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  • Erosion-Formed River and Coastal Landforms: A Comprehensive Guide
    Many river and coastal features are formed by erosion, which is the process of wearing away and transporting rock, soil, and sediment. Here are some examples:

    Rivers:

    * Canyons: Deep, narrow valleys carved by river erosion over long periods. The Grand Canyon is a famous example.

    * Gorges: Similar to canyons, but often narrower and steeper-sided, often formed by rivers cutting through resistant rock.

    * Waterfalls: Formed when a river encounters a change in rock type, with a resistant rock layer overlying a softer layer. The resistant layer erodes more slowly, creating a drop in elevation.

    * Meanders: Winding, looping bends in a river channel, formed as the river erodes the outer bank of a curve and deposits sediment on the inner bank.

    * Oxbow Lakes: U-shaped lakes formed when a meander is cut off from the main river channel by erosion.

    * Floodplains: Flat, low-lying areas adjacent to a river, formed by sediment deposited during floods.

    * Terraces: Step-like landforms along a river valley, formed by the river eroding downward over time.

    Coasts:

    * Cliffs: Steep rock faces along the coastline, formed by the erosive action of waves and wind.

    * Sea Caves: Cavities eroded into cliffs by waves, often containing air pockets that can create echoes.

    * Sea Stacks: Isolated rock formations that stand out from the coastline, formed by wave erosion of a cliff.

    * Archways: Natural openings in cliffs formed by wave erosion.

    * Beaches: Areas of sand or shingle deposited by waves and currents.

    * Sand Dunes: Ridges of sand deposited by wind, often found along coastlines.

    * Headlands: Prominent stretches of high ground that jut out into the sea, often formed by resistant rock that erodes more slowly than surrounding areas.

    * Bays: Indentations in the coastline, often formed by the erosion of less resistant rock.

    It's important to remember that these features are often shaped by a combination of erosion and other geological processes, such as deposition, weathering, and tectonic activity.

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