Strandklitterne parallelt til stranden består af såkaldte unge klitter. De er 'unge', fordi de først er dannet siden middelalderen. Unge klitter er stadig i udvikling, især på havsiden, hvor vinden har størst indflydelse og konstant fører ny sand til. Unge klitter kan derfor vokse højt.
Afgrænsningen af de unge klitter på landsiden dannes mange steder af en stejl indre klitrand med høje klittoppe.
Afgrænsningen på havsiden dannes af strandkysten, klitkæden lige langs stranden, der fungerer som en havbeskyttende klit.
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