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The image shows four stages of headland erosion in diagrams: 1) Initial "Erosion of a headland" where weak areas of rock are eroded. 2) "Cave becomes arch" highlighted with an example of Durdle Door in Dorset. 3) The "water beats against roof stack," focusing on the impact of water on the structure. 4) Finally, it illustrates "headland retreating," resulting in the formation of a stack and a stump. Each stage is represented with arrows indicating the direction of water flow and the impact on rock structures.
Given the complexity of the image, the above description may not be entirely accurate.
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The diagram illustrates how a headland is eroded by waves in the ocean through several phases. The process of erosion is divided into four stages: weak areas, the cave becomes an arch, water beats against the roof, and the headland retreats.
To be more detailed, the first phase is forming weak areas in the land because of the erosion of rocks at the base. As a result, a cave becomes the arch, which is as huge as a Durdle Door or Dorest.
The third stage is how water beats against the roof, which leads to the headland being broken into two pieces; the object in front of the head is a large stack. Eventually, the headland retreats and cracks into three parts, including a stack and a stump.
Clearly, as the water or high tide level hits the base with the continuously strongest intensity, the headland is gradually eroded.
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