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Spits are formed when longshore drift travels past a point where the dominant drift direction and shoreline do not veer in the same direction.
long-shore drift
Spits are formed when longshore drift travels past a point where the dominant drift direction and shoreline do not veer in the same direction.
Longshore drift is the process of sediment moving along a beach due to wave action. It is driven by the longshore current, which is a current that flows parallel to the shoreline. Therefore, longshore drift is the result or effect of a longshore current.
throught the processes of long shore drift and transportation & deposition
Longshore drift and longshore currents can produce landforms such as spits, tombolos, barrier islands, and sand dunes. These landforms are typically found along coasts with significant wave action and sediment movement.
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The direction of longshore drift is typically parallel to the coastline. It moves sediment and materials along the shoreline in a zigzag pattern due to the angle of incoming waves.
longshore drift
longshore drift
Devices: Wave power generators. Groynes. Natural processes: Long-shore drift.
Longshore drift or laminar flow occurs along beachs where the surf comes in at a horizontal angle to the beach. If the beach runs North-South, and the waves come in from the Southwest, you're likely to experience longshore drift to the North.