Geo: Tectonics and stuff Flashcards
Parts of or earth
Crust:
This is the outside layer of the earth and is made of solid rock, mostly basalt and granite. oceanic and continental.
Mantle:
The mantle lies below the crust and is up to 2900 km thick. It consists of hot, dense, iron and magnesium-rich solid rock
Outer core:
Inner core:
Extremely dense, iron and nickel. spins the fastest Temperatures sizzle at 5,400°
Convection currents
Heated mantle material is shown rising from deep inside the mantle, while cooler mantle material sinks, creating a convection current.
Continental drift: Plants-animals
—Similar plant and animal fossils are found around the shores of different continents, suggesting that they were once joined.
Movements
Continental drift: puzzle
–Also noticed that the plates were able to fit together
Continental drift: same
–Identical rocks, of the same type and age, are found on both sides of the Atlantic Ocean. Wegener said the rocks had formed side-by-side and that the land had since moved apart.
Mountain ranges with the same rock types, structures, and ages are now on opposite sides of the Atlantic Ocean
Continental drift: magnets
–Older rocks that are the same age and are located on the same continent point to the same location, but that location is not the current north magnetic pole.
Older rock that are of different ages do not point to the same locations or to the current magnetic north pole.
In other words, although the magnetite crystals were pointing to the magnetic north pole, the location of the pole seemed to wander. Scientists were amazed to find that the north magnetic pole changed location through time
Continental drift: argument
Was highly debated- due to no one understanding how the plates where able to move and was only later found out to be moved by convection currents
Plate theory: Plate types
Oceanic:
thin and heavy
Contiental:
thick and light
Plate theory
Divergent/ constructive:
When the plates move apart and magma is released, volcanic activity and shallow earthquakes
Convergent/ Destructive:
When an oceanic plate goes under a continental, earthquakes and a line of volcanoes
Transform/Conservative:
when 2 plates slide past each other, earthquake.
Volcanos: impacts and effects:
Geothermal energy
Attracts tourists
Brings nutrients to environment
Could create large explosion
Ash create problems for people and aircraft
Destroys nature and infrastructure
Composite volcanoes
Found at convergent tectonic plate boundaries.
Erupt explosively.
Instead of basaltic lava, composite volcanoes erupt andesitic lava.
Andesitic lava is thicker than basaltic lava because it has more silica in it.
Because andesitic lava is thicker, it travels less far and composite volcanoes have steeper sides, forming a cone shape.
Mount Pinatubo, Mount Vesuvius in Italy and Mount Fuji in Japan are examples
Shield volcanoes
Found at divergent tectonic plate margins or hotspots (like in the Pacific).
Not particularly explosive.
They release ‘basaltic lava’ when the volcano erupts. Basaltic lava is like a liquid that flows gradually, creating a volcano with a gentle gradient (rather than a steep slope).
Shield volcanoes do not produce any ash.
Iceland case study- Eyjafjallajokull
Location:
Southern tip of iceland, near katla volcano- march 2010
Background:
Shield volcano,1651 meters tall, covered by ice above
Physical factors:
Lies on constructive mid atlantic ridge
Human factors:
Human geo thermal harvesting may effect current
Social impacts:
No casualties but reparation problems, Tourism stop during eruption but increase due to volcano tourism.
Economic impacts:
Falling ash makes farming difficult, but higher lead after due to heat and nutrients for ash.
Environmental impacts:
Flash floods, settling ash effects animals respiration and plant respiration
Political impact: most amount of flights closed over euro since ww2, civil protection deployed to control situation
Short: 700 people evacuated, trauma support for young children
Long term: google travel and trad disrupted, major benefit to biodiversity
Key terms: earthquakes
Focus- exactly where earthquake starts.
Epicenter- directly above focus on ground
seismic waves- waves which transmit force
Earthquakes: Impacts and effects
Kills people and wildlife
Destroyed building
Mineral underground brought to surface
Can create tsunamis
Destroyed roads, railways and infrastructure