7) Plate Tectonics Flashcards
Type of earths crust
-oceanic
-continental
Most tectonic plate contain both types of crust but some only have oceanic crust
Alfred Wegener (1880-1930) Coined term "continental drift"
In 1915 wrote the origins of continents and oceans
Basis of hypothesis:
-shape of Atlantic Ocean
-similarities of fossils and rock sequences on opposite sides of the Atlantic
-fossils of tropical plants in the arctic
Types of continental margins
- active: margin of continent is a plate boundary
- passive: margin of a continent does not include a plate boundary
Earths upper mantle and crust
- Lithosphere: rigid crust + top of mantle
- Asthenosphere: partially molten part of the mantle, source of basalts
Divergent plate boundaries
-mid-ocean ridges
-continental rifts
In both, new ocean crust is created by basalts and gabbros that originate as magmas in the mantles asthenosphere
Feature of convergent boundaries
- new ocean crust is created
- earthquakes are typically small
- very active basalt volcanism
Convergent boundaries
- island-arc subduction: subduction of ocean crust under ocean crust
- Andean-type subduction: subduction of ocean crust under continental crust
- continent-continent collusion
Features of ocean crust subduction
- consumption of ocean floor
- large earthquakes
- Explosive volcanism is dominated by dacite and andesite lavas
Benioff zone -> earthquake generating zone
Earthquakes that are associated with subduction are causes by friction between the subducting plate and the overlying crust or mantle
Featured of continental collisions
- Produce long, talk mountain belts
- can produce large earthquakes
Features of transform fault boundaries
- they are offsets in crustal plate boundaries, especially mid-ocean ridges
- can occur on land
- no crust is created or consumed
- can produce large earthquakes
- volcanism is very rare
Evidence for active plate tectonics
- earthquake distribution
- volcanic activity
- direct measurements (GPS, ground-based)
Evidence for past plate tectonics
- fits continental margin
- match of geological belts on different continents
- volcanic hot-spot traces
- flora and fauna at “wrong” latitudes
- geomagnetic record
- age of ocean floor
Magnetic “stripes” at mid-ocean ridges
- magnetic reversals are mirror images in both sides of ridge
- rocks are progressively older away from ridge
- > demonstrate the existence of divergent plate tectonic boundary
- > demonstrate past reversals in the earth’s magnetic field