The Ocean Floor Flashcards
Abyssal plains
Deep, flat features
Likely the most level places on earth
Thick accumulations of sediment have buried an otherwise rugged ocean floor
Oceanic ridges
Underwater mountain ranges
Form along divergent plate
Sea floor sediment
Vast majority of the ocean floor is covered with sediment
Deposited by turbidity currents, snow settling
Organic debris that sinks from higher in the water column
Some flakes fall before finally reaching the ocean floor
Three categories
Terrigenous - derived from water
Minerals from the weathering of terrestrial rock
Hydrogenous - derived from water
Minerals that crystallize directly from seawater through chemical reactions
Biogenous - derived from organisms
Shells and skeletons
Salinity
Total amount of solid material dissolved in water
Parts per thousand
Average salinity of ocean water = 3.5 ppt
Salinity in saline prairie lakes can exceed 200 ppt
Temperature and precipitation determine salinity levels
At mid latitude and near the equator, lower salinities - extensive rainfall dilutes surface ocean water
At tropics evaporation is greater than precipitation resulting in higher salinity
At poles fresh water from melting ice decrease surface salinity
Acidity
Anthropogenic changes to acidity
Thermocline
Layer where temp changes with depth
Seen at low and mid latitudes
Isothermal
Same temp
No thermocline
Seen at high latitudes