Plate Tectonics and the Ocean Floor Ch.2 Flashcards
Crust composition
low-density, mainly silicate minerals
mantle composition
mainly iron, and magnesium silicate minerals
core
high-density, mainly iron and nickel
Lithosphere
cool rigid shell, includes crust and upper mantle, about 100 km thick, forms tectonic plates
Asthenosphere
- relatively hot
- flows with high viscosity
- base of lithosphere to about 700km deep
Continenatl crust
granite (light coloured ingenous rock), density of 2.7 g/cubic cm, avg thickness of 35 km
oceanic crust
basalt (dark igneous rock), density of 3, avg thickness of 8km
Earthquake activity mirrors blank
tectonic plate boundaries
most large earthquakes occur where?
at subduction zones
Pangaea
one large continent existed 200 million years ago
Panthalassa
one large ocean (200 million years ago)
destructive margins (driving mechanism for plate motions)
at subduction zones at deep-sea trench
constructive margins
at mid-ocean ridges at spreading ocean ridge
litoshpere
rigid tectonic plates that float on ductile asthenosphere
paleomagnetism
study of earth’s ancient magnetic field
evidence for plate tectonics
- earth’s magnetic field
- polar wondering
- magnetic polarity reversals
sea floor spreading evidence
- magnetic anomalies; regular pattern of north-south magnetism
- stripes were symmetrical about long underwater mountain range
ocean crust formation
- ocean crust forms at mid-ocean ridge
- ocean crust moves away from mid-ocean ridge and cools and subsides
- and thickens (crustal underplating)
divergent plate boundary
- plates move away from each other
- mid-ocean ridge; Rift Valley
- new ocean floor created
convergent plate boundary
- plates move toward each other
- oceanic crust destroyed; ocean trench, volcanic arc
transform plate boundary
-plates slide past each other
2 types
-oceanic transforma fault ; ocean floor only
-continrntal transform fault; cuts across continent
volcanic hotspots
-a region of high volcanic activity not located at a tectonic plate boundary
-it is caused by upwelling of deep mantle plumes
-hotspots are intraplaye surface manifestiations of mantle plumes
-
seamounts
rounded tops located between” islands”
tablemounts or Guyot
flattended tops below the sea surface
coral reef development
fringing reef —-> barrier reef —–> Atolls ——>
fringing reefs
develop along margin of landmass
barrier reef
seperated from landmass by lagoon
Atolls
reef continues to grow after volcanoes are submerged, reef surounds a lagoon
the oldest volcanoe
Maupiti
Paleography
the study of ancient continents
continental accrection
continental material added to edges of continents through plate motion
Wilson cycle
life cycle of ocean basins; formation, growth, and destruction