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created by the wind blowing over the surface of the water |
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the vertical distance between a trough and a crest |
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horizontal distance between adjacent crests |
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at the Surface and Beneath the Waves Move in Circular Orbits |
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As Waves Travel Away From a Storm Center, |
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They Evolve Into Broad, Rounded Waves Called Swells |
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Swells Become Higher As They |
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As waves approach the shore |
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the wave base drags on the shallowing seafloor causing the waves to slow down, increase in height, and become more closely spaced |
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Close to shore, waves evolve into |
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sharp-crested features called breakers |
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Breakers roll forward into a foamy |
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bubbly surface called surf along the surf zone |
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Waves run up onto the beach as |
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swash; run back down as backwash |
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As waves approach the beach |
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the rows of waves bend in a direction more parallel to the shore (wave refraction |
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End further from shore is moving |
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faster and catches up to near-shore end, causing wave to bend parallel with coastline |
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End nearest the shore encounters |
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shallow seafloor first, slowing down |
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Wave Refraction Causes The Waves To |
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Align Almost Parallel To Beach |
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Waves washing up and back on beach cause |
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grains to move downbeach in zigzag pattern known as beach drift |
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Longshore current also created |
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Depositional features are related to beach drift and longshore currents: |
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Barrier spits – Bay barriers (baymouth bars) – Tombolos – Barrier islands – Beaches |
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ridge of sand deposited by beach drift and longshore currents that extends out from the beach into an adjacent bay or cove |
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may eventually extend to the other side of the bay, forming a continuous ridge of sediment called a Bay Barrier |
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occurs when sediment deposits connect the shoreline with an offshore island or sea stack |
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are the most familiar feature on a coastline undergoing sediment deposition: |
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Beaches are the most familiar feature on a coastline |
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Some are stable – Others cycle seasonally |
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Quartz sand typically dominate beaches: |
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Quartz survives weathering processes |
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Beach stabilizes a coast by absorbing |
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– Long sandbars not connected to onshore beaches – Constructed by longshore currents – Common along stable continental margins |
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High energy wave and current action – Fairly straight shoreline – Sand on beach typically clean, well sorted and rounded with ripples and cross bedding |
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deposits – Very irregular shoreline – Tidal marsh mud and peat deposits |
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Characteristics of Barrier Islands |
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Created by tidal currents that flow through inlets: |
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deposited landward of the inlet such as within a lagoon behind a barrier island during rising tide |
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deposited on seaward side of the inlet during falling tide |
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deposited during high tide, when Gulf water flows into lagoon |
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Ebb tidal delta deposited |
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during low tide, when lagoon water flows out into Gulf |
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Features along coasts undergoing erosion include: |
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– Sea cliffs – Marine terraces – Wave-cut platforms – Sea caves – Sea arches – Sea stacks |
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back while bays and coves build outward through addition of sediment |
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Erosion of a headland leaves |
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behind sea stacks and sea arches |
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common features of coastlines undergoing erosion |
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If coast is also undergoing uplift, then |
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wave-built terrace can be elevated above sea level to become wave-cut terrace |
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Emergent coastlines due to tectonic uplift or sealevel fall can result in significant coastal erosion |
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Submerging coastlines due to land subsidence and/or rising sea level can result in drowned river valleys called estuaries |
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Factors that affect beach erosion include |
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– Proximity to sediment-laden rivers – Degree of tectonic activity/subsidence – Topography and composition of land – Wind and weather patterns – Configurations of coastline and near-shore areas |
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Jetties Groins Breakwaters Seawalls geotubes |
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are barriers at entrance to harbor |
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constructed perpendicular to beach |
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are offshore barriers parallel to beach |
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constructed behind the beach |
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buried at vegetation line behind beach |
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Various Constructions That Attempt To Control Beach Drift And Longshore Drift |
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Disrupt Sediment Movement |
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Galveston Groins Constructed To Keep |
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Beach Sand In Place, But Are Not Very Effective |
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Seawall Constructed Along Beach to |
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Protect Structures Behind It |
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simple marine animal with a saclike body called a polyp: – Secretes calcium carbonate to form a hard, external skeleton |
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Corals function in a symbiotic relationship with algae: |
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– Algae photosynthesize some food for the coral – Coral provides some nutrients and shelter for the algae |
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warm marine water between latitudes 30o N and 30o S |
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stark white by expelling nutrient-supplying algae: – Occurring in Caribbean Sea, Indian Ocean, offshore Australia, Florida, Texas etc. |
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Why corals eject their symbiotic partner is unknown: |
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– Pollution? – Disease? – Changes in salinity? – Warming of sea-surface? – Increasing acidity of oceans? |
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About one-third of human-generated carbon dioxide currently ends up in the oceans |
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Atmospheric CO2 dissolved in seawater forms carbonic acid, lowering the ocean’s pH: |
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– Surface waters of the oceans have already absorbed enough CO2 since preindustrial times to lower pH by 0.1 pH units – Current trend of CO2 emissions could result in pH decrease of at least 0.2 pH units by the year 2100 |
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Increasing ocean acidity threatens a |
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variety of calcite-secreting organisms including microbes and corals |
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Wetlands are saturated with water often enough to support plants that grow in water or very wet soil |
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Wetlands occur in a variety of locations: |
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– Coastlines – Bogs (land areas where water table is high) – Potholes in prairie lands – Cypress swamps – River bottom – Flood plains – Arctic and subarctic environments that experience permafrost |
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Coastal wetlands are of two general types |
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Salt marshes Mangrove swamps |
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Occur along tropical coastlines |
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Which of the following statements is NOT true regarding surface water in the oceans? |
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Most surface water originates near Greenland and Antarctica and afterwards flows as surface water towards the equator. |
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Atoll, barrier, and fringing describe different types of __ |
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Why does ocean water have higher salinity in subtropical regions than along the equatorial belt? |
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Evaporation exceeds precipitation in the subtropical region, whereas the reverse occurs along the equator. |
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0 out of 1 points Which of the following statements about beach drift and longshore currents is TRUE? |
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Beach drift transports sediment in the same direction as does longshore current. |
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The salinity of oceans vary from 34 to 37 parts per thousand. What is the definition of salinity? |
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Grams of dissolved ions in 1 kilogram of solution. |
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Which of the following will cause a global rise in sea level? |
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Global warming during an interglacial cycle |
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Which of the following statements is TRUE? |
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Global sea level has risen and fallen many times throughout Earth history |
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For incoming ocean waves approaching a coast, which of the following wave forms occur closest to the beach? |
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Which of the following is LEAST LIKELY associated with wetlands |
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Which of the following statements regarding waves approaching a coast is FALSE? |
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. Waves speed up when approaching the beach. |
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Which of the following depositional features along a coast is called a Bay barrier or baymouth bar?
[image] |
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Which of the following structures is a breakwater?
[image] |
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For the following figure, where is the greatest amount of coastal erosion occuring?
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The following configuration of the Earth-Moon-Sun system will result in__________.
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