oceanography Flashcards
general geography
71% of surface is ocean or marginal sea
south hemisphere mostly water
four main ocean basins
pacific-largest & greatest in depth
atlantic- half size of pacific & not as deep
indian- slightly smaller than atlantic; largely s. hemi body
arctic- 7% size of pacific
passive continental margin
not assoc w/ plate boundaries (Atlantic Coastline)
experience little volcanism
few earth quakes
active continental margin
ocean lithosphere subducted beneath continents
pacific rim
assoc with deep ocean trenches
passive
continental shelf slope cont rise submarine canyons & turbidity currents deep sea fan
continental shelf
flooded extension of continent
gently sloping from shoreline to deep ocean
thick accumulation of shallow water sediments
contains oil & important mineral deposits
continental slope
seaward edge of continental shelf
boundary btwn ocean & continental crust
continental rise
slope become more gradual incline
turbidity currents follows submarine canyon
submarine canyons & turbidity
deeps steep sided valleys cut into cont slope
some are seaward extensions of river valleys
most appear to be eroded away from turbidity currents
originate along cont slope
downslope movement of dense sediments- laden water
deposits are called turbidites
sediment deposit show graded bedding
deep sea fan
dense muddy currents emerge from the mouth of a canyon onto the relatively flat ocean floor
deposits form a fan
active
subduction
volcanic activity
continental slope descends into deep sea trench
accumulation of deformed sediments & scraps of ocean crust form accretionary wedges
may have little or no accumulation of sedimenets
deep ocean basins
trenches
abyssal plains
guyots
plateaus
trenches
long relatively narrow features deepest parts of ocean challenger deep, marianas: 11022 m most located in pacific ocean ocean lithosphere plunge into mantle generates earthquakes assoc with volcanic activity pacific "ring of fire" volcanic island arcs continental volcanic arc
abyssal plains
likely the most level places on earth
sites of thick accumulation of sediments
found in all oceans
seamounts, guyots, and oceanic plateaus
seamounts- isolated volcanic peaks
many form near oceanic ridges, still volcanic activity and still grow
guyots- tablemounts , submerged flat top volcanoes, dormant, become flat top by wave action
oceanic plateaus- similar to continental flood basalt provinces
oceanic ridge system
70,000km long
crest stands 2-3km above adjacent ocean basin
divergent plate boundaries- new crust created
ocean ridge
broad features-not narrow as ridge would imply
1,000-4,000 kn wide
broken into segments 10-100s km long
segments separated by transform faults
consists of layers of newly transformed basalitc rocks
rift valleys
deep down faulted structures along ridge crest
50 km wide 2,000 m deep
volcanic cones common
rugged topography
similar to continental rift valley (E. Africa)
types of seafloor sediments
terrigenous
biogenous
hydrogenous
terrigenous sediment
material weathered from continental rock
fine particles remain suspended for long time
oxidation often produces red & brown colored sediments
deposition rate 1 cm/50,000 yrs
continental margin area
biogeneous sediment
shells, skeletons of marine animals & plants
most common: calcareous oozes produces from microscopic organisms
siliceous oozes- skeletons of diatoms & radiolarians
phosphate rich materials-bones, teeth and scales of fish, & other organisms
hydrogenous sediment
minerals that crystallize
most common type- manganese nodules, calcium carbonates, metal sulfides, evaporites
only small portion deposits in ocean
composition of sea water
consists of 3.5% dissolved minerals
avg. salinity is 35%
major constituents is sodium chloride
salinity
total amt of solid material dissolved in water
brackish-mix of fresh & sea water (estuaries &deltaic environ)
hypersaline- excessive salinity, avg 42% (Red Sea, Dead Sea, Great Salt Lake)
halocline- zone of rapid change in salinity btwn depths of 300-1000 m
low latitudes- low salinity
high latitudes- high salinity
process that affect salinity
low salinity- precipitation, runoff from land, iceberg melting, sea ice melting,
high salinity- evaporation, formation of sea ice