs.
What happens to the plates at converging plates boundaries at continental/ocean margins?
- the denser oceanic plate is subducted by slab pull
- less dense continental crust gets buckled and folded, to form mountain chains
What happens to the plates at converging plate boundaries at continental margins?
- continental plates have similar densities so no subduction
- fold mountains are created to relieve pressure
- earthquakes can occur at these
How are hotspots formed?
- plumes of magma rise to the crust
- forms volcanoes at the surface
- as the plate continues to move, more volcanoes form
- as continental volcanoes move, they become extinct
What are earthquakes along diverging plate boundaries like?
Shallow and related to volcanic activity
What are earthquakes like at oceanic boundaries?
Frequent and powerful, may cause tsunamis
What are earthquakes like at continental boundaries?
Mainly shallow, can be powerful and hazardous if humans inhabit the area