The diagram below shows the stages in the erosion of a headland.

The provided diagram meticulously delineates the progressive erosion of a

headland

until its complete dissolution.

This

intricate natural process unfolds across four discernible phases, commencing with the gradual disintegration of rocks and culminating in the formation of a solitary stack.

Initially

, erosion selectively targets the vulnerable strata of the

headland

, instigating a gradual metamorphosis of the landscape. Over time,

this

relentless erosive force meticulously sculpts the rocky outcrop into an elegant arch, reminiscent of iconic coastal features

such

as the renowned Durdle Door in Dorset.

However

, the relentless assault of aqueous elements precipitates the eventual dissolution of the arch's roof, leaving behind a solitary stack as a testament to nature's inexorable forces. In the ultimate phase, the residual stack, accompanied by a vestigial stump and vestiges of the original

headland

, serves as a poignant reminder of the dynamic interplay between geological dynamics and erosive processes, reshaping coastal topographies in perpetuity. In summation, the diagram intricately elucidates the incremental erosion of a

headland

, underscoring the nuanced interplay of natural forces.

While

succinct, it poignantly encapsulates the profound temporality inherent in geological phenomena, epitomizing the inexorable march of nature's transformative prowess.