Lecture 5- Marine Geology 2 Flashcards
Pangaea
Pangaea
the supercontinent that split apart to form the present-day configuration
Wilson Rock Cycle
- process in which continents have repeatedly collided and broken apart
- happened even before Pangaea
divergent boundaries occur between
- ocean and ocean
- continent and continent
convergent boundaries occur between
- ocean and ocean
- ocean and continent
- continent and continent
3 plate boundaries
- transform
- divergent
- convergent
earth’s 2 types of crust
- oceanic
- continental
oceanic crust
- thin (5 km)
- more density so floats deeper in the mantle
- consists mostly of basalt
continental crust
- thick (70 km)
- less dense so they float higher in the mantle
- consists mostly of granite
divergent boundaries
- occur where plates are moving apart
- most of these boundaries are mid-ocean ridges and less commonly, continental rifts
examples of new divergent boundary
East Africa rift zone
example of mature divergent boundary
mid-ocean ridges
hydrothermal vent systems
found at mid-ocean ridge spreading centers
continental boundary: ocean and continental
- ocean is more dense so it subducts and is pushed back down into the mantle
- generates deep ocean trenches and explosive volcanoes
examples of ocean crust colliding with continents
- North Cascade Mountains
- Andes Mountains
- Mt. Saint Helens (volcano)
continental boundary: oceanic and oceanic
- the plate that gets subducted is the one furthest from its spreading center
- deep oceanic trench (sometimes filled with sediment)
- older, colder, and more dense subducts
Island Arc
- chain of volcanoes
- ex. Aleutian Islands
continental boundary: continent and continent
- neither wants to subduct
- results in mountains (ex. Mt. Everest)
transform plate boundary
- plates slide laterally relative to one another
- example: San Andreas Fault
type of marine sediment
- terrigenous
- red clay
- calcareous ooze
- siliceous ooze
sediment rate of red clay
less than or equal to 1 cm per 1000 year
sediment rate of ooze
1-5 cm per 1000 year
terrigenous sediment
causes sediment thickness to be high near coast
red clay
- found in open ocean
- created by slow rain of continental dust and very low biological addition
calcareous/ siliceous ooze
- found in high biological productivity
- absence of terrigenous sediment and dilute red clay
accumulation of sediment
- very slow
- a 10 m sediment core can represent a record of a million years of earth history
proxy measurement of past ocean conditions
remains of planktonic organisms contained within the sediment cores reveal information about growth conditions of the ocean
calcite in shells
calcite in shells grown in colder temperatures have more 18O than calcite grown in warmer temperatures
6th mass extinction
caused by humans