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As **waves** approach the **shoreline**, they interact with the **seabed**, leading to **wave** transformation. This is where things get interesting. When the **wave** enters shallower water, the **orbital** motion of the water molecules is disrupted, causing the **wave** to slow down. This slowing down is what que idioma se habla en puerto rico causes the **wave** to build up and eventually break. This process is called **shoaling**. The shape of the **seabed** plays a crucial role in how the **waves** break. A steep **slope** leads to more powerful, barreling **waves**, while a gentle **slope** creates softer, more forgiving **waves**.
