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AICE Marine 2.2-2.3

TermDefinition
weathering break down of rocks/sediment; produces small fragments
erosion carried away/removal of sediment
chemical weathering more acidic water will break down rocks shells, & corals exoskeleton
physical weathering the movement of water & suspended sediment/sand will break down rocks & coral's skeleton
organic weathering AKA biological weathering; burrowing animals & coral's predators
ice glaciers move & weather/carve & create fjords; deposit sediment in new locations as the glacier moves
water ice glaciers move & weather/carve & create fjords; deposit sediment in new locations as the glacier moves water
wind wind can carry sediment great distances
gravity particles will be dragged down through the depths due to gravity (think: the edge of a cliff falling off & sinking to the sea floor; submarine landslide)
sedmentation deposition/build-up/accumulation of sediment/suspended particles
larger particle size takes more energy to move/erode
larger particle be at high tide mark
smaller particle be at low tide mark
faster the movement of water the more energy there is to move the particles/sediment & therefore the larger the particles it can carry
littoral zone intertidal region on a shoreline, between the highest and lowest spring tide marks
rochy shores Waves, currents, & tides weather the rocky shore / rocks
rocky shores Little erosion (granite & igneous rocks are resistant to weathering)
rocky shores Very little sedimentation
rocky shores Can form rock/tide pools
rocky shores Rocks provide an attachment site/hiding places/more habitats than sandy shores
rocky shores More producers = higher productivity = more food than sandy shores
marine terraces weathered and eroded when the sea level was higher
sandy shores Typically smaller waves than on a rocky shore
sandy shores gradual slope
sandy shores Sand/sediment constantly shifts (not much energy is needed to move the small particles)
sandy shores Animals burrow/infauna
sandy shores Waves, currents, tides, & wind weather & erode sediment (more so in the winter months)
sandy shores Waves, currents, tides, & wind deposit sediment (sedimentation) (more so in the summer months)
muddy shores Somewhat protected from waves
muddy shores Very little weathering / erosion
muddy shores formed by sedimentation
muddy shores Smallest particle size (silt)
muddy shores low in oxygen
muddy shores Animals burrow / infauna
muddy shores Very gradual slope / mud flats
deltas Where a river ends at the sea
deltas Rivers' moving water weather and erode; deposit sediment at the end, on the continental shelf
deltas Shaped by sedimentation
estuary Sheltered or semi-enclosed bodies of water where fresh & salt water mix (AKA brackish); therefore low salinity
estuary Sheltered from weathering and erosion by waves, silt & fine sand is deposited here; can have high turbidity
estuary AKA: lagoon, bay, sound, slough
drowned river valley formed at the end of the last ice age; increase in sea level flooded the river delta
fjords formed as a result of weathering and erosion from moving glaciers
bar built formed by a sand bar or barrier island
tectonic formed by tectonic activity; land subsided & sea water flooded in
tides The vertical movement of water on the coast/the change in water height on the coastline; due to the gravitational pull of the Moon & Sun
tidal range The distance on the coast between the high and low water/tides (changes daily)
straight line= greater gravitational pull
greater gravitational pull= larger tidal range
larger tidal range= spring tides
right angles= less gravitational pull
less gravitational pull= smaller tidal range
coastal geomorphology As the coast narrows, water piles up on itself, increases the tidal range
wind Increased wind speed will push more water on & off of the coast, increasing the tidal range
lower air pressure= increased tidal range
larger body of water= greater tidal range
smaller body of water= little to no tidal range
spring tide occurs twice a month
spring tide greatest gravitational pull
spring tide when Earth, Moon, and Sun are in a straight line
spring tide New & Full moon
neap tide occurs twice a month
neap tide weakest gravitational pull
neap tide when Earth, Moon, & Sun are at right angles
neap tide 1st and 3rd quarter moon
currents continuous moving ocean water--deep & surface currents
cold surface currents move from high lats to low lats
warm surface currents move from low lats to high lats
dense water sinks and forms deep currents
Coriolis effect phenomenon that causes surface currents to be deflected to the right in the N hemisphere & to the left in the S hemisphere (creates gyres)
upwelling the movement (current) of cold, nutrient-rich water from the deep/bottom of the sea to the surface; caused by wind at the surface (creating a low pressure) and steep-sided topography
global ocean conveyor belt Cold, salty (dense) water sinks in high latitudes; forms deep currents
global ocean conveyor Upwells near the equator & where there are steep-sided topographic features (west coast of N & S America)
global ocean conveyor belt Brings cold, nutrient rich water to the surface & carries warm water away from low latitudes
normal condition wind E-W
normal condition surface currents E-W
normal condition Surface water piles up/higher Australia/Indonesia
normal condition Good upwelling off of S. America
normal condition Cold, dry conditions S. America
normal condition Warm, wet conditions Australia/Indonesia
el nino wind reverses W-E
el nino Surface currents reverse W-E
el nino Upwelling slows/stops
el nino Cool, dry conditions Australia/Indonesia
el nino Warmer waters = less nutrients, less phytoplankton, low productivity, less food, fish die
el nino Warmer waters = zooxanthellae die, coral bleaches, coral dies
el nino Cool & dry in Australia/Indonesia = droughts & fires
el nino Warm & Wet in S. America = flooding & landslides
Created by: s40148365
 

 



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