Chapter 2 - Plate Tectonics Flashcards
Francis bacon
Noticed that Africa fits with South America
Give evidence for theory of continental drift
1) fossils of Mesasorus found coming to South Africa and Brazil
2) Geological evidence (rocks of similar age, type and structure)
3) coal deposits found under Antarctic ice caps and glaciations scars in warm areas
4) mid Atlantic Ridge
- 1000km wide
- 2.5km high
- young volcanic rocks
5) earth’s magnetic pole has had 171 reversals over the last 76 million years
6) seafloor spreading
Earths layers
Oceanic crust
- consists of mainly basalt
- Average 6 to 10 km thick
Continental crust
-70 km thick
Mantle
- 2900 km deep
- temperature reaches 5000°C
1) upper mantle : composed of silicate rocks rich in iron and magnesium, and is rigid layer
2) asthenosphere - semi molten state
Core
-Consist of iron and nickel, and is the size of Mars
-Centre is 6371 km below earths surface
-temperature is 6200°C
Outer core is in a semi molten state and the inner core is solid
What moves tectonic plate
Convection cell currents
Magnetic declination
The Earth’s magnetic field tilt 11° to the planets rotational axis therefore the geographical poles of the Earth do not coincide exactly with the magnetic poles and this difference is called the magnetic declination
Palaeomagnetism
The record of ancient strength and orientation of the Earth’s magnetic field preserved in a rock
Polar wander path
A curved line traced out by success of positions of date at Paleopoles
What is a Paleopole
Refers to the supposed position of the Earth’s magnetic North Pole in the past
Mid ocean ridges
Elongated submarine mountain ranges who’s peaks lie only 2 to 2.5 km below sea level
Deep ocean trenches
When the ocean floor reaches depths of 8 to 12 km which define elongated gated trenches
Seamount chains
Chain of isolated submarine mountains which were once active volcanoes
Fractured zones
Narrow band of vertical fractures at roughly right angles to mid ocean ridges
Describe the nature of the oceanic crust
Much of the ocean floor is covered by a layer of sediment composed of Clay and the tiny shells of dead plankton but ocean ridges have no sediment on.
Contains no Grannite and no metamorphic rock
Common rock types on continents but only contains basalt and gabbro
Active and passive plate boundaries
Active plate boundaries coincide with tectonic plate boundaries
Passive plate boundaries do not coincide with tectonic plate boundaries and characteristic of such plate boundaries is the development of a continental shelf
Continental shelf
Abroad, shallow region on the surface of a thick accumulation of sediment cover that were deposited along a massive margin with a continental crust is thinner the norm