The Northern European Plain does not extend farther north primarily due to the presence of the Scandinavian Mountains and the Arctic regions, which create a natural barrier. This mountainous terrain limits the flat, fertile land characteristic of the plain, as well as the climatic conditions suitable for such landscapes. Additionally, the harsh climate and permafrost in the far northern areas are not conducive to the agricultural and geological features that define the plain. Thus, the combination of topography and climate restricts its northern extension.
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