Ch14 Flashcards
Internal processes build terrain Reshape crustal surface of earth Have taken place billions of years Effects don't work independently Cause earthquakes/volcanoes/ massive crustal rearrangement and operate to shape/reshape earth
Internal processes on landscape
- Continents seemed fixed from human perspective.
- till mid 20th century scientists believed earths continents were rigid.
- Supercontinent beliefs
- till recently idea not accepted
Rigid earth to plate tectonics
1915 Alfred Wegener Pangea “while land”
Wegener continental drift
-# of close affinities on both sides of Atlantic
-margines of SAmerica/Africa fit
Mountains in Scandinavia and British isles match Appalachian mountains
-mesosaurus both sides of Atlantic
Similar fossilized plants s America India Antarctica and Australia
- vast distributional coincidences
Supporting evidence Wegeners continental drift
Paleontology supports continental drift
Glaciated continents reconstructed make sense
Continents fit
Similar geologic feature on diff continent coasts
Extra evidence for Wegeners continental drift
1) crust was “too rigid” I permit large scale motions, how could solid rock plow solid rock ?
2) Wegener didn’t offer suitable mechanism that could displace large masses for a long journey
Why the theory was ignored and impossible
Plate boundaries
Sea floor spreading
Paleomagnetism
Convection and plate tectonics
Evidence of plate tectonics
Vast abyssal plains if undersea volcanoes
Seamounts
Theory proposing that Mid-ocean ridges are formed by currents of deep seated magma rising up from the mantle. (Often during Volcanic eruptions) creating new basaltic ocean floor (crust regions) that spreads away laterally from the ridge and creating the newest crust
Sea floor spreading
This process explains trenches. It is the sight where old crust descends and then is melted. These ocean trenches contain the oldest crust. Older lithosphere descends into asthenosphere in “” where it is “recycled” into the convective cycle that operates in earth.
Subduction
Earthquakes occur along this line
Correspond w/ locations of trenches and ridges on sea floor
Plate boundaries
- Iron on cooled magma orients itself w/the magnetic poles & provides record of past magnetic fields
- sea floor has a relative symmetrical pattern of magnetic orientation in both sides of ridges, indicating it has spread laterally by addition of new crust.
- used to find age of ocean floor (sea floor spreading)
- magnetic field has reversed more than 170 times
Paleomagnetism
Verification of “” by paleomagnetism and ocean floor core sampling
Seafloor spreading
Core holes drilled in the ocean show that Sediment age/thickness increase with distance from ridges.
Ocean floor cores/core sampling
Ocean floor cores proved Wegener wrong because both continents AND The “” are drifting by sea floor spreading
Lithosphere
-Theory behind the motion of lithosphere plates
- plates float on asthenosphere
- 7 major plates
- 7 intermediate
- 12 smaller
Plates are being subducted
Framework relates wide range of internal processes and topographic patterns.
Plate tectonics
- Slow convection in earths mantle
- convection can push plates away from each other
Driving plate tectonics
-Divergent boundaries
-Subduction zones
-Collision of India w/Eurasia
-Transform faults and boundaries
All evidence of
Plate boundaries
3 types of plate boundaries are
Converge toward
Diverge from
Slide laterally past
Plates move away from each other because Magma from asthenosphere wells up in between plates. Plutonic solidifies below. Represented by mist common, “mid ocean ridge” but also occurs within continent “continental Rift Valley” associated with shallow earthquakes and volcanic activity. “Constructive” because adds material to crust surface .
Divergence boundaries
Sea floor spreading is also known as
Divergence
Associated with 2 Plates colliding
“Destructive” normal type associated with one plate being subducted but showing crumpling at the edges where they meet. Removal or compression of crust.
Responsible for massive landforms
Mountain ranges/volcanoes/oceanic trenches.
3 types
Convergence boundaries
What are the three types
Ocean- cont convergence
Ocean -ocean convergence
Cont-cont convergence
The “” under rides the “” because its denser, which makes it sink into the asthenosphere through “subduction” . Usually Creates oceanic trench and coastal mountains. Accompanied by earthquakes along margins and volcanos along plates. -metamorphic rocks form. “Blue schist”
Ocean -continental convergence