EQ1- Why Are Some Locations More At Risk From Tectonic Hazards Flashcards
Define tectonic hazards
Include earthquakes and volcanic eruptions, as well as secondary hazards such as Tsunami’s. Can be classified as seismic or volcanic.
Describe the distribution pattern of earthquakes and volcanoes in relation to plate boundaries
Most earthquakes and volcanoes occur on the border of plate boundaries.
Most of the worlds volcanoes and earthquakes occur on the pacific plate, the ring of fire. 70% of earthquakes take place there.
The most powerful earthquakes are at convergent or conservative boundaries.
Rare intra-plate volcanoes and earthquakes can happen in the middle of plates, due to ancient faults or hotspot volcanoes.
Define the Oceanic fracture zone (OFC)
Is a belt of activity through the oceans along the mid-ocean ridges, coming ashore in Africa, The Red Sea and California.
Define the continental fracture zone (CFZ)
Is a belt following the mountain ranges from Spain, via The Alps to the Middle East and the Himalayas
Give an example of major, minor and micro plates
Major- Eurasian, African, Antarctic, Pacific
Minor- Nazca, Cocos, Caribbean, Scotia
Micro- Burma, Banda Sea Plate
Explain 3 examples of Intra Plate locations and explain how they occurred
Rhine Rift valley- localised divergence, crust cracked and fell downwards causing an earthquake. Found between France and Germany
African Rift Valley- localised divergence, magma rises and drives plates apart. Found in East Africa, will separate Somalia from mainland Africa.
Tibetan Plateau- faults in crust happen thousands of km behind plate boundary. Found in Central Asia
Explain and draw the formation of Hotspot Volcanoes which cause intra- plate volcanoes
Mantle plumes occur in the middle of a plate away from the boundary.
Give a constant source of heat called a hotspot, which rises through the mantle and melts the asthenosphere and base of the lithosphere.
Magma rises through the weakness in the crust, it erupts onto the sea floor and forms a seamount.
Continuous eruptions occur causing the seamount to break through the surface of the water and form an Island Volcano.
Shield volcanoes form in oceanic hotspots due to the magma being basaltic, at continental hotspots lava is viscous with the potential to erupt explosively.
As the plate moves the Island is carried away from the hotspot, cutting it off from the magma and stoping volcanic activity. The plate continues to move and the process continues leaving Island Chains such as Hawaii.
Define mantle plumes as a cause of intra-plate activity
Are especially hot areas of the mantle that move upwards underneath the crust and push it up, can cause weak points in the crust which can become hotspots
Define a hotspot as a cause of intra plate activity
Is magma from the mantle that has broken through a weak point in the crust
Define intra-plate earthquakes
Occur in the middle of tectonic plates and are much rarer than boundary earthquakes
Define plate tectonics
Refers to a set of concepts and theories that explain the formation and distribution of the earth’s major structural features and seismic and volcanic events.
Involves the structural layers of the earth, existence of major lithospheric players and the movement of plates by various mechanisms
State the layers of the earth and how its movement takes place
Crust- movement occurs from plate boundaries
Mantle- movement occurs from convection currents
Outer core- movement occurs from the spinning of the axis
Inner core- movement occurs due to rotations
State the processes which can be used to explain plate tectonic theory (plate movement)
Mantle convection Slab pull Subduction Seafloor spreading Paleomagnetism
Explain mantle convection as a process explaining plate tectonic theory (plate movement)
Occurs where heat is produced by the decay of radioactive elements in the core and heats the lower mantle, creating convection currents. These hot liquid magma currents move in circles in the asthenosphere, causing plates to move.
Explain slab pull as a process explaining plate tectonic theory (plate movement)
Occurs where newly formed oceanic crust at mid-ocean ridges becomes denser and thicker as it cools, causing it to sink into the mantle under its own weight and pull down the rest of the plate with it.
Explain subduction as a process explaining plate tectonic theory (plate movement)
Destroys new crust being created. As two oceanic plates or one oceanic and one continental plate move towards each other, the denser plate slides under the other into the mantle and melts in the subduction zone.
Explain seafloor spreading as a process explaining plate tectonic theory (plate movement)
Occurs where huge mid-ocean ridges are formed when hot magma us forced up from the asthenosphere and hardens. This new crust pushes the tectonic plates apart in a process known as seafloor spreading
Explain Paleomagnetism as a process explaining plate tectonic theory (plate movement)
Is the study of the earth’s magnetic field where solidified magma aligns with the North Pole and moves plates sideways away from the mid- ocean ridge
State the Seismic activities found at Divergent plate boundaries (4)
Earthquakes
Volcanoes
Ocean ridges
Rift valley
State the seismic activities found at conservative plate boundaries
Eathquakes
State the seismic activities found at convergent plate boundaries (5)
Earthquakes Volcanoes Fold mountains Ocean trench Island arcs
Explain the process of a divergent plate movement
Divergent boundaries are often found in the sea, if the eruption is strong magma can build up high enough to form an island.
Convection currents rise and then diverge creating high temperatures that cause the uplifting of the crust. Tensional forces pull the playes apart to from rift valleys.
As the two plates move away from each other a gap appears between the two plates, filled by magma rising from the asthenosphere. Reduced pressure allows the magma to rise.
The magma bubbles gently to the surface to from low volcanoes, where eruptions are frequent but relatively gentle, and shallow focus earthquakes
Explain the process of a convergent (subduction) plate boundary
Occurs where the oceanic and continental plates meet and the denser oceanic plate is forced under the lighter continental plate.
As it is forced down it rubs against the continental crust, this friction causes great heat and melts the oceanic crust into magma.
As more and more magma is created it puts great pressure on the crust above it. As the oceanic crust moves down the rates of movement can trigger major earthquakes along the line of the subducting plate.
Composite volcanoes are formed with explosive eruptions and a high silica level