A
B
C
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E
100

This type of ocean sediment is commonly found from precipitation of minerals at hydrothermal vents

hydrogenous

100

a complex of living organisms interacting together with their abiotic environment

Ecosystem

100

A large sea surface wave created not by wind, but by seismic activity

Tsunami

100

This process causes fluids moving in the Southern Hemisphere to be deflected to their left

Coriolis Force

100

The average salinity of seawater

35‰

200

This is an area of rapid change in salinity with a change in depth

halocline

200

These are large, circular sea surface flow patterns caused by global air currents

gyres

200

Dissolved salts in seawater ultimately comes from a chemical reaction between these three things

water, CO2 and rocks on land

200

This is an area of rapid change in temperature with a change in depth

thermocline

200

This is an area of rapid change in density with a change in depth

pycnocline

300

The part of the water column that has more than 0% but less than 1% of surface sunlight

Disphotic zone

300

Besides NaCl, these are the two most abundant dissolved ions in seawater

magnesium and sulfate

300

Higher than average sea surface salinity is typically found at this latitude

~30° N/S

300

These air currents combine with the Coriolis Force to produce the Trade Winds and Westerlies

Hadley cells

300

Ocean crust will typically be thinner the farther away it is from this ocean feature

divergence zone/mid-ocean ridge

400

Old oceanic crust is destroyed in these ocean regions

subduction zones/trenches/convergent plate boundaries

400

Subduction zones are found at this type of plate boundary

Convergent

400

A cold-core ring is usually associated with this oceanographic process

upwelling/high primary production

400

Ekman transport causes the topmost layer of the sea surface to be deflected at this angle to the right of wind

45 degrees

400

A name for biogenous sediment that is >30% calcite or silica  

ooze

500

A flat-topped seamount that was once a volcanic island but subsided beneath the sea surface

Guyot

500

Global thermohaline circulation is initiated by this process occurring in high latitude seawater

ice formation/high salinity cold surface water/sinking

500

A strong pycnocline prevents/reduces this process from occurring

mixing/upwelling/nutrient input

500

Ekman transport causes net movement of the entire Ekman layer at this angle relative to wind

90 degrees

500

Formation of coastal mountain ranges and volcanic island chains are typically found along this type of continental margin

active

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