Topography
Plate Boundaries
Currents
Tides
Waves
100

Area where ocean plate slides below continental plate; created by subduction

trench

100

Type of plate boundary that produces a trench

Convergent boundary

100

Currents that flow from the equator are always__.

Warm

100

Tides are caused this.1

Gravitational pull of the moon (and sun).  But the moon has a greater effect, since it is closer!

100

Waves are caused by this

Wind blowing across the water

200

Steep area that is part of the continental margin

Continental Slope

200

Type of plate boundary that produces a large mid-ocean ridge that circumnavigates the earth

divergent boundary

200

Currents that flow from the poles are always___

Cool

200

When the sun, earth, & moon make a ninety-degree angle we have these tides.

Neap tides (low high & high low tides)

200

Tsunamis are caused by this

Earthquakes or volcanic eruptions under the ocean.  Remember they have nothing to do with tides!

300

Flat area in the deep ocean basin

Abyssal Plain

300

Type of plate boundary where shearing/sliding occurs, therefore creating lots of earthquakes

transform plate boundary
300

Currents are caused by differences in _________

Density

(Temperature or salinity differences create density differences.)

300

When the sun, moon, & earth are in a straight line, we have these tides.

Spring tides  (highest high tides/lowest low tides)

300

The highest point of a wave

Crest

400

Active undersea volcano with a rounded top

Seamount

400

Type of plate boundary that is found around much of the Ring of Fire

Convergent boundary

400

Gyres in the northern hemisphere flow this direction due to the Coriolis Effect.

Clockwise

400

Moon phases in which the high tides are highest & low tides are lowest

Full & New Moons

400

The lowest point of a wave

Trough

500

Inactive undersea volcano with a flat top

guyot  (pronounced gee-oh)

500

Type of plate boundary the runs down the middle of the Atlantic Ocean causing it to get bigger

Divergent Boundary

500

Currents in the southern hemisphere always flow this direction due to the Coriolis Effect.

Counter-clockwise

500

Moon phases in which the tidal range does change much

Quarter Moons
500

The distance between the crests (or troughs)

Wavelength

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