dynamics of earth's crust Flashcards
internal structure of the earth
- crust
- mantle
- outer core
- inner core
core
2 distinct regions
Liquid outer core (2,300 km thick)
Solid inner core (1,200 km thick)
Makes up significant proportion of Earths mass due to very high density
Comprised mostly of iron and some nickel
mantle
Thick layer of rock that separates the core from the crust (2,800 km thick)
Makes up most of the earths volume
Much richer in iron and magnesium than the crust which makes it more dense
crust
Outer layer of rock that forms a thin skin over the earths surface (up to 70 km thick under mountain ranges)
Less dense than the mantle (least dense layer)
2% of earths volume and less than 1% of earths mass
what kinds of crust exist
continental and oceanic crust
what is continental crust
(sial composition)-the material of the upper or continental part of the earth’s crust, characterized as being of relatively low density and rich in silica and alumina.
25-70 km thick
Rich in silicates and aluminum (granitic)
Lighter and less dense than oceanic crust so it floats higher
what is oceanic crust?
composed of sima (the material of the lower part of the earth’s crust, underlying both the ocean and the continents, characterized as relatively dense and rich in silica and magnesia.)
5-7 km thick
Rich in silicates and magnesium (and iron) which make it very
dense (basaltic)
Thinner, denser & younger than continental crust
what makes up tectonic plates?
lithosphere
what is the lithosphere?
crust + upper mantle (~100 km)
what’s is plate tectonics?
massive, irregularly shaped slab of solid
rock, often composed of both continental and oceanic crust
what is continental drift?
theory proposed in 1915 by Alfred Wenger which says that
continents migrate around the planet
like ice floes
evidence for plate tectonics
In the 40s and 50s, development of echo sounders led to the discovery of mid-ocean ridges (underwater mountain chains)
1978: glomar challenger deep sea drilling rig that cross-crossed the mid Atlantic ridge between South America and Africa
evidence from deep sea cores
Crust youngest at the ridges, where plates are moving away from each other
evidence from temperature data
Water hottest at the plate boundary using bathythermographs
evidence using magnetometers
Records magnetic field of the earth
Magnetic orientation reversals periodically occur