Plate Tectonics Flashcards
(104 cards)
What is a Geoid and how is it formed?
Bulging at equator due to centrifugal forces (kids on a roundabout)
What is the oceanic crust?
5-10km, occasionally broken layer of basalt known as ‘Sima’ – Silica and Magnesium
What is the continental crust?
up to 70km, mostly granite known as ‘Sial’ – Silica and Aluminium
Difference between ‘Sial’ and ‘Sima’
‘Sial’ (Conti) is less dense and thicker, found above ‘Sima’ (Ocean)
What is the Lithosphere?
Tectonic plates are formed here
upper-mantle + crust (100km)
What is the Mantle?
(2900km) – great heat and pressure results in liquid dense the deeper you go
Core Characteristics
Core (5000’C) is 4 times denser than crust
Outer Core characteristics
Outer Core – semi-liquid=Iron
Inner Core Characteristics
Inner Core=Iron + Nickel
Convection currents are causes by..?
The heat generated by the core creates convection current
Who and when - Theory of Continental Drift
Alfred Wegner – 1912
6 Things the theory of continental dift is based on:
1) Jigsaw fit of SA and A
2) Matching rock in East Cnd to NW Sco
3) Coal beneath Antarctica
4) Fossils in India matched in Aus
5) Unique Mesosaurus in A + Bra
6) Glacial deposits in Bra match west A
Scientific Community reaction to Theory of Continental Drift
Evidence but no explanation dismissed his theories
Theory - 1950’s?
50s – nuclear submarines – Oceanic Floor Mapping
1962?
Sea floor spreading – youngest rock in the middle of Atlantic, newest in Iceland
Palaomagnitism?
During Polarity every 400,000 years, there were eruptions of magnetite, Symmetrical patterns either side of the Atlantic ridge – confirming sea floor spreading
Explain Convection Currents
Plates are driven by convection currents which rise and spread in the asthenosphere before cooling and sinking back down
Oceanic Crust Contructive Formations
Mid-Ocean Ridge
Faults cut across separating sections of the ridge widening at different rates, creating shallow focus earthquakes
Rift valleys in the middle of ridges
Submarine volcanoes can eventually create volcanic islands
Continental Crust Contructive Formations
Rift Valleys
Lithosphere splits – fractures in parallel faults
Oceanic > Continental Destructive Formations
Denser Oceanic Plate subducts beneath Continental = deep ocean trench
Continental land is uplifted, compressed and folded > chains of fold mountains
Oceanic land is destroyed/melted between 100-700 km (Benioff Zone) due to heat and friction which may also cause deep-focus earthquakes
Turned into magma, oceanic rock is less dense than asthenosphere =rising in faults where the continental plate has buckled, before reaching the surface to form explosive volcanic eruptions
Oceanic > Oceanic Destructive Formations
The faster/ denser plate subducts > deep ocean trench
Rising magma melted in the Benioff zone > volcanic island arcs
Continental > Continental Destructive Formations
Subduction does not occur because continental is not dense enough > High Fold Mountains
Shallow focus earth-quakes can be triggered
Conservative Formations
Crust is not destroyed and no subduction > no volcanic activity + no formation of new crust
Extremely active
Shallow Focus Earthquakes when sticking occurs and stress builds
Contructive Crust and Volcanoes
Oceanic crust is formed by basaltic magma rising from the asthenosphere
Basic submarine volcanoes
Volcanic islands