Currents within the surf zone that flow parallel to the shore are known as longshore currents. These currents are generated by waves approaching the shore at an angle, creating a flow of water along the coastline. Longshore currents can significantly influence sediment transport and beach erosion, shaping coastal landscapes over time. They often interact with rip currents, which flow seaward and can pose hazards to swimmers.
Johnny Maestro lived in Bay Shore, New York, for many years, specifically in the area known as the South Shore. His residence there became well-known among fans and locals, as he was a prominent figure in the music scene. Maestro, famous for his work with the Crests and later the Brooklyn Bridge, often spoke fondly of his time in Bay Shore. However, the exact address of his home is not widely publicized for privacy reasons.
A public fan phone number for Jersey Shore is not known at this time. WikiAnswers will not provide personal contact information for celebrities and noncelebrities alike.
Dinah Shore did not sue her parents. There is no documented evidence or information available to suggest that she took legal action against her parents. Dinah Shore was a successful singer, actress, and television personality known for her career in the entertainment industry, not for any legal disputes with her family.
No, Dinah Shore was not Lorne Greene's daughter. Dinah Shore was a famous American singer and actress, while Lorne Greene was a Canadian actor best known for his role on "Bonanza." They were both prominent figures in the entertainment industry, but there is no familial relationship between them.
Dinah Shore's birth name is Shore, Frances Rose.
Longshore currents
These currents are called LongShore or Feeder Currents.
When waves move parallel to the shore, they are known as longshore currents. These currents can transport sediment along the coastline, resulting in the formation of features like sandbars and spits. Additionally, longshore currents can affect the erosion and deposition of coastal areas.
Riptides, also known as rip currents, are strong, narrow currents that flow from the shore back to the open ocean. They can pull swimmers out to sea and are dangerous for those caught in them. It is important to swim parallel to the shore if caught in a rip current to escape its pull.
Long-shore currents are generated when waves approach the coast at an angle, causing water to move parallel to the shore. When waves hit the shore head on, there is less tendency for water to move laterally along the coast, resulting in weaker or non-existent long-shore currents.
Long ridges of sand parallel to the shore are known as sandbars. They are formed by the action of waves and currents depositing sand in shallow areas along the coast. Sandbars can shift and change shape over time due to the movement of water.
This phenomenon is known as longshore currents. They are caused by the movement of waves hitting the shoreline at an angle, creating a current that flows parallel to the coast. Longshore currents can transport sediment along the coastline, affecting beach erosion and deposition.
Long shore currents form when waves approach the shoreline at an angle, causing the water and sediment to move parallel to the shore. This movement is a result of the wave's swash and backwash, creating a current that flows along the coastline. Long shore currents are influenced by wave direction, wave energy, and the shape of the coastline.
What are two kinds of near shore currents
Longshore currents move sand along the coast by carrying it parallel to the shoreline. As waves approach the shore at an angle, they generate a current that moves sediments in a zigzag pattern. This process helps to redistribute sand along the coastline.
Longshore currents are the movement of water within the surf zone that parallels the shore. These currents are responsible for transporting sand and sediment along the coastline and can be influenced by wave direction and beach topography. Longshore currents can be strong and pose a hazard to swimmers and surfers.
Waves approach a shore obliquely (at an angle) due to the effects or the tides, currents the coriolis effect etc. and then retreat due to gravity straight. A good analogue is to roll a marble up a slope at an angle; it will fall more linearly on its return. Hope this helps.