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Movement of the Seas 6.2

Horizontales
The most regular and predictable movements of water in the oceans
If both high tides rise to the same level and both low tides fall to the same level
Results from differences in density
Deep ocean currents
Breakers wash up onto the beach in a mass of foaming water
Waves that are different sizes and move in various directions
Carry large volumes of water from the shore to the sea
Sensor network to detect earthquake activity
Weaker then normal tides
Current which may wash sand from beneath the feet of swimmers
Water maybe trapped near the beach by the sandbar and flow parallel to the beach as a
Breaks or topples forward to form a
The length of time between one crest the next
Gentle rolling waves that may appear even during calm weather
Higher then normal at high tide and lower than normal at low tide
Verticales
When one high tide is higher than the other high tide, one low tide is lower then the other low tide
One high tide and one low tide each day
Generally limited to the first 400mbelow the surface
Rhythmic back-and-forth motion of water
Occurs when mud or silt mixes the water
Highest point of a wave
Large streams of ocean water that flow at or below the surface
White foamy crests
Depression in the water between crests is called
They move in a circular path