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词汇 example_english_longshore-drift
释义

Examples of longshore drift


These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
It is still debated what process or processes have resulted in this odd structure, though longshoredrift is the most accepted hypothesis.
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A fourth element of the environment in which hapua form is the strong longshoredrift component.
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As the ice sheets melted, sea level gradually rose and longshoredrift caused a spit to form between this and other islands along the moraine.
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It is a physical barrier to stop sediment transport in the direction of longshoredrift (also called longshore transport).
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Spits occur when longshoredrift reaches a section of headland where the turn is greater than 30 degrees.
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The inlet has evolved over the years due to natural processes, especially longshoredrift.
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Its mouth has been diverted eastwards for more than 1 km by a spit resulting from longshoredrift.
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The terminal groyne prevents longshoredrift from bringing material to other nearby places.
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This often occurs in the opposite direction to longshoredrift.
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Where longshoredrift occurs in opposite directions, two spits merge into a triangular protrusion along a coastline or lakeshore.
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There are three artificial groynes had been placed at northern part of the sandspit, to accumulate sediment from longshoredrift.
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Trained entrances can provide better navigation, water quality and flood mitigation services, but can also cause beach erosion due to their interruption of longshoredrift.
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Sediment is transported along the coast in the direction of the prevailing current (longshoredrift).
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In the ocean, groynes create beaches, or prevent them being washed away by longshoredrift.
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The sediment provided is not adequate to nourish the coast against its typical high energy waves and strong longshoredrift.
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Because of longshoredrift, sediments are picked up from the headland and deposited according to size and based on wave energy.
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Due to longshoredrift some sediment can end up further along the beach from where it started.
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The movement of cuspate forelands is commonly explained by longshoredrift acting as the main process.
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The 2 million project created two large rock groynes to halt longshoredrift as well as revetments to break the waves.
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Most revetments do not significantly interfere with transport of longshoredrift.
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The deposits are constantly being re-worked by wave action and are gradually migrating to the northeast due to longshoredrift.
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It stops the movement of the original beach material through longshoredrift and retains a natural look to the beach.
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When sediment reaches the coast it is then entrained by longshoredrift and littoral cells until it is accreted upon the beach or dunes.
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Longshoredrift can generally be defined in terms of the systems within the surf zone as seen in figure 1.
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Not only do ports and harbours pose a threat to longshoredrift in the short term, they also pose a threat to shoreline evolution.
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Longshoredrift, however, is the most accepted hypothesis for creation.
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It also plays a large part in longshoredrift as well.
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During low to medium river flows, the outlet from the lagoon to the sea becomes offset in the direction of longshoredrift.
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It is gradually extending westwards due to wave action and longshoredrift.
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Longshoredrift, along with wave energy, has shaped the shore.
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They naturally conform to the shape of the underlying beach or dune profile, and adjust well to moderate erosion, especially longshoredrift.
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In this case, longshoredrift as well as prevailing wind and waves bring sediment together from opposite directions.
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This can be used to build up beaches suffering from beach starvation or erosion from longshoredrift.
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Longshoredrift is dominantly to the north along the shore.
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The loch would have been cut off and a lagoon formed if the longshoredrift was allowed to occur naturally.
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The phenomenon is called longshoredrift.
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The impact of longshoredrift sediments on this inlet system is highly influenced by the variation in the number of lagoon entrances and the location of these entrances.
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These bars usually consist of accumulated gravel and sand carried by the current of longshoredrift and deposited at a less turbulent part of the current.
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Also, longshoredrift is not hindered.
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Its backbone is formed by glacial moraines, but much of its coastline has been shaped by the longshoredrift of coastal sand, which forms many of its famous sandy beaches.
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Longshoredrift is influenced by numerous aspects of the coastal system, with processes that occur within the surf zone largely influencing the deposition and erosion of sediments.
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The hotel was converted into private accommodation as flats in the late 1970s at around the same time as most of the beach had been eroded by longshoredrift.
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A spit is a type of bar or beach that develops where a re-entrant occurs, such as at cove's headlands, by the process of longshoredrift.
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During storms, sea walls help longshoredrift.
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These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
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