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☆☆☆☆☆As waves approach the shore, interaction with the sea floor slows the waves down and the crests of the waves bunch up. They increase in height as the energy in each wave compresses into a shorter horizontal distance, but the period of the wave does not change. Eventually, the waves break.
Along cold water currents from the poles to the equator.
Mr poppins is coming
Conductivity can be used to calculate the salinity of the water.
density
The alluvial silt that covers the land during flooding increases its fertility. This is in addition to the ready supply of fresh water required for any large societal group.
fetch
Could the team have won if it had let Andre play?
key terms and lesson objectives.
graphic organizer ( Apex)
spring
The only difference - is the direction of flow. A sea breeze blows from the sea onto the land. A land breeze flows in the opposite direction.
The polar jet stream lies between the polar easterlies and trade winds
