topic 4 plate tectonics Flashcards
Landforms are the result of what major groups of processes?
Land building: volcanic and tectonic forces (initial landforms ‘primary’) and Land denudation: weathering and erosion (sequential landforms ‘secondary’)
Landforms reflect a balance between internal earth forces and bring fresh rock to the surface and denudation processes that remove and transport mineral matter
what transports the most rock and soil annually?
- rivers 53 billion tons 2. humans 45 billion tons 3. oceanic volcanoes 30 billion tons 4. mountain building 14 billion tons 5. glaciers 4.3 (10) billion tons
earth structure
Core, mantle, and crust/lithoshere
increasing temperature and density of material with depth
Continental drift
the idea that all landmasses were once all one large continent, pangea, surrounded by a single ocean.
Pangea broke apart over hundreds of millions of years ago because of development of rift zones within continents
continents spread apart and ocean basins developed by process of sea-floor spreading
plate tectonics
The theory describing the origin, movement, and recycling of lithosheric plates and the resulting landforms
origin was the theory of seafloor spreading; new lithosphere forms at mid-ocean ridges, and old lithosphere is recycled deep into the mantle through subduction
what is subduction?
the process in which oceanic lithosphere from one plate bends and dives into the mantle beneath another plate
subduction only occurs where Oceanic lithosphere subducts beneath continental lithosphere/oceanic lithosphere
concept of a lithospheric ‘plate’
Rigid lithospheric rocks are “floating” on the denser, plastic asthenosphere
The lithosphere is broken into large plates (AKA ‘tectonic’ plates)
plates are flexible yet brittle (fractures are known as “faults”)
Two types of plates
14 total plates (7 primary plates, 7 secondary plates)
Primary plates: the African plate, Antarctic plate, Eurasian plate, Indo-Australian plate, North American plate, Pacific plate, and the South American plate
secondary plates: the other 7
How to find plate boudaries?
Earthquake activity reveals plate boundary locations
Earthquakes occur in geographic patterns that delineates the outlines of lithospheric plates
How do plates move?
Ridge push: rising magma along a mid-ocean ridge lifts oceanic lithosphere and forms slopes
mantle drag: movement of plates caused by friction between moving asthenosphere and the lithosphere
Slab pull: the weight of the subducting portion of a plate accelerates plate movement by pulling the plate deeper into the mantle
absolute velocity
how fast the plate is moves in relation to a fixed point
Relative velocity
How fast a plate moves in relation to the speed of an adjacent moving plate
What is uplift?
change in land/rock surface vertical position relative to a fixed datum (e.g. sea level)
Total uplift
the sum of Tectonic uplift (due to collisions and tectonic movements) and isostatic uplift (due to the difference in density between mantle and the crust)
when erosion occurs, there is an isostatic adjustment (due to the difference in density between crust and mantle). for each meter of erosion, isostatic response lifts the underlying rock up by ~82cm
Plate boundaries
Divergent: where two plates move apart
Convergent: where two plates move towards each other
transform: where one plate slips laterally past another