Lecture 16 Flashcards
Relief
Shape of land, more specifically, the elevation difference between highest and lowest point in area.
Orders of relief
Different scales.
1st order - broadest scale. Continents and ocean basin. Largest landforms.
2nd order - major features of first orders (mountain ranges, plains).
3rd order - individual landforms (a valley, a beach).
2nd order in ocean basins
Mid ocean ridge (underwater ocean range). Abyssal plains (most of ocean floor). Continental margin; continental rise (gentle rise up from deep sea floor), continental slope (steeper rise), continental shelf (gentle rise, continent merges with ocean basin).
2nd order of relief on continents
Mountain chains (actively growing). Mountain roots (not active wearing down). Shields (tectonically quiet, relatively flat). Exposed shields (bedrock at surface). Covered shields (covered by sediment).
Continental drift
When accurate maps were map, a jigsaw fit of continents became apparent. Matching fossils were found and rock types and mountain ranges match up.
Alfred Wegener
Took fit of continents seriously and sought an explanation. Suggested that continents once were together; Pangea.
Paleomagnetism
Shift in magnetic poles occurs; now north, other times south.
Sea floor spreading
New material created in mid-ocean ridges, then moves away to both directions. Showed that crust does move around and that Wegener was correct.
Convection cells in asthenosphere/mantle
The leading theory of movement. AKA the plastic/moving layer.
Divergent plates
Plates move away from each other and a new crust is created.
Mid ocean ridges, ocean basins grow, Rift Valley; beginning of ocean.
Ocean-continent convergence
Oceanic plates and continental plates hit.
Continental crust is less dense, so stays on surface, oceanic crust sub-ducted.
Continent-continent convergent
Continental crust crumbles to form mountains.
Ocean-ocean convergent
Two oceanic plates meet. Subduction causes melting, some magma rises, causing volcanoes of continental margin.
Transform faults
Two plates slide past each other.
Can cause earthquakes.
Common on mid ocean ridges, some on continents.
Terranes
Mini plates that join up with major plates.