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shorelines

geolgoy

AB
wave heightdistance from low spot (trough) to high spot crest
wave lengthdistance between successive high points or low points
wave periodamount of time it takes as one wave length passes a point
oscillatoryup and down like a circle
translationalelliptical shape
surf zonearea where wave begun to fall forward
swash zonewhere water moves up and back
longshore currentmovement of water parallel to coastline because of wave refraction
longshore driftmovement of sediment parallel to shoreline
coastal straighteningdeposition and drift, current make headlands erode away
rip currentsfast moving perpendicular offshore
spitssand extends partway across bay
baymouth barwhen sand extends all the way across
tombolocould end up being reconnected this is what the ridge is known as
barrier islandssand dune sits parallel to shoreline
jettiesperpendicular to shoreline reduce speed sand is moving
groinsindividual placed perpendicular to shore if waves come in on angle acts like impediment
breakwaterspour concrete down
spring tidesfull moon gravity stronger
neap tidesquarter moons


kim

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