Chapter 2: Geological Oceanography Flashcards
Textbook Chapter (38 cards)
What are the World’s Ocean Basin?
1) Pacific
2) Atlantic
3) Indian
4) Arctic
5) Southern Ocean
How did Earth and Oceans form?
Big Bang 15 bya
Earth originated with solar system
4.5 bya
Density stratification of molten earth was
Density = mass/volume
Core: inner and outer
4000 degrees
Inner
Iron and solid
Outer
Iron, nickel alloy, gold, platinum, and uranium, and molten
Mag field
Due to spinning inner core
Mantle: lower and upper
1) Magnesium + iron
2) Lower solid, upper plastic (semisolid swirls)
Crust
Oxygen, silicone dioxide, magnesium, irons
Two kinds of crusts
Oceanic and continental
Oceanic crust (basalt)
1) Density about 3.0 g/cm^3
2) Only about 5km (3mi) thick
3) Geologically young
4) Dark in color
5) Rich in iron and magnesium
Continental crust (granite)
1) Density about 2.7 g/cm^3
2) 20 to 50 km ( 12 to 30 mi) thick
3) Can be very old
4) Light in color
5) Rich in sodium, potassium, calcium, and aluminum
What shaped Ocean Basin?
1) Geological time scale
2) Continental move
Initial evidence of continental drift
1) Shape of continents when we started exploring and mapping coast
2) Similar geo and fossils on opposite sides
Alfred Wegener (1912)
Theory of Continental Drift, Pangea and Panthalassa
Harry Hess
Seafloor Spreading
What is seafloor spreading?
Magma from mantle rises up at mid-ocean ridges and make new seafloor while pushing crust
Theory of Plate Tectonics
1) Mid-ocean ridges, trenches, and transform faults reveled by sonar
2) Active mid-ocean ridges
3) Sediment layers on seafloor near ridge is thin
4) Rock/sediment further away from ridge older than ones nearer ridge
5) Magnetic anomalies
Lithospheric plates made of
Crust and uppermost part of upper mantle
Plates can have any kind of
Crusts
Plate float on
Plastic upper mantle equals to movement
Plates move apart at ridges and collide at
The trenches
Trench formation
When two plates collide one subducts