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Marine Bio CH1

Terms

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photic zone
the portion of the ocean where light intensity is sufficient to accommodate plant growth
Density
ratio of the mass of a substance to its volume
seafloor spreading
a global process of organic crust moving away from and rise system where it formed
ozone
0*3 formed by the action of UV light acting on atmosphere 0*2
visible light
the portion of the electromagnetic radiation to which the human eye is sensitive
shelf break
the outer edge of the continental shelf
latent heat of fusion
the heat that must be extracted from a liquid to freeze it to a solid at the same temp
salinity
a measure of the total amount of dissolved ions in seawater
Continental slope
the relatively steep portion of the sea bottom
Ion
an electrically charged atom or molecule formed by gaining or losing an electron
Continental shelf
the relatively smooth underwater extension of the edge of the continent that slopes gently seaward to a depth of about 200 m
seamounts
underwater volcanoes
Atolls
a ring shaped chain of coral reefs from which a few low islands project above the sea surface
temperature
a relative intensity measure of the condition caused by heat
Abyssal plains
flat, sediment covered areas in the ocean basin usually 3,000 to 5,000 m deep
pycnocline
the ocean layer, usually near the bottom of the photic zone marked by a sharp change in density
Convection
the transfer of energy by the flow or mixing of a gas or liquid
thermocline
the ocean layer, usually near the bottom of the photic zone
Heat Capacity
the measure of energy required to change the temperature of a 1 g substance
ionic bond
in crystalline structures an atom bond formed between adjacent oppositely charged ions
trenches
deep area in the ocean floor, generally deeper than 6,000 m
latent heat of vaporization
the heat required to convert to convert a liquid to a gas at the same temperature
Pangaea
the super continent
Calories
a unit of heat energy equivalent to the amount of energy required to change the temp of 1 g of water 1 C
Hydrogen bond
a weak bond formed by the attractive by the attractive force between the charged ends of water molecules and other charged ions
Continental drift
the gradual movement of continents in response to seafloor spreading process
viscosity
the resistance of water molecules to external forces that would separate them
last glacial maximum
the time that the last major continental glacial advance in the northern hemisphere reached it maximum height 18,000 years ago
ridge and rise system
the interconnecting chain of seafloor mountains that trace the edges of crustal plates and the sites of new oceanic crust production
Conduction
the molecular transfer of heat through a medium
plate tectonics
the collective geologic processes that move the crustal plates of the earth
surface tension
the mutual attraction of water molecules at the surface of a water mass
reefs
massive near-shore deposits of coral skeletal material

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