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the broad area or strip of land and water where various processes create characteristic coastal landscapes |
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a narrower belt or subsection of the coast |
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the actual contact border between land and water |
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from the highest water line to a point where the water is about 200 ft deep (where large waves will first be acted upon the the ocean bottom |
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coastal zone of sediment shaped by wave action |
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undulations of water produced by wind energy being transferred to water (wave) energy * size determined by wind velocity, direction, duration, & fetch (distance over which the wind blows) |
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1) height: vertical distance between crest & the trough 2) length: horizontal distance from one crest to the next 3) period: time interval between 2 successive crests passing a fixed point |
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series of open ocean waves |
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when the swell begins to be affected by the ocean bottom |
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a wave whose height exceeds vertical stability and falls forward or “breaks over” |
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a series of breaking waves |
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the thin sheet of water that slides up the beach after a wave breaks |
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the water from the swash that flows back toward the ocean |
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wave bending; caused by the irregular shape of the shore compared to the incoming wave or by areas of shallow water offshore |
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generated by refracted waves; moves parallel to the coast, helping to move sand laterally down the beach (pg. 510) create longshore drift or beach drift |
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narrow stream-like flows which move perpindicular to the shore and thus move water and sand away from the shore |
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the cyclical rise & fall of water level on the shore due to 3 forces: 1) earth's rotation 2) gravitational pull of the moon & 3) of the sun |
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vertical difference between high tide & low tide; * avg = 2-4 m (6 - 12 ft); one extreme --- Bay of Fundy, Nova Scotia = about 15 m (50 ft) |
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Processes: 1) hydraulic action: work of moving water against the shore 2) corrasion: use of rock fragments in a wave to help erode the shore; similar to abrasion in a stream or glacier 3) corrosion: chemical breakdown 4) attrition: pounding waves reduce large fragments to smaller ones |
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the result of erosion by waves on a headland |
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created by waves undercutting at base of a sea cliff |
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the slightly sloped foot at base of sea cliff |
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rock arch under which water can flow |
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isolated columns or bits of the former headland |
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the area that is always submerged, even at low tide, out to a depth of about 200 ft; may contain longshore bars |
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the area exposed at low tide and covered at high tide |
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the area from high tide line to dunes; berms (flat sandy beach area beyond daily wave action) develop here |
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created by eolian (wind) processes, normally vegetated and relatively stable |
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elongated extension of beach into open water in front of a bay or other inlet; formed by longshore drift |
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a sandspit which grows entirely across a bay opening · Creates a lagoon behind it; lagoon: shallow body of water that lies etween a barrier island and the mainland and is usually oriented perpendiculat to the shore |
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a sandspit which joins an island with the mainland; usually oriented perpendicular to the shore |
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permanent offshore or longshore bar, upwards of 20 feet asl, 1-3 miles wide, several miles long & commonly up to 6-7 miles offshore; FIG. 16.15 & 16.16 ; material is sediment brought down by rivers off continent
EX: Cape Hatteras, Miami Beach, Atlantic City, St. Simons, Jekyll, Cumberland, Sapelo, |
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broad indentation into a coastline; smaller than a gulf |
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those that have seemingly been uplifted, either due to sea level falling or land being raised EX. U.S. West Coast * evidence of this type of coastline: sea cliffs, wave-cut platforms, sea stacks, etc. |
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those that seemingly are sinking, either by sea level rising or the land sinking * evidence of this type of coastline: estuaries, bays, fjords, barrier islands, sandy beaches, etc EX: U.S. east coast and gulf coast |
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those created by, or composed primarily of living organisms |
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built of coral & the marine limestone (CaCO3) deposits they create |
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a circular coral reef with a lagoon in the middle |
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trees in tropical areas (Florida) |
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